Appendix 10-B Visual Impact Assessment

Appendix 10-B
Visual Impact Assessment
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
Prepared for Mineral Resources Ltd
Prepared by Bioscope Environmental Consulting Pty Ltd
29 August 2016
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Revision History
Date
21 September 2015
Version
0
Author
S. Finucane
Reviewer
D. Temple-Smith
28 March 2016
1
S. Finucane
D. Temple-Smith
5 April 2016
2
S. Finucane
S. Bateman
29 July 2016
3
S. Finucane
D. Temple-Smith
5 August 2016
4
S. Finucane
S. Bateman
29 August 2016
5
S. Finucane
D. Temple-Smith
Purpose
Draft LVIA report, for client
review and input
Final draft VIA report for
client review
Final draft VIA report for
independent peer review and
regulator review
Revised VIA report for client
review
Revised VIA report for closeout of independent peer
review
Final report
Cover Photograph
Photographer: Sonia Finucane
Photograph used with permission from the photographer
Limitations
Bioscope Environmental Consulting Pty Ltd (Bioscope Environmental) has prepared this report in accordance
with the usual care and thoroughness of the consulting profession for the use of Mineral Resources Limited. It
is based on generally accepted practices and standards at the time it was prepared. No other warranty,
expressed or implied, is made as to the professional advice included in this report. It was prepared in
accordance with the scope of work and for the purpose outlined in the proposal dated 29 April 2015.
The methodology adopted and sources of information used by Bioscope Environmental are outlined in this
report. Bioscope Environmental has made no independent verification of this information beyond the agreed
scope of works and Bioscope Environmental assumes no responsibility for any inaccuracies or omissions. No
indications were found during our investigations that information contained in this report as provided to
Bioscope Environmental was false.
This report is based on the information reviewed at the time of preparation. Bioscope disclaims responsibility
for any changes that may have occurred after this time.
This report should be read in full. No responsibility is accepted for use of any part of this report in any other
context or for any other purpose or by third parties. This report does not purport to give legal advice. Legal
advice can only be given by qualified legal practitioners.
 Bioscope Environmental
This publication is copyright. Apart from the limited exceptions permitted under the Copyright Act 1968, no
part may be reproduced or communicated by any process without written permission from the author.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page i
EXECUTIVE SUMMARY
Mineral Resources Limited (MRL) proposes to develop the J5 and Bungalbin East Iron Ore Project
(the Proposal), approximately 100 km north-northeast of Southern Cross, within the Shire of Yilgarn,
Western Australia (WA). The Proposal comprises construction, operation and closure of:




Open pits and Waste Rock Landforms (WRLs) at J5 and Bungalbin East.
Areas required for the temporary storage of cleared vegetation and topsoil/subsoil.
Access tracks and haul roads.
Supporting mine infrastructure and other facilities.
Ore from the J5 and Bungalbin East pits will be transported via the J4 haul road to the Carina
operations for dry crushing and screening before loading on trains at the Mt Walton rail-siding. A
total of 30 km of bituminised haul roads will connect the mine operations to the J4 haul road.
The Proposal is located within and adjacent to the Helena-Aurora Ranges (HAR), within the Mt
Manning – Helena-Aurora Ranges Conservation Park (MMHARCP). The MMHARCP was gazetted in
2005 and is vested in the Conservation and Parks Commission. The park managed by the
Department of Parks and Wildlife (DPaW) for the purpose of “recreation by members of the public
as is consistent with the proper maintenance and restoration of the nature environment, the
protection of indigenous flora and fauna, and the preservation of any feature of archaeological,
historical or scientific interest“. It offers a relatively undisturbed natural environment that provides
visitors with an opportunity to experience a remote, outback experience within a varied landscape
that contains diverse native flora and fauna. Activities typically conducted in the park include
tourism and recreation including four-wheel driving, camping, hiking and nature appreciation.
The scenic qualities of the MMHARCP emanate primarily from the distinctive rock formations and
rugged ridgelines of the HAR, and contrasting vegetation patterns in the park. The HAR’s high level
of visibility and the complexity of the landform and its habitats contribute to the overall “sense of
place” experienced by visitors to the MMHARCP. Despite this, the park has relatively low visitation
rates.
The Proposal is being assessed by the WA Environmental Protection Authority (EPA) as a Public
Environmental Review (PER) under Part IV of the Environmental Protection Act 1986 and as a
controlled action under the Environment Protection and Biodiversity Conservation Act 1999. The
Proposal is being assessed under the Bilateral Agreement between the Commonwealth of Australia
and the State of WA.
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Visual Impact Assessment
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Page ii
One of the preliminary key environmental factors for this Proposal is “Amenity”. The EPA’s objective
for this factor is to ensure that impacts to Amenity are reduced as low as reasonably practicable. The
Environmental Scoping Document issued by the EPA nominates the relevant aspects of the Proposal
as:
 clearing of native vegetation; and
 mining construction, operation and closure.
“Amenity” covers a range of topics including visitor access and use, noise, air quality, light and visual
landscape. This report addresses only visual amenity.
EPA Guidance Statement No 33 outlines broad principles and some of the factors to be considered
during Visual Impact Assessment (VIA). It does not prescribe methodologies for this type of study,
but states that practitioners should use a “recognised methodology”, generally one acceptable to
the Department of Planning or DPaW. The 2007 Visual Landscape Planning in Western Australia
manual is one such methodology having being produced by the Western Australian Planning
Commission and Department of Planning and Infrastructure with input from DPaW, Main Roads WA
and other agencies that manage landscapes and landforms in WA. The methodology utilised for this
VIA is based broadly on the protocols outlined in this manual.
The Proposal will result in localised changes to the existing landscape character during the
construction, operation and closure of development areas. Some of these changes will be
temporary, but others will result in the permanent conversion of parts of the area to a mining
landscape character. Aspects of the Proposal that could result in visual impacts include:





Progressive clearing of native vegetation over pit areas and the WRL footprints, along roads
and other linear corridors, and over areas required for supporting infrastructure.
Altered landforms due to mining excavation and WRL development.
Altered surface drainage patterns in localised areas.
Dust generation during construction and operation of the Proposal as a result of earthworks,
ore haulage, waste rock disposal and other transport activities, and during rehabilitation and
closure earthworks.
Installation and use of lighting for safety and security of the operations.
Alterations to the contour of ridgelines and crests will occur as a result of mining activities, with
open pits being developed over a total area of 207.45 ha and WRLs being developed over a total
area of 185.1 ha adjacent to the HAR. These changes will result in permanent, but localised, changes
to the scenic amenity of these areas.
There will be views of the J5 and Bungalbin East mines from the four main access routes and two
regional viewpoints (Mt Manning and Mt Dimer) assessed in this study. However, the extent of the
visual impact will depend on the position of the viewer in the landscape, the distance between the
viewer and the mine(s), and the screening effect of landform and vegetation. Therefore, the visual
impact rating varies across the MMHARCP from Not Evident to Blending to Prominent.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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Page i
TABLE OF CONTENTS
PAGE
INTRODUCTION ......................................................................................................... 1-1
1.1
The Proposal ....................................................................................................................... 1-1
1.2
The Mt Manning - Helena-Aurora Ranges Conservation Park .............................................. 1-1
1.3
Environmental Assessment Process .................................................................................... 1-3
1.4
Structure of this Report....................................................................................................... 1-7
METHODOLOGY......................................................................................................... 2-1
2.1
Relevant Guidelines ............................................................................................................ 2-1
2.2
VIA Definitions .................................................................................................................... 2-1
2.3
Study Area Definition .......................................................................................................... 2-3
2.4
Approach to this Study ........................................................................................................ 2-3
2.5
Desktop Analysis ................................................................................................................. 2-6
2.5.1
Data Sources ...................................................................................................................... 2-6
2.5.2
Identification of Landscape Analysis Criteria....................................................................... 2-6
2.5.3
Selection of Study Sites ...................................................................................................... 2-7
2.6
Field Assessments ............................................................................................................. 2-10
2.7
Stakeholder Engagement .................................................................................................. 2-10
2.8
Data Analysis and Impact Assessment ............................................................................... 2-11
2.8.1
Landscape Characterisation.............................................................................................. 2-11
2.8.2
Photographic Montages and Viewshed Modelling ............................................................ 2-12
2.8.3
Impact Assessment and Management .............................................................................. 2-14
Visual Landscape Character ....................................................................................... 3-1
3.1
Regional Setting .................................................................................................................. 3-1
3.2
Regional Landscape Character Type .................................................................................... 3-2
3.3
Landscape Characteristics of the Helena-Aurora Ranges ..................................................... 3-4
3.3.1
Lithology ............................................................................................................................ 3-4
3.3.2
Landforms .......................................................................................................................... 3-6
3.3.3
Waterforms ..................................................................................................................... 3-13
3.3.4
Vegetation ....................................................................................................................... 3-13
3.4
Landscape Character Units ................................................................................................ 3-15
3.4.1
Overview ......................................................................................................................... 3-15
3.4.2
Western Range LCU ......................................................................................................... 3-17
3.4.3
Central and Eastern Ranges LCU ....................................................................................... 3-17
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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3.4.4
Plains LCU ........................................................................................................................ 3-18
3.4.5
Drainage Lines LCU........................................................................................................... 3-19
3.5
Scenic Qualities ................................................................................................................. 3-19
3.6
Visual Receptors and Viewing Points ................................................................................. 3-21
3.6.1
Key Visual Receptors ........................................................................................................ 3-21
3.6.2
Access and Travel Routes ................................................................................................. 3-22
3.6.3
Vantage Points and Viewing Locations ............................................................................. 3-23
3.7
View Experience ............................................................................................................... 3-25
3.7.1
J5 ..................................................................................................................................... 3-25
3.7.2
Bungalbin East ................................................................................................................. 3-26
3.7.3
Travel Routes ................................................................................................................... 3-26
3.7.4
Mt Manning ..................................................................................................................... 3-30
3.7.5
Mt Dimer ......................................................................................................................... 3-31
Visual Impacts and Management .............................................................................. 4-1
4.1
Relevant Aspects................................................................................................................. 4-1
4.2
Visual Management Objectives ........................................................................................... 4-1
4.3
Existing Disturbance and Impacts ........................................................................................ 4-1
4.4
Predicted Visual Impacts ..................................................................................................... 4-2
4.4.1
Construction and Operations Impacts ................................................................................ 4-2
4.4.2
LCUs................................................................................................................................... 4-2
4.4.3
View Experience................................................................................................................. 4-7
4.5
Cumulative Visual Impacts ................................................................................................ 4-12
4.6
Visual Management Zones, Strategy and Techniques ........................................................ 4-13
4.6.1
Definition of Amenity Management Zones ....................................................................... 4-13
4.6.2
Construction and Operations Stages ................................................................................ 4-13
4.6.3
Decommissioning and Closure Stage ................................................................................ 4-14
4.7
Residual Visual Impacts ..................................................................................................... 4-16
4.8
Monitoring and Contingency Measures ............................................................................. 4-17
Conclusion ................................................................................................................. 5-1
References ................................................................................................................. 6-1
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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Page iii
List of Appendices
A
Visual Impact Assessment Stakeholder Engagement Register
List of Tables
1-1
Mining Tenure held by Polaris Metals Limited relevant to the Proposal
1-2
ESD Required Work for the Amenity Factor
2-1
Data Sources
2-2
Selected Landscape and Landform Analysis Criteria
2-3
Study Site Distance Zones
2-4
Visual Impact Assessment Sites
3-1
Kalgoorlie Plain Regional Landscape Character
3-2
Lithology of the Helena-Aurora Ranges
3-3
Elevation Data for the Helena-Aurora Ranges
3-4
Slope Data for the Helena-Aurora Ranges
3-5
Aspect Data for the Helena-Aurora Ranges
3-6
Topographic Position Index Data for the Helena-Aurora Ranges
3-7
Solar Radiation Data for the Helena-Aurora Ranges
3-8
Wetness Index Data for the Helena-Aurora Ranges
3-9
Vegetation Height Data for the Helena-Aurora Ranges
3-10
Visual Landscape Summary
3-11
Visual Quality Classification of the Helena-Aurora Ranges and Surrounding Plains
3-12
Local and Regional Vantage Points and Viewing Locations
4-1
Visual Impact Categories
4-2
Visual Impact Summary for LCUs
4-3
Visual Impact Summary for View Experience
4-4
Area of Disturbance within the Helena-Aurora Ranges
4-5
Areas of Disturbance within the Local Assessment Unit
List of Flowcharts
2-1
Visual Landscape Evaluation and Impact Assessment Process
2-2
Approach to the Joint Assessment of Landform and Visual Impacts
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Visual Impact Assessment
29 August 2016
Page iv
List of Figures
1-1
Regional Location
1-2
Land Tenure
2-1
Study Area
2-2
Local Field Assessment Sites
2-3
Regional Field Assessment Sites
3-1
J5 Conceptual Geomorphology
3-2
Bungalbin East Conceptual Geomorphology
3-3
Lithology of the Helena-Aurora Ranges
3-4
Elevation
3-5
Slope
3-6
Aspect
3-7
Topographic Position Index
3-8
Solar Radiation
3-9
Wetness Index
3-10
Vegetation Height
3-11
Landscape Character Units
3-12
View Experience – J5
3-13
View Experience – Bungalbin East
3-14
View Experience – Koolyanobbing Track
3-15
View Experience – Bullfinch-Evanston Track & Marda Track
3-16
View Experience – Gus Luck Track and Mt Dimer Track
3-17
View Experience – Pittosporum Rocks/Menzies Track
3-18
View Experience – Mt Manning Track
3-19
View Experience – Mt Manning
3-20
View Experience – Mt Dimer
4-1
Existing Disturbance Area
4-2
Visual Impact Modelling - Site 26
4-3
Visual Impact Modelling - Site 3
4-4
Visual Impact Modelling - Site 16
4-5
Visual Impact Modelling - Site 16 – No Vegetation
4-6
Visual Impact Modelling - Site 14
4-7
Visual Impact Modelling - Site 8
4-8
Visual Impact Modelling - Site 9
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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Page v
4-9
Visual Impact Modelling - Site 11
4-10
Visual Impact Modelling - Site 19
4-11
Visual Impact Modelling - Site 22
4-12
Visual Impact Modelling - Site 21
4-13
Visual Impact Modelling - Site 21 – No Vegetation
4-14
Visual Impact Modelling - Site 20
4-15
J5 & BE Mine Perspective – Pre-mining
4-16
J5 & BE Mine Perspective – During Mining
4-17
J5 & BE Mine Perspective – Post Mining
4-18
J5 Mine Perspective – Pre-mining
4-19
J5 Mine Perspective – During Mining
4-20
J5 Mine Perspective – Post Mining
4-21
Bungalbin East Mine Perspective – Pre-mining
4-22
Bungalbin East Mine Perspective – During Mining
4-23
Bungalbin East Mine Perspective – Post Mining
4-24
Amenity Management Zones
List of Plates
3-1
Western Range LCU looking generally west from Site 4.
3-2
Rounded hills at Site 13 in the Western Range LCU.
3-3
Western Range LCU viewed from Site 26 on the Koolyanobbing Track.
3-4
A “monolith” at Site 15.
3-5
Rounded hills at Site 3 in the Western Range LCU obscured by vegetation.
3-6
View of the Western Range LCU from Site 2 on the Marda Track obscured by vegetation.
3-7
Bungalbin Hill within the Central and Eastern LCU, as viewed from Site 3.
3-8
The Central and Eastern Ranges LCU, as viewed from Mt Dimer (Site 31).
3-9
View of the Central and Eastern Ranges LCU above vegetation near Site 6.
3-10
View of the Central and Eastern Ranges LCU partially screened by vegetation near Site 8.
3-11
Gravelly soils at Site 16.
3-12
Cliff faces and outcropping northwest of Site 24.
3-13
Caves to the northeast of Site 12 (the former campsite at Bungalbin East).
3-14
Broad Valley and Sandplain landforms of the Plains LCU to the south of the HAR, viewed
from Site 12.
3-15
Undulating Plains in the Plains LCU to the north of the HAR, looking northeast from Site 15.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page vi
3-16
Drainage Lines LCU dissecting the Plains LCU, as viewed from Site 53. The Central and
Eastern Ranges LCU is visible in the background.
3-17
Drainage Lines LCU dissecting the Plains LCU, as viewed from Site 16. The Western Ranges
LCU is visible in the background.
3-18
Exploration area east of J5, at Site 13.
3-19
Excavated material adjacent to an exploration costean at Site 11.
3-20
Campsite at Site 8 on the Pittosporum Rocks/Menzies Track.
3-21
Former Bungalbin East campsite at Site 12.
Photographer for Plates 3-1 to 3-7, 3-9 to 3-13, 3-15 and 3-17 to 3-21: Sonia Finucane.
Photographer for Plates 3-8, 3-14 and 3-16: David Temple-Smith.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 1-1
INTRODUCTION
1.1
The Proposal
Mineral Resources Limited (MRL) proposes to develop the J5 and Bungalbin East Iron Ore Project
(the Proposal), approximately 100 km north-northeast of Southern Cross, Western Australia (Figure
1-1). The Proposal comprises construction, operation and closure of:




Open pits and Waste Rock Landforms (WRLs) at J5 and Bungalbin East.
Areas required for the temporary storage of cleared vegetation and topsoil/subsoil.
Access tracks and haul roads.
Supporting mine infrastructure and other facilities.
Ore from the J5 and Bungalbin East pits will be transported via the J4 haul road to the Carina
operations for dry crushing and screening. The ore will then be loaded onto trains at the Mt Walton
rail-siding. A 30 km bituminised haul road will connect the mine operations to the J4 haul road.
The Proposal will be developed on the following leases within the Shire of Yilgarn (Figure 1-2):



Mining leases M77/1095-I, M77/1096-I and M77/1097 (pending).
Miscellaneous licences L72/253, L72/254, L72/269 and L72/270.
General purpose lease G77/124 (pending).
The Proposal occurs within, and adjacent to, the Helena-Aurora Ranges (HAR). The HAR comprises
Banded Iron Formations (BIFs) and basalts, and is surrounded by an outwash plain derived from
these geological units (Gibson et al., 1997). This landscape feature is located within the Mt Manning
– Helena-Aurora Ranges Conservation Park (other than A class) (MMHARCP) (Figure 1-2). See Section
1.2 for information on the park.
1.2
The Mt Manning - Helena-Aurora Ranges Conservation Park
The conservation value of the HAR and adjacent Mt Manning Range was recognised in the 1960s70s. The Mt Manning Range Nature Reserve (class C) was created in 1979, but Mt Manning itself was
excluded from the Nature Reserve to allow mining as this area had already been designed a Mining
Act Ministerial Temporary Reserve.
It had been recommended that the HAR be included in an expansion of the Mt Manning Range
Nature Reserve, but instead the Government decided to create the MMHARCP (Department of
Environment and Conservation [DEC], 2012). The MMHARCP was gazetted in 2005 and included the
Mt Manning Range (which had previously been excluded from the Mt Manning Range Nature
Reserve) as well as the HAR.
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Page 1-2
The MMHARCP is vested in the Conservation and Parks Commission (CPC). The CPC was established
in May 2016 following changes to the Conservation and Land Management Act 1984 (CALM Act) in
late 2015, and replaces the Conservation Commission of WA and the Marine Parks and Reserves
Authority to become the vesting body for conservation lands, forest and marine reserves and to
provide advice to the Western Australian Government on conservation matters. It has a formal
planning role for the management of regional parks, enabling the Department of Parks and Wildlife
(DPaW) to manage these ecologically significant areas in cooperation with landowners (Anon, 2016).
The MMHARCP is managed by the DPaW for the purpose of “recreation by members of the public as
is consistent with the proper maintenance and restoration of the nature environment, the
protection of indigenous flora and fauna, and the preservation of any feature of archaeological,
historical or scientific interest“. It offers a relatively undisturbed natural environment that provides
visitors with an opportunity to experience a remote, outback experience within a varied landscape
that contains diverse native flora and fauna (DEC, 2008). It is used for tourism and recreation
including four-wheel driving, camping, hiking and nature appreciation (DEC, 2008).
The MMHARCP is accessible from locations such as Kalgoorlie, Southern Cross and Perth. Access to
the MMHARCP is via unsealed tracks from the south (Koolyanobbing Track), west (the Marda Track
leading from the Bullfinch-Evanston Road), east (the Gus Luck/Mt Dimer Track) and north-east
(Pittosporum Rocks/Menzies Track). Visitors accessing the MMHARCP from the west and south
must cross mine haul roads associated with the Windarling and J4 mines. A number of tracks within
the park are historical or current mining exploration tracks. Not all tracks are maintained on a
regular basis and some are not maintained at all.
Visitors to the MMHARCP include private individuals and families, commercial tour groups,
conservation groups such as the Wilderness Society and recreational four-wheel drive groups such
as the FJ Cruiser Club of Australia. Despite the range of visitor types, annual visitor numbers are low.
Data from traffic counters deployed in two separate locations by DPaW during 2013-2015 indicate
that an average of 340 vehicles access the MMHARCP annually, corresponding to an annual average
visitation of 1,362 persons. Visitation generally occurs during the cooler months of the year April to
October) due to the lack of water sources, remoteness of the area and higher temperatures during
summer months. Wetter periods also likely to be avoided due to a higher risk of tracks become
waterlogged and impassable to four-wheel drive vehicles (DEC, 2008).
There are no formal visitor facilities such as toilets or camp grounds within the MMHARCP, but two
frequently-used campsites are located in the vicinity of the HAR. The first of these is a signposted
campsite located on the Pittosporum Rocks/Menzies Track to the north of the HAR. The second is
located at Bungalbin East, but it is understood that the DPaW has now prohibited camping at this
location. The presence of fire pits elsewhere on the HAR (including J5) and the surrounding plains
suggest ad hoc use of the area for camping.
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Page 1-3
The MMHARCP is classified as an ‘other than A class’ reserve, which means that activities such as
mining can be carried out with the approval of the Minister for Mines in consultation with the
minister responsible for the reserve. In the case of the MMHARCP, the responsible minister is the
WA Minister for Environment.
Mineral exploration at the HAR first occurred in 1969 and 1970 when BHP undertook exploration
drilling for iron ore at Bungalbin Central and Bungalbin East. Portman Resources NL, in a joint
venture with Heron Resources (Heron), then undertook exploration drilling for iron ore at J5 in the
Mt Jackson Range during 2005 and 2006. Heron’s iron ore assets, which included various exploration
and mining tenements in the Mt Jackson Range and the HAR, were subsequently acquired by Polaris
Metals NL (Polaris) in 2006. In turn, MRL acquired Polaris in 2010. Polaris’ tenements within the
MMHARCP and relevant to the Proposal are listed in Table 1-1.
Table 1-1: Mining Tenure held by Polaris Metals Limited relevant to the Proposal
Tenement
Mining Lease 77/580
Mining Lease 77/1095-I
Mining Lease 77/1096-I
Mining Lease 77/1097
Miscellaneous Licence 77/253
Miscellaneous Licence 77/270
Miscellaneous Licence 77/269
General Purpose Lease 77/124
Date of Grant
15 June 1993
9 May 2011
9 May 2011
Pending
Pending
Pending
Pending
Pending
Area
(ha)
702.45
997.95
992.35
998
581
108.25
70.42
437.70
MRL’s Aurora Village is located south of the Proposal on Mining Lease 77/580 and provides support
for the company’s exploration activities within the MMHARCP and the operation of the nearby J4
mine. The camp will continue to be used during the construction phase for the Proposal.
1.3
Environmental Assessment Process
On 16 May 2014, Polaris referred the Proposal to the Environmental Protection Authority (EPA)
under Section 38, Part IV, of the Environmental Protection Act 1986. On 1 December 2014, the EPA
set the level of assessment for the proposal at Assessment of Proponent Information – Category B
(API-B). EPA Report 1537 was published on 12 January 2015 (EPA, 2015a) and was appealed. The
Western Australian Minister for Environment subsequently directed the EPA to assess the Proposal
at a Public Environmental Review (PER) level of assessment.
Polaris referred its Proposal to the Commonwealth Department of the Environment (DotE) under the
Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act). The Proposal is a
controlled action under the EPBC Act and is being assessed under the Bilateral Agreement between
the Commonwealth of Australia and the State of WA.
Subsequent to submission of these referrals, the proponent for the Proposal was changed to MRL.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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Page 1-4
An Environmental Scoping Document (ESD) has been prepared in relation to the environmental
assessment of the Proposal. The ESD identifies the preliminary key environmental factors or issues
to be assessed and addresses the requirements of both the WA EPA and the Commonwealth DotE.
The ESD was authorised by the EPA Chairman on 27 August 2015.
The ESD identifies Amenity as one of the preliminary key environmental factors for the Proposal.
The EPA’s objective for this factor is to ensure that impacts are reduced to as low as reasonably
practicable (EPA, 2015b). No definition for Amenity is provided in the ESD, but a number of aspects
that need to be considered are identified including land use and access, noise and vibration, dust,
light spill, and visual amenity. This Visual Impact Assessment (VIA) report addresses only visual
amenity, though reference is made where appropriate to the way in which visual amenity can be
affected by dust, light spill and alterations to landform (Table 1-2). The remaining aspects associated
with the Amenity factor will be assessed more fully in the PER and associated documents.
Table 1-2: ESD Required Work for the Amenity Factor
Required Work as defined in the ESD
42
43
44
Work completed in this VIA
Characterise the land use and amenity values of the
Conservation Park particularly noting the sensitive
receptors and important areas for human use that
could be affected by noise, dust and light-spill
emissions, visual amenity issues and alterations to
the landforms from mining.
The visual amenity values of the
Conservation Park are described in Section 3
(Visual Landscape Character). Assessment of
other amenity values such as land use and
issues such as noise is beyond the scope of
this study.
Include relevant maps to show the locations of the
sensitive receptors likely to be affected by the
proposal.
Characterise the environment by providing baseline
data on noise, dust and light-spill emissions at
sensitive receptor sites, as identified above, that
could be affected by noise, dust and light-spill
emissions.
Characterise the environment by providing a
description of the visual landscape character and
scenic quality values, and provide maps of the
visual landscape units that may potentially be
visually affected. This should include, but not be
limited to landforms, vegetation and any
waterways, and can be undertaken by way of 3
dimensional modelling and/or photographs.
A map of known campsites is provided as
Figure 4-1.
Reference is made in this report to dust and
light-spill emissions in relation to visual
impact only. Noise does not affect visual
amenity, so is not considered in this report.
A description of visual landscape character is
provided in Sections 3.2-3.4. Scenic qualities
are described in Section 3.5.
Visual impacts are described in Section 4.
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Table 1-2 (cont.)
Required Work as defined in the ESD
45
Identify and discuss the potential sources and
impacts of noise, dust and light-spill and alteration
to landforms from the proposal.
Work completed in this VIA
Potential sources of light-spill and dust from
the Proposal are identified in Section 4.4.
Impacts on visual amenity due to dust and
light-spill are discussed in Section 4.4.
Impacts due to alterations to landforms are
also discussed in Section 4.3 and 4.4 where
relevant to visual amenity.
46
47
48
Design and undertake a visual impact assessment
(VIA) for before, during and after the proposed
mining activities, to assess the impacts of the
proposal on visual amenity in accordance with the
Western Australian Planning Commission (2007)
Visual Landscape Planning in Western Australia: a
manual for evaluation, assessment, siting and
design, and in consultation with Parks and Wildlife.
The VIA should identify and describe the aspects of
the proposal which may potentially affect the visual
landscape character and scenic quality values both
temporarily and permanently, using agreed (by
EPA, in consultation with Parks and Wildlife)
reference and vantage points of surrounding areas
including travel routes and use area's viewer
positions and perceptions.
A peer review of the VIA information by a suitably
qualified individual with appropriate experience
and expertise is also required.
It is noted that separate reports have been
prepared in relation to landform impacts
(Bioscope Environmental, 2016a), noise
(Herring Storer Acoustics, 2016) and dust
(Pacific Environment Limited, 2016).
VIA design is based on Visual Landscape
Planning in Western Australia manual.
DpaW has been consulted on a number of
occasions in relation to the design and
outcomes of this VIA.
A discussion of vantage points and important
places is provided in Section 3.6.
Potential sources of visual impact resulting
from implementation of the Proposal are
outlined in Section 4.
Consultation on selection of study sites with
the EPA and DPaW has been conducted by
DPaW. See Section 2.7 and Appendix A for
further information.
Independent peer review of this report was
completed by Ecoscape. This report has
been revised to address the peer reviewer’s
comments, where relevant.
A close-out report has been prepared to
demonstrate how these comments were
addressed in this report and has been
provided to MRL under separate cover.
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Table 1-2 (cont.)
Required Work as defined in the ESD
49
Predict the residual amenity impacts from the
proposal on the landscape and sensitive receptors
and important areas for human use after
considering and applying avoidance and
minimisation measures. Impact predictions are to
include, but not be limited to:
a)
the likely extent, severity and duration of
the impacts from noise, dust, light-spill,
and alterations to the landscape, landform
and to amenity; and
b) simulations/modelling of the predicted
residual impacts from the proposal,
including changes to the landscape from
the agreed reference and vantage points.
Include the cumulative impacts on
amenity from the proposal and other
currently approved developments.
50
51
Demonstrate how the EPA's objective for this factor
can be met.
Identify management and mitigation measures for
the proposal including closure and rehabilitation
outcomes to ensure residual impacts are not
greater than predicted. The PER is to include:
a) A description of the management and
mitigation measures;
b) Develop management zones, prescriptions
and strategies for managing visual
landscape character relative to each stage
of the proposed operation; and
c) Environmental management plans
outlining the environmental
outcomes/objectives; other key regulatory
requirements; management actions;
monitoring (including methodology,
frequency, location and rational); trigger
criteria; contingency actions; review;
reporting; and consultation.
Work completed in this VIA
Management measures relevant to visual
impacts are outlined in Section 4.6. Potential
residual visual impacts are outlined in
Section 4.7.
Assessment of other amenity values and the
potential of the impact of noise and dust
were not part of the scope of this study.
Noise has no impact on visual amenity so is
not addressed in this report. Refer to
Herring Storer Acoustics (2016).
Bioscope Environmental is not aware of any
other mining developments that have been
approved, or that are reasonably
foreseeable, within the Conservation Park, so
cumulative impacts have not been
considered further in this report.
This is addressed in the PER.
Development of an environmental
management plan for visual amenity is
beyond the commissioned scope of work for
this study, though recommendations for
management and mitigation measures are
provided in relation to visual impacts in
Section 4.6.
An environmental management plan for all
of the components of Amenity (including
includes management of visual impacts) has
been prepared (Bioscope Environmental,
2016b). This plan will be appended to the
PER.
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1.4
Structure of this Report
This report describes the objectives, methodology and outcomes of this VIA.
Section 2 outlines the methodology utilised in this study. This VIA was conducted in conjunction
with a Landform Impact Assessment (LIA) and this is reflected in the design of the study
methodology. The outcomes of the LIA are reported separately (Bioscope Environmental, 2016a).
Section 3 describes the visual landscape character of the HAR and its local and regional setting. This
section includes data in relation to landforms, waterways and vegetation of the HAR and
surrounding plains. Information is also provided on known vantage points in surrounding areas,
travel routes and areas of important for human use.
Section 4 assesses the potential visual impacts of the Proposal and outlines proposed management
measures.
The report conclusions are presented in Section 5.
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METHODOLOGY
2.1
Relevant Guidelines
In developing the approach adopted for this VIA, it was recognised that WA does not have a single
model for landscape planning in the context of the State’s current planning system (Western
Australian Planning Commission [WAPC] and Department of Planning and Infrastructure [DPI], 2007).
However, reference is made to the assessment and management of visual impacts in a number of
documents including:

EPA Guidance for the Assessment of Environmental Factors No 6 (Rehabilitation of
Terrestrial Ecosystems) which was published in 2006 (EPA, 2006).

EPA Guidance Statement No 33 (Environmental Guidance for Planning and Development)
which was published in May 2008 (EPA, 2008).

Visual Landscape Planning in Western Australia. A Manual for Evaluation, Assessment, Siting
and Design (WAPC and DPI, 2007).

Reading the Remote: Landscape Characters of Western Australia (Department of
Conservation and Land Management [CALM] et al., 1994).
CALM’s 1989 Policy Statement No. 34 on Visual Resources Management on Lands and
Waters Managed by CALM.
Guidelines for Preparing Mine Closure Plans, which were first published by the Department
of Mines and Petroleum (DMP) in 2011 and updated in May 2014 (DMP and EPA, 2014).


2.2
VIA Definitions
The terms used in this VIA report are defined below.
Landscape
The term “landscape” is defined by EPA (2015c) as “all the features
of an area that can be seen in a single view, which distinguish one
part of the earth’s surface from another part”. The EPA recognises
that landscapes can be either natural (largely unaffected by human
activity) or human (created or significantly modified by human
activity), and that natural landscapes consist of a variety of
landforms (EPA, 2015c).
The appearance of a landscape is strongly influenced by the
underlying geology, landforms, soils, ecology, land uses and other
factors, all of which can influence the way in which landscape is
experienced and valued (Institute of Environmental Assessment
and The Landscape Institute, 1995, in EPA, 2008).
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Landscape Character Types
Landscape Character Type (LCTs) are distinct types of landscape
that are relatively homogenous in character. They commonly share
similar combinations of geology, topography, land cover and
historical land use (Tudor, 2014).
LCTs consist of Landscape Character Units (LCUs). See below.
Landscape Character Units
LCUs are similar to LCTs in that they also comprise homogenous
patterns of characteristics, but LCUs are smaller units than LCTs.
LCUs are characterised based on landform, waterform, vegetation
and land use (e.g. natural, rural or built) as well as individual
landscape features (WAPC and DPI, 2007).
Visual Amenity
EPA (2008) defines “visual amenity” as visual landscape character
that is valued by the community and notes that protection of visual
amenity of the surrounding environment is important to the sense
of well-being and quality of life of the community.
Visual Landscape Character
The term “visual landscape character” refers to the appearance of
the basic landscape elements (landform, vegetation, water bodies
and human land use) that makes an area identifiable or unique
(WAPC and DPI, 2007). A range of descriptors can be used to define
visual landscape character. These included in “Reading the
Remote” are form, line, colour, texture and scale (CALM et al.,
1994).
Visual Catchment
Visual catchment is defined as the extent of potential visibility to or
from a specific area, feature or proposal.
Viewshed
A viewshed or “seen area” is defined as the land that is actually
visible from a point or series of points, such as a lookout, road or
campsite. Normally, the extent of area that can be viewed is
limited by landform, vegetation and distance (WAPC and DPI,
2007).
Distance Zones
Distance can affect an observer’s perception of the landscape and
features viewed. Therefore, distance zones are used to measure
visibility in terms of distance from the observer to the landscape
and are based on the amount of colour and textural detail that is
visible to the observer (WAPC and DPI, 2007).
The distances zones adopted for this VIA are as defined by WAPC
and DPI (2007). These are as follows:



Foreground: from the viewer to 500 m.
Middle-ground: 500 m to 6.5 km.
Background: 6.5 to 16 km and beyond.
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2.3
Study Area Definition
The indicative footprint for the Proposal is shown on Figure 2-1 and contains the physical elements
listed in Section 1.1 (i.e. the open pits, WRLs and other areas required for the construction,
operation and closure of the J5 and Bungalbin East mines). This footprint includes the Potentially
Affected Landforms (PALs) defined in the ESD.
The boundary of the HAR used in this VIA report is as defined in the ESD (see Figure 2-1). The ESD
states that this landform boundary was determined based on geology and morphology, and
comprises the area having a slope of five degrees or greater together with an additional 50 m buffer
to allow for lower resolution source data.
Based on the ESD boundary of the HAR, this landform comprises six main areas. For ease of
reference, these are designated as L1-L6. See Figure 2-1.
To characterise the significance of the HAR landform in a local context, the ESD defines a Local
Assessment Unit (LAU). The boundary of the LAU in relation to the HAR and the MMHARCP (in
which the HAR is located) is shown on Figure 2-1.
To provide regional context, the EPA defined a regional study area boundary (see Figure 2-1).
According to the ESD, this regional study area is confined to the Mount Manning area with a focus
on indicative areas of BIFs and is derived from data from the Geological Survey of Western Australia
(GSWA) and land systems spatial data from the Department of Agriculture and Food Western
Australia (DAFWA). However, MRL has used a wider regional study area boundary for assessment of
the Proposal.
2.4
Approach to this Study
EPA Guidance Statement No 33 (EPA, 2008) outlines broad principles and some of the factors to be
considered during VIA. It does not prescribe methodologies for this type of study, but states that
practitioners should use a “recognised methodology”, generally one acceptable to the Department
of Planning or DPaW. The 2007 Visual Landscape Planning in Western Australia manual is one such
methodology having being produced by the WAPC and DPI with input from DPaW, Main Roads WA
and other agencies that manage landscapes and landforms in WA.
The methodology utilised for this VIA is based broadly on the protocols outlined in WAPC and DPI
(2007). This manual outlines two overlapping stages as follows:
1. Visual landscape evaluation, which aims to:





Define the scope and context of the assessment.
Describe the visual landscape character.
Evaluate how the visual landscape character is viewed, experienced and valued by
stakeholders.
Develop strategies for managing visual landscape character.
Integrate these strategies into the project planning system.
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Page 2-4
2. Visual impact assessment, which aims to:





Identify visual management objectives.
Describe the proposed development.
Predict the potential visual impacts.
Outline visual management measures.
Develop recommendations and options for monitoring.
The relationship between these stages is illustrated in Flowchart 2-1. In developing the VIA
methodology, reference was also made to Reading the Remote: Landscape Characters of Western
Australia (CALM et al., 1994).
Flowchart 2-1: Visual Landscape Evaluation and Impact Assessment Process
Visual landscape evaluation
Visual impact assessment
Define scope
and set context
Determine visual
management objectives
Describe visual
landscape character
Describe proposed
development
Describe potential
visual impacts
Evaluate how visual
landscape character is
viewed, experienced and
valued
Develop strategies for
managing visual landscape
character
Develop visual
management measures
Prepare final
recommendations and
monitor options
Implementation
Existing planning mechanisms
Planning outcomes
Development options
Consultation and review
Source: Visual Landscape Planning Manual (WAPC and DPI, 2007)
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MRL commissioned Bioscope Environmental to conduct a VIA for the proposal in conjunction with
the LIA (Bioscope Environmental, 2016a). The relationship between landform and visual impact
assessments was considered in developing the methodology to minimise or eliminate duplication.
Given the degree of overlap between the visual landscape evaluation, visual impact assessment and
landform impact assessment, the study tasks were designed to address the requirements of both
this VIA and the LIA. Flowchart 2-2 illustrates the relationship between this VIA and the LIA.
Flowchart 2-2: Approach to the Joint Assessment of Landform and Visual Impacts
Determine landform and visual
management objectives
Define scope and set context
Desktop Analysis
Describe construction,
operation and closure of
proposed development
Describe landform and visual
landscape character
Evaluate how landform and
visual landscape character are
viewed, experienced and
valued
Evaluate EPA position on
landform and visual impact
assessment
Select visual and landform
evaluation criteria
Site Assessment
Describe potential
landform impacts
Describe potential
visual impacts
Visual Data Analysis
and Impact Assessment
Landform Data Analysis
and Impact Assessment
Develop visual
management
strategies and
measures
Develop landform
management
strategies and
measures
VIA Report
(this report)
LIA Report
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2.5
Desktop Analysis
2.5.1
Data Sources
The study commenced with collation and review of the data and information listed in Table 2-1. This
information was used to establish landscape analysis criteria used during the field assessment
(Section 2.6) and data analysis (Section 2.8).
Table 2-1: Data Sources
Type of Data
Topography
Soils and landforms
Flora, vegetation and fauna
Surface drainage patterns
Tenements
Landholders
Geological and exploration information
Roads, tracks and drill lines
Aboriginal and European heritage sites
Landscape character types
Viewing locations, view experience and
stakeholder values
Aerial photography
2.5.2
Data Source
MRL, NASA SRTM, Geoscience Australia
MRL, Department of Agriculture and Food Western
Australia
MRL, Department of Parks and Wildlife
MRL, Landgate, Department of Water
MRL, Department of Mines and Petroleum
MRL, Department of Parks and Wildlife, Landgate
MRL, Department of Mines and Petroleum
MRL, Landgate
MRL, Department of Aboriginal Affairs and Heritage
Council
Public websites and other publicly available information
Public websites and other publicly available information
MRL, Landgate, Geosage ELS 2000
Identification of Landscape Analysis Criteria
A number of factors can be used to describe landscape, but some of these are constrained by
limitations such as incomplete datasets, limited public availability of existing databases and the risk
of subjective interpretation.
To reduce subjectiveness, it was proposed that the factors selected for this assessment be
measurable, preferably with data already held by Polaris or in public databases. A large number of
factors were tabled and discussed during a workshop attended by personnel from MRL, CAD
Resources and Bioscope Environmental on 18 May 2015. During this workshop, seven factors were
selected for use as landscape analysis criteria. The factors are:







Elevation.
Slope.
Aspect.
Topographic Position Index (TPI).
Wetness Index.
Solar Radiation.
Vegetation Height.
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Definitions for these criteria are provided in Table 2-2.
Table 2-2: Selected Landscape and Landform Analysis Criteria
Criterion
Elevation
Slope
Aspect
Topographic Position Index
Wetness Index
Vegetation Height
Solar Radiation
Definition
The relative height above sea level of the landform features at and
around the site
The angle of the landform. Provides an indication of steepness and
roughness (steeper slopes are usually rougher). Slope position is the
position of the slope relative to the features above and below it, and
is utilised to identify the valleys, ridges, upper and lower slopes.
Compass orientation of the face of the slope. Useful for determining
position relative to sun and wind conditions (north facing - more sun;
south facing - less sun).
Classifies the landscape into a number of categories such as Valleys,
Lower Slopes, Gentle Slopes, Steep Slopes (greater than 25° in this
case), Upper Slopes and Ridges.
Representation of the water movement across the slope faces.
Provides an indication of how the water will track into gullies etc.
Determined by using the difference between the ground returns and
non-ground (vegetation in this area) returns collected during the
LiDAR survey in 2011. The result is the height of the vegetation
across the survey area.
Measure of the amount of solar radiation against the slope faces at
specific times of the year or generally. Takes into account sun
position throughout the year.
Source: CAD Resources
2.5.3
Selection of Study Sites
During the desktop analysis, preliminary selection of study sites was made through consideration of
the factors outlined in Table 2-2. Groundtruthing of these sites and selection of additional study
sites occurred during the field assessments conducted in 2015 and 2016 (see Section 2.6). A total of
53 sites was selected through this process (Figures 2-2 and 2-3).
When assessing visual impacts, a key consideration in the selection of study sites is “visual
accessibility”. This is assessed based on those locations from which people will, and will not, be able
to observe components of the Proposal. These include fixed point locations such as campsites and
open viewing areas such as regional roads used to access or bypass the HAR.
Factors affecting visual accessibility at these locations include:


duration of exposure, which can be influenced by travel speed and direction of travel,
availability of camping facilities and lookouts, and other aspects;
foreground closure (i.e. visual barriers such as vegetation cover, topographic features and
man-made structures);
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Page 2-8


the extent to which opportunities to view the area of interest are confined to key travel
routes and roads in the immediate vicinity of the area; and
other factors such as traffic density, foreground interest and distraction, weather conditions
and other land uses in the area.
As indicated in Section 2.2, the distances zones adopted for this VIA are as defined by WAPC and DPI
(2007). These are as follows:



Foreground: from the viewer to 500 m.
Middle-ground: 500 m to 6.5 km.
Background: 6.5 to 16 km and beyond.
MRL engaged with the EPA and DPaW in January and February 2016 in relation to the location of the
initial study sites (Sites 1-26). Following this consultation process, two additional study sites (Sites
27 and 28) were selected for inclusion in the background distance zone. Subsequent to DPaW’s
review of an earlier version of this report in June 2016, a meeting was held with the DPaW on 16
June 2016 and additional study sites (Sites 29-53) were selected.
The study sites and their distance zones (based on distance between the study site and either J5 or
Bungalbin East) are listed in Table 2-3 and illustrated in Figures 2-2 and 2-3. A number of these sites
provide views for more than one distance zone.
Table 2-3: Study Site Distance Zones
Site No
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
Foreground
(up to 500 m from
Proposal Area)
Distance Zones
Middle-ground
(500 m – 6.5 km from
Proposal Area)
















Background
(more than 6.5 km from J5
or Bungalbin East)





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Table 2-3 (cont.)
Site No
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
51
52
53
Foreground
(up to 500 m from
Proposal Area)
Distance Zones
Middle-ground
(500 m – 6.5 km from
Proposal Area)


Background
(more than 6.5 km from J5
or Bungalbin East)


































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2.6
Field Assessments
An initial three-day site visit (including travel) was conducted by environmental personnel from MRL
and Bioscope Environmental on 1-3 July 2015. Field observations and data in relation to both this
VIA and the LIA were recorded at 26 sites within and adjacent to the Project Area in relation to:



Weather conditions.
Landscape character units and features (landform, waterform, vegetation, disturbance and
land use features).
Visual aspects of landscape character (scale, enclosure, diversity, texture, form, line, colour,
balance, movement and pattern).
Photographs were taken during the site assessment using a Nikon D7000 camera fitted with a Nikon
18-200 mm lens. Photographs to be used in photographic montages for visual impact assessment
were taken using a 70 mm focal length.
The weather was overcast on 1-2 July 2015, but good conditions were experienced on 3 July.
A second site visit was conducted on 23 February 2016 by environmental personnel from MRL to
take photographs at two additional sites (Sites 27 and 28). The camera used for these photographs
was the same as used during the July 2015 site visit. The weather ranged from fine to cloudy with
rainy patches during this site visit.
The third site visit was conducted on 28-30 June 2016 by an environmental officer from MRL and a
cartographer from CAD Resources to take photographs and collect data at Sites 29-53. The camera
used for these photographs was the same as used during the July 2015 site visit. The weather was
fine on 28 June 2016, partly cloudy to overcast with patchy rain on 29 June, and fine on 30 June.
2.7
Stakeholder Engagement
MRL recognises that successful project development requires active stakeholder engagement and
that this is a key component of the environmental assessment process. “Stakeholders” include both
internal and external stakeholders who are likely to affect, to be affected by, or to have an interest
in a proposed project. Early engagement with stakeholders enables proponents to better understand
and manage their expectations and the potential risks associated with the construction, operation
and closure of mining operations.
MRL has engaged with the following stakeholders are relevant to this VIA:






OEPA.
DPaW.
Non-Government Organisations (NGOs) and environmental groups.
Recreational groups.
Commercial tour operators.
Community members.
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Stakeholder engagement conducted by MRL in relation to this VIA included face to face meetings
and correspondence with the OEPA and DPaW, and telephone interviews with three NGOs (HARA,
Wilderness Society and Wildflower Society), four recreational groups (Adventure 4WD, WA 4WD
Association, Eastern Goldfields 4WD Club and All Tracks 4WD Club), three community members
known to use the HAR for recreational purposes (comprising a Perth-based individual and two
Southern Cross residents), and a commercial tour operator (Coates Wildlife Tours). A visitor use
survey was utilised by MRL to guide these interviews which included questions on the frequency and
purpose of park visitation, duration of stay and activities undertaken. In essence, the focus was on
how visitors access the MMHARCP, where they went to view the landscape, and what landscape
features they valued. Most interviews also included substantial unstructured conversations that
covered many aspects not included in the survey questionnaire.
See Sections 3.6, Section 3.7 and Appendix A for further information.
2.8
Data Analysis and Impact Assessment
Data from desktop data analysis (Section 2.5) and the field assessment (Section 2.6) were analysed
in relation to the criteria identified in Section 2.5.2 to determine the extent of the potential visual
impact arising from the Proposal.
2.8.1
Landscape Characterisation
To facilitate characterisation of the HAR in relation to the selected landscape criteria defined in
Section 2.5.2, MRL supplied CAD Resources with the data from two LiDAR surveys conducted on 2126 November 2011 and 22 June 2013. These data were supplied as point (xyz) data processed into a
continuous surface for analysis. The analysis methods described below were chosen to best describe
the HAR.
An initial elevation model was generated and then categorised into 20m elevation bands describing
the range of heights throughout the HAR. Following this, the surface was processed to classify the
landform by its slope using the gradient, or rate of maximum change in z-value, from each cell of the
surface. This slope model was then categorised into five bands to describe the range.
The next step was to determine the aspect of the surface. Aspect identifies the downslope direction
of the maximum rate of change in value from each cell to its neighbours, and gives a result as the
compass direction.
Following processing of aspect data, the TPI was investigated to classify the site into various classes
of slopes, ridges and valleys. This was conducted by examining the cell position in relation to those
that surround it and thereby determining its relative position and slope. This procedure was
developed by Weiss (2001) and Jenness (2006). See also Guisan et al. (1999) and Jones et al. (2000).
A Wetness Index was developed over the HAR to show the accumulation of flow relative to the
landform slope and catchment areas. The purpose of this is to show the hydrological process at work
in the region and identify areas of flow accumulation relative to the range and proposed disturbance
areas.
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Determination of incoming solar radiation was conducted based on methods from the hemispherical
viewshed algorithm developed by Rich (1990) and Rich et al. (1994) and further developed by Fu and
Rich (2002). This analysis was developed for the Spring Equinox and summarised across a number of
categories to show which faces of the range are subject to the most or least amount of sun.
A final model was run as a result of both the ground and non-ground (vegetation in this area) returns
collected during the LiDAR survey in 2011. Using these data, CAD Resources was able to determine
the difference between these two datasets and as a result determine the height of the vegetation.
The result has been categorised to show the way the vegetation heights vary across the slopes and
elevations. The data have also been incorporated into the visual impact assessment of the Proposal.
A simplified map of the LCUs was generated using the high resolution LiDAR TPI. The components
are defined as follows:

Western Range: This category comprises the Ridges, Lower Slopes, Mid Slopes, Upper Slopes
and Steep Slopes data for L1-L3 as defined by the TPI. Polygons of less than one hectare
were removed and the remaining polygons were generalised slightly with a 10m buffer.
Minor data edits were undertaken to remove small island "holes" within the polygons to
reduce the detail of the TPI data.

Central and Eastern Ranges: as for the Western Range, but for L4-L6.

Drainage Lines: This category comprises those areas calculated by the Wetness Index of
value 18 to 25 (i.e. the upper extent of the cumulative processing) with a buffer of 25m
applied. The confluence area of the drainage to the south west of the HAR was incorporated
using the Wetness Index values of greater than 12 to better capture the full extent of the
drainage area in this location.

Plains: This category comprises those areas not defined as above.
In generating the LCU map, reference was also made to the regional landform mapping within the
LAU by Newbey (1985).
2.8.2
Photographic Montages and Viewshed Modelling
A viewshed is defined as the land visible from a point or series of points, such as a lookout, road or
campsite (WAPC and DPI, 2007).
Photographic montages were prepared by CAD Resources to illustrate the viewsheds for 11 of the 53
study sites visited during the field assessments (Table 2-4). In selecting these sites, it was recognised
that:

The J5 and Bungalbin East areas are not directly visible from a number of the study sites.
The sites selected for viewshed analysis provide representative views of these areas.

A number of tracks currently provide access to the HAR. It is expected that most of these
will remain open to public access during the life of the Proposal, but a number of local road
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 2-13
closures will occur to ensure public safety. Potential road closures were considered in
selecting the sites for viewshed analysis.

There are no officially-designated campsites within the HAR and visitors to the MMHARCP
can select their own campsites. It is apparent that regular use has been made of the
Bungalbin East campsite at Site 12, but is understood that the DPaW has now prohibited
camping at this location. It appears that regular use is also made of the campsite at Site 8 as
this location is identified in the camping and day trip guide for the HAR produced by the
Wilderness Society and Helena and Aurora Ranges Advocates Inc (HARA) (undated). It is
understood that signage has now been added by DPaW to designate this as a campsite.

There are no formal look-outs or other facilities within the MMHARCP, and visitor use of the
HAR is not restricted to defined tracks and exploration gridlines. Hikers and other visitors
can access off-road areas at numerous locations across the HAR and throughout the park. It
is not practical to prepare photograph montages for all possible views given such variable
access, but representative viewsheds have been selected.
Modelling was conducted for these sites to demonstrate visual conditions before, during and
following cessation of mining.
Table 2-4: Visual Impact Assessment Sites
Site No.
3
8
9
11
14
16
19
20
21
Comments
This site was selected for viewshed analysis as it looks towards Bungalbin Hill.
This site was selected for viewshed analysis as it is used as a campsite by visitors to the
MMHARCP.
This site is located on the track to Pittosporum Rocks and the Hunt Range.
This site is located on the northern side of the HAR, off the Pittosporum Rocks Track.
This site is located adjacent to the J5 area and provides views of the proposed mine
site.
This site is located adjacent to the J5 area and provides direct views of the proposed
mine site. It provides a long view of the western portion of the HAR and encompasses
nearly all of the area visible from that site (including the J5 site) in a single view.
Modelling of the viewshed before, during and after mining with no vegetation was also
conducted for this site.
This site is located at the junction of the southern access track and the Mt Dimer track,
southwest of the Bungalbin East mine site.
This site was selected as it is located at a high point in the landscape and offers views of
the eastern portion of the HAR.
This site is located at an informal campsite on the Mt Dimer track. Modelling of the
viewshed before, during and after mining with no vegetation was also conducted for
this site.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 2-14
Table 2-4 (cont.)
Site No.
22
26
Comments
This site is located on the Mt Dimer track and offers direct views of the Bungalbin East
mine site. Modelling of the viewshed before, during and after mining with no
vegetation was also conducted for this site.
This site is located approximately 6.5 km southwest of Bungalbin Hill and includes
views of the areas to the west of the hill including the J5 area. This site was selected as
it offers one of the first views of the HAR when approached from the south and covers
a wider area of the range to the west of the hill.
The 2007 Visual Landscape Planning in Western Australia manual states that the most basic form of
viewshed analysis identifies an area of landscape that would be visible assuming that it has no
vegetation cover or built structures, and assesses the visual impact that would occur based on
landform alone and not taking into account potential screening by vegetation (WAPC and DPI, 2007).
However, the manual also states that vegetation should be mapped (or at least described) if it is
relevant to a particular assessment because it affects viewer experience. Vegetation is very relevant
to this VIA as it strongly affects viewer experience by enhancing it and by restricting it (by screening
the landform, thereby limited viewing opportunities). However, modelling of the viewsheds before,
during and after mining at J5 (Site 16) and Bungalbin East (Site 21) have been included for
completeness.
Most of the viewshed analysis focuses on views towards the HAR. However, views from campsites
at J5 (Site 15) and Bungalbin East (Site 12) have been included in this assessment as these specific
views will be lost if the Proposal is implemented.
2.8.3
Impact Assessment and Management
An assessment of the visual impacts that could arise from implementation of the Proposal was
conducted using the data and information outlined above. This assessment considered the likely
extent, severity and duration of direct and indirect impacts, and whether these impacts would be
temporary or permanent. Following this initial assessment, environmental management measures
were developed to mitigate, manage and monitor the predicted visual impacts. The extent of
potential visual impacts was then assessed.
J5 and Bungalbin East Iron Ore Project
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Page 3-1
VISUAL LANDSCAPE CHARACTER
3.1
Regional Setting
The HAR occurs in the region covered by the Bungalbin 1:100,000 geological map sheet (Chen and
Wyche, 2003), which encompasses an area in the central part of the Southern Cross GraniteGreenstone Terrane of the Yilgarn Craton. The Yilgarn Craton is described by Markey and Dillon
(2010) as “a sizeable area of Archaean bedrock that harbours a series of metamorphosed volcanic
and sedimentary mineral belts embedded in granitoids“. Much of the Yilgarn Craton has weathered
into gently undulating plains overlain by deeply weathered regolith (Markey and Dillon, 2011).
The Bungalbin region (as mapped by Chen and Wyche, 2003) covers a series of greenstone belts1
separated by large areas of granitoid rocks of mainly monzogranitic composition. Greenstone belts
of mafic volcanics and BIF are common in the northern and eastern parts of the Yilgarn Craton and
outcrop as isolated ranges, elongate ridges and discrete, prominent hills above plains of weathered
Cainozoic sediments (Markey and Dillon, 2011). From a distance, these features appear as dominant
focal points, but have a more commanding presence when viewed in close proximity. The terrain is
dissected by scattered chains of salt lakes that can become linked after heavy rains (CALM et al.,
1994).
“Banded Iron Formation” is a sedimentary rock of biochemical origin. BIFs were formed in sea water
as the result of oxygen being released by photosynthetic bacteria. The oxygen combined with
dissolved iron in the sea water to form insoluble iron oxides. The iron oxides precipitated out,
forming a thin layer on the ocean floor. Each band is assumed to be the result of cyclic variability of
the oxygen content of the sea water. The BIFs of the HAR formed during the Archaean,
approximately 3.0 Ga (Chen and Wyche, 2003). The BIF consists of alternating layers of iron oxides
(magnetite [Fe3O4] or hematite [Fe2O3]), chert, jasper and shale. The width of the alternating layers
can be from a few millimetres to several metres, with the formation itself being tens to hundreds of
metres in both width and thickness. The colour of the BIF is related to its bands with the iron oxide
bands ranging from a steel grey-blue to red, and the chert bands ranging from white through to
black, grey or yellow. The dark, blood-red bands are jasper (D. Kettlewell, pers. comm.).
Formation of the HAR was a complex process involving three deformational events to give the
current land surface. The HAR underwent thrust faulting in the first deformational stage which
caused a repetition of the HAR BIF units in the Bungalbin Syncline. By the close of the third
deformational event, the HAR had been uplifted, refolded and slightly rotated to reach its current
northwest dipping current position (Chen and Wyche, 2003).
1
The southeastern portion of the Marda-Diemals Greenstone Belt, the northern portion of the Hunt Range Greenstone Belt, the
southern end of the Mount Manning Greenstone Belt and a small portion of the Yerilgee Greenstone Belt.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-2
Following uplifting, the BIF ranges were subject to weathering processes that eroded the lateritic
duricrust that had formed above the BIF. The BIF is resistant to erosion and forms the hills and
ridges that remain after other materials have been eroded away (Chen and Wyche, 2003; HARA,
undated).
The current surface of the HAR is a mixture of goethite and hematite-weathered BIF covered in part
by a laterite derived from the underlying weathered BIF. The more siliceous parts of the BIF have not
weathered and these account for the steep flanks of the range as well as the main ridgeline. In areas
of structural weakness, the BIF has been altered to massive goethite with some hematite. The main
concentrations of these areas are the J5 and Bungalbin East iron deposits (D. Kettlewell, pers.
comm.).
3.2
Regional Landscape Character Type
The HAR and surrounds occur within the Kalgoorlie Plain Landscape Character Type (CALM et al.,
1994). A detailed description of the landforms, waterforms, vegetation and land uses of this region
is provided in CALM et al. (1994) and summarised in Table 3-1.
Table 3-1: Kalgoorlie Plain Regional Landscape Character
Landscape Character
Landform
Visual Aspect
Form
Line
Colour
Texture
Scale
Waterform
Vegetation
Form
Line
Colour
Texture
Form
Line
Colour
Description
Level to gently inclined landform; conspicuous low hills and
ranges; low windformed dunes; blocks and conical mullock
hills.
Level horizon.
Blue grey horizon; rust and blue grey streaked granite; soils
from soft peach to warm rosy pink reds to vivid coppers;
burnt red ironstone.
Craggy summmits; stony hills with rock-peppered surfaces;
rugged peaks; rocky edges.
Long, mostly uninterrupted views under big skies over the
almost level terrain.
Shallow depressions and floodways; rock pools; salt flats.
Tortuous linear chains of salt lakes.
Silver; blue; milky; transparent.
Smooth mirrored surface.
Slender, whippy trunks; Flat topped trees; rounded
broombushes; sheaths of discarded bark; low bushy heath.
Strong diagonal line of mallees and salmon gum trunks and
branches; strong horizontal layer from three definite
vegetation layers; fluid line of trunks.
Shimmering glossy leaves; silver grey, cream to pale salmon
pink and warm peach of salmon gum trunks; olive bronze to
copper trunks; dark stumps; light silvery brown; dark leaved
mallees; dull greens; grey discarded twigs and branches; soft
silver and gold grasses; dull red; profusion of vividly-coloured
wildflowers; bright yellow wattle blossoms; pale grey
Smokebush; bright tangerine Grevilleas.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-3
Table 3-1 (cont.)
Landscape Character
Vegetation
Visual Aspect
Texture
Scale
Land Use
Form
Line
Colour
Texture
Description
Scrubby undergrowth; smooth glossy trunks; flaking bark;
dusty and furry leaves; soft grasses and Smokebush; spiky
Honeymyrtle.
Mallee and salmon gum woodland encloses and channels long
views, and depth of view into woodland extensive; heath
vegetation channels views and visual penetration into heath is
minimal.
Pyramid mullock heaps; corrugated iron; form of historical
buildings.
Horizontal flat-topped man-made hills; angular poppetheads
and headframes; tall slender funnels of nickel smelter;
waterpipe; geometric line of roofing and building materials.
Red dust; silver grey waterpipe; rusting metal; shades of
roofing and building materials; greying fence posts; iron
railings.
Rough, scaly, rusting metal; mullock heaps and rubble-strewn
ground; roofing and building materials; flaking paint.
Source: CALM et al. (1994)
The region in which the Proposal is located is typically characterised by an expansive, gently inclined
landform which appears to be level in many areas, but is interrupted by conspicuous hills and low
ranges such as the HAR. From a distance, these features appear as dominant focal points, but have a
more commanding presence when viewed in close proximity. The terrain is dissected by scattered
chains of salt lakes that can become linked after heavy rains (CALM et al., 1994).
The region’s vegetation is considered by CALM et al. (1994) to be one of the intrinsic visual
components of this landscape. Located within the Great Western Woodlands, the vegetation of the
area comprises a mosaic of woodland, mallee, grassland, shrubland and unvegetated areas (Watson
et al., 2008). Perhaps the most visually dominant vegetation type is the tall eucalypt woodlands
which tend to enclose and channel long views. Views which penetrate deeply into the woodlands
are generally obscured, in part or in full, by the upper canopy while mid-section views are
interrupted by slender tree trunks (CALM et al., 1994). The lower storey within woodland areas is
variable in colour and texture, and can include the softer greys of saltbush. The woodlands are
interspersed with patches of low bushy heath that allow broader views over the gently undulating
landscape (CALM et al., 1994). In Spring, assuming that there have been good winter rains, the large
diversity of flora species for which the Great Western Woodlands is known (Watson et al., 2008)
becomes evident in a profusion of vividly-coloured wildflowers that appear among the green-grey
health (CALM, 1994) or as colourful vistas (Watson et al., 2008).
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
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Page 3-4
3.3
Landscape Characteristics of the Helena-Aurora Ranges
3.3.1
Lithology
A landform can be defined through the combination of its geology (composition) and morphology
(form) (EPA, 2015b). The relationship between the landforms at J5 and Bungalbin East and their
underlying geology is illustrated in Figures 3-1 and 3-2. The lithology of the HAR is outlined below.
The current surface of the HAR comprises a mixture of goethite and hematite-weathered BIF
covered in part by a laterite derived from the underlying weathered BIF (see Table 3-2 and Figure 33). Indeed, the most common lithological unit within the HAR is Siliceous BIF at 38.4%. This is also
the most common unit occurring within the Bungalbin East pit area (37.6%) and the second most
common unit within the J5 pit area (29.1%). The more siliceous parts of the BIF have not weathered
and these account for the steep flanks of the range as well as the main ridgeline. In areas of
structural weakness, the BIF has been altered to massive goethite with some hematite (D. Kettlewell,
pers. comm.). The main concentrations of these occur at the J5 and Bungalbin East deposits, with
Goethite Mineralisation being the third most common unit at these sites (at 14.8% and 20.8%,
respectively). It is noted that this unit only covers a small area within the wider HAR (2.7%). The
most common unit within the J5 pit area is Colluvium Scree (32.0%), which is the second most
common unit within the Bungalbin pit area (23.9%) and the HAR (21.1%).
Table 3-2: Lithology of the Helena-Aurora Ranges
Lithological Unit
Banded Iron
Formation
(Siliceous BIF)
Colluvium Scree
Jasperlite-rich
BIF
Description
HAR
Millimetre to metre scale beds of alternating
silica and ironstone (magnetite, hematite, and
commonly goethite). Many variations of BIF are
found across the range including abundant red
jaspilite, pale cherts and enriched bodies of
goethite and sometimes hematite.
Loose, unconsolidated sediments that have been
deposited at the base of hill slopes by rain-wash,
sheet wash, slow continuous downslope creep,
or a variable combination of these processes.
The colluvium is typically composed of subangular to well-rounded pebble to cobble sized
BIF, basalt, jasperlite and chert.
An iron-rich, chalcedonic quartz which occurs in
the BIF and banded chert horizons.
38.4%
Area
J5 Pit
Bungalbin
Area
East Pit Area
29.1%
37.6%
21.1%
32.0%
23.9%
13.8%
0.0%
0.3%
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-5
Table 3-2 (cont.)
Lithological Unit
Goethite
Mineralisation
Alluvium
Welded Detritals
Canga and
Scanga
Tuff
Goethite-rich BIF
Magnetite-rich
BIF
Hematite
Mineralisation
Bedded Goethite
Basalt
Description
HAR
Total replacement of BIF through chemical
weathering occurring as bands/horizons within
altered BIF, iron-rich basalt, and canga. Goethite
is the principal iron mineralisation type.
Loose, unconsolidated silt, clay, sand and gravel.
Alluvium is restricted to areas where clear
drainage channels are present.
Late stage detrital material comprising clasts of
host rock (BIF and chert dominant) in a recemented, siliceous, fine grain matrix. Typically
found as a thin ‘veneer’ at the base of the nonmineralised BIF sections of the range.
Pisolitic detrital units re-cemented in a hard,
iron rich matrix, formed by the chemical and
mechanical weathering of bedded iron deposits.
Scanga is interpreted as a canga with high silica
content either within the matrix or clasts. This
unit is generally identified down slope (at the
base) of bedded iron deposits.
A soft, fine grain, sometimes porphyritic unit
predominantly found in low lying saddles and
occasionally on the flanks of the range.
A goethite-rich BIF generally occurring on the
margins of the main deposits. Silica still remains
although iron is dominant. It has also been
observed within highly mineralised rock.
Magnetite iron ore widely distributed as bands
in the BIF and as interstitial crystals in mafic and
ultramafic rocks.
Weathering product of magnetite occurring as
beds/horizons within altered BIF, iron-rich
basalt, and canga.
Generally total replacement of BIF by goethite
+/- hematite and/or limonite. Minor patchy silica
still remains in parts. This rock type is the
primary unit comprising the Bungalbin East
mineralisation. The goethite beds typically
comprise a steep scarp profile on the south
eastern flanks of the range.
A volcanic rock occurring as tholeiitic and highMg types in the foothills of the range. Rare,
small occurrences on the flanks of the range.
2.7%
Area
J5 Pit
Bungalbin
Area
East Pit Area
14.8%
20.8%
0.2%
0.0%
2.4%
5.5%
0.0%
0.0%
3.0%
8.4%
2.8%
1.7%
0.0%
4.7%
1.1%
5.4%
5.2%
0.1%
0.0%
0.0%
0.0%
0.0%
0.0%
Source: Reynolds and Scarlett (2016) and CAD Resources
This unit is mapped on Figure 3-3 as
Goethite Mineralisation
0.7%
0.0%
0.0%
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-6
As a result of its geological setting and lithology, the HAR is characterised by fractured rock surfaces,
fissures and depressions, and is surrounded by outwash plains dissected by drainage lines. The
characteristics of these landforms are described in Sections 3.3.2 to 3.3.4 and mapped in Figures 3-4
to 3-10.
3.3.2
Landforms
Elevation
The HAR has a similar range of elevations to those of Mount Manning, Mount Jackson and Die Hardy
ranges (Bioscope Environmental, 2016a), but provides a dominant visual focus within the MMHARCP
as it represents a high point in a relatively wide area of undulating plains. Although the highest point
at the HAR is 702 mAHD, only a very small portion of the range (0.3%) occurs within the highest band
of elevation (680-702 mAHD) (Table 3-3 and Figure 3-4). Indeed, around one third of the range
occurs within the 480-520 mAHD band (35.5%) and around one third occurs at 520-560 mAHD
(30.6%).
The landforms surrounding the J5 pit are generally of lower elevation than the wider HAR, with
approximately 73% of the area being 480-520 mAHD (Table 3-3). Maximum elevations at J5 are 520540 mAHD. In contrast, the landforms surrounding the Bungalbin East pit are generally of higher
elevation than at J5, with 77.9% of the pit area occurring at 540-640 mAHD. Of the landforms
occurring in this elevation band within the Bungalbin East pit area, 29.4% are 540-580 mAHD and
47.5% are 580-640 mAHD. Maximum elevations are between 680 mAHD and 702 mAHD (0.5%).
Landforms within the indicative footprints for the WRLs, roads and other infrastructure mainly occur
in areas of lower elevation (Figure 3-4).
Slope
Slope data for the HAR, J5 pit and Bungalbin East pit are provided in Table 3-4 and Figure 3-5. Nearly
51% of the HAR has a slope of up to 10°, 28.7% has a slope of 10-20° and 15.3% has a slope of 2030°. The Bungalbin East pit area is also characterised by slopes in these categories with 24.4% of the
area having a slope of up to 10°, nearly 35.0% having a slope of 10-20° and 29.1% having 20-30°
slopes. In contrast, nearly 59% of the J5 pit area has a slope of up to 10° and 35.4% has a slope of
10-20°, but only 4.5% of the area has a slope of 20-30°.
Landforms within the indicative footprints for the WRLs, roads and other infrastructure mainly occur
in areas with more gentle slopes (Figure 3-5).
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-7
Table 3-3: Elevation Data for the Helena-Aurora Ranges
Elevation
430 - 440 mAHD
440 - 460 mAHD
460 - 480 mAHD
480 - 500 mAHD
500 - 520 mAHD
520 - 540 mAHD
540 - 560 mAHD
560 - 580 mAHD
580 - 600 mAHD
600 - 620 mAHD
620 - 640 mAHD
640 - 660 mAHD
660 - 680 mAHD
680 - 702 mAHD
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
0.23
0.01
50.92
1.48
296.43
8.59
505.78
14.66
719.43
20.85
642.48
18.62
414.79
12.02
258.56
7.49
186.37
5.40
142.39
4.13
113.01
3.27
71.98
2.09
39.13
1.13
9.50
0.28
3,451
100
Area within J5 Pit
ha
%
0
0.00
0.51
0.84
14.57
23.93
26.04
42.77
18.20
29.88
1.57
2.58
0
0.00
0
0.00
0
0.00
0
0.00
0
0.00
0
0.00
0
0.00
0
0.00
60.9
100
Area within Bungalbin East Pit
ha
%
0
0.00
0
0.00
0
0.00
0
0.00
9.51
6.49
14.41
9.83
16.53
11.28
26.58
18.14
31.13
21.24
22.61
15.42
15.92
10.86
4.72
3.22
4.40
3.00
0.76
0.52
146.6
100
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 3-8
Table 3-4: Slope Data for the Helena-Aurora Ranges
Slope
00 to 05 degrees
05 to 10 degrees
10 to 15 degrees
15 to 20 degrees
20 to 25 degrees
25 to 30 degrees
30 to 35 degrees
35 to 40 degrees
40+ degrees
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
718.90
20.83
1,062.88
30.80
561.62
16.27
426.30
12.35
313.74
9.09
214.72
6.22
104.59
3.03
29.22
0.85
19.09
0.55
3,451
100
Area within J5 Pit
ha
%
9.38
15.41
26.51
43.54
16.44
27.00
5.08
8.35
1.84
3.02
0.88
1.44
0.40
0.66
0.17
0.28
0.18
0.30
60.9
100
Area within Bungalbin East Pit
ha
%
12.02
8.20
23.80
16.24
26.03
17.76
25.25
17.23
24.29
16.57
18.36
12.53
9.20
6.27
3.60
2.46
4.03
2.75
146.6
100
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Visual Impact Assessment
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Page 3-9
Aspect
Aspect is an important consideration in VIA as it affects the direction in which a viewer can face and
therefore the landscape views available to that viewer.
Aspect data for the HAR, J5 pit and Bungalbin East pit are provided in Table 3-5 and Figure 3-6.
These data indicate that the dominant aspect for these areas is southeast to southwest at 42.3%
(HAR), 53.9% (J5) and 62% (Bungalbin East). It is noted that 21% of the J5 pit area has a northeast
aspect, compared to 10.8% of the HAR and 3.6% of the Bungalbin East pit area. Landforms within the
indicative footprints for the WRLs, roads and other infrastructure have variable aspects (Figure 3-6).
Topographic Position Index
Data in relation to the topographic position (or slope position) are provided in Table 3-6 and Figure
3-7. The TPI classifies the landscape into a number of categories such as Valleys, Lower Slopes,
Gentle Slopes, Steep Slopes (greater than 25°), Upper Slopes and Ridges. The classification works by
using the difference between a cell elevation value and the average elevation of the neighbourhood
(100m in this case) around that cell. Positive values mean the cell is higher than its surroundings
while negative values mean it is lower. The degree to which it is higher or lower, plus the slope of
the cell, can be used to classify the cell into slope position. If it is significantly higher than the
surrounding neighbourhood, then it is likely to be at or near the top of a hill or ridge. Significantly,
low values suggest the cell is at or near the bottom of a valley. TPI values near zero could mean
either a flat area or a mid-slope area, so the cell slope can be used to distinguish the two.
The data provided in Table 3-6 and Figure 3-7 indicate that the HAR is dominated by Gentle Slopes
with nearly 75% of the area falling into this category. The J5 and Bungalbin East pit areas are also
dominated by Gentle Slopes (at 74.9% and 45.5%, respectively), but Steep Slopes (18.2%) and Upper
Slopes (18.9%) also commonly occur with the Bungalbin East pit area. Landforms within the
indicative footprints for the WRLs, roads and other infrastructure are characterised primarily by
Gentle Slopes (Figure 3-7).
Solar Radiation
Solar radiation refers to the amount of sunlight received by the HAR. This plays an important role in
the visual appearance of the ranges. For example, strong sunlight can cause areas to appear
“washed out” of colour while shadows can add depth to a landscape, though it is noted that it can
be difficult to distinguish certain landscape features where these occur in heavy shadow.
Solar radiation data for the HAR, J5 pit and Bungalbin East pit are provided in Table 3-7 and Figure 38. The higher levels of solar radiation are received by gentler slopes. The lowest levels are recorded
in areas with steep slopes such as the tops of ridges, breakaways and cliff faces on the more southfacing components of the HAR (see the lighter areas shown on Figure 3-8). With their steep slopes,
they receive less direct sunlight and tend to have more shadowed areas. Landforms within the
indicative footprints for the WRLs, roads and other infrastructure receive high levels of solar
radiation (Figure 3-8).
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Page 3-10
Table 3-5: Aspect Data for the Helena-Aurora Ranges
Aspect
Flat (-1)
North (337.5 to 22.5)
North East (22.5 to 67.5)
East (67.5 to 112.5)
South East (112.5 to 157.5)
South (157.5 to 202.5)
South West (202.5 to 247.5)
West (247.5 to 292.5)
North West (292.5 to 337.5)
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
0.03
0.00
508.47
14.73
372.86
10.80
293.54
8.51
419.87
12.17
602.19
17.45
438.69
12.71
389.94
11.30
425.61
12.33
3,451
100
Area within J5 Pit
ha
%
0
0.00
5.84
9.58
12.76
20.95
5.69
9.34
7.59
12.47
12.93
21.23
12.3
20.20
2.3
3.78
1.48
2.44
60.9
100
Area within Bungalbin East Pit
ha
%
0
0.00
9.9
6.75
5.32
3.63
16.37
11.17
41.89
28.58
32.96
22.49
15.61
10.65
11.74
8.01
12.77
8.71
146.6
100
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Table 3-6: Topographic Position Index Data for the Helena-Aurora Ranges
TPI
(Slope Position)
Valleys
Lower Slopes
Gentle Slopes
Steep Slopes
Upper Slopes
Ridges
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
20.83
0.60
224.33
6.50
2,584.71
74.90
309.08
8.96
244.43
7.08
67.63
1.96
3,451
100
Area within J5 Pit
ha
%
0.41
0.67
4.64
7.63
45.63
74.93
1.24
2.03
7.06
11.60
1.92
3.15
60.9
100
Area within Bungalbin East Pit
ha
%
3.33
2.27
16.66
11.37
66.70
45.50
26.70
18.22
27.65
18.87
5.53
3.77
146.6
100
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Table 3-7: Solar Radiation Data for the Helena-Aurora Ranges
Solar Radiation
Less than 3,500 WM/m2
3,500 to 3,800 WM/m2
3,800 to 4,100 WM/m2
4,100 to 4,400 WM/m2
4,400 to 4,700 WM/m2
More than 4,700 WM/m2
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
183.85
5.33
201.48
5.84
392.19
11.36
1,191.2
34.52
1,137.82
32.97
344.56
9.98
3,451
100
Area within J5 Pit
ha
%
2.04
3.35
2.82
4.64
11.38
18.70
21.09
34.64
21.54
35.38
2.00
3.29
60.9
100
Area within Bungalbin East Pit
ha
%
22.80
15.55
22.07
15.06
31.57
21.54
37.18
25.37
20.95
14.30
12.01
8.19
146.6
100
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3.3.3
Waterforms
There are no permanent or semi-permanent water bodies within the HAR or in adjacent areas.
Instead, drainage lines are ephemeral and tend to be relatively narrow and shallow.
The Wetness Index data provided in Table 3-8 and Figure 3-9 indicate that is a high level of run-off in
areas with steep slopes such as the tops of ridges, breakaways and cliff faces on the more southfacing components of the HAR. These areas rank lower on the Wetness Index (see the darker areas
shown on Figure 3-9). This run-off is received by drainage lines within the HAR, which in turn drain
to waterways on the plains surrounding the HAR. Consequently, these areas rank higher on the
Wetness Index (see the orange-red areas shown on Figure 3-9).
3.3.4
Vegetation
Vegetation across the HAR and in surrounding areas has been surveyed by ecologia Environment
(2016). In total, 45 vegetation units were identified and mapped. The vegetation types in the J5 and
Bungalbin East pit areas are dominated by Eucalyptus, Banksia and Allocasuarina woodlands over
mixed shrublands and tussock grasslands. These vegetation types commonly occur across the HAR.
In contrast, the sandplains and other plains surrounding the HAR include Acacia shrublands,
Allocasuarina woodlands, Eucalyptus woodlands, Atriplex shrublands, and Eremophila and Olearia
shrublands (ecologia Environment, 2016).
Vegetation height data for the HAR, J5 pit and Bungalbin East pit are provided in Table 3-9 and
Figure 3-10. Vegetation height is important as it can have a masking or screening effect.
The data provided in Table 3-9 and Figure 3-10 indicate that vegetation in the J5 and Bungalbin East
pit areas is of similar heights to the vegetation occurring across the wider HAR. Most of the
vegetation in these areas is 2-5 m tall, with 46.7% of the vegetation at the J5 pit, 45.7% of the
vegetation at the Bungalbin East pit and 43.5% of vegetation in the wider HAR area occurring in this
category. Vegetation 5-10 m tall is also reasonably common in these areas with 28.0% of the
vegetation at the J5 pit, 21.9% of the vegetation at the Bungalbin East pit and 22.9% of vegetation in
the wider HAR occurring in this category.
Vegetation heights within the indicative footprints for the WRLs, roads and other infrastructure are
also quite variable (Figure 3-10).
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Table 3-8: Wetness Index Data for the Helena-Aurora Ranges
Wetness Index
0 to 2
2 to 4
4 to 6
6 to 8
8 to 10
10 to 12
12 to 14
14+
Total
Area within the Helena-Aurora Ranges
ha
%
4.15
0.12
272.34
7.89
1798.06
52.10
1060.45
30.73
252.98
7.33
51.19
1.48
9.99
0.29
2.02
0.06
3,451
100
Area within J5 Pit
ha
%
0.35
0.57
9.29
15.26
39.79
65.35
10.12
16.63
1.08
1.77
0.23
0.38
0.03
0.05
0
0.00
60.9
100
Area within Bungalbin East Pit
ha
%
4.30
2.93
53.86
36.74
75.83
51.73
9.35
6.38
2.37
1.62
0.79
0.54
0.08
0.05
0
0.00
146.6
100
Source: CAD Resources
Table 3-9: Vegetation Height Data for the Helena-Aurora Ranges
Vegetation Height
0 to 0.5m
0.5 to 1m
1 to 2m
2 to 5m
5 to 10m
10m +
Total
Source: CAD Resources
Area within the Helena-Aurora Ranges
ha
%
158.18
4.58
430.54
12.48
566.48
16.42
1500.55
43.48
790.64
22.91
4.81
0.14
3,451
100
Area within J5 Pit
ha
%
2.38
3.91
4.93
8.10
8.06
13.23
28.42
46.68
17.06
28.02
0.04
0.06
60.9
100
Area within Bungalbin East Pit
ha
%
6.49
4.43
15.87
10.83
24.03
16.40
67.01
45.72
32.09
21.90
1.08
0.73
146.6
100
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Page 3-15
3.4
Landscape Character Units
3.4.1
Overview
Detailed mapping of local landscape characteristics and the regional landform mapping by Newbey
(1985) were utilised to identify the following LCUs within the LAU:




Western Range.
Central and Eastern Ranges.
Plains.
Drainage Lines.
These LCUs are mapped on Figure 3-11 and described in Sections 3.4.2-3.4.5. In summary, the Plains
LCU (as mapped) covers the largest area of the LAU (Table 3-10). This unit is broad, open and
relatively flat, and occupies a lower position in the landscape. The terrain is gently undulating and
includes a number of low ridges and other elevated features, but none of these are as visually
dominant in the LAU as the Western Range LCU and the Central and Eastern Ranges LCU. The LCU
provides open views where lower shrublands occur, but views become partially or completely
enclosed where the vegetation is higher and/or denser.
Western Range LCU and the Central and Eastern Ranges LCU are both described in Table 3-10 as
being elevated with generally broad, open views that become partially enclose by woodlands and
taller shrublands. However, the Western Range LCU is visually different to the Central and Eastern
Ranges LCU as it has a generally lower elevation and has hills that are generally more rounded than
those in the Central and Eastern Ranges (see Sections 3.4.2 and 3.4.3). The Western Range LCU (as
mapped) covers the smallest area of the LAU (Table 3-10).
The Drainage Lines LCU covers an area about three times the size of the Western Range LCU, but
smaller than the Central and Eastern Ranges LCU (Table 3-10). Its presence low in the landscape is
similar to that of the Plains LCU, though it can be distinguished visually from elevated areas based on
changes in vegetation patterns. Where vegetation is taller and/or denser, views become more
enclosed and can be obscured.
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Table 3-10: Visual Landscape Summary
LCU
Western Range
Central and Eastern
Range
Plains
Drainage Lines
Unmapped Area
Total
View Experience
Elevated with generally broad, open views.
Partially enclosed by woodlands and the taller
shrublands.
Elevated with generally broad, open views.
Partially enclosed by woodlands and the taller
shrublands.
Broad, open and relatively flat. Lower position in
the landscape. Open views across lower
shrubland communities, but partially enclosed by
woodlands.
Lower position in the landscape. Incised to broad
drainage features. Taller and denser vegetation
encloses views.
Indicative Area
(ha)
Infrastructure
WRL
and Roads
Indicative Area
within LAU
(ha)
Pit(s)
727.66
54.74
16.98
4.07
75.79
2,723.57
146.14
0.07
1.22
147.44
24,514.79
6.59
167.92
187.58
362.08
0.08
21.06
21.14
185.06
213.92
606.45
2,120.48
4,733.27
34,819.76
207.45
Total
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3.4.2
Western Range LCU
The Western Range LCU comprises L1-L3 and is generally natural in appearance. A number of tracks
and exploration gridlines traverse this LCU and a number of informal campsites are present. J5 is
located at the eastern end of L3 (Figure 3-11).
This LCU is visually different to the Central and Eastern Ranges LCU (see Section 3.4.3) as it is lower
in height and the hills are generally more rounded than those in the Central and Eastern Ranges
(Plates 3-1 to 3-4).
When viewed from a distance, the Western Range LCU appears as a rolling blue feature with curved
lines just visible above the plains vegetation (Plate 3-3). However, closer views reveal a more
textured landscape dotted with rugged rocky outcrops in shades of reddish brown.
The visually irregular nature of these outcrops depends on their resistance to weathering processes.
Those rock types more susceptible to weathering have a lower profile and more rounded
appearance than those that are resistant to weathering. The 10 m high “monolith” at J5 (Site 15) is
an example of more resistant rocky material (Plate 3-4).
Closer views of the Western Range LCU, such as those provided along the Marda Track, reveal a
ridgeline vegetation in muted greens with patches of grey shrubs (Plate 3-4). As the hills in this LCU
are relatively low, views of this portion of the HAR are often obscured by vegetation (Plates 3-5 and
3-6).
Weathering processes are also responsible for the textured appearance of the gravelly soils that
occur along the ridgeline. These are defined by Soil Water Consultants (SWC) as SMU 1: Skeletal
Gravels (SWC, 2016). With increasing distance downslope, the thickness of the surface gravels
gradually increases due to colluvial deposition, resulting in the formation of SMU2: Shallow – Deep
Gravels. With the majority of the coarser textured particles (i.e. gravels) deposited in upslope areas,
the soils become predominately fine textured as distance downslope increases. These finer textured
soils have been defined by SWC (2016) as SMU 3: Deep Alluvial Clays and effectively form the plain
soils surrounding the outcropping ridges (SWC, 2016).
3.4.3
Central and Eastern Ranges LCU
The central portion of the HAR comprises the largest continual area of the ranges and includes
Bungalbin Hill (at the western end of L4) and the Bungalbin East mine (at the eastern end of L4).
Two smaller areas of the HAR occur to the northeast of L4 and are termed L5 and L6. These three
areas of the HAR have a generally higher elevation than the western portion (see Section 3.3.2) and
collectively comprise the Central and Eastern Ranges LCU.
The Central and Eastern Ranges LCU is generally natural in appearance though access tracks,
historical exploration disturbances and campsites are present in this LCU. Due to its elevation, this
LCU is quite visible even when viewed from a distance (Plates 3-7 and 3-8). At a distance, this LCU is
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29 August 2016
Page 3-18
bluish in colour, but in closer proximity, the palette becomes dominated by the muted greens and
olives of the open eucalypt woodland and acacia shrublands. The discontinuous canopy of the
woodlands opens up in places to allow clear views of the HAR though at some locations it screens or
obscures the view of the range (Plates 3-9 and 3-10). Rugged bedrock exposures and rocky outcrops
are common on the steep slopes and crests of the Central and Eastern Ranges LCU. Additional
texture is added by the gravelly soil that occurs along and downslope of the ridgelines (Plate 3-11)
and which becomes increasingly fine-textured as distance downslope increases (SWC, 2016). Small
cliff faces and caves are also present in some areas, more on south and east facing slopes (Plates 312 and 3-13).
3.4.4
Plains LCU
The Plains LCU surrounds the Western Range and Central and Eastern LCUs. It is generally natural in
appearance, but is traversed by the four major access tracks to the HAR (the Koolyanobbing Track,
Marda Track, Mt Dimer Track and Pittosporum Rocks/Menzies Track) as well as minor tracks. A
number of informal campsites occur within this LCU as well as the more established campsite at Site
8.
The Plains LCU has been described by Newbey (1985) as containing Broad Valleys, Sandplains and
Undulating Plains (Greenstone). The visual character of this LCU is illustrated in Plates 3-14 and 315.
The Broad Valley landform (Plate 3-14) comprises the choked remnant of a former drainage system
which was active under a higher rainfall regime than occurs now. The valley floors occur 20-50 m
below the surrounding Sandplain landform and are flat to gentle-concave with slopes of less than 2°.
Newbey (1985) notes that the soils of this landform have an intricate history of in situ weathering,
colluvial, alluvial and aeolian actions, and that valley carbonates have been largely leached from the
surrounding Sandplain (Newbey, 1985).
The Sandplain landform comprises the almost flat upland plain and the upper and middle valley
slopes (Plate 3-15). Newbey (1985) defines the dividing line between Sandplain and Broad Valley as
the change from erosional to colluvial valley slopes. Sandplain slopes rarely exceed 2° and the
internal relief is rarely more than 15 m (Newbey, 1985).
Newbey (1985) notes that Sandplain soils have developed over a long period of time and have been
laterized to some extent. Extensive sand sheets with a major component of colluvium from slightly
higher places on the Sandplain have developed in some places, and, occasionally, vegetated
remnants of small dunes from drier periods are present (Bowler [1976] notes that the last major dry
period appears to have occurred about 15,000 years ago). These dunal remnants provide a small
degree of variety in this visual landscape. There are no definitive drainage lines, but flows may occur
over short distances following heavy and intense falls of rain (Newbey, 1985).
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Page 3-19
The last of the landform units within the Plains LCU mapped by Newbey (1985) is the Undulating
Plains (Plate 3-15). The landform type comprises low rises and ridges interspersed with colluvial flats
that range from 50 m to 500 m in width and are drained by channels up to 1 m deep and 5 m wide.
Most rises and ridges are less than 5 m above the flats and have slopes that rarely exceed 10°. Soils
on the colluvial flats rarely exceed 1 m in thickness, are shallow on the rises and skeletal amongst
bedrock exposures on the ridges (Newbey, 1985).
The vegetation of the Plains LCU is dominated by eucalyptus woodland and acacia shrubland that
include medium to large shrubs interspersed occasionally with large trees in varying density. The
shrubland tends to be lower and denser than the woodland, though both have canopies with muted
colours of khaki and light brown. The more gravelly soils typically have red to coffee browns hues,
while the sandy soils are lighter in colour.
3.4.5
Drainage Lines LCU
As stated in Section 3.3.3, there are no permanent or semi-permanent water bodies within, or the
vicinity of, the HAR. Consequently, the presence of this LCU within the wider landscape is defined
more by vegetation patterns than the presence of water. For example, the correlation between
vegetation height and the water-gaining drainage lines is evident when the Wetness Index map
(Figure 3-9) is compared to the vegetation height map (Figure 3-10).
The creeks within the Drainage Lines LCU are ephemeral, relatively narrow and shallow. However,
there is often a higher level of soil moisture in the drainage lines which can support denser and often
taller vegetation (as well as different plant species) that enhances the visibility of these features as
they traverse the Plains LCU (Plates 3-16 and 3-17).
3.5
Scenic Qualities
High scenic quality, particularly scenery with natural landscapes, is often a primary reason that
people choose to visit conservation parks and similar areas (United States Department of Agriculture
[USDA], 2000). Scenic quality is based on landscape character and scenic integrity, as defined below:

Landscape character is the overall visual impression of attributes that provides a landscape
with an identity and sense of place. The combination of physical, biological and cultural
attributes is what makes each landscape identifiable and distinct (USDA, 2000).

Scientific integrity is a measure of the wholeness or completeness of the landscape,
including the degree of visual deviation from the landscape character valued by viewers
(USDA, 2000).
The HAR landscape comprises distinctive rock formations and rugged landforms that rise above the
undulating plains. The key scenic qualities of the HAR and surrounds were identified in consultation
with key stakeholders and are summarised in Table 3-11. This classification is based on the frame of
reference provided in CALM et al. (1994).
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Table 3-11: Visual Quality Classification of the Helena-Aurora Ranges and Surrounding Plains
Scenic Quality
High



Moderate



Low

Landform
Bungalbin Hill.
Central portion and eastern portions
of the HAR where views of the rugged
ridgetops are evident above or
through vegetation.
Assemblages of small caves,
particularly in the eastern part of the
central portion of the HAR.
Small monolith at J5.
Cliff faces.
Western portion of the HAR where
views of the range are partially
obscured by vegetation.
Expanses of similar landforms such as
foothills which are often visually
obscured by denser vegetation and
which provide few landmarks.
Waterform

Nil

Nil


Incised valleys.
Shallow drainage lines in the foothills
and on adjacent plains.
Vegetation
Seasonal wildflower displays, mainly in
the months of September and
October.
Stands of vegetation (woodlands,
mallees) that create distinctive forms,
colours or spacing in comparison to
surrounding vegetation.

Vegetation stands that exhibit the
range of size, form, colour, texture and
spacing that occur commonly in the
surrounding landscape.

Extensive areas of similar vegetation
with limited variation in colour and
texture.
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The landforms and vegetation within the MMHARCP are predominantly intact, but are not in pristine
condition. Regional mineral exploration for iron ore by BHP began in the 1950s and subsequently
included areas of the HAR. Exploration drilling at J5 by Portman Iron Ore (now Cliffs Natural
Resources) was also conducted in 2005-06, prior to the gazettal of the MMHARCP. Existing
disturbance within the park includes historical exploration gridlines and access tracks, drill pads,
sumps, drill holes, costeans, samples and sample bags, drums and other refuse (Plates 3-18 and 319).
It is estimated that 16.2 ha of disturbance is present within the HAR. Within the LAU, which has an
approximate area of 34,820 ha, there are approximately 151 ha of existing disturbance. This
includes tracks and disturbances associated with camping and other recreational activities (Plates 320 and 3-21).
3.6
Visual Receptors and Viewing Points
3.6.1
Key Visual Receptors
Visual impacts relate to the changes made to the composition of available views of landscapes. The
significance of these impacts depends on the type and extent of modification to the existing
landscape, whether these are temporary or permanent modifications, and people’s responses to
these changes. For the purposes of this assessment, key visual receptors comprise visitors travelling
through the area without stopping as well as those who make day trips or stay for longer periods.
The sensitivity of these receptors to changes in visual amenity depends on a range of factors
including:







their level of interest in the visual environment;
magnitude of the change in visual amenity and duration of the change (temporary or
permanent);
duration of the viewing opportunity (e.g. short or prolonged viewing opportunities);
number of viewers and their distance/angle of view of the affected area;
extent of screening/filtering of the view, where relevant;
the extent to which the change or modification to the landscape can be integrated within
the existing landscape and views; and
effectiveness of proposed mitigation and management measures.
Much of the Proposal is located within the MMHARCP (No. 48470) which, as discussed in Section 1.2,
is managed by the DPaW. EPA (2015a) states that the MMHARCP was created to facilitate
recreational activities consistent with the conservation of flora and fauna, and the preservation of
archaeological, historical or scientific features. Interestingly, a camping and day trip guide produced
by the Wilderness Society and HARA states that the area is not managed for recreational use
(Wilderness Society and HARA, undated).
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MRL obtained information on visitor use of the MMHARCP during engagement with the DPaW and
other stakeholders (see Appendix A). In summary, the MMHARCP is a destination for commercial
tours, recreational groups and others visiting the Great Western Woodlands, particularly during peak
wildflower viewing during the months of September-October. Based on information collated during
MRL’s stakeholder engagement program, key activities include four-wheel driving, sightseeing,
wildflower viewing, bird/wildlife viewing, bushwalking/hiking, camping, photography,
picnicking/barbequing, and relaxing. Around half of the four-wheel drive enthusiasts mentioned the
“tread lightly” philosophy.
Nearly all of those consulted during MRL’s stakeholder engagement program for this VIA
participated in most of the activities listed above (Appendix A). However, visiting Aboriginal/cultural
sites is not a popular activity. Reasons for this include lack of interest and cultural sensitivity (i.e. not
wishing to visit these places in the absence of an appropriate guide). High-energy activities such as
rock climbing, abseiling and cycling were also not popular activities within the MMHARCP.
Camping trips are organised by a range of organisations including the Wilderness Society in
conjunction with the HARA (Wilderness Society and HARA, 2015). Visitors are able to select their
own campsites and a number of these were located during the field assessments including the
former Bungalbin East campsite (Plate 3-18), a campsite north of the Pittosporum Rocks/Menzies
Track (Plate 3-17), and informal ad hoc campsites within and adjacent to the HAR (see Section 4.3).
Most of the campsites observed during the field assessments were clean and tidy at those times, but
litter and domestic waste were observed at the Bungalbin East campsite. It is understood that the
DPaW now prohibits camping at this site.
Despite being readily accessible from Perth, Kalgoorlie and Southern Cross, the MMHARCP has
relatively low visitation rates. Data from two vehicle counters installed by the DPaW (one to the
southwest of the Bungalbin East campsite and the other close to the campsite on the northern side
of the HAR) indicate that the number of vehicles recorded within the park averages between the low
100s to just over 200 vehicles in a six-month period during 2013-15. Based on assumptions made
regarding the number of people in each vehicle, this corresponds to around 160-200 visitors every
six months or so (Bioscope Environmental, 2016b). During the MRL stakeholder engagement
program, it was found that the serenity of the area and the fact that it does not have high visitation
rates are drawcards for most of the stakeholders consulted, as is the relative ease of access from
Perth.
3.6.2
Access and Travel Routes
A number of unsealed tracks provide access to the MMHARCP and the HAR itself (Figure 2-3). These
are:


the Koolyanobbing Track, which provides access from the south;
the Marda Track, which provides access from the west leading from the Bullfinch-Evanston
Road);
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

the Gus Luck/Mt Dimer Track, which provides access from the east; and
the Pittosporum Rocks/Menzies Track, which provides access from the northeast.
The Koolyanobbing Track is the main access route used by those consulted during MRL’s stakeholder
engagement program for this VIA (Appendix A). In general, these stakeholders could identify this
access route by name, but there was very little name recognition for the other tracks other than by
professional tour guides and environmental groups (NGOs). These groups were very familiar with
the area and provided precise information, but the majority of those consulted did not have detailed
knowledge of the area and generally stay on the tracks and in vehicles until they get into the HAR
where most will drive as far as possible and then walk to a high vantage point (see Section 3.6.3).
3.6.3
Vantage Points and Viewing Locations
The main viewing locations and vantage points (including tracks to and within the MMHARCP)
identified by the DPaW and other key stakeholders (see Section 2.7 and Appendix A) are listed in
Table 3-12. The significance levels used in Table 3-12 are as identified by WAPC and DPI (2007).
These are:

Level 1: national/State significance. WAPC and DPI (2007) indicates that examples of these
include:
o State highways and other main roads (sealed or unsealed) with high levels of vehicle
usage;
o designated tourist routes and scenic drives;
o recreation, conservation, cultural or scenic sites, areas, viewpoints and lookouts of
State or national significance, including their access routes;
o walk, cycle or riding tracks of national or State significance;
o towns, settlements or residential areas; and
o views of national or State importance.

Level 2: regional significance. Examples provided by WAPC and DPI (2007) include:
o main roads with moderate levels of regional usage (sealed or unsealed);
o recreation, conservation, cultural or scenic sites, areas, viewpoints and lookouts of
regional or high local significance, including their access routes;
o walk, cycle or riding tracks of national or State significance; and
o views of regional importance.

Level 3: local significance. Examples of these are identified by WAPC and DPI as:
o all remaining roads with low levels of regional usage;
o locally significant tracks or roads;
o recreation and other use areas of local significance;
o walk, cycle or riding tracks of local significance; and
o views of local importance.
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Table 3-12: Local and Regional Vantage Points and Viewing Locations
Significance Level
Level 1
Level 2
Location
MMHARCP
Bungalbin East former campsite
Campsite on the Pittosporum
Rocks/Menzies Track (Site 8)
J5 lookout
Bullfinch-Evanston Road/Marda Track
Koolyanobbing Track
Mt Manning
Mt Manning Track
Level 3
Pittosporum Rocks/Menzies Track
Pittosporum Rocks
Gus Luck/Mt Dimer Track
Mt Dimer
Description
Designated tourist site of state/regional
significance.
This location has been used as an informal
campsite for many years. It is understood
that the DPaW recently prohibited camping
at this location, but it is still accessible to
visitors and is used as a lookout.
Informal camping area on northern side of
the HAR.
Although an informal campsite, it is
understood that the DPaW recently
installed a sign identifying this site as a
camping ground.
Informal lookout on a ridge top in the
western portion of the HAR.
The Bullfinch-Evanston Road is a major
unsealed road leading to Mt Jackson, the
Die Hardy Range and the town of Menzies.
The Marda Track is a local unsealed track
between the Bullfinch-Evanston Road and
the western entry to the MMHARCP and the
HAR.
Minor unsealed track between
Koolyanobbing and Mt Dimer, leading to
the southern entry to the MMHARCP and
the HAR
Regional high point and scenic location of
high local significance. The Mt Manning
Track provides access to this location, but
this does not extend beyond the base of the
range.
Unsealed track between the BullfinchEvanston Road, and the western entry
points to the Mt Manning Range Natures
Reserve and the MMHARCP (Mt Manning).
Local unsealed track between Pittosporum
Rocks and the northeastern entry to the
MMHARCAP and the HAR.
This track is designed as 4WD only on local
maps (see, for example, Wilderness Society
and HARA [undated]).
Scenic site of local significance
Minor unsealed track between Jaurdi
Station and the eastern entrance to the
MMHARCP and the HAR
Regional high point and scenic site of local
significance.
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WAPC and DPI (2007) recognises that the significance level of access routes increases with:





the importance of the views including type, features and rarity;
the volume of use of roads and trails;
the degree of sensitivity of viewers (such as tourists);
the degree to which viewing the landscape is integral to the enjoyment of the travel route or
site; and
the duration of view, e.g. glimpses along the roads compared to long, uninterrupted views
from a key viewing location.
Regional vantage points to view the HAR include Mt Manning and Mt Dimer as well as major access
routes to the MMHARCP.
As indicated in Section 3.6.2, the Koolyanobbing Track is the main access route used by those
consulted by MRL. The majority of those consulted generally stay on the tracks and drive as far as
possible, then walk to a high vantage point such as the Bungalbin East former campsite, the J5
campsite and Bungalbin Hill.
Most of those consulted by MRL could not name the high points of the HAR, but it was evident that a
key objective of these visitors is to get up as high as possible into the range and observe panoramic
views from accessible locations. These include the Bungalbin East former campsite, J5 lookout and
Bungalbin Hill, but it is recognised that other high points are readily accessible. In addition to the
views, high points are favoured for provision of mobile telephone connections.
3.7
View Experience
The view experiences from J5 and Bungalbin East are described in Sections 3.7.1 and 3.7.2. These are
as experience by the field personnel conducting the third field assessment (see Section 2.6). Other
visitors may have difference experiences.
NGO/environmental groups consulted by MRL for this VIA noted that they liked the views from J5 to
Bungalbin East, and vice versa (Appendix A). In general, south and east facing views are favoured.
There was recognition within this stakeholder group that the southerly views differed from the
northerly views.
As indicated in Section 3.7.3, the main viewing locations and vantage points in relation to the HAR
are the main access tracks to and within the MMHARCP, Mt Manning and Mt Dimer. The view
experiences for these routes and locations are described in Sections 3.7.3 to 3.7.5.
3.7.1
J5
The Western Range of the HAR (L1-L3) is readily accessible by vehicles from the Marda Track.
Although this section of the range is relatively low in elevation compared with the Central and
Ranges (L4-L6), there are nonetheless expansive views in most directions from key vantage points.
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The outcropping ironstone comprises the highest part of the ridgeline in the Western Range. Site 15
is located just north of, and beneath, the tallest and largest ironstone outcrop on the ridgeline of L3.
Consequently, views from Site 15 to the south of the HAR are completely obscured though there are
sweeping views over open eucalypt woodland northeast along the flanks of the Central and Eastern
Ranges, north towards Mt Manning in the background and west along the northern flanks of the
Western Range.
Site 53 is located a relatively short distance from Site 15 at the eastern extent of the ironstone
outcrop, yet affords expansive views towards most points of the compass with the exception of
views to the west, which are obscured by the range itself. From this site, the view across eucalypt
woodland and acacia shrubland to the Koolyanobbing Range (some 40 km away) is uninterrupted.
The rolling summits of the central portion of the HAR, including Bungalbin Hill, dominate the skyline
to the east of the site (Figure 3-12). The view in this direction comprises an open woodland of
sandplain mallee mixed with a tall open shrubland of granite wattle interspersed occasionally with
orange-brown rocky outcrops and cliffs. To the north of Site 53, the views are similar to those from
Site 15.
3.7.2
Bungalbin East
The HAR in the vicinity of the Bungalbin East deposit is readily accessible via an unsealed four-wheel
drive track that branches off the Pittosporum Rocks Track and leads to the top of the range. This
portion of the HAR contains some of the tallest summits of the range and consequently provides
expansive views that stretch to the horizon.
Site 48 is located at the former Bungalbin East camping area (DPaW has now prohibited camping at
this location) at a point directly above a cliff-line on the southern side of the HAR. This site provides
expansive views to the north-northeast along the rocky ramparts and overhangs of the adjacent
ridgeline, east over the Great Western Woodlands towards Hunt Range, Mt Dimer and beyond, and
south-southeast towards the Finnerty Range and the Koolyanobbing Range (Figure 3-13).
There are generally no views to the northwest, west or southwest from Site 48 as they are obscured
by the HAR itself. In contrast, Site 49 (which is located only a short distance to the north of Site 48)
provides some views to the west (Figure 3-13).
3.7.3
Travel Routes
Koolyanobbing Track
The Koolyanobbing Track traverses eucalyptus woodland in the south near Koolyanobbing. Heading
north along this track, the vegetation transitions to extensive acacia shrubland on granite sandplains
then eucalypt woodland in the vicinity of Aurora mine. Within the granite sandplains, shrubs of
Acacia sp. frequently overhang the edges of the track, limiting visibility of the adjacent landscape.
Occasional larger eucalypt trees are also present in this area.
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The MMHARCP entrance is located at Site 38 (Figure 3-14). The view from this site is generally
representative of the view experience within the granite sandplains. There are no views of the HAR
looking north from this viewpoint, as shown in Figure 3-14. The view experience is predominantly
small scale and enclosed by vegetation with muted colours of khaki and light brown. Typical species
are Acacia neurophylla, Acacia beauverdiana and Acacia resinomarginea.
The first view of the HAR heading north along the Koolyanobbing Track occurs well within the
boundary of the MMHARCP. During the July 2015 field assessment, this occurred at Site 26.
However, during the June 2016 site assessment, this occurred at Site 52 as recent track maintenance
had pushed over some of the larger acacia shrubs that overcrowd the edge of the track, revealing
recently burnt areas with vegetation of smaller stature. As this vegetation is relatively low there are
views across the sandplain to the HAR, which appears low on the horizon (Figure 3-14).
From Site 52 northward along the Koolyanobbing Track, there are only occasional glimpses of the
HAR. For example, at Site 25 glimpses of the range occur through the surrounding woodland (Figure
3-14).
Bullfinch-Evanston Road and Marda Track
Heading north from Bullfinch, the Bullfinch-Evanston Road traverses low-lying sandplains
interspersed with linear chains of salt lakes associated with the extensive Lake Deborah system.
Middle and background views are generally not available from the road due to the height of
surrounding vegetation.
Immediately north of Lake Deborah, the Bullfinch-Evanston Road traverses medium woodland of
York Gum, Salmon Gum and Gimlet with an open, simple character. However, all views beyond the
foreground are obscured by large trees in every direction. Site 39 is a typical example of this view
experience (Figure 3-15).
Site 40 on the Bullfinch-Evanston Road provides a fleeting glimpse of the HAR to the east (Figure 315). This site marks a transition from medium woodland to the acacia shrubland that typifies the
granite sandplains. Accordingly, the vegetation in this area is a mixture of medium to large shrubs
interspersed occasionally with large trees that are dense in some areas and sparse in others.
Site 41 occurs further north along the Bullfinch-Evanston Road within the granite sandplains. It
affords an expansive view over acacia shrubland to the HAR and parts of the Jackson Range, which
appear low on the horizon (Figure 3-15). The landscape character at this site can be described as
smooth in texture, having rolling form with muted colour and generally harmonious balance.
There are no further views of the HAR whilst travelling in a northerly direction to the junction of the
Bullfinch-Evanston Road with the Marda Track. The Jackson Range tends to dominate the view
experience in this regard, although it is only evident occasionally through eucalypt woodland in
proximity to that range and beyond as far as the Die Hardy Range.
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The Marda Track extends from Marda Dam near Mt Jackson along the length of Jackson Range in an
easterly direction as far as the HAR. It initially traverses eucalypt woodland of York Gum, Salmon
Gum and Gimlet on the northern side of the range.
Site 44 provides the first glimpse of the western section of the HAR from the Marda Track as it is
situated adjacent to a locally elevated ridgeline that parallels the Jackson Range to the south. The
landscape around this site is large and open with diverse vegetation in the form of trees, shrubs and
groundcover. However, the vegetation adjacent to the track is more enclosed and channels long
views of the HAR (see Figure 3-15). It appears discordant due to the views in the middle distance
being juxtaposed with tall trees in the immediate foreground. A more extensive, although partially
obscured, view of the central portion of the HAR occurs at Site 46 from within a brachychiton mixed
open woodland/acacia closed shrubland (Figure 3-15).
Between Sites 44 and 46, the Marda Track passes immediately to the north of MRL’s J4 iron ore
mine. There is no visual evidence of this mine rom this track other than some basic signage, the
gated closure of the pre-mine track alignment over the Jackson Range and the demarcation of
several Aboriginal heritage places.
East of Site 46, the Marda Track affords glimpses of the HAR before the track traverses the range in
the vicinity of Site 2 (Figure 2-2). The track then continues eastward along the southern side of the
range within tan wattle (Acacia hemiteles) tall open shrubland. This shrubland affords glimpses of
the low ridgeline of L1-L3 adjacent to the track such as those present at Site 1 (Figure 3-15). At
times, the muted green of the ridgeline shrubland is indiscernible from the canopy of the tall open
shrubland beneath, being similar in colouration.
Towards the eastern end of L3, the higher and more extensive ridgeline associated with J5,
Bungalbin Central and Bungalbin Hill becomes noticeable (relative to the viewer’s position at J5),
where it tends to dominate the view experience. However, at Site 14 (which is effectively at the
junction of the Marda Track, the Pittosporum Rocks Track and the Koolyanobbing Track), the acacia
tall open shrubland of the drainage line encloses the view experience to the extent the neither the
western nor central portions of the HAR are particularly evident (Figure 3-15).
Gus Luck Track and Mt Dimer Track
There are distant views of the HAR from elevated positions within the Finnerty Range, ranging from
clear vistas to obscured views (e.g. see Site 29 on Figure 3-16. It should be noted that Site 29 does
not occur on the Gus Luck/Mt Dimer Track, but is located on an access track to MRL’s Carina mine
operation and therefore is closed to the public). However, where the Gus Luck/Mt Dimer Track
traverses the eucalypt woodland (Salmon Gum, York Gum and Gimlet) immediately west of the
Finnerty Range, view of the HAR are limited. This extensive woodland occurs at a lower elevation in
the landscape and, whilst large in scale and open, does not generally afford any views beyond the
foreground (relative to the viewer’s position on the track). Site 30 provides an example of this view
experience (Figure 3-16).
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From the junction of the Gus Luck Track with the Mt Dimer Track, the latter heads west toward
Vector Resources’ Mt Dimer gold mine and then towards the central portion of the HAR. The track
diverts to the south of the Mt Dimer gold mine, emerging from the eucalypt woodland onto an area
of higher elevation with an acacia open shrubland of turpentine mulga with mixed casuarina trees
(she-oak).
Site 28 (at the Mt Dimer go-around) provides the first view of the HAR along the Mt Dimer Track
(Figure 3-16). This site is surrounded by low to medium acacia shrubs, but is relatively open as a
result of recent fire. In the middle-ground (relative to the viewer on the track) the muted green
canopy of the eucalypt woodland provides diversity against a rolling background in which the HAR is
visible.
Further west of Site 28, the Mt Dimer Track splits in two, with one branch extending west-southwest
towards the Aurora gold mine and the other north then west to towards Bungalbin East. The
southern branch of the track traverses eucalypt woodland for its entire length until it meets the
Koolyanobbing Track. Whilst the woodland is relatively open beneath the tall trees of York Gum,
Salmon Gum and Gimlet, it affords no views of the HAR due to the largely enclosed canopy.
The northern branch of the Mt Dimer Track traverses open eucalypt woodland of Salmon Gum and
Gimlet over bladder saltbush, old man saltbush and silver emu bush. The open woodland permits
glimpses of the ridgeline of the HAR between gaps in the discontinuous green canopy upon
approach to Bungalbin East, such as at Site 21 (Figure 3-16).
In proximity to the HAR, the range becomes visually evident as a landform looming beyond the
canopy, but again only glimpses are occasionally available due to the tall but chaotic timber of the
open woodland. Sites 19 and 22 provide examples of this view experience (Figure 3-16). This view
experience continues along the Mt Dimer Track as it winds its way around the southern flanks of the
HAR, to the junction with the Koolyanobbing Track just to the south of Bungalbin Hill.
Pittosporum Rocks/Menzies Track
Pittosporum Rocks comprise a small, low, bare granite outcrop situated about two kilometres west
of Hunt Range. It is surrounded by scattered eucalypt trees and an acacia shrubland in varying
shades of green that becomes progressively more closed with distance from the Rocks. Site 32
provides an example of the view experience from Pittosporum Rocks, being large in scale, smooth in
texture and rolling in form as the eye settles on the slate blue HAR in the background (Figure 3-17).
Heading southwest along the Pittosporum Rocks/Menzies Track from Site 33, the view of the HAR
becomes obscured by the enclosed acacia shrubland before becoming briefly visible again in the
direction of travel in proximity to Site 33 (Figure 3-17). This view experience continues for most of
the length of the track, with glimpses of the HAR occurring occasionally immediately southwest of
Site 34 and then more frequently between Site 35 and Site 47 (Figure 3-17). All of these sites occur
within Acacia shrubland, some of which shows evidence of recent fire (where the shrubland is
typically less dense and often lower in height). It is noted that Site 34 itself, which is located at a
MMHARCP entry point, provides no views of the HAR (Figure 3-17).
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As the Pittosporum Rocks/Menzies Track approaches the HAR, the ridgeline becomes progressively
more visually evident within the landscape and the slate blue colouration typical of the background
view gives way to red coffee browns and muted greens of the soil, rocks and vegetation. Site 47 is
the final location, in this direction of travel, from which a clear view of the HAR can be obtained
before the acacia shrubland gives way to eucalypt open woodland in proximity to the range. This
woodland tends to obscure views of the HAR in part or in full in some areas. For example, at Site 8
(a campsite located on the northern side of the Pittosporum Rocks/Menzies Track), views of the HAR
are partially obscured by eucalypt trees and understory species (Figure 3-17). However, the HAR is
more visible where the vegetation opens up. See, for example, Site 6 on Figure 3-17.
The Pittosporum Rocks/Menzies Track is lined with Eucalypt open woodland until its junction with
the Marda Track and Koolyanobbing Track immediately east of the J5 deposit. The open woodland
affords lingering glimpses of the foreboding steep flanks and ridgeline of the HAR through the
canopy of soft green leaves.
Mt Manning Track
The Mt Manning Track departs the Bullfinch-Evanston Road in an easterly direction in the vicinity of
the Die Hardy Range (Figure 3-18). In this location, the track traverses medium woodland of York
Gum, Salmon Gum and Red Mallee with restricted views resulting from the enclosed canopy.
Further east along the Mt Manning Track, the woodland transitions to acacia mixed open shrubland
on sandy soils, marking a gradual descent from an elevated breakaway associated with the Die Hardy
Range to the lower country between the Die Hardy and Mt Manning ranges.
Site 42 provides a vast view experience east to the Mt Manning Range in the middle ground and
south to the HAR in the background (Figure 3-18). The rolling, dominant hills of the Mt Manning
Range appear as blue-green whilst the impressive extent of the HAR is clearly evident in slate blue
across an undulating green carpet of acacia shrubland and eucalypt woodland.
The view experience from Mt Manning is described in Section 3.7.4.
3.7.4
Mt Manning
The ridgeline of the Mt Manning Range is only accessible on foot from an unsealed vehicular access
track that leads to the base of the range. At the base of the range, from the unsealed track there are
views of the surrounding acacia mixed open shrubland against the dominant backdrop of the
rounded hills and sloping ridgeline of the Mt Manning Range.
Site 43 is located at the top of the western extremity of the Mt Manning Range. The elevation gain
relative to the access track below provides the visitor with vast and expansive views of the HAR, the
Mt Jackson Range and the Die Hardy Range, as well as views to the north and north-west that take in
the western side of the Mt Manning Range (Figure 3-19). This view is characterised by the muted
shades of smooth green vegetation generally in the mid-ground with angular to rolling slate blue
hills in the background. In the foreground, there is a diversity of colourful vegetation of light-green
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acacia, stunted grey-white trunks of eucalypt trees, green-grey tussock grass overlying the burnt
orange soil and oxidised blue ironstone rock of the Mt Manning Range.
3.7.5
Mt Dimer
Mt Dimer is located between the southern end of the Hunt Range and northern end of the Finnerty
Range, approximately 20 km east of Site 48 at Bungalbin East (Figures 2-2 and 2-3). It is accessed via
an unsealed, infrequently used and at times overgrown track meandering through mixed open
woodland of desert kurrajong and closed shrubland of granite wattle, the latter being more
prevalent on elevated, rocky slopes such as Mt Dimer.
The top of Mt Dimer is accessible on foot via a heavily overgrown four-wheel drive track, but even
with only modest elevation gain there are views to the south, west and north inclusive of the HAR.
The view from the top of Mt Dimer is vast in scale across a dense carpet of juniper green
woodland/shrubland transitioning to Aegean blue in the distance, set against the slate grey-blue
backdrop of the HAR (Figure 3-20). The view is expansive, although occasionally obscured by taller
vegetation in greens and olives in the foreground depending on the viewing position.
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Page 4-1
VISUAL IMPACTS AND MANAGEMENT
4.1
Relevant Aspects
The ESD for the Proposal identifies clearing of native vegetation and mining construction, operation
and closure as the aspects of relevance to the assessment of Amenity, including visual amenity. This
places primary focus on the J5 and Bungalbin East pits, WRLs, access routes and supporting
infrastructure.
4.2
Visual Management Objectives
The overarching Visual Management Objective (VMO) for the Proposal is to ensure that visual
impacts are reduced to as low as reasonably practicable. This aligns with the EPA’s objective for
Amenity.
In relation to the construction and operation phases of the Proposal, MRL aims to:


undertake best practice siting and design in order to reduce the visual impact of those areas
affected by Proposal implementation; and
protect and maintain the visual landscape character of those portions of the HAR not
affected by Proposal implementation to ensure that these retain their visual prominence.
In relation to the closure phases of the Proposal, MRL will seek to restore and/or enhance those
areas where visual landscape character has become degraded due to Proposal implementation,
where practicable.
The management targets and actions for light, dust and visual landscape are outlined in the Amenity
EMP (Bioscope Environmental, 2016b). This EMP should be read in conjunction with this VIA.
4.3
Existing Disturbance and Impacts
As discussed in Section 3.5, the HAR and surrounds are relatively intact, but are not pristine.
Disturbance has occurred at J5 and Bungalbin East, and throughout the wider HAR and MMHARCP,
as a result of recreational use, mineral exploration and road/track development and usage (Figure 41).
The presence of existing disturbances in the form of tracks and exploration gridlines improves access
to the HAR. Vehicle usage of the tracks in the MMHARCP results in the generation of dust. Dust liftoff also occurs from bare areas such as campsites under dry and windy conditions.
There are no permanent sources of light at the HAR or immediate surrounds, but the use of roads
and campsites in the area result in temporary and localised sources of light. Other sources of light
within the region include the Koolyanobbing iron ore mine to the south the HAR.
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4.4
Predicted Visual Impacts
4.4.1
Construction and Operations Impacts
Those aspects of the Proposal that could result in visual impacts include:

Progressive clearing of up to 606.45 ha of native vegetation over pit areas and the WRL
footprints, along roads and other linear corridors, and over areas required for supporting
infrastructure. This would be required for:
o Development of open pits at J5 and Bungalbin East. The voids remaining following
the cessation of mining operations represent a permanent change in the ranges.
o Development of WRLs on the plains adjacent to the J5 and Bungalbin East pits.
These features also represent a permanent change in the landform of these areas.
o Development of offices and other supporting infrastructure required for the
Proposal. These are considered to be temporary land use changes as these facilities
will be removed and the disturbance footprints will be rehabilitated following
cessation of operations.
o Development of the J5 and Bungalbin East haul roads. The haul roads will be
rehabilitated when no longer required, so are considered to be a temporary impact.

Dust generation during construction and operation of the Proposal as a result of earthworks,
ore haulage, waste rock disposal and other transport activities, and during rehabilitation and
closure earthworks. Dust lift-off will also occur from exposed WRL surfaces, ore stockpiles,
topsoil stockpiles and other disturbances during construction and operations, and from
rehabilitated and unrehabilitated surfaces during and following site closure. Dust can
adversely affect scenic amenity although such effects are transient in nature.

Installation and use of lighting for safety and security of the operations. Light-spill can be
distracting and annoying, and can affect sleep, particularly if the light is bright (EPA, 2008).
There are few, if any, existing light sources in the HAR area so it is likely that lights from the
Proposal will be visible from locations that have a direct line of sight, predominantly those at
higher elevations within the landscape. These lights will include:
o Static floodlights associated with mining operations.
o Directional lighting around mining areas, WRLs and supporting infrastructure.
o Vehicles moving around the site at night.
o Lighting emanating from mine site buildings.
4.4.2
LCUs
As discussed in Section 2.7.2, photographic montages and modelling of visual conditions before,
during and after mining were prepared for 11 study sites to facilitate assessment of the visual
impacts potentially associated with the Proposal. These sites were selected in consultation with,
and agreed to by, the OEPA and the DPaW.
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Visual impact has been classified according to the WAPC and DPI (2007) categories presented in
Table 4-1 and is discussed below. Those sites relevant to J5 (Sites 26, 3, 16 and 14) are discussed
first, followed by those sites relevant to Bungalbin East (Sites 8, 9, 11, 19, 22, 21 and 20).
Table 4-1: Visual Impact Categories
Type of Visual Impact
Not Evident
Blending
Prominent
Description
Development may be hidden, screened or not visible from specified
viewing locations
Development may be evident, but generally not prominent in that it
borrows from the existing landscape setting
Development may be a dominant feature in the landscape, drawing
attention to itself.
Source: WAPC and DPI (2007)
Site 26 provides a long view (background) of the Western Range LCU from the Koolyanobbing Track.
When approaching the HAR from the south (i.e. when travelling in a northerly direction along this
track), it is likely that one of the first views of the J5 pit and WRL at the eastern end of L3 will occur
in the vicinity of this site. During construction and operations, dust and night lighting may be visible
from this viewpoint. Permanent changes to L3 resulting from development of the J5 pit and WRL will
be visible during and following mining (Figure 4-2a). On this basis, the overall impact rating from this
site is predicted to be Prominent.
The Bungalbin East mining area will not be visible from Site 26 due to the screening effect of the
shrubland vegetation (Figure 4-2b). Therefore, the overall impact rating for this viewpoint in
relation to Bungalbin East is predicted to be Not Evident.
Site 3 is located within the Western Range LCU. It was selected for assessment as it can be accessed
by visitors to the HAR via a track that extends onto L3 (Figure 2-2). The viewshed shown in Figure 43 looks to the east towards J5, and demonstrates the way in which local topographic features and
vegetation obscure direct views of the mine. On this basis the overall impact rating is predicted to
be Not Evident. Dust and lighting associated with the J5 mine may be visible above the ridgeline, but
these are only temporary impacts.
The approximate location of the Bungalbin East mine is also shown on Figure 4-3, but it is considered
to be too far from Site 3 to result in either direct or indirect visual impacts. Therefore, the overall
impact rating for this viewpoint in relation to Bungalbin East is predicted to be Not Evident.
Site 16 is located within the Central and Eastern Ranges LCU, to the north of Bungalbin Hill. It was
selected for assessment as it is accessible from one of the main access routes around the HAR via an
exploration track and provides a clear, high-elevation view of the area proposed for the J5 mining
development on L3 within the Western Range LCU. The components of the J5 operations that will
be visible from this part of the HAR include the J5 pit and the J5 WRL. Dust and lighting associated
with construction, operation and closure of the J5 mine will also be visible at this viewpoint, but
these are only temporary impacts.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-4
The upper walls of the northern side of the pit will be visible from Site 16, but the lower portions and
base of the pit are unlikely to be visible. The ridgeline at the J5 pit will be altered by pit
development and the pit will remain visible following closure of the operation (Figures 4-4 and 4-5).
Therefore, the overall impact rating is predicted to be Prominent.
The WRL at J5 will be located on the Plains LCU adjacent to the J5 pit. The top of the WRLs will be
below the ridgeline, which reduces visual impacts. However, the WRL and other infrastructure will
be visible from Site 16 and adjacent areas. The closure design for, and rehabilitation of, the WRL will
maximise opportunities for visual blending of the facility with surrounding areas. If MRL is effective
in its rehabilitation and closure of the WRL and infrastructure, the overall impact rating is predicted
to be Blending.
Site 14 is located within the Plains LCU and provides views of the Western Range LCU in which the J5
pit will be developed. The visual impact modelling for this viewpoint suggests that existing
vegetation will screen views of the mine (Figure 4-6), so the overall impact rating is predicted to be
Not Evident. Dust and lighting associated with the J5 mine are likely to be visible above the canopy,
but these are only temporary impacts.
Site 8 is located on the Pittosporum Rocks/Menzies Track to the north of the HAR. It occurs within
the Plains LCU and has views of the northern side of the Central and Western Ranges LCU. This
viewpoint was selected for assessment as this is the campsite referenced in the HAR camping and
day trip guide (Wilderness Society and HARA, undated) (Figure 2-2).
Neither the J5 or Bungalbin East mine sites should be directly visible from the campsite as local
topographic features and vegetation should obscure views of the mines (Figure 4-7). Therefore, the
overall impact rating is predicted to be Not Evident. Dust and lighting associated with activities at
these mines may be visible at this location from time to time, but these are only temporary impacts.
Site 9 is also located on the Pittosporum Rocks/Menzies Track to the north of the HAR (Figure 2-2).
It also occurs within the Plains LCU and provides views of the Central and Western Ranges LCU. This
site was selected for assessment to determine if the Bungalbin East development would be visible to
travellers using this track as well as visitors who spend a longer period of time in this part of the
HAR.
Figure 4-8 indicates that mining at Bungalbin East will permanently alter the ridgeline that can be
viewed from this site, but that the WRL should not be visible. The woodlands in the vicinity of this
site tend to enclose and channel long views towards Bungalbin East, but it is recognised that the
mine and resultant landform changes will be more evident if a viewer is in a position closer to the
operations. Depending on the viewer’s location, the overall impact rating will be Blending to
Prominent. As with other sites with partial or full views of Bungalbin East, dust and lighting
associated with activities at this mine may be visible at this location, but these are only temporary
impacts.
Site 11 is located on the northern boundary of the Central and Eastern Ranges LCU and provides
views of Bungalbin East mine (Figure 4-9). Temporary visual impacts associated with dust and night
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-5
lighting are expected to occur at this site, but visual impact modelling for this viewpoint suggests
that existing landforms and/or vegetation will screen views of the mine (Figure 4-9), so the overall
impact rating is predicted to be Not Evident.
Site 19 is located at the western end of the Mt Dimer Track’s northern branch (Figure 2-2). This
viewpoint was selected as public access to the Mt Dimer track in this area could be maintained
during Proposal implementation. It occurs within the Plains LCU and provides views of the Central
and Western Ranges LCU.
The viewshed shown on Figure 4-10 looks in a northeasterly direction from Site 19 towards
Bungalbin East. Although the woodlands at this site are relatively open, visual penetration through
the vegetation becomes limited with distance. Therefore, views of the Bungalbin East mining
development from Site 19 are likely to be partly or even fully obscured (Figure 4-10). Dust and
lighting associated with mine construction, operation and closure will be visible at this location from
time to time, but the overall impact rating is predicted to be Not Evident.
Site 22 is located on undulating plains to the south of the Bungalbin East pit and southwest of the
Bungalbin East WRL and supporting infrastructure area (Plains LCU). The upper part of the ridge in
this part of the HAR (i.e. the Central and Eastern LCU) is of sufficient elevation to be visible above the
tree canopy. Figure 4-11 indicates that the upper benches of the Bungalbin East pit will be visible
from this viewpoint, so the overall impact rating is Prominent.
Figure 4-11 indicates that views of the Bungalbin East WRL from Site 22 will be partially obscured by
surrounding eucalypt woodlands. The WRL is likely to be visible from this site following closure of
the operations, though it is expected that the closure design for this new landform will maximise
opportunities for visual blending with surrounding areas. On this basis, the overall visual impact of
the WRL is expected to be Blending if rehabilitation and closure of this landform is effective.
Dust and lighting associated with activities at Bungalbin East are expected to be visible at this
location, but these are only temporary impacts.
Site 21 was selected for assessment as it is possible that public access may be maintained along the
Mt Dimer Track (northern branch). The viewshed shown on Figures 4-12 and 4-13 is from an
informal campsite on the northern side of the track looking in a northwesterly direction towards
Bungalbin East. As for Site 19, the woodlands at this site are relatively open, but visual penetration
through the vegetation becomes limited with distance. Therefore, views of the Bungalbin East
mining development from Site 21 may be partly obscured, but the Bungalbin East pit is expected be
visible at this location (Figures 4-12 and 4-13). Therefore, the overall impact rating is Prominent.
Site 20 is located to the east of the HAR (Figures 2-2 and 2-3). The site is located on low sand dunes
within the Plains LCU in an area previously subject to exploration. The condition of the road leading
to this site suggests that it is not accessed frequently. Due to the height of the sand dunes and the
Central and Eastern Ranges LCU, the Bungalbin East pit and associated development will be visible
above the woodland and shrubland vegetation present between this viewpoint and the mine. If dust
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-6
management is effective, it is less likely that significant volumes of dust would be visible from Site
20, but night lighting is likely to be visible.
The ridgeline within this portion of the Central and Eastern LCU (i.e. L4) is expected to be modified
as a result of mining at Bungalbin East. Although Figure 4-14 suggests that the general alignment of
the ridgeline is unlikely to change significantly, the overall impact rating is predicted to be
Prominent.
The location of the J5 pit is shown on Figure 4-14, but the height of the HAR between J5 and Site 20
means that this mining development should not be directly visible from Site 20.
The visual impact outcomes predicted above are summarised in Table 4-2.
Table 4-2: Visual Impact Summary for LCUs
Site No.
26
3
16
14
8
9
11
19
22
21
20
Visibility
The J5 mine will be visible from this viewpoint.
It is unlikely that the J5 mine will be directly visible from
this viewpoint as the L3 ridgeline is expected to obscure
views of the mine.
The J5 mine will be visible from this viewpoint.
The J5 mine is unlikely to be visible from this viewpoint.
It is unlikely that either the J5 or Bungalbin East mines will
be directly visible from this site.
The Bungalbin East pit will be visible from this viewpoint,
but the WRL should not be visible.
The Bungalbin East mine is unlikely to be visible from this
viewpoint.
Views of the Bungalbin East mine from this viewpoint are
likely to be partly or even fully obscured by vegetation.
The Bungalbin East pit and WRL will be visible from this
viewpoint.
The Bungalbin East pit will be visible from this viewpoint.
The Bungalbin East mine will be visible from this viewpoint.
Overall Impact Rating
Prominent
Not Evident
Blending - Prominent
Not Evident
Not Evident
Blending - Prominent
Not Evident
Not Evident
Blending - Prominent
Prominent
Prominent
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Visual Impact Assessment
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Page 4-7
4.4.3
View Experience
As discussed in Sections 3.6.2 and 3.7.3, there are four main access routes to the HAR (Figure 2-2).
These are:




the Koolyanobbing Track, which provides access from the south;
the Marda Track, which provides access from the west leading from the Bullfinch-Evanston
Road);
the Gus Luck/Mt Dimer Track, which provides access from the east; and
the Pittosporum Rocks/Menzies Track, which provides access from the northeast.
The view experiences from these tracks, along with those from J5, Bungalbin East, Mt Dimer and Mt
Manning, are described in Section 3.7. These travel routes and viewpoints were selected in
consultation with, and agreed to by, the OEPA and the DPaW. The predicted visual impact of the
Proposal on these view experiences has been classified according to the WAPC and DPI (2007)
categories presented in Table 4-1 and are summarised in Table 4-3. These relate primarily to visual
impacts associated with permanent landform changes. For all of the locations and travel routes
discussed in Section 3.7, there is potential for temporary visual impacts due to such factors as
vegetation clearing, dust and night lighting.
Table 4-3: Visual Impact Summary for View Experience
Viewpoint
Koolyanobbing Track
Bullfinch-Evanston Road and
Marda Track
Pittosporum Rocks/Menzies
Track
Visibility
Views of the HAR commence
approximately 12.5km south of L3. The
J5 mine will be visible from these
viewpoints.
The J5 mine will be visible from parts of
the Bullfinch-Evanston Road, though
the distance between the road and the
mine reduces the visual impact.
Due to the screening effects of
landform and vegetation, it is unlikely
that the J5 mine will be evident along
the Marda Track until closer to the
eastern end of this track.
The Bungalbin East mine will probably
be visible from the Pittosporum
Rocks/Menzies Track immediately west
of L5, but it is unlikely that it will be
evident from the more southwesterly
or northeasterly sections of the
Pittosporum Rocks/Menzies Track due
to screening effects of landform and
vegetation.
Overall Impact Rating
Prominent
Not Evident to Blending
Not Evident to Blending
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-8
Table 4-3 (cont.)
Viewpoint
Gus Luck/Mt Dimer Track
Mt Manning Track
Mt Manning
Mt Dimer
J5 and Bungalbin East
Visibility
The Bungalbin East mine will be visible
from elevated sections of this track and
in closer proximity to the mine.
The J5 mine may be visible from
sections of the Mt Manning Track
depending on the elevation of the track
and degree of screening (both of which
vary along the track). However, the
track is approximately 50 km north of
the HAR, so the significance of any
visual impact is reduced.
There is a line of sight from Mt
Manning point to the Western Range
LCU and it is possible that the northern
side of the J5 mine (such as ridgeline
changes due to pit development) could
be visible from this viewpoint.
However, Mt Manning is more than 40
km from J5 so the significance of any
visual impact would be reduced.
There is a line of sight from Mt
Manning point to the Central and
Eastern Ranges LCU, but it is expected
that L5 will mask views of the Bungalbin
East mine, depending on the elevation
of the observer. In the event that the
mine is visible, the distance from this
viewpoint to the mine means that any
visual impact would be reduced.
The Bungalbin East mine will be visible
from Mt Dimer.
Development of the J5 and Bungalbin
East mines means that it will no longer
be possible to experience the views
from those sites. However, the wide
expanse of adjacent elevated areas
means that similar views can be
obtained from other locations adjacent
to, and further afield from, these sites.
Overall Impact Rating
Not Evident to Prominent
Not Evident to Blending
Not Evident to Blending
Prominent
NA
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-9
Based on the information discussed below (as summarised in Table 4-3), it is apparent that there will
be views of the J5 and Bungalbin East mines from the four main access routes and two regional
viewpoints (Mt Manning and Mt Dimer) assessed in this study. However, the extent of the visual
impact will depend on the position of the viewer in the landscape, the distance between the viewer
and the mine(s), and the screening effect of landform and vegetation. Therefore, the visual impact
rating varies across the MMHARCP from Not Evident to Blending to Prominent.
Koolyanobbing Track
The Koolyanobbing Track is the main access route used by those consulted during MRL’s stakeholder
engagement program for this VIA (Appendix A). Views in the direction of the HAR from this track are
shown on Figure 3-14. Modelling of the potential visual impact of Proposal implementation was
conducted for Site 26 (Figure 4-2a) as first view of the HAR heading north along this track occurs in
the vicinity of this site, which is well within the boundary of the MMHARCP. This modelling shows
that permanent changes to L3 from development of the J5 pit and WRL will be visible during and
following mining from this location. Consequently, the overall impact rating is predicted to be
Prominent. The Bungalbin East mine will not be visible from this viewpoint on the Koolyanobbing
Track due to the screening effect of the shrubland vegetation.
Bullfinch-Evanston Road/Marda Track
The Bullfinch-Evanston Road and Marda Track are used to access the HAR from the west. Distant
views of the HAR occur in places along the southern portions of the Bullfinch-Evanston Road where
vegetation is lower in height (Figure 3-15). It is possible that the J5 mine will be visible from these
locations, but the distance to the HAR means that significant impact is unlikely. Large trees and
taller shrubs obscure views of the HAR for much of this route (Figure 3-15) and in these areas, there
will be little or no visual impact due to the screening effect of this vegetation. On this basis, the
overall impact rating is predicted to be Blending to Not Evident.
There are no views of the HAR from the northerly portions of the Bullfinch-Evanston Road as it
approaches and intersects with the Marda Track. Indeed, the first views of the HAR occur on a
locally elevated ridgeline in the vicinity of Site 44 (Figure 3-15). The Marda Track traverses the
Western Range LCU in the vicinity of Site 2 and then heads generally in an easterly direction towards
J5. The height and density of vegetation adjacent to the Marda Track provides a screening effect
(Figure 3-15), so it is unlikely that the J5 mine will be visible until the observer is closer to the eastern
end of this track. On this basis, the overall impact rating is predicted to be Blending to Not Evident.
The Marda Track joins (and effectively becomes) the Pittosporum Rocks/Menzies Track in the vicinity
of Site 14 (Figure 2-2). The visual modelling conducted for this viewpoint suggests that the overall
impact rating will be Not Evident (see Section 4.4.2 and Figure 4-6).
Pittosporum Rocks/Menzies Track
The Pittosporum Rocks/Menzies Track is located to the north of the Central and Eastern Ranges, and
heads in a generally northeast direction generally parallel with the HAR (Figure 2-2). The HAR is
visible above the tree canopy for much of this travel route, though some views are partially obscured
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-10
due to vegetation height and density (Figure 3-17). Modelling of the potential visual impact of
Proposal implementation was conducted for Sites 8 and 9. This shows that neither the J5 or
Bungalbin East mine sites should be directly visible from the campsite at Site 8 as local topographic
features and vegetation should obscure views of the mines (Figure 4-7). Therefore, the overall
impact rating for this site is predicted to be Not Evident. However, mining at Bungalbin East will
permanently alter the ridgeline that can be viewed from Site 9 (Figure 4-8). Depending on the
viewer’s location, the overall impact rating at this section of the track is expected to be Blending.
It is unlikely that the Bungalbin East mine will be evident from those sections of the Pittosporum
Rocks/Menzies Track located southwest or northeast from Site 9 due to screening effects of
landform and vegetation.
Gus Luck/Mt Dimer Track
There are distant views of the HAR from elevated positions within the Finnerty Range, ranging from
clear vistas to obscured views. However, as discussed in Section 3.7.3, where the Gus Luck/Mt
Dimer Track traverses the eucalypt woodland immediately west of the Finnerty Range, views of the
HAR are limited or non-existent. Indeed, Site 28 (at the Mt Dimer go-around) provides the first view
of the HAR along the Mt Dimer Track (Figure 3-16). Whether there are views of the HAR further
along the Mt Dimer track depends on the openness of the woodland canopy. Where the canopy is
more open or woodland species are absent, glimpses and view of the HAR are available. However,
no views of the HAR occur where there is an enclosed canopy (Figure 3-16). This view experience
continues along the Mt Dimer Track as it winds its way around the southern flanks of the HAR, to the
junction with the Koolyanobbing Track just to the south of Bungalbin Hill.
Modelling of the potential visual impact of Proposal implementation was conducted for Sites 19, 21
and 22 (Figure 2-2). As discussed in Section 4.4.2, the level of visual impact likely to be experienced
at these sites depends on proximity to the Bungalbin East mine and the screening effect of
vegetation (Figures 4-10 to 4-13). Consequently, the overall impact rating for the Gus Luck/Mt
Dimer Track varies from Prominent to Blending to Not Evident.
Due to the screening effect of the Central and Eastern Ranges LCU, the J5 mine will not be evident
from the Mt Dimer Track.
Mt Manning Track
The western section of the Mt Manning Track traverses a eucalypt woodland, the canopy of which
restricts views of the HAR. Further east along the track, this woodland transitions to an acacia
shrubland, marking a gradual descent from an elevated breakaway associated with the Die Hardy
Range to the lower country between the Die Hardy and Mt Manning ranges. Views of the HAR occur
where not obscured due to local variations in landform and vegetation. For example, Site 42
provides a vast view experience (Figure 3-18).
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Page 4-11
The J5 mine may be visible from sections of the Mt Manning Track depending on the elevation of the
track and degree of screening (both of which vary along the track). However, it is recognised that
this track is located approximately 50 km north of the HAR, so the significance of any visual impact is
reduced. Therefore, the overall impact rating is predicted to be Blending to Not Evident.
Mt Manning
As discussed in Section 3.7.4, the upper elevations of Mt Manning provide the visitor with vast and
expansive views of the HAR (Figure 3-19). Mt Manning is located generally north of J5, so it is
possible that the northern side of this mine (such as ridgeline changes due to pit development) could
be visible from this viewpoint. However, Mt Manning is more than 40 km from J5 so the significance
of any visual impact would be reduced. Therefore, the overall impact rating is predicted to be
Blending.
Mt Manning is located generally north-northeast of Bungalbin East. Although there is a line of sight
from this viewpoint to the HAR, it is expected that L5 within the Central and Eastern Ranges LCU will
mask views of the Bungalbin East mine, depending on the elevation of the observer. In the event
that the northern side of this mine (such as ridgeline changes due to pit development) is visible from
this viewpoint, the distance from this viewpoint to the mine means that any visual impact would be
reduced. On this basis, the overall impact rating is Blending to Not Evident.
Mt Dimer
Mt Dimer is located between the southern end of the Hunt Range and northern end of the Finnerty
Range (Figures 2-2 and 2-3) and, with even only modest elevation gain, provides views of the HAR
(Figure 3-20). It is expected that the Bungalbin East mine will be visible from this viewpoint, so the
overall impact rating is Prominent. However, the distance from this viewpoint to the mine means
that any visual impact would be reduced.
J5 and Bungalbin East
In addition to the above viewpoints towards the HAR, this VIA considered the potential for the loss
of views from the HAR across the surrounding plains. The development of mining at Bungalbin East
will result in the removal of a former campsite that provides views of the areas generally east to
southwest of the HAR (see Figure 3-13). Although DPaW has now prohibited camping at this site, it
is still open to public access and can be used as an informal lookout.
An informal campsite also exists at J5 and provides views of the areas generally to the north and east
of the Western Ranges LCU. Figure 3-12 shows views from Sites 15 and 53. The elevation and wide
expanse of the surrounding area means that similar views can be obtained from other locations
adjacent to, and further afield from, J5 and Bungalbin East.
Despite the comments above, it is recognised that removal of the former Bungalbin East campsite
and closure of the track to this site will reduce access to the top and southern areas of that portion
of the HAR and this may limit the ability of some visitors to access views from these areas.
J5 and Bungalbin East Iron Ore Project
Visual Impact Assessment
29 August 2016
Page 4-12
4.5
Cumulative Visual Impacts
Direct disturbance will occur within the HAR due to pit development at J5 and Bungalbin East if the
Proposal is implemented. No more than 208 ha of land will be cleared during pit development
(Table 4-4). Development of these pits will increase the disturbance footprint within the HAR to
6.48% (including existing disturbance).
Table 4-4: Areas of Disturbance within the Helena-Aurora Ranges
Element
Area covered by the HAR (as defined using the OEPA’s boundary)
Estimated area of existing disturbance within the HAR
Area of disturbance proposed for the J5 pit
Area of disturbance proposed for the Bungalbin East pit
Total
Area
(ha)
3,451
16.2
60.88
146.57
Percentage
(%)
0.47
1.76
4.25
6.48
Source: MRL and CAD Resources
Within the wider LAU of approximately 34,820 ha, there are approximately 153.6 ha of existing
disturbance (0.44%). Additional direct disturbance of no more than 606.45 ha (1.74%) will occur if
the Proposal is implemented (Table 4-5), which will increase the disturbance footprint within the
LAU to around 2.2% (including existing disturbance).
Table 4-5: Areas of Disturbance within the Local Assessment Unit
Element
Area covered by the Local Assessment Unit
Estimated area of existing disturbance within the LAU
Area of disturbance proposed for the J5 pit
Area of disturbance proposed for the J5 WRL
Area of disturbance proposed for the J5 supporting infrastructure
Area of disturbance proposed for the J5 haul road
Area of disturbance proposed for the Bungalbin East pits
Area of disturbance proposed for the Bungalbin East WRL
Area of disturbance proposed for the Bungalbin East supporting
infrastructure
Area of disturbance proposed for the Bungalbin East haul road
Total
Area
(ha)
34,820
153.60
60.88
87.39
46.03
56.26
146.57
97.67
44.09
Percentage
(%)
67.52
0.19
2.18
0.44
0.17
0.25
0.13
0.16
0.42
0.28
0.13
Source: MRL and CAD Resources
The Proposal will result in localised changes to the existing landscape character during the
construction, operation and closure of development areas. Some of these changes will be
temporary, but others will result in the permanent conversion of parts of the area to a mining
landscape character (Figures 4-15 to 4-23) and change their scenic qualities.