URSA MAJOR MINERALS INCORPORATED
A report describing the Caro Lake surface exploration diamond drilling program on the URSA
Major Disraeli Lake Property, District of Thunder Bay, Ontario
March and April 2011
located in the LECKIE LAKE AREA, LITTLE STURGE LAKE AREA and the RIGHTANGLE
LAKE AREA (G-0067)
Thunder Bay, Mining Division, Ontario
1:50,000 NTS Map Sheet
Zone 16U 052 H03 Eaglehead Lake and 052 H02 Shillabeer Lake Sheets, Western Ontario.
Report Prepared By:
Harold J. Tracanelli, Getn. P.Geo., 1156,
Onaping, Ontario
Ian Dasti; HBSc. Geo
Thunder Bay, Ontario
April 12th., 2011
Table of Contents:
1.0
Executive Summary
2.0
Property Location and Access
3.0
Property Ownership
4.0
URSA Major Minerals Incorporated
Disraeli Lake Property, Thunder Bay Mining Division, Ontario
5.0
Physiography and
6.0
Vegetation and Wildlife
7.0
Brief Exploration History
8.0
URSA Disraeli Property – Caro Lake Diamond Drilling Project
9.0
Geology
9.1
Geology in Diamond Drill Hole U-17-01 of the Caro Lake
Diamond Drilling Project, on the URSA Disraeli Property
10.0
Results of the Diamond Drill Program
10.1
URSA Major Minerals Incorporated QA / QC
Program
11.0
Conclusions
12.0
Recommendations
13.0
Certificate of Qualifications
14.0
List of Reference Materials Used within this Report
LISTING OF TABLES
Table: 1 Listing of The URSA Major Minerals Incorporated – Disraeli Lake Property Leckie
Lake Area (G-0067), Claims on Record with the Ontario Ministry of Northern Development
Mines and Forestry
LISTING OF FIGURES.
Figure: 1. URSA Major Minerals Incorporated – Disraeli Lake Property Location Map, Leckie
Lake Area (G-0067) Thunder Bay Mining Division, Ontario
Figure: 2 URSA Major Disraeli Lake Property – Caro Lake Diamond Drilling Program, Location
Map.
LISTING OF PHOTOGRAPHS.
Photograph: 1 Entrance of the Mawn Lake Road off of Provincial
Highway 527
Photograph: 2 View facing north west over part of Disraeli Lake
APPENDIX I,
Cross Sections and Plans for Diamond Drill Hole U-17-01
APPENDIX II,
Diamond Drill Hole Core Logs and For DDH Hole U-17-01
APPENDIX III,
Assay Certificates for samples collected in DDH U-17-01
APPENDIX IV,
Supporting Project Expenditure Related Documentation
1.0
Executive Summary
This assessment report covers one 375 meters deep hole used to test an airborne geophysical
response in the area of Caro Lake area.. Caro Lake is located approximately 1,200 meters south
of the south end of Disraeli Lake – Leckie Lake Area.
This report describes the various efforts and results associated with the initiation and completion
Caro Lake surface diamond drilling program in March and April of 2011.
The URSA Major - Disraeli Lake Property, is located approximately 65 kilometers NNE of the
city of Thunder Bay, District of Thunder Bay, Ontario.
The property includes 23 contiguous, manually staked mining claims, consisting of 350 units
covering an area of 14,000 Acres, or 5,600 hectares. The property covers parts of four specific
areas referred to as: Rightangle Lake Area, Little Sturge Lake Area, Eaglehead Lake Area and
Leckie Lake Area, and are part of the Ministry of Northern Development Mines and Forestry,
Thunder Bay Mining Division Administrative District.
Part of the property includes 9 manually staked mining claims which were acquiredfrom Rio
Tinto Exploration Canada Inc., in November of 2010.
URSA Major is currently the 100% ownerof the Disraeli Lake Property, and has been fully
responsible for providing the entire exploration funding required for the Caro Lake surface
diamond drilling program.
In October of 2010, URSA Major contracted out Aeroquest Airborne of Mississauga, Ontario,
636 line kilometers of Helicopter – Borne AeroTEM System Electromagnetic & Magnetic
surveying over the Disraeli Lake Property. By December 2010, Aeroquest had completed the
required survey processing, report and map generation, presented to URSA Major. This survey
covers the northern part of the property.
On March 14, 2011, co-author Harold Tracanelli and Richard Sutcliffe, CEO of URSA Major,
completed a reconnaissance of the property with a helicopter chartered out of the Thunder Bay,
Ontario and determined the location of the Caro lake drill hole. This effort was necessary to
assessanomaly locations and examine some of the exposed geological formations, access road
conditions and the like in advance of the mobilization of the diamond drilling equipment – crews
and the on ground geological support.
As a result of these initial reconnaissance efforts it was decided that the Caro Lake airborne
coincidental geophysical anomaly should be tested first. It is the diamond drilling carried out at
Caro Lake for which has been described within this report.
On March 16th., 2011, Harold Tracanelli, accompanied by Scott Nichol for George Downing
Estate Drilling Ltd., traveled out to the Caro Lake area and proceeded to locate the site for which
to locate a potential drill. Based on some predetermined UTM coordinates, a suitable location
approximately 50 meters west of the shore of Caro Lake was located. At that time diamond drill
hole U-17-01 was spotted to be drilled at 082 degrees Azimuth with an inclination of - 45
degrees.
The diamond drill machine that would be used to drill the hole was an LF-70 hydrocore drilling
machine, a machine which is well suited for drilling shallow to intermediate depth doles down to
nominally 800 meters +/- producing NQ core.
The principal objective in terms of mineral exploration on the Disraeli Lake Property is to target
potentially PGM – Ni and Cu bearing peridotite-melagabbro intrusions similar to the host rocks
at Magma Metals Limited's ("Magma's") platinum-palladium discovery at Current Lake, 45 km
north of Thunder Bay, Ontario.
The objective of the diamond drill hole was to best fit test a cluster of 3 EM anomalies in an area
of coincidental magnetic response, in an attempt to determine if such responses might be caused
by possible sulphide bearing, mafic – ultramafic sills or conduit like features developed within
flat lying sedimentary of the Nipigon Basin rocks know to be present in the area.
In an attempt to pass through and examine the cause of the anomalies it was proposed that a hole
be drilled to a depth of approximately 400 meters, as such considered to be long enough to
ensure that the downward plotted anomalies could be properly tested. It was interpreted that one
of the anomaly responses could be encountered at about 125 meters down the hole, while the
second, and further out anomaly response could be encountered at approximately 345 meters
down the hole. As a potentially added complication, a possible structural zone was also
interpreted to possibly be encountered at a depth of approximately 200 meters in the drill hole.
On March 20th., 2011, diamond drill hole U-17-01 was collared into Sibley group sediments
after sinking casing through 19,56 meters of boulder overburden. The initial drill collaring
monitoring efforts were being managed by geologist Patrick Chance. A short time later, the on
ground management of the diamond drilling program, core logging and sampling efforts were
handed off to geologist Ian Dasti.
On March 31st., 2011, diamond drill hole U-17-01 was completed to a final depth of 375 meters
into Sibley formation sedimentary rocks. The hole was stopped when no further signs of
encouragement to be expected with any further depths.
Initial core logging was started by Patrick Chance. The bulk of the core logging was carried out
by Ian Dasti.
The geology of diamond drill hole U-17-01 is best described as multiple laminated, somewhat
flat lying sequences of Sibley Group sedimentary rocks consisting of a variation of alternating
like greywacke’s and finer grained undifferentiated clastic sediments. These sedimentary rocks
have been intruded by sill or dyke like injections of diabase, gabbro, and olivine bearing gabbro
rocks. The thicknesses of these rocks in cross section seem to vary from 3 meters to 35 and 40
meters in the particular area.
An interesting intersection of magnetite rich – pyrite – pyrrhotite and chalcopyrite bearing
materials were encountered in the diamond drill hole in an area from: 130.80 meters to 138.95
meters down the hole. The mineralization at that particular location in the drill hole might
explain the cause of the first geophysical anomaly initially interpreted to be encountered at
approximately 125 meters down the hole.
As a result, 18 samples were collected from the mineralized interval which included one field
blank and on duplicate sample. The assay work was carried out by Accurassay, in Thunder Bay,
Ontario. The assay results are available within the appendix of the report.
A preliminary review of the mineralization encountered within from these initial drilling efforts
might suggest that the drill hole may have encountered a possible “IOCG-“ “skarn-” like or some
possible sub horizontal magnetite rich, cobalt and copper bearing igneous unit associated with
the evolution and the known mafic – ultramafic sill like intrusions in the same area.
The encountering of the unusual magnetite rich, cobalt and copper bearing materials –
occurrence identified in diamond drill hole U-17-01, may presently be considered rather unique
in this particular area. The location of the diamond drill hole used to test the coincidental
electromagnetic anomalies and magnetic area, in conjunction with the metal bearing unit, might
suggest that the exploration efforts may have encountered a potentially larger scale environment
for which follow up exploration should be given consideration.
As such follow diamond drilling so as to test the potential depth and strike extent of the
mineralized horizon is being recommended.
2.0
Property Location and Access:
The URSA Major Minerals Incorporated, Disraeli Lake Property, is located 65 kilometers NNE
of the city of Thunder Bay, District of Thunder Bay, Ontario.
The property which consists of 23 manually staked, contiguous mining claims are situated over
parts of four specific areas referred to as: Rightangle Lake Area, Little Sturge Lake Area,
Eaglehead Lake Area and Leckie Lake Area, and are part of the Ministry of Northern
Development Mines and Forestry, Thunder Bay Mining Division Administrative District.
From the Thunder Bay Airport, the Disraeli Lake Property can be reached by traveling east along
the Trans Canada Highway 17 and then North on Provincial Highway 527 to the Mawn Lake
Road a distance of approximately 105 kilometers. On the Mawn Lake Road it is necessary to
travel east a distance of 24.2 kilometers into the central part of the property, which more
specifically allows one to drive an automobile to within 500 meters of the site of diamond drill
hole U-17-01.
Much of the area has been subject to previous forest harvesting operations over the years, as such
there are many old forestry roads which traverse the area that would allow access to various parts
of the property either by pickup truck, ATV- snowmobile or on foot.
There are a number of larger scale lakes on the property such as Disraeli Lake and Leckie Lake
for which under appropriate weather conditions it may be possible to land a fixed wing aircraft.
Charter helicopter services are available out of the Thunder Bay airport, and can be used and can
land on some parts of the property.
Photograph: 1 Entrance of the Mawn Lake Road off of Provincial
Highway 527.
3.0
Property Ownership
The 23 claim URSA – Disraeli Lake Property, are currently owned and being operated by:
URSA Major Minerals Incorporated. The company head office is located at Suite 1300 – 8 King
Street East, Toronto, Ontario, M5C 1B5
The 14 contiguous claims (4247670 to 4247673, 4247676 to 4247677, 4247664 to 4247669 and
4247678 to 4247679) of the 23 claim property were acquired by manual claim staking and are
100% owned by URSA Major and were recorded on March 31st., 2009. The mining claims come
due for renewal each year on March 31st.
The 9 contiguous claims (4247121 through to 4247129 inclusive) of the 23 claim property were
acquired through an agreement between URSA Major and Rio Tinto Exploration Canada Inc.
The Rio Tinto claims were recorded on December 12th., 2000, and were transferred to URSA
Major on November 25th., 2010. The 9 mining claims come due for renew on April 12th., 2011.
THUNDER BAY Mining Division - 303758 - URSA MAJOR MINERALS INCORPORATED
Township/Area
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LECKIE LAKE
AREA
LITTLE STURGE
LAKE AREA
LITTLE STURGE
LAKE AREA
LITTLE STURGE
LAKE AREA
LITTLE STURGE
LAKE AREA
LITTLE STURGE
LAKE AREA
LITTLE STURGE
LAKE AREA
RIGHTANGLE
LAKE AREA
RIGHTANGLE
LAKE AREA
Claim
Recording
Claim Due
Status
Number
Date
Date
4247121 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc Optioned
From Rio Tinto Exploration Canada Inc.
4247122 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc.
4247123 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc.
4247124 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc.
4247125 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioed
From Rio Tinto Exploration Canada Inc..
4247126 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc.
4247127 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc..
4247128 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc. Optioned
From Rio Tinto Exploration Canada Inc.
4247129 2008-Dec-12 2011-Apr-12 URSA Major Minerals Inc.Optioned
From Rio Tinto Exploration Canada Inc..
4247670 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247671 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247672 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247673 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247676 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247677 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247664 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247665 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247666 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247667 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247668 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247669 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247678 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
4247679 2009-Mar-31 2011-Mar-31 100% Owned By:
URSA Major Minerals Incorporated
Percent
Option
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
100 %
Table: 1 Listing of The URSA Major Minerals Incorporated – Disraeli Lake Property Leckie
Lake Area (G-0067), Claims on Record with the Ontario Ministry of Northern Development
Mines and Forestry.
4.0
URSA Major Minerals Incorporated
Disraeli Lake Property, Thunder Bay Mining Division, Ontario
The URSA Major Minerals Incorporated, Disraeli Lake Property, located in the LECKIE LAKE
AREA, LITTLE STURGE LAKE AREA and the RIGHTANGLE LAKE AREA, Thunder Bay
Mining Division, District of Thunder Bay, Ontario is made up of 23 contiguous, manually staked
mining claims, consisting of 350 units covering an area of 14,000 Acres, or 5,600 hectares.
Figure: 1. URSA Major Minerals Incorporated – Disraeli Lake Property Location Map, Leckie
Lake Area (G-0067) Thunder Bay Mining Division, Ontario
5.0
Physiography and Climate
Photograph: 2 View facing west over part of Wolf Lake
The Disraeli Lake Property, occurs near the southern part of the Nipigon Basin, north of Lake
Superior. The terrain in the area is characterized by rounded and steep sided hills with typical
elevations in the order of 50 or 60 meters. The underlying geology of principally flat lying
sedimentary rocks of the Sibley Group and at the later emplacement diabasic – gabbroic and
granitic rocks in the area has significantly influenced the present characteristics of the
surrounding geography.
Thunder Bay and the area experience a humid continental climate (Köppen climate classification
Dfb)that is influenced by Lake Superior, with especially noticeable effects in the city's north end.
This results in cooler summer temperatures and warmer winter temperatures for an area
extending inland as far as 16 km. The average daily temperatures range from 17.6 °C in July to
−14.8 °C in January. The average daily high in July is 24.2 °C and the average daily high in
January is −8.6 °C. On January 10, 1982, the local temperature in Thunder Bay dropped to −36
°C, with a wind speed of 54 km/h for a wind chill temperature that dipped to −58 °C. As a result,
it holds Ontario's record for coldest day with wind chill.
The city is quite sunny, with an average of 2167.7 hours of bright sunshine each year, ranging
from 283.4 hours in July to 88.8 hours in November, sunnier than any city in Canada located to
the east of it.
6.0
Vegetation and Wildlife
Much of the surround geographic areas are dominated by an abundance of softwood species such
as Jack Pine, Tamarack, Poplar, White Birch, Black Spruce and Balsam Fir with locally thick
understory brush wood species such as Speckled Alder, Beaked Hazel and Willow growth.
Many of the lakes in the area are reported to be quite shallow and somewhat swampy. Some of
the lakes are reported to contain healthy populations of Northern Pike and Walleye. Some lakes
in the area are said to be deep and clean enough to support Lake Trout.
The area is said to contain a large population of Moose. During the initial reconnaissance efforts
a large Timber Wolf was observed on the Mawn Lake Road.
7.0
Brief Exploration History
The following summary is extracted from Hart and Magyarosi, Precambrian Geology of the the
Northern Black Sturgeon River and Disraeli lake area, Nipigon Embayment, Northwestern
Ontario, OGS Open File Report 6138, 2004.
“Mineral exploration and prospecting in the area has been sporadic with the first recorded
activity being the exploration for iron ore in the early 1900s (Coates 1972). The discovery of
sporadic copper mineralization near Disraeli Lake in 1965 stimulated the exploration for copper
and the other base metals in the late 1960s (Coates 1972). Uranium mineralization was first
reported in the Black Sturgeon Lake area in 1947, but exploration was not reported until 1975
(Scott 1987). A number of companies were reported to be actively exploring for uranium during
the late 1970s (Fenwick et al. 1980). A uranium occurrence was discovered by R.H. Sutcliffe
during the 1981 field season and subsequently acquired and explored by Uranerz Exploration
and Mining Corporation Limited until 1985 (Scott 1987). Several companies investigated the
potential of sedimentary-hosted base metal mineralization in the Sibley Group in the early
1990s, but other than an airborne geophysical survey completed by Cominco in 1993, little ofthe
work was recorded. Exploration for platinum group element (PGE) mineralization intensified
after the 1998 discovery of mineralization in the Seagull. Leckie Lake intrusion (Osmani and
Rees 1998). The best diamond-drill intersection to date is 1.71 ppm Pt and 1.87 ppm Pd across
2.1 m in basal pyroxenite ofthe Seagull. Leckie lakes intrusion, which contains 10% disseminated
to net-textured pyrite, pyrrhotite and minor chalcopyrite (Durham 2000).”
“A number of companies have explored in the area of Disraeli Lake since the discovery of
copper mineralization in 1965. Mineralization consists of chalcocite hosted by the diabase sill or
underlying Sibley Group sedimentary rocks (Coates 1972).”
Mineralization in the Seagull intrusion is hosted by the peridotite and is exposed in partially
filled-in trenches located on the logging road between Seagull and Leckie lakes. Sampling of
these trenches by Avalon Ventures Limited returned assays up to 2610 ppb Pt and 1145 ppb Pd
in the Central zone (Osmani and Rees 1998). Work on the property has included prospecting,
geological mapping, and magnetic and electromagnetic geophysical surveys (e.g., Schnieders et
al. 2003). Eighteen diamond-drill holes, totalling approximately 8328 m, have been completed in
the Seagull intrusion to investigate the platinum group element (PGE) mineralization, with
details of the diamond drilling provided in MRD 133.The most significant mineralization was
intersected at or near the basal contact of the peridotite with metasedimentary rocks of the
Quetico Subprovince. The best intersection returned 1.71 ppm Pt and1.87 ppm Pd over 2.1 m in
a biotite pyroxenite containing 10% disseminated to net-textured sulphide minerals including
pyrite, pyrrhotite and minor chalcopyrite (Durham 2000).”
In the immediate area of the Caro Lake, Avalon Ventrures drilled five short holes totalling 784
metres were also drilled on their Disraeli Lake property in 2000. These were designed to test
airborne EM conductors in the Disraeli Lake layered ultramafic intrusion to a maximum depth of
300 metres. No significant copper-nickel-PGE mineralization was intersected in these holes, but
none tested the intrusion to the corresponding depths of the mineralized horizon in the Seagull
intrusion and further work is planned for this property in 2001.
8.0
URSA Disraeli Property – Caro Lake Diamond Drilling Project.
The URSA Major Disraeli Lake – Caro Lake diamond drill program consisted of one 375 meters
deep hole used to test an airborne geophysical response in the area of Caro Lake area. Caro Lake
is located approximately 1,200 meters south of the south end of Disraeli Lake.
Figure: 2 URSA Major Disraeli Lake Property – Caro Lake Diamond Drilling Program, Location
Map.
On March 16th., 2011, diamond drill hole U-17-01 was located spotted at the Nad 83 UTM
coordinate of: Zone 16U 0356500 East and 5440795 North, by: Harold Tracanelli, Getn, P.Geo.
The diamond drill hole site was located near the southern part of mining claim 4247672.
The hole foresights were aligned at 082 degrees Azimuth using a hand held Silva compass set a 1
degrees west declination. The hole number and the inclination of the hole @ -45 degrees was
indicated on the collar picket.
On March 20th., 2011, diamond drill hole U-17-01 was collared into Sibley formation sediments
after sinking casing through 19.56 meters of boulder overburden. The initial drill collaring
monitoring efforts were managed by Patrick Chance.
A short time later, the on ground management of the diamond drilling program, core logging and
sampling efforts were handed off to geologist Ian Dasti.
On March 31st., 2011, diamond drill hole U-17-01 was completed to a final depth of 375 meters
into Sibley formation sedimentary rocks. The hole was stopped when no further signs of
encouragement to be expected with any further depths.
Initial core logging was started by Patrick Chance. The bulk of the core logging was carried out
by Ian Dasti.
9.0
Geology
The URSA Major Disraeli Property is located approximately 25 km north of Magma Metals's
Current Lake Pt, Pd, Ni, Cu deposit and is underlain bythe sedimentary rocks of the Sibley
Group, peridotite-melagabbo rocks of the Disraeli Intrusion, and Nipigon diabase sills. The
Disraeli Intrusion and diabase sills are intrusive into the sedimentary rocks of the Sibley Group.
The Disraeli Lake Property has several copper showings hosted by both intrusive rocks and
Sibley group sediments. The Disraeli Intrusion is related to the Proterozoic Mid-Continent rift
magmatism.
There are some reported similarities between the rocks known to occur on the Disraeli Lake
Property and the Magma Metals, Current Lake platinum-palladium discovery on its' Thunder
Bay North Property. This relatively new discovery which is reported to be one of the best
advanced platinum group metal exploration projects in North America with excellent widths, is
reported to have a 1:1 ratio of platinum to palladium, significant copper and nickel credits, and
the potential for a large mineralization system. Intersections of up to 61.7 m at 5.61 g/t platinum
and palladium, 0.7% copper and 0.4% nickel have been reported by Magma Metals.
9.1
Geology in Diamond Drill Hole U-17-01 of the Caro Lake
Diamond Drilling Project, on the URSA Disraeli Property
Initial core logging was started by Patrick Chance. The bulk of the core logging was carried out
by Ian Dasti.
The geology of diamond drill hole U-17-01 is best described as multiple laminated, somewhat
flat lying sequences of Sibley Group sedimentary rocks consisting of a variation of alternating
like greywacke’s and finer grained undifferentiated clastic sediments. These sedimentary rocks
have been intruded by sill or dyke like injections of diabase, gabbro, and olivine bearing gabbro
rocks.
Assuming that the sedimentary strata is relatively flat lying, the deposited sediment bed would
seem to vary in thickness from as thin as 3 to 8 meters to as thick as 35 and 40 meters in cross
section. The diabase gabbro sills and or dykes tend to be somewhat thinner and vary from 3
meters to 15 meters and seem to increase from 15 meters to 35 meters with increasing depth with
the stratigraphy.
From approximately 130.80 meters through to 139.95 meters, a rather interesting and potentially
unique mineral occurrence rich in magnetite, pyrite with some visible chalcopyrite was
encountered in the diamond drill hole. Such is currently though to represent a previously
unidentified mineralizing environment currently unheard of for the Nipigon sedimentary basin.
A preliminary review of the mineralization encountered within from these initial drilling efforts
might suggest that the drill hole may have encountered a possible “IOCG-“ “skarn-” like or some
possible sub horizontal magnetite rich, cobalt and copper bearing igneous unit associated with
the evolution and the known mafic – ultramafic sill like intrusions in the same area.
Ian Dasti; HBSc.,Geo who carried out and completed the drill core logging for DDH U-17-01,
for which four main lithologies were encountered.
At different intervals, each had varying degrees of alteration and thickness while textural features
were more or less maintained.
Clastic unit – fine grained matrix supported clastics with large light cream-pink clasts resembling
blobby paint splatter on canvas. Often, only a few clasts are present but are up to cobble size.
Clasts are made up of carbonate and are round to sub-elongate. Bedding is usually absent, with
rare areas of lamination present. Overall hard, silica rich, no visible sulfide. Non magnetic.
Wacke unit – probably best described as a red mudstone that occasionally has white clasts within
bedding that are sub-elliptical and vary from 2 to 7 cm. Rarely, more angular fragments of red
mudstone are found within the purple clastics and vice versa, most commonly near contacts
between units. Non magnetic.
Gabbro – diabase - This unit is comprised of aphanitic to sub aphanitic fine grained diabase with
common plagioclase and occasional pyroxene laths. Within thicker sections, the unit commonly
coarsens and fines with sharp internal contacts 35-40 degrees TCA. Coarse sections appear
gabbroic and have approximately 15-20% hornblende, 30-40% pyroxene, 0-5% olivine, 35-45%
plagioclase, 1% magnetite and trace sulfides, usually pyrite. Rarely, sections with up to 15%
biotite were encountered from 242.02 to 287.53 and were not commonly greater than 1m in
thickness. Where aphanitic, groundmass is dark green. Intermediate zones with assimilated
sediment have a red and black “salt and pepper” texture and are commonly 30-40cm where
present. One intermediate zone was much thicker and had a peculiar texture (242.02-246). The
zone was made up of 40% coarse grained hornblende, 35% alkali feldspar, 10% plagioclase,
10% quartz, trace magnetite and had up to 5% cavities very similar to the cavities in the “scarn”
section. Contacts between diabase and hornfels / sediments were easily distinguished based on
magnetism.
“Scarn”- The skarn – like unit from 130.80 meters through to 139.95 meters consisted of 70-80%
fine sub-mm grains of euhedral magnetite, 5-10% alteration clays, 5-12% sulfides, and 5% 1-3
cm cavities. Sulfides mostly consisted of pyrite infilling cavities and as veinlets, with crystals
commonly greater than .5 cm. Chalcopyrite and pyrrhotite, when present, were disseminated as
fine grains within magnetite. Rarely, minor chalcopyrite was found within Pyrite veinlets.
Overall, the rock is highly magnetic, black, and porous. The top contact has sections (10-30 cm)
of magnetite/chlorite bands. The chlorite layers are pure clay and can be up to 3mm wide.
Magnetite grains within bands are fine grained and can be up to 5mm wide. Banded
magnetite/chlorite sections become rare and then absent away from the skarn contact.
10.0
Results of the Diamond Drill Program
As a result of the drilling of the 375 meters deep hole U-17-01, an interesting area of magnetite
rich, cobalt and copper bearing oxide and sulphide mineralization was encountered. The
materials encountered and examined looked encouraging enough to warrant the collection of 16
representative samples. Within the sample stream were included I field blank and one duplicate
sample.
Diamond
Drill Hole
Number
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
U-17-01
Sample
Number
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
From
Meters
130.8
131.5
132
132.5
133
133.5
134
134.5
135
135.5
136
136.5
136.5
137
137.5
138
138.5
BLK
To
Meters
131.5
132
132.5
133
133.5
134
134.5
135
135.5
136
136.5
136.5
137
137.5
138
138.5
138.95
BLK
Length
Meters
0.7
0.5
0.5
0.5
0.5
0.5
0.5
0.5
0.5
0.5
0.5
0
0.5
0.5
0.5
0.5
0.45
QA / QC
Samples
DUP of 11
BLK
BLK = Field Blank
DUP = Duplicate Sample
The above samples collected were submitted to Accurassay in Thunder Bay, Ontario for Multi
Element ICP plug gold analysis on Tuesday March 29th., 2011 and were received from the
laboratory on Monday April 11th., 2011
URSA Major Minerals Inc.
Date Created: 11-04-11 01:58:38 PM
Job Number: 201141257
Date Received: 03/30/2011
Number of Samples: 18
Type of Sample: Core
Date Completed: 04/11/2011
Project ID:
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
96326
96327
96328
96329
96330
96331
96332
Au ppb
5 DL
<5
<5
<5
13
15
<5
22
9
<5
7
8
8
7
8
7
7
<5
7
<5
Client ID
UR-17-10-01-001
UR-17-10-01-002
UR-17-10-01-003
UR-17-10-01-004
UR-17-10-01-005
UR-17-10-01-006
UR-17-10-01-007
UR-17-10-01-008
UR-17-10-01-009
UR-17-10-01-010
UR-17-10-01-010
UR-17-10-01-011
UR-17-10-01-012
UR-17-10-01-013
UR-17-10-01-014
UR-17-10-01-015
UR-17-10-01-016
UR-17-10-01-017
UR-17-10-01-018
Pt ppb
15 DL
19
<15
38
<15
<15
<15
<15
26
<15
15
<15
<15
<15
24
<15
<15
<15
<15
<15
Pd ppb
10 DL
<10
14
18
11
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
<10
The results of the precious metals analysis from the 18 samples collected from DDH U-17-01 are
typically quite low to only slightly elevated above the analytical methods lower detection limits.
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
UR-17-10-01007
UR-17-10-01-
Ag
Al
As
B
Ba
Be
ppm
%
ppm
ppm
ppm
Ppm
<1
2.77
15
84
49
<2
<1
2.77
7
58
89
<2
<1
2.12
3
72
74
2
<1
3.64
11
100
140
3
<1
1
3.18
1.07
4
2
75
64
47
9
3
5
96322
96323
96324
96325
96326
96327
96328
96329
96330
96331
96332
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
96326
008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
UR-17-10-01007
UR-17-10-01008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
2
0.47
<2
56
6
5
1
0.2
3
50
10
6
1
0.14
<2
45
9
5
1
0.13
<2
49
12
6
1
0.12
<2
49
11
5
1
0.11
<2
54
11
6
1
0.11
<2
56
11
6
1
0.11
<2
55
10
6
<1
0.12
<2
45
9
5
1
0.14
<2
44
8
6
2
<1
<1
0.14
0.19
0.05
<2
<2
<2
45
51
42
7
7
4
6
6
<2
Bi
ppm
Ca
%
Cd
ppm
Co
ppm
Cr
ppm
Cu
Ppm
16
3.63
7
60
44
133
6
1.22
<4
47
245
82
21
0.97
13
180
197
215
18
0.51
12
68
30
185
15
0.73
10
54
24
116
45
0.09
31
228
20
1055
47
0.05
34
189
10
1042
66
0.32
39
524
14
1404
58
0.09
36
386
12
1141
64
0.14
40
492
20
1838
60
0.14
39
490
19
1814
61
0.42
39
1233
13
1012
58
0.43
38
1324
11
969
96327
96328
96329
96330
96331
96332
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
96326
96327
96328
96329
96330
96331
96332
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
UR-17-10-01007
UR-17-10-01008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
59
0.39
38
868
9
1387
58
0.15
37
1366
17
1103
59
0.18
39
1555
18
1075
60
0.22
42
613
12
1235
58
0.49
41
545
17
1445
5
0.07
5
252
45
347
Cu
ppm
Fe
%
K
%
Li
ppm
Mg
%
Mn
Ppm
133
8.35
0.49
108
3.89
1356
82
4.69
0.8
133
4
1282
215
16.94
0.7
54
4.82
769
185
16.13
1.21
102
7.99
858
116
14.19
0.38
141
6.5
1646
1055
37.76
0.04
18
4.94
653
1042
42.48
<0.01
14
3.72
522
1404
46.53
<0.01
7
1.88
512
1141
45.06
<0.01
8
1.73
486
1838
48.66
<0.01
8
1.77
563
1814
47.86
<0.01
7
1.74
554
1012
46.86
<0.01
6
1.51
535
969
46.48
<0.01
5
1.48
530
1387
46.92
<0.01
7
1.58
510
1103
46.64
<0.01
10
1.8
560
1075
47.59
<0.01
12
2.01
579
1235
>50
<0.01
11
1.68
517
1445
49.11
<0.01
11
2
517
347
7.88
<0.01
4
0.45
120
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
96326
96327
96328
96329
96330
96331
96332
Acc #
91316
96315
96316
96317
96318
96319
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
UR-17-10-01007
UR-17-10-01008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
Mo
ppm
Na
%
Ni
ppm
P
ppm
Pb
ppm
Sb
Ppm
14
0.18
58
694
26
<5
7
0.07
253
912
7
<5
23
0.06
222
483
47
<5
22
0.06
17
217
65
5
22
0.05
22
280
49
<5
61
0.02
197
143
68
6
64
0.02
298
<100
81
6
68
0.02
437
477
222
6
65
0.02
487
177
87
<5
71
0.02
721
410
83
<5
71
0.02
714
403
79
<5
69
0.03
549
1648
67
<5
67
0.03
543
1676
53
<5
66
0.03
707
1247
61
<5
68
0.02
538
323
63
<5
71
0.02
661
262
60
<5
70
0.01
723
<100
82
5
71
0.01
465
<100
78
6
24
0.02
303
112
12
<5
Se
ppm
Si
%
Sn
ppm
Sr
ppm
Ti
ppm
Tl
Ppm
<5
0.13
<10
47
2645
7
<5
0.15
<10
21
5800
<2
<5
0.14
<10
21
4244
<2
<5
0.06
<10
21
1180
<2
<5
0.12
<10
16
1145
7
<5
0.08
<10
3
317
10
96320
96321
96322
96323
96324
96325
96326
96327
96328
96329
96330
96331
96332
Acc #
91316
96315
96316
96317
96318
96319
96320
96321
96322
96323
96324
96325
96326
UR-17-10-01007
UR-17-10-01008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
Client ID
UR-17-10-01001
UR-17-10-01002
UR-17-10-01003
UR-17-10-01004
UR-17-10-01005
UR-17-10-01006
UR-17-10-01007
UR-17-10-01008
UR-17-10-01009
UR-17-10-01010
UR-17-10-01010
UR-17-10-01011
UR-17-10-01012
<5
0.07
<10
3
232
3
<5
0.04
13
<3
<100
21
<5
0.04
12
<3
<100
23
<5
0.03
13
3
<100
8
<5
0.03
11
3
<100
9
<5
0.04
<10
5
<100
11
<5
0.04
10
5
<100
20
<5
0.03
11
4
<100
5
<5
0.03
10
<3
<100
13
<5
0.04
11
<3
<100
44
<5
0.05
12
<3
<100
19
<5
0.06
11
<3
<100
9
<5
0.05
<10
<3
<100
<2
V
ppm
W
ppm
Y
ppm
Zn
ppm
62
<10
7
156
105
<10
4
48
89
<10
3
201
31
<10
9
268
26
<10
10
157
21
<10
<2
230
18
<10
<2
111
23
<10
<2
820
22
<10
<2
228
28
<10
<2
173
28
<10
<2
172
23
<10
2
145
23
<10
2
139
96327
96328
96329
96330
96331
96332
UR-17-10-01013
UR-17-10-01014
UR-17-10-01015
UR-17-10-01016
UR-17-10-01017
UR-17-10-01018
25
<10
2
135
32
<10
<2
137
32
<10
<2
128
24
<10
<2
114
26
<10
<2
124
33
<10
<2
27
A preliminary review of the mineralization encountered within from these initial drilling efforts
might suggest that the drill hole may have encountered a possible “IOCG-“ “skarn-” like or some
possible sub horizontal magnetite rich, cobalt and copper bearing igneous unit associated with
the evolution and the known mafic – ultramafic sill like intrusions in the same area.
The multi-element spectral analysis indicates an unusual rock chemistry with very high Fe
(locally over 50% Fe) and low Si (less than 1%). The chemical results suggest a vertical
fractionation in the intersection with the upper part having relatively higher Al, Si, Mg, Ba, Ti
and Cr and the lower part having higher Co and Fe. The central part of intersection has higher
Cu and Ni. These results would be consistent with a primary fractionation in a magmatic
intrusion with more silicate minerals to the top of the intersection and sulphide minerals being
concentrated toward the center (R. Sutcliffe 2011)
Please refer to APPENDIX III to review the assay data certificates as has been provided by
Accurassay Laboratory.
10.1
URSA Major Minerals Incorporated QA / QC Program
There have been 18 samples that were collected for diamond drill hole U-17-01. The samples
have been submitted to Accurassay Laboratories in Thunder Bay, Ontario, to processed and
subject to a ICP Multi Element analysis plus gold.
As part of the sampling process, barren field blank materials and duplicate samples have been
inserted in the sample stream on 18 samples collected from the drill hole.
At the lab, Accurassay collects and run lab duplicates, from every 11th sample in a submitted
sample stream.
The results of the field blank materials, duplicate samples and laboratory duplicate samples are
compared to ensure that there are no significant discrepancies, and that the results of such efforts
are within reasonably expectable limits -tolerances.
11.0
Conclusions
The URSA Major - Disraeli Lake Property, is located approximately 65 kilometers NNE of the
city of Thunder Bay, District of Thunder Bay, Ontario.
The property includes 23 contiguous, manually staked mining claims, consisting of 350 units
covering an area of 14,000 Acres, or 5,600 hectares. The property covers parts of four specific
areas referred to as: Rightangle Lake Area, Little Sturge Lake Area, Eaglehead Lake Area and
Leckie Lake Area, and are part of the Ministry of Northern Development Mines and Forestry,
Thunder Bay Mining Division Administrative District.
Part of the property includes 9 manually staked mining claims which were acquiredfrom Rio
Tinto Exploration Canada Inc., in November of 2010.
URSA Major is currently the 100% ownerof the Disraeli Lake Property, and has been fully
responsible for providing the entire exploration funding required for the Caro Lake surface
diamond drilling program.
In the Autumn of 2010 an airborne geophysical survey was carried out over the Disraeli Lake
Property. A number of coincidental electromagnetic and magnetic anomalies were detected.
As a result of the initial property exploration efforts it was decided that the Caro Lake airborne
coincidental geophysical anomaly should be tested first. It is the diamond drilling carried out at
Caro Lake for which has been described within this report.
On March 16th., 2011, Harold Tracanelli, accompanied by Scott Nichol for George Downing
Estate Drilling Ltd., traveled out to the Caro Lake area and proceeded to locate the site for which
to locate a potential drill. Based on some predetermined UTM coordinates, a suitable location
approximately 50 meters west of the shore of Caro Lake was located. At that time diamond drill
hole U-17-01 was spotted to be drilled at 082 degrees Azimuth with an inclination of - 45
degrees.
On March 20th., 2011, diamond drill hole U-17-01 was collared into Sibley group sediments after
sinking casing through 5.30 meters of boulder overburden. The initial drill collaring monitoring
efforts were being watched over by geologist Patrick Chance. A short time later, the on ground
management of the diamond drilling program, core logging and sampling efforts were handed off
to geologist Ian Dasti.
On March 31st., 2011, diamond drill hole U-17-01 was completed to a final depth of 375 meters
into Sibley formation sedimentary rocks. The hole was stopped when no further signs of
encouragement to be expected with any further depths.
Some rather unique mineralization was encountered in the diamond drill hole, a style and
intensity that had not been previously recognized in the area before. As such further follow up
exploration work has being recommended.
12.0
Recommendations
The encountering of the unusual magnetite rich, cobalt and copper bearing materials –
occurrence identified in diamond drill hole U-17-01, may presently be considered rather unique
in this particular area. The location of the diamond drill hole used to test the coincidental
electromagnetic anomalies and magnetic area, in conjunction with the metal bearing unit, might
suggest that the exploration efforts may have encountered a potentially larger scale environment
for which follow up exploration should be given consideration.
As such follow diamond drilling so as to test the potential depth and strike extent of the
mineralized horizon is being recommended.
13.0
Certificate of Qualifications
I, Harold Joseph Tracanelli, Getn, P.Geo., do hereby certify that:
I haveprovide geological related consultative services based from:
192 North Shore Road,
Onaping, Ontario.
P0M 2R0
I have graduated from Cambrian College of Applied Arts and Technology, in Sudbury, Ontario with a
Geological Engineering Technician Diploma in 1986.
I have been actively involved in various prospecting efforts since 1976, and since 1983 have been actively
engaged as an Exploration Geologist, performing many of the required duties and functions on gold, base
metal and industrial mineral exploration projects in Canada and Mexico.
I am a member of the Prospectors and Developers Association of Canada, the Sudbury Prospectors and
Developers Association, and the Ontario Prospectors Association.
I am a member in good standing with the Associated Professional Geoscientists of Ontario (APGO) No. 1156,
having attained the status of practicing member in November 2004.
I am responsible for preparing certain sections of the report describing the Caro Lake surface exploration
diamond drilling program on the URSA Major Disraeli Lake Property, District of Thunder Bay,
Ontario March and April 2011 located in the LECKIE LAKE AREA, LITTLE STURGE LAKE
AREA and the RIGHTANGLE LAKE AREA (G-0067), Thunder Bay, Mining Division, Ontario
I am not presently aware of any material fact or material change with respect to the subject matter as presented
in the Executive Summary that is not reflected in the main body of the Technical Report.
I have not have any prior involvement with the property that is the subject or described within the report.
I have partaken and have been present for exploration related activities in the field on the URSA Major –
Disraeli Lake Property on March 14th 2011 to March 16th., 2011, and in addition have overseen and provided
geological – exploration support while the Caro Lake diamond drilling program was underway, the details of
which have been described within the report.
I am independent of (URSA Major Minerals Incorporated and Rio Tinto Exploration Canada Inc.) I presently
neither retain, nor expect to retain any designated interest in any corporation involved in the described
property, either directly or indirectly, nor do I currently own any interest or hold securities nor have been
promised such equities or positions in the described corporation and or its affiliates.
As of this date hereof, to the best of my knowledge, information and belief, this report has been prepared and
contains all of the scientific and technical information and items required and disclosed in such a manner so as
to prevent such a report from being misleading.
Dated the 12th, day of April 2011.
_________________________________________
Harold J. Tracanelli, Getn, P.Geo., 1156
Hart and Magyarosi, Precambrian Geology of the the Northern Black Sturgeon River and
Disraeli lake area, Nipigon Embayment, Northwestern Ontario, OGS Open File Report 6138,
2004.
APPENDIX I,
Cross Sections and Plans for Diamond Drill Hole U-17-01
APPENDIX II,
Drill Core Log for Diamond Drill Hole U-17-01. Core Logging Carried Out By: Ian Dasti;
HBSc.Geo.
APPENDIX III,
Assay Certificates for samples collected in diamond drill hole U-17-01
APPENDIX IV,
Supporting Project Expenditure Related Documentation
Project Start Up Efforts March 2011
Richard Sutcliffe
March 14th., 2011, 1 Day = $1,000.00
Richard Sutcliffe, Return Airfare Toronto – Thunder Bay – Toronto =
$ 907.55
Wiskair Helicopter Charters
$3,476.67
Harold Tracanelli
March 14th., 2011 to March 16th., 2011 3 Days =
Harold Tracanelli, Return Airfare Sudbury – Thunder Bay – Sudbury =
Harold Tracanelli, Accommodations Thunder Bay =
Harold Tracanelli, Pickup Truck Rental (R. Sutcliffe)
Harold Tracanelli, Project Related Out of Pocket Expenses
Gasoline
Meals
Supplies
Parking
$1,525.25
$1,664.77
$ 141.53
$ 317.12
$
$
$
$
95.52
22.54
8.68
36.00
Project Geological Support March and April 2011
Harold Tracanelli An Accumulation of Efforts =
3 Day =
$1,525.25
Patrick Chance
6 Days
Patrick Chance Expenses
Patrick Chance Return Airfare Toronto – Thunder Bay – Toronto =
$3,000.00
Ian Dasti
Ian Dasti Pickup Truck Rental
Expenses of Ian Dasti
$2,034.00
$135.64
6 Days =
$1,604.18
George Downing Estate Drilling Limited
Mobe and Demob
Diamond Drill Hole U-17-01 1
$65,783.90
$19,847.50
Accurassay Laboratory 18 Samples from DDH U-17-01
$
656.98
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PROVINCIAL MINING RECORDER'S
OFFICE
Date I Time of Issue:
348000E
349000E
350000E
352000E
355000E
356000E
362000E
363000E
Mining Land Tenure
Map
MINISTRY OF NORTHERN
DEVELOPMENT AND MINES
Sun Mar 13 10:22:03 EST 2011
TOWNSHIP I AREA
LECKIE LAKE AREA
364000E
/
PLAN
G-0067
5449000N
ADMINISTRATIVE DISTRICTS I DIVISIONS
Mining Division
Land Titles/Registry Division
Ministry of Natural Resources District
TOPOGRAPHIC
D
5447000N
AREA
Ll l)TLE
424
I
Admiols~ative
Thunder Bay
THUNDER BAY
NIPIGON
Land Tenure
F~ehold
Boundaries
F>alent
D
Town<lllp
[i]
SurtBDO And Mining Rights
0
0
0
CMre<.>lon, Lol
r:l
Swfuc,e RlghisOnly
~
Mlnl~g RlgMis Ooly
~
s.,rn,.,., And Mining Rights
~
Sum.re RlgMis Only
~
Mining Righi< Only
~
lndl~n Re~rve
Cliff. F'll & Pile
....
5446000N
Conlllur
Mine ShBfls
Uren<>e of ODoopaUon
•
HeBd~Bme
Mine
u~s
Not Spec.ifle.d
S<Jrf>ire And Mining Rights
Rosd
SurtBre RighlsOnly
• ••••••
TrBII
•••••••
NBiural C..s F>ipellne
- . - ..
UUIIUe•
Mlnlflg Righls
+
Tower
o~Jy
Order In Coundl (Not open for si.Bklflg)
f'"·' j
Water Power
~ -- ---- 1
LeB~ Agree men I
Mlnlflg Claim
1 2~4567
1
L -----~
I
...... .....
,· ~·
~------1
Flied Only Mining Claims.
I
1234567
1
L-----~
LAND TENURE WITHDRAWALS
G
4249105
I
I
I
(
'""-'"'""
....
Aren Wllhdr"Bwn fromDispo>iUon
W<m
s""•"' And «;n;,g Rghl• Wilhd"'""
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....
IMPORTANT NOTICES
6
4247671
Sc&le 1:23284
--------
-
-
Om
BOOm
2.4km
LAND TENURE WITHDRAWAL DESCRIPTIONS
5440000N
-
4~9111
I
I
5439000N
)
5438000N
23
42471 il
5437000N
4247125
5436000N
5435000N
4254912
4247 128
424
7
4
7128
5434000N
r/
-~
J
1216198
358000E
UTM Zone 16
1000m grid
361
Friday April 08th.,2011
General Information and Limitations
Thos. wishin~ lo sloke miniog tloim> should wnsull wilh I he Provintial Miniog Recorders' Offite oflhe Minislr; of No1lhern Oevelopmenl ond Mines for oddiliooal inlormalion on I he slolus oflhe londs shown hereon
This mop is nol inlended for navigolioool. SLIIVey, or lond lille delenninolion pllrposes os I he inlonnolion shown on I his map is compiled n·om various sourtes. Coml>leleoess ond otourooy ore ool guoranl•ed Addilioool
inlormolion moy olso be oblained lhrough I he loool Lond Tilles or Regislr; Oflite. or I he Minislr; ol Nolurol Resources
The informolion shown is derived from digilal d•l• ovoilable in I he Provintial Mining Ret orders' Oflite >II he lime of downloodin~ from I he Minislr; of Norlhern Developmenl and Mines web sile
Conlotllnformolion
Toll Free
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Tel: I (BBB) 41 5-9B4 5 e>l 57 4 2
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Ho1ne Page: W>MN.mndm.gov.on.coiMNDMIMINESILANDSimlsmnpge.hlm
Mop Dolum: NAD B3
Projeclion: UTM (6 degree)
Topogr.phit Dolo Source: Lond lnlormolion Onlario
MininQ Lond Tenllre Sourt e: Provinciol Mil\in~ Recorrler's Office
This mop may nol show uore~i>lered land !enure •nd inleresls in land intludiog oerlain polenls. leoses.
eosemenls. rig hi ol ways, nooding righls. lioenses. or olher lorms ol disposilion of riQhls •nd ioleresl fro1n I he
Crown. Also oerlain lond !enure and lond uses I hoi reslriol or prohibil free enlr;lo sloke mining tloims moy
ool be illuslraled
lclenlifier
Type
Dale
2311
W-TB-102194
W-TB-124109
W•m
Wom
Wm
Jon I . 2001
Ool 20. I 094
Det 15. 2009
FLOODINC; ELEVATION: I 04 FT FILE: 1394Bg PLAN: L21-15 L.O. 5009
S.R. & M.R. WITHDRAWN FROM STAkiNC; ORDER NO W-TB-1 02104 NWR 94110120
<a href=" Mp:llwww.mndm.gov.oo.t alminesllandslwilhreoplorders2009lwlbl 24-09.pdf
">W-TB-124103 M.R.O. wilhdrawol S.3~ Mioing At I RSO 1999, December 151h, 2009 Cliti(ID
lin I' lo wilhdr,wal order<la•
URSA Major Minerals Incorporated
URSA Disraeli Lake Property
Caro Lake Doamond Drilling Program
Area:
Leckie Lake Area, Thunder Bay Mining Division, Ontario
URSA Diamond Drill Hole Number:
DDH U-17-01
NAD 83 UTM Coordinate Location of the Diamond Drill Hole:
Zone 16U 0356500 East and 5440795 North
Diamond Drill Hole Collared on Mining Claim Number:
4247672 Staked Mining Claim
Date Diamond Drill Hole Started:
March 20, 2011
Date Diamond Drill Hole Completed:
March 31, 2011
Azimuth of Diamond Drill Hole:
082 Degrees Azimuth
Inclination of the Diamond Drill Hole:
-45.0 Degrees
Diamond Drilling Carried Out By:
George Downing Estate Drilling Ltd
Machine Type:
LF-70
Diamond Drill Core Logging Carried Out By:
Ian Dasti; HBSc. Geo.
Diamond Drill Hole Objective:
Total Depth of Diamond Drill Hole:
To test cause of the coincidental electromagnetic and magnetic anomalies
identified in the Caro Lake area as result of the recenet Aeroquest airborne geophysical survey.
375 Meters
Assay Laboratory Work Order Numbers:
201141257
Labratory Methods: ALP1, ALFA1, ALAR1, Au + Multi Element ICP
Length (m) Code
Unit
Description
0
0
Casing
Rubble
Not recovered (overburden)
Mixed Sibley Group rubble with occasional rounded, rotted gneissic cobbles. Mostly
bedded to laminated, siltstones to wackes. Bedding tends to ~40° CA but occasionally
other angles. Locally fine, <1 mm wide fractures - pale hematitic red with narrow
bleached margins. Adjacent wallrock has streaky pale red colouration.
0
Wacke
Deep purplish grey, not obviously banded, very fine grained, compact, well indurated
wacke. Coarse sand size with occasional, very fresh looking, lensoid, lithic clasts.
Contains trace of fine pyrite aggregates and irregular, steely, non-magnetic, metallic
grains (specular hematite?).
Diamond
Drill Hole
U-17-01
From (m) To (m)
0.00
5.30
5.30
19.65
Length
(m)
5.30
14.35
19.65
20.87
1.22
From (m) To (m)
Litho Unit
1
20.87
49.70
28.83
0
Clastics
49.70
58.40
8.70
0
Diabase
58.40
65.50
7.10
0
Wacke
65.50
68.80
3.30
0
Diabase
68.80
78.00
78.00
81.30
9.20
3.30
0
0
Wacke
Diabase
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. May locally be hornsfelsed where core takes on a
finer grained, more massive appearence.
Medium grained, with relict olivine grains and ~10% greenish, plagioclase laths.
Fracture pattern suggests blocky appearence ~15-30 cm fracture spacing. Contains
trace vfg sulphide grains (pyrite). Strongly magnetic.
Blocky, locally slag-red colouration. Not obviously bedded / laminated. Probably
hornfelsed.
Very dark, bluish grey, fine grained, blocky with smooth surface. 5-10% irregular,
resorbed olivine grains. ~50% plagioclase laths. Very little sulphide evident. Strongly
magnetic.
Sibley; blocky, pale toned, wacke?
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
81.30
83.80
83.80
89.90
2.50
6.10
0
0
Wacke
Diabase
Sibley; blocky, pale toned, wacke?
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
89.90
100.10
10.20
0
Wacke
slag-red colouration. Not obviously bedded / laminated. Probably hornfelsed.
100.10
108.00
7.90
0
Diabase
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
108.00
115.20
7.20
0
Clastics
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. May locally be hornsfelsed where core takes on a
finer grained, more massive appearence. Minor clasts of slag-red wacke
0.4
Clastics
0
Wacke
silicious, minor carbonate, prolific hematite staining and alteration clays, 5% coarse
vesicles.
Blocky, locally slag-red colouration. Not obviously bedded / laminated. Hornfelsed.
1
2
1
2
1
2
1
2
1
2
1
115.20
1
1
115.60
131.48
15.88
1
121
130.6
1
3
115.60
127
130.7
6
0.1
Very broken, RQD 0. At bottom contact, chlorite increases greatly
Chlorite/C Veinlet of alternating fibrous carbonate and chlorite
alcite
Olivine
Fine grained olivine gabbro with minor sulfide (pyrite), 45 degree contacts.
Gabbro
Hornfels Visible layering of proto-wacke, blocky, silicious. Intermediate zone before magnetite
skarn. Extreme chlorite alteration, minor magnetite/chlorite veinlets.
131.48
132.43
0.95
0
132.43
133.93
1.50
0
133.93
139.10
5.17
0
Skarn
5-7% vesicles increases away from contacts. 75-80% magnetite, up to 10% sulfides,
mostly pyrite as veinlets. Occasional pyrrhotite and chalcopyrite disseminated fg-mg
(occasionally blebs). Chlorite and other alteration clays up to 10%.
139.10
141.90
141.90
145.50
2.80
3.60
0
0
Wacke
Diabase
Slag-red hornfelsed sibley sediments, blocky
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
Moderate red (hematite) staining
1
4
1
2
145.50
162.00
16.50
0
Wacke
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. May locally be hornsfelsed where core takes on a
finer grained, more massive appearence. Towards bottom contact becomes
increasingly broken and blocky (RQD 0 over last 1 m)
162.00
184.50
22.50
0.15
0
Clay
Diabase
57.52
0
Wacke
Unlithofied grey clay
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
Moderate red (hematite) staining
Variably colored, minor clastics. Moslty cream-tan colored fg – mg with intermittent
bedding.
wacke, light green/grey color with some small calcite veinlets parallel to bedding (45
degrees)
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. Blobier calcite veinlets present
184.50
242.02
1
1
2
1
160
1
160.15
197.5
200
2.5
Wacke
200
205
5
Clastics
205
208.8
3.8
Wacke
wacke, light green/grey color with some small calcite veinlets parallel to bedding
208.8
216.2
7.4
Clastics
216.2
223.6
224.3
223.6
224.3
225
7.4
0.7
0.7
Clastics
Wacke
Wacke
225
226.8
1.8
Clastics
226.8
227.3
227.3
242.02
0.5
14.72
0
Wacke
Wacke
Diabase
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments.
clastics, light green/grey color. Texturally identical to above clastics
Equigranular mg wacke, light pink to purple
Deep purplish grey, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. More hematite staining
clastics, light green/grey color, with moderate hematite staining. Texturally identical to
above clastics.
dark brown-cream colored wacke, bedding at 45 degree angle
light green / grey wacke with minor clastics
overall fine – medium grained diabase. Biotite common in visibly layered sections.
242.02
246
3.98
Gabbro
medium up to coarse grained, intermediate zone. Large hornblende (up to 3 cm long)
and plagioclase crystals, Potassic and silicious alteration with minor magnetite
246
249.5
3.5
Diabase
249.5
252
255.5
252
255.5
261
2.5
3.5
5.5
Diabase
Diabase
Diabase
261
278.5
17.5
Diabase
278.5
281.3
2.8
Diabase
Same mineralogy as intermediate zone above, but much finer grained. Less potassium
feldspar and less quartz. Medium grained phenocrystic plagioclase and pyroxenes
common to uncommon
increasingly fractured downhole to bottom contact
rubble (fault?) pebble to sand sized particles
fracturing decreases downhole away from structure. Fine grained, with fewer medium
grained pyroxenes and plagioclase phenocrysts
oscillating layers of medium grained gabbro with layers of fine grained, sub-aphanitic
diabase. Both have identical mineralogy, only textural features differ. Minor relic
olivine
Fine grained sub-aphanitic diabase, plagioclase has a weak green tinge (chloritization?)
281.3
287.53
6.23
Diabase
1
1
1
1
1
1
1
1
1
2
242.02
287.53
45.51
3
2
2
2
2
2
2
2
Intermediate zone, chilled margin. Increasing potassic alteration and hematitic stains,
minor biotite, overall lighter colored than other diabase.
1
287.53
324.91
37.38
1
2
1
1
288.1
0
Wacke
clastics
clastics, light green/grey color. Texturally identical to above clastics. Hornfels?
287.53
288.1
288.35
288.35
289.5
Diabase
clastics
fine grained sub-aphanitic diabase (dike?)
clastics, light green/grey color. Texturally identical to above clastics. Hornfels?
289.5
296.4
wacke
296.4
298.4
clastics
298.4
300.7
300.7
303
303
305.4
305.4
314.16
314.16
317.47
Diabase
equigranular wacke with .5-1.5 cm bedding, minor calcite veinlets parallel to bedding
(45 degrees TCA)
deep purple/green, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. Small perpendicular jointing present. Hematite
staining, sericite, and chlorite present
equigranular wacke with .5-1.5 cm bedding, minor calcite veinlets parallel to bedding
(45 degrees TCA)
deep purple/green, slag toned, intermittantly bedded, occasionally laminated,
generally fine grained sediments. Small perpendicular jointing present. Hematite
staining, sericite, and chlorite present
equigranular wacke with .5-1.5 cm bedding, minor calcite veinlets parallel to bedding
(45 degrees TCA)
Bright red, intermittantly bedded, occasionally laminated, generally fine grained
sediments. Small perpendicular jointing present.
3 small (20 – 40 cm each) diabase dikes with chloritized clastics between them.
317.47
324.91
Wacke
1
1
1
1
1
2
1
2
1
324.91
331.19
6.28
0
Diabase
331.19
375.00
43.81
0
Wacke
EOH
EOH
End of Diamond Drill Hole U-17-01
Core Logging Carried Out By: Ian Dasti
Bright red, intermittantly bedded, occasionally laminated, generally fine grained
sediments. Small perpendicular jointing present.
Fine to medium grained with fine, well-developed plagiocase laths. Strongly magnetic.
Small (10 cm) chill zone at both contacts
Red sibley sediment, alternating between clastics (white carbonate concretion
splotches within red sediments) and bedded wacke.
Monday, April 11, 2011
Certificate of Analysis
URSA Major Minerals Inc.
8 King St. E., Ste. 1300
Toronto, ON, CAN
M5C1B5
Ph#: (416) 864-0615
Fax#: (416) 864-0620
Email: [email protected]
Acc #
Client ID
91316
Date Received: 03/30/2011
Date Completed: 04/11/2011
Job #: 201141257
Reference:
Sample #: 18
Au
ppb
Pt
ppb
Pd
ppb
UR-17-10-01-001
<5
19
<10
96315
UR-17-10-01-002
<5
<15
14
96316
UR-17-10-01-003
<5
38
18
96317
UR-17-10-01-004
13
<15
11
96318
UR-17-10-01-005
15
<15
<10
96319
UR-17-10-01-006
<5
<15
<10
96320
UR-17-10-01-007
22
<15
<10
96321
UR-17-10-01-008
9
26
<10
96322
UR-17-10-01-009
<5
<15
<10
96323
UR-17-10-01-010
7
15
<10
96324 Dup
UR-17-10-01-010
8
<15
<10
96325
UR-17-10-01-011
8
<15
<10
96326
UR-17-10-01-012
7
<15
<10
96327
UR-17-10-01-013
8
24
<10
96328
UR-17-10-01-014
7
<15
<10
96329
UR-17-10-01-015
7
<15
<10
96330
UR-17-10-01-016
<5
<15
<10
96331
UR-17-10-01-017
7
<15
<10
96332
UR-17-10-01-018
<5
<15
<10
Rh
ppb
PROCEDURE CODES: ALP1, ALPG1, ALAR1
Certified By:
The results included on this report relate only to the items tested
The Certificate of Analysis should not be reproduced except in full,
without the written approval of the laboratory
AL907-0464-04/11/2011 1:58 PM
Page 1 of 1
Monday, April 11, 2011
Certificate of Analysis
URSA Major Minerals Inc.
8 King St. E., Ste. 1300
Toronto, ON, CAN
M5C1B5
Ph#: (416) 864-0615
Fax#: (416) 864-0620
Email: [email protected]
Acc #
Client ID
91316
Date Received: 03/30/2011
Date Completed: 04/11/2011
Job #: 201141257
Reference:
Sample #: 18
Au
ppb
Pt
ppb
Pd
ppb
Ag
ppm
Al
%
As
ppm
B
ppm
Ba
ppm
Be
ppm
Bi
ppm
Ca
%
Cd
ppm
Co
ppm
Cr
ppm
Cu
ppm
Fe
%
K
%
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Na
%
Ni
ppm
P
ppm
Pb
ppm
Sb
ppm
Se
ppm
Si
%
Sn
ppm
Sr
ppm
Ti
ppm
Tl
ppm
V
ppm
W
ppm
Y
ppm
Zn
ppm
UR-17-10-01-001
<5
19
<10
<1
2.77
15
84
49
<2
16
3.63
7
60
44
133
8.35
0.49
108
3.89
1356
14
0.18
58
694
26
<5
<5
0.13
<10
47
2645
7
62
<10
7
156
96315
UR-17-10-01-002
<5
<15
14
<1
2.77
7
58
89
<2
6
1.22
<4
47
245
82
4.69
0.80
133
4.00
1282
7
0.07
253
912
7
<5
<5
0.15
<10
21
5800
<2
105
<10
4
48
96316
UR-17-10-01-003
<5
38
18
<1
2.12
3
72
74
2
21
0.97
13
180
197
215
16.94
0.70
54
4.82
769
23
0.06
222
483
47
<5
<5
0.14
<10
21
4244
<2
89
<10
3
201
96317
UR-17-10-01-004
13
<15
11
<1
3.64
11
100
140
3
18
0.51
12
68
30
185
16.13
1.21
102
7.99
858
22
0.06
17
217
65
5
<5
0.06
<10
21
1180
<2
31
<10
9
268
96318
UR-17-10-01-005
15
<15
<10
<1
3.18
4
75
47
3
15
0.73
10
54
24
116
14.19
0.38
141
6.50
1646
22
0.05
22
280
49
<5
<5
0.12
<10
16
1145
7
26
<10
10
157
96319
UR-17-10-01-006
<5
<15
<10
1
1.07
2
64
9
5
45
0.09
31
228
20
1055
37.76
0.04
18
4.94
653
61
0.02
197
143
68
6
<5
0.08
<10
3
317
10
21
<10
<2
230
96320
UR-17-10-01-007
22
<15
<10
2
0.47
<2
56
6
5
47
0.05
34
189
10
1042
42.48
<0.01
14
3.72
522
64
0.02
298
<100
81
6
<5
0.07
<10
3
232
3
18
<10
<2
111
96321
UR-17-10-01-008
9
26
<10
1
0.20
3
50
10
6
66
0.32
39
524
14
1404
46.53
<0.01
7
1.88
512
68
0.02
437
477
222
6
<5
0.04
13
<3
<100
21
23
<10
<2
820
96322
UR-17-10-01-009
<5
<15
<10
1
0.14
<2
45
9
5
58
0.09
36
386
12
1141
45.06
<0.01
8
1.73
486
65
0.02
487
177
87
<5
<5
0.04
12
<3
<100
23
22
<10
<2
228
96323
UR-17-10-01-010
7
15
<10
1
0.13
<2
49
12
6
64
0.14
40
492
20
1838
48.66
<0.01
8
1.77
563
71
0.02
721
410
83
<5
<5
0.03
13
3
<100
8
28
<10
<2
173
96324D
UR-17-10-01-010
8
<15
<10
1
0.12
<2
49
11
5
60
0.14
39
490
19
1814
47.86
<0.01
7
1.74
554
71
0.02
714
403
79
<5
<5
0.03
11
3
<100
9
28
<10
<2
172
96325
UR-17-10-01-011
8
<15
<10
1
0.11
<2
54
11
6
61
0.42
39
1233
13
1012
46.86
<0.01
6
1.51
535
69
0.03
549
1648
67
<5
<5
0.04
<10
5
<100
11
23
<10
2
145
96326
UR-17-10-01-012
7
<15
<10
1
0.11
<2
56
11
6
58
0.43
38
1324
11
969
46.48
<0.01
5
1.48
530
67
0.03
543
1676
53
<5
<5
0.04
10
5
<100
20
23
<10
2
139
96327
UR-17-10-01-013
8
24
<10
1
0.11
<2
55
10
6
59
0.39
38
868
9
1387
46.92
<0.01
7
1.58
510
66
0.03
707
1247
61
<5
<5
0.03
11
4
<100
5
25
<10
2
135
96328
UR-17-10-01-014
7
<15
<10
<1
0.12
<2
45
9
5
58
0.15
37
1366
17
1103
46.64
<0.01
10
1.80
560
68
0.02
538
323
63
<5
<5
0.03
10
<3
<100
13
32
<10
<2
137
96329
UR-17-10-01-015
7
<15
<10
1
0.14
<2
44
8
6
59
0.18
39
1555
18
1075
47.59
<0.01
12
2.01
579
71
0.02
661
262
60
<5
<5
0.04
11
<3
<100
44
32
<10
<2
128
96330
UR-17-10-01-016
<5
<15
<10
2
0.14
<2
45
7
6
60
0.22
42
613
12
1235
>50.00
<0.01
11
1.68
517
70
0.01
723
<100
82
5
<5
0.05
12
<3
<100
19
24
<10
<2
114
96331
UR-17-10-01-017
7
<15
<10
<1
0.19
<2
51
7
6
58
0.49
41
545
17
1445
49.11
<0.01
11
2.00
517
71
0.01
465
<100
78
6
<5
0.06
11
<3
<100
9
26
<10
<2
124
96332
UR-17-10-01-018
<5
<15
<10
<1
0.05
<2
42
4
<2
5
0.07
5
252
45
347
7.88
<0.01
4
0.45
120
24
0.02
303
112
12
<5
<5
0.05
<10
<3
<100
<2
33
<10
<2
27
PROCEDURE CODES: ALP1, ALPG1, ALAR1
Certified By:
The results included on this report relate only to the items tested
The Certificate of Analysis should not be reproduced except in full,
without the written approval of the laboratory
-0464-04/11/2011 3:43 PM
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