Unit 1: Physical Geography
Top Tips:
1. Landform Formations:
Use the phrase “Over-Time”
2. Landform Formations:
-Do you know the sequence of how one thing leads to the next?
-Coastal Erosion Landforms have 5 steps each-can you remember them?
-Each plate boundary has 5 steps each-can you remember them?
3. Compare and Contrast:
Use the phrases “In contrast to...whereas...”
4. Case Studies
-Do you know when and where they happened?
-Does the case study need to know the causes?
-Does the case study need to know the impacts? (positive/negative,
primary/secondary, Social/Economic/Environmental/Political)
-Does the case study need to the responses? (short/long term)
The Restless
Earth
Unit 1 :
Physical
The Restless Earth
• The Earth’s crust is made up from an inner core, outer core,
mantle and crust.
• The crust is divided by lots of slabs called tectonic plates,
(floating on the mantle).
• Plates are made up of two types of crustContinental crust is thicker and less dense than Oceanic which is
thinner and more dense.
• The plates are moving because the rock in the mantle
underneath them is moving.
• The places where plates meet are called boundaries, or plate
margins.
Plate Margins
Destructive Margins:
Where 2 plates are moving towards each other,
e.g. along the east coast of Japan and the
Nazca plate sub-ducting under the South
American plate.
When an oceanic plate (Nazca) and a
continental plate meet, the denser oceanic
plate is forced down into the mantle and
destroyed.
This often creates volcanoes and ocean
trenches (very deep sections of the ocean floor
where the oceanic plate goes down).
Constructive Margins:
Are where 2 plates are moving away from each
other.
e.g. at the mid-Atlantic ridge- Iceland.
Magma (molten rock) rises from the mantle to
fill the gap and cools, creating new crust.
Conservative Margins
The San Andreas Fault is an example of
conservative margins. The 2 plates are
moving sideways, past each other, or in
the same direction but one moving
faster than the other.
Crust isn’t created or destroyed.
Fold Mountains
-Fold Mountains are formed on
destructive plate margins.
-Rivers carry sedimentary rocks such
as sandstone and limestone.
-They are deposited into
depressions.
-After a few million years the
sediments are compressed into
sedimentary rocks then forced
upwards into a series of folds by the
movement of tectonic plates.
The Himalayas in Asia were formed by
2 continental plates.
The Andes in S.America were formed by an oceanic and continental plate.
Where the rocks are folded upwards,
they are called anticlines. Where the
rocks are folded downwards, they are
called synclines. Severely folded and
faulted rocks are called nappes.
Fold Mountains
• Fold Mountains have very steep slopes which are rocky, often
with snow and glaciers in the highest bits and lakes in the
valleys between the mountains.
Human activity in Fold Mountain Areas:
Farming: Higher mountain slopes aren’t great for growing crops, but are for grazing
animals such as goats. Sometimes the land is terraced to accommodate crops.
Mining: Fold mountains are a major source of metal ores,
however the steep slopes have to be carved into zigzag roads
for easy access.
Hydro-electric power (HEP): Steep slopes and lakes
(to store water) are ideal for generating HEP.
Forestry: Can grow conifers, used for fuel, building materials and paper and
furniture.
Tourism: Scenery, winter sports, summer walks. Tunnels have been built for fast
communications.
Case Study!
• The Alps is a Fold Mountain range, formed around 30 million
years ago by the collision of the African and European plates.
• Population: 12 million
•
•
•
•
•
Farming: Slopes have been terraced for vineyards- Lavaux Switzerland and goats are grazed for
cheese, meat and milk
HEP: Switzerland gets 60% of its electricity from HEP stations in the Alps.
Mining: Has declined due to cheaper foreign sources.
Forestry: Scots Pine is planted all over the Alps as it’s more resilient to goats.
Tourism: 100 million tourists per year= huge part of economy. 70% of tourists visit in winter.
New villages have been built, e.g. Tignes in France.
Adaptations people have made
1) Steep relief: Goats are farmed because they’re well adapted to steep mountains. Man
made defences are used to protect against avalanches and rock slides.
2) Poor soils: The soil isn’t great for crops, so animals are grazed.
3) Limited communications: Brenner Pass between Austria and Italy has been built but snow
often blocks it up and it takes a while to travel along it. So tunnels have been cut through for
fast transport links. For example, the Lotschberg Base Tunnel has been cut through the
Bernese Alps in Switzerland.
Quiz…
What are the layers the Earth is made from called?
Inner core, outer core, mantle, crust
What are the 2 types of crust and their differences?
Oceanic- thinner and denser and
Continental-thicker and less dense
How many types of plate margins are there and what are
they called?
Destructive
Constructive
Conservative
What happens at the different plate margins and give examples?
Destructive- move towards, Nazca plate and S.American and on the east coast of Japan.
Constructive- move away from each other, Eurasian and North American (over Iceland-mid Atlantic
ridge).
Conservative- side by side, San Andreas Fault
Where do fold mountains occur and what are they?
They occur at destructive plate margins when they collide and fold the sediments upwards.
5 Human uses of fold mountains and an example of one?
Mining, forestry, tourism, HEP, farming
The Alps, Himalayas, Andes
Using one example give some facts related to these 5 uses
ALPS
Tourism- 70% in winter
Farming- Terraced land for vineyards (Lavaux , Switzerland)
HEP- 60% OF Swiss electricity from HEP in Alps.
Mining- declined due to cheaper foreign sources
Forestry- Scots Pine is planted as it is more resilient to goats and made into furniture
How have people adapted in the Alps?
Steep relief: Goats are farmed and man made defences have been built to protect against avalanches
and rock slides
Poor soils: Crops aren’t grown but more animals are grazed
Poor communications: Tunnels have been built to provide fast communication links, e.g. Lotschberg Base
Tunnel.
Volcanoes
• Are found at destructive AND constructive plate margins.
• At destructive plate margins:
The denser oceanic plate sub-ducts under the continental plate- creating an ocean trench.
Where the oceanic plate is destroyed in the mantle the magma rises through cracks in the
crust called vents.
The magma erupts onto the surface (now called lava) forming a volcano.
• At constructive plate margins:
The magma rises up into the gap created by the plates moving apart, forming a volcano.
Some volcanoes also form over parts of the mantle that are really hot (hotspots) e.g. in
Hawaii.
Types of volcano:
• Composite: Made up of layers of ash and
lava that have cooled and hardened into
layers.
• The lava is usually thick and flows slowly. It
hardens to form a steep sided volcano.
• Example: Mount Fuji, Japan
• Shield: Made up of only lava = lava
layers. Lava is runny, flows quickly and
spreads over a large area. This forms a low,
flat volcano.
• Example: Mauna Loa, Hawaii
• Dome: Made up of only lava, the lava
•
is thick, flows slowly and hardens
quickly, forming a steep sided volcano
Example: Mount Pelée, Caribbean
Scientists try and predict volcanic eruptions
by monitoring escaping gas, tiny
earthquakes and changes in shape and size
of the volcano.
Case Study!
• The Soufriere Hills in Montserrat erupted on June
25th 1997.
• 19 killed
• Montserrat is above a destructive plate margin,
where the Atlantic Plate is being forced under the
Caribbean plate.
• Magma rose, forming an underground pool of
magma.
• The rock above the pool collapsed, opening a
vent and causing the eruption.
Impacts
Primary Impacts
1) Large areas were covered in volcanic material- the capital city,
Plymouth was buried under 12m of mud and ash.
2) Over 20 villages and two thirds of homes on the island were
destroyed by pyroclastic flows (fast moving clouds of super heated
gas and ash).
3) Schools, hospitals, the airport and the port were destroyed.
4) Vegetation and farmland were destroyed.
5) 19 people died and 17 were injured.
Secondary Impacts
1) Fires destroyed many buildings including local government offices,
the police headquarters and the town’s central petrol station.
2) Tourists stayed away and businesses were destroyed disrupting the
economy.
3) Population decline- 8000 of the island’s inhabitants have left since
the eruptions began in 1995.
4) Volcanic ash from the eruption has improved soil fertility.
5) Tourism on the island is now increasing as people come to see the
volcano.
Responses
Immediate Responses
1) People were evacuated from the south to safe areas in the north.
2) Shelters were built to house evacuees.
3) Temporary infrastructure was also built, e.g. roads and electricity
supplies.
4) The UK provided £17 million of emergency aid (Montserrat’s an
overseas territory of the UK).
5) Local emergency services provided support units to search for and
rescue survivors.
Long-term responses
1) A risk map was created and an exclusion zone is in place. The south of the island is off limits while the
volcano is still active.
2) The UK has provided £41 million to develop the north of the island – new dock, an airport and houses
have been built in the north.
3) The Montserrat Volcano Observatory has been setup to try and predict further eruptions.
Supervolcanoes
• Are massive volcanoes- only at destructive margins. E.g.
Yellowstone National Park- USA.
Formation
1) Magma rises up through cracks in the crust to form a large magma basin below the surface.
The pressure of the magma causes a circular bulge on the surface several kms wide.
2) The bulge eventually cracks, creating vents for lava to escape through. The lava erupts out of
the vents causing earthquakes and sending up gigantic plumes of ash and rock.
3) As the magma basin empties, the bulge is no longer supported so it collapses- spewing up
more lava.
4) When the eruption’s finished there’s a big crater (called a caldera) left where the bulge
collapsed. Sometimes these get filled with water to form a large lake, e.g. Lake Toba in Indonesia.
Characteristics of a supervolcano:
-Flat (unlike normal ones which are mountains).
-Cover a large area
-Have a caldera (normal volcanoes just have a crater at
the top).
Consequences of Supervolcanoes
• Thousands of cubic kms of ash, rock and lava
will be thrown out with the eruption.
• A thick cloud of super heated gas and ash will
flow at high speed from the volcano, killing,
burning and burying everything it touches.
• Everything within 10 miles is destroyed.
• Ash shot high into the air will block out
sunlight over whole continents.
Quiz…
Where are volcanoes found?
At destructive and constructive plate margins.
Describe how volcanoes are formed
Destructive: The denser oceanic plate sub-ducts down into the mantle and is
destroyed, creating an ocean trench. Magma rises through cracks in the crust called
vents. The magma erupts, causing a volcano.
Constructive: As the plates move apart the magma rises to fill the gap and a volcano
is formed.
Name the 3 types of volcanoes, give a description of them and an example.
Composite: Made up of layers of lava and ash. Lava is thick and flows slowly. It
hardens to form a steep sided volcano. Mount Fuji in Japan is an example.
Shield: Gentle slopes, runny, thin lava. Layers of lava only, low and flat. Example,
Mauna Loa Hawaii.
Dome: Layers of lava only. Steep sided volcano with thick slowly flowing lava. Mount
Pelée in the Caribbean is an example.
How do scientists try and predict volcanic eruptions?
By monitoring escaping gas, changes in size of the volcano and tiny earthquakes.
Give an example of a volcanic eruption with dates, people killed and why it exploded.
Soufriere Hills in Montserrat erupted on the 25th June 1997 killing 19 people.
It erupted when the Atlantic plate which had been pushed into the mantle by the Caribbean plate. Magma rose,
forming a pool of magma, the rock above collapsed allowing magma to escape through vents and causing the
eruption.
Name 3 primary and 3 secondary impacts from this eruption.
PRIMARY: Plymouth- the capital city was buried in mud and ash,
Schools, hospitals, airports and the port were destroyed,
19 people died and 17 were injured,
Vegetation and farmland were destroyed, 20 villages were destroyed by pyroclastic flows.
SECONDARY: Fires destroyed many building including the police headquarters, businesses were destroyed, due to
lack of tourists, there was a population decline- 8000 inhabitants fled to avoid the eruption.
Volcanic ash improved soils- more fertile, tourism is now on the rise as tourists see the volcano as an attraction.
Name 3 immediate and long-term responses.
Immediate: People were evacuated from the south of the island to safer parts in the north, shelters were built to
house evacuees, the UK provided £17million of emergency aid, temporary infrastructure were built (roads,
electricity supplies) and local emergency services provided support to help search and rescue people.
Long-term: The Montserrat Volcano Observatory was set up to try and predict eruptions in the future, a risk map
was created and exclusion zones are in place, the UK provided £41 million to develop the north of the island.
Explain the formation of Supervolcanoes and give an example of one.
Supervolcanoes are formed when magma rises up through cracks in the crust to form a large
magma basin. The pressure of the magma causes a flat, circular bulge to be created above. The
bulge eventually cracks, creating vents for the lava to escape through and causing earthquakes. As
the magma basin empties the bulge collapses and a caldera is formed.
Earthquakes
• Occur at all 3 types of plate margins.
• Are caused by tension that builds up.
Destructive margins:
Tension builds up when one plate gets stuck as it’s
moving down past the other into the mantle.
Constructive margins:
Tension builds along cracks within the plates as they
move away from each other.
Conservative margins:
Tension builds up when plates that are grinding past each
other get stuck.
The plates eventually jerk past each other sending out shockwaves
(vibrations) = earthquake.
The waves spread out from the focus (the point in the Earth where the
Earthquake starts).
The nearer the focus the waves are the more destructive and stronger
they are.
The epicentre is the point on the Earth’s surface straight above the
focus.
Earthquakes can be measured
The Richer Scale: measures the amount of
energy released (magnitude). (1+ where 5 is major)
The Mercalli Scale: measures the effects
of an earthquake. (1-12)
Case Study!
Rich and poor countries are affected differently by earthquakes.
L’Aquila- Italy
6th April 2009
6.3 on Richter scale
Kashmir-Pakistan
8th Oct 2005
7.6 on Richter scale
No local disaster planning was in place
Italy had laws on construction standards
Buildings were not earthquake proof
Italy has a Civil Protection Department- trains volunteers for rescue
Primary effects:
operations
80,000 deaths, hundreds of thousands injured
Primary effects:
3 million homeless
290 deaths- collapsed buildings
Water pipelines and electricity supplies were cut off
Hundreds injured
Secondary effects:
Thousands homeless
Landslides buried buildings and people
Secondary effects:
Diseases such as diarrhoea spread due to unclean water
Fires caused damage
Immediate responses:
Broken waterpipe caused landslide
Help didn’t reach many areas for days or weeks
Immediate responses:
People had to be rescued by hand without any help from the emergency
Camps were set up for homeless with medical care
services
Cranes and diggers used to remove rubble
International aid was given (helicopters and rescue dogs)
Money was provided by government
Long-term responses:
40,000 people been relocated to new towns
Long-term responses:
Training
has
been
provided
to
help rebuild more buildings as earthquake
PM promised to build new town
resistant
An investigation to find out why some buildings weren’t earthquake
New health centres have been set up
proof.
Tsunamis- Case Study!
A tsunami is a series of continuous waves caused when huge amounts of water get displaced
West Coast of Indonesia/ Indian Ocean
26th December 2004
9.1 Richter Scale
Waves 30m high :O
Indonesia, India, Thailand and Sri Lanka were the worst affected.
There was NO EARLY WARNING SYSTEM
-230,000 people were killed
-Whole towns and villages were destroyed- 1.7 million lost their homes
-Infrastructure (roads, waterpipes electricity lines) were severely damaged
-5-6 million people needed emergency food, water and medical supplies
-Economic damage: fisherman lost livelihoods and tourism plummeted because of total destruction + afraid of it repeating
-Environmental damage: salt from sea all over plants prevented growth
Short-term responses:
1)
2)
Hundreds of millions of pounds had been pledged by foreign govs, charities to give survivors food, water, shelter, medical
attention
Foreign countries sent ships, planes and soldiers to help rescue people, distribute food and help clear mess
Long-term responses:
1)
2)
3)
4)
5)
Billions of pounds pledged to help re-build
Programmes set up to help people get back to work
A tsunami warning system has been put in place in the Indian Ocean
Disaster Management Plans have been put in place in some countries
Volunteers have been trained for future tsunamis
Coastal
Landscapes
Living
World
Foundation Paper: June 2013
Foundation Insert
Foundation Insert
Foundation Insert
Foundation Insert
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark
Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Foundation Mark Scheme
Higher Paper: June 2013
Higher Insert
Higher Insert
Higher Insert
Higher Insert
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Higher Mark
Scheme
Foundation Paper: June 2010
Foundation Insert: June 2010
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Foundation
Mark Scheme
Higher Paper: June 2010
Higher Insert
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme
Higher
Mark Scheme