Distribution/ Glacial Processes and Landforms Flashcards

0
Q

What are the four different types of cold environments?

A

Glacial, Periglacial, Alpine and Polar.

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1
Q

What are the three main reasons that environments are cold?

A

The three main reasons that environments are cold are; high altitude, high latitude or because the effect of continentality.

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2
Q

What are glacials environments and where are they found?

A

Glacial environments are areas of land that are permanently covered by ice (glaciers or ice sheets) They are found at high altitude or high latitude, not in the middle of continents as there is not enough snow there

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3
Q

What is a glacier? Describe the two different types.

A

Glaciers are masses of ice that flow downhill.

Valley Glaciers fill valleys and can be several kilometres long e.g. The Franz Josef Glacier, NZ

Corrie Glaciers are smaller and found in bowl shaped hollows up in the mountains e.g. Lower Curtis Glacier, Washington, USA

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4
Q

What’s an ice sheet?

A

Domes of ice that cover huge areas of land e.g. The Antarctic Ice Sheet (Southern Hemisphere) or the Greenland Ice Sheet (Northern Hemisphere)

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5
Q

Give two examples of Glacial environments that exist at high altitude.

A

Glaciers are found in the Himalayan mountains, regardless of the latitude (30) because there the highest mountain range in the world. Another example is the Antizana Glacier, Ecuador which is right on the equator.

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6
Q

What is a Periglacial Environment?

A

Periglacial environments are places where the temperature is frequently or constantly below freezing but not covered by ice. They contain a layer of permafrost on or below the surface.

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7
Q

Where are Periglacial environments found?

A

They are found at high altitude, high latitude and in the interior of land masses.

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8
Q

Give an example of Periglacial environments found at high altitude.

A

Periglacial conditions exist around ice masses in mountain ranges. They also found on high altitude plateau areas e.g. The Tibetan Plateau, Asia and The Bolivian plateau, South America.

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9
Q

Where can you find Periglacial conditions at high latitude?

A

You can find Periglacial conditions in the northern parts of Asia, North America and Europe.

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10
Q

Why can Periglacial conditions exist at lower latitude and altitude?

A

They can exist at lower latitude and lower altitude because of the effect of continentality e.g. Siberia, Central Asia.

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11
Q

What is an Alpine environment and where can they be found?

A

An alpine environment is a cold area of land that exists above the tree line. They are always found at high altitude e.g. The Himalayas, Asia OR The Andes, South America OR The Alps, Europe.

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12
Q

Can Alpine areas exist at any latitude?

A

Yes. An example of this is the Rocky Mountains, North America which contain alpine conditions at a latitude of 30-50.

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13
Q

Can alpine environments include Periglacial and glacial conditions?

A

Yes. Permafrost may exist above and below the tree line and snow and ice may exist even higher as temperatures decreases as altitude increases.

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14
Q

Where is the Arctic Polar environment found?

A

This is found in the North Pole, it can be defined as the Arctic circle (66N) ❄️

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15
Q

Give me some facts about the Arctic circle. For example why is it cold?

A

The Arctic circle is cold because it is 66N so therefore exists at Beth high latitude. The area around the North Pole is made up of sea ice which shrinks in the summer and refreezes in the winter.

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16
Q

Where is the Antarctic Polar environment found?

A

It is found in the South Pole (66S) ❄️

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17
Q

Why is the Antarctic Polar environment cold?

A

It’s cold because of its high latitude however some of the environment is also cold because it’s at a high altitude- the ice in some places is so thick it reaches an altitude of over 4000m. The interior of Antartica is also cold as the centre is hundreds of kilometres away from the warming of the oceans.

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18
Q

Name the inputs of the glacial system.

A
  1. Snow (from precipitation and avalanches)
  2. Condensation (from water vapour which freezes)
  3. Sublimation of water vapour to ice crystals
  4. Rock (collected from erosion)
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19
Q

Name the stores of the glacial system.

A
  1. Ice
  2. Meltwater found on, in or below the ice
  3. Debris (rocks, sand and gravel)
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20
Q

Name the outputs of the glacial system.

A

Ice- which can melt and flow out of the glacier as meltwater and snow- that can be blown away by strong winds or melt and evaporate. Both snow and ice and sublimate to water vapour and lastly another output is the effect of calving.

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21
Q

What is calving?

A

Calving is where blocks of ice fall from the snout of the glacier into the sea to create ice bergs.

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22
Q

A) What is accumulation?

B) What is ablation?

C) What happens if there is the same amount of each over a year?

A

A) The input of snow and ice into the glacier

B) The output of water from a glacier

C) If there is the same amount of accumulation and ablation over a year, the glacier stays the same size and the position of the amount doesn’t change

23
Q

What’s the difference between a positive regime and a negative regime?

A

A positive regime is where there is more accumulation than ablation over a year causing the glacier to advance whereas a negative regime is where there is more ablation than accumulation over a year so the glacier retreats.

24
Q

How do glaciers form?

A
  1. Firstly snow settles with a loose fluffy consistency
  2. The weight of more snow turns the snow into a dense and granular kind called FIRN
  3. Air is squeezed out and particles of ice are compressed together by the adding of snow and ice
  4. Water also melts and refreezes in the air spaces making the ice even more dense.
25
Q

What is a warm-based glacier?

A

In warm based glaciers the base is warmer than the melting point of ice because of friction from movement and geothermal heat from the earth. Because of this the ice at bottom melts and acts as a lubricant which makes it easier for the glacier to move causing lots of erosion.

26
Q

What is a cold based glacier?

A

In cold based glaciers the base is usually well below the melting point of ice so melting does not occur. The ice is frozen to the base of the valley so there’s little movement not even in summer. Because of this cold based glaciers don’t cause much erosion.

27
Q

What is basal sliding?

A

Basal sliding is the main way warm based glaciers move. Meltwater underneath a glacier allows the glacier to slide over the ground.

28
Q

What is rotational flow?

A

When glaciers move in an arc shape when they’re in a hollow by basal sliding.

29
Q

What is internal deformation?

A

This is the main way cold based glaciers move. It is where the ice bends and warps to flow downhill like s liquid. It is caused my ice crystals shifting past each other.

30
Q

What is extensional flow?

A

At the head of the glacier the valley is steep so there’s a strong gravitational force pulling the ice downwards which makes it move very quickly. Because the ice is moving very quickly there’s more tension which causes the ice to fracture into thick layers which then slip downwards.

31
Q

What is compressional flow?

A

Lower down the glacier the ice is moving more slowly because the valley is less steep. The faster ice from the head of the glacier pushes down on the slow ice and compresses it. The high pressure caused the ice to fracture layers and the layers slip forwards.

32
Q

What factors determine the speed in which the glacier flows?

A

The gradient of the valley floor, the thickness of the ice and the temperature of the base. Ice also moves faster near the glaciers surface and in the middle rather than the edges.

33
Q

What are crevasses and why are they caused?

A

Crevasses are stresses and strains in the ice which can be caused by extensional and compressional flow, calving and tension (between the ice attached to the sides and back wall and the rest of the glacier)

34
Q

What is the bergschrund?

A

A big semi circular crevasse at the back of the glacier caused by the ice pulling away from the ice attached to the back wall.

35
Q

What are two types of erosion that erode the valley floor and sides?

A

Plucking and abrasion.

36
Q

What is plucking?

A

Ice in contact with rock surfaces can thaw and then refreeze around rocks protruding from the sides and wall of the valley. When the glacier moves forwards it plucks away the rock.

37
Q

What is abrasion?

A

Debris carried along by the glacier can scrape material off the valley walls and floor.

38
Q

What is meltwater erosion and what does it do?

A

Glaciers can produce huge amounts of meltwater making streams that are powerful enough to erode the valley floor and sides by fluvioglacial river processes.

39
Q

What are the three ways debris is transported by a glacier? Explain each type.

A
  1. Supraglacial material is carried on top of the glaciers surface.
  2. Englacial material is carried within the body of the glacier.
  3. Subglacial material is moved along at the base of the glacier.
40
Q

What is till?

A

Till is unsorted sediment deposited by the glacier. It can be anything from boulders to pebbles and clay. Glaciers can drop any till anywhere. Till points in the direction that the glacier is flowing.

41
Q

Describe the two different types of till.

A

Lodgement till is spread onto the valley floor beneath the ice by moving glaciers.

Ablation till is dropped by a glacier as it melts. The till is mainly deposited close to the glacier snout because this is where most ablation happens.

42
Q

What is a moraine? What are the different types?

A

Moraine is different formations of till.

A) Lateral moraine is deposited where the sides of the glacier were.

B) Medial moraine is deposited in the centre of the valley where two glaciers converge (two lateral moraines join together)

C) Terminal moraine builds up at the end of the glacier and is deposited as semicircular hillocks of till.

43
Q

How is a corrie formed?

A

Corries form on one side of a mountain peak where there is the least sun and coldest winds. The snow collects in hollows and turns to ice. Basal sliding, abrasion and plucking deepen the Hollow into the corrie. When the ice in the hollow is thick enough it flows over the lip and downhill as a glacier. The back wall is steepened by plucking and frost shattering.

44
Q

What is an Arête?

A

An arête is a steep sided ridge that is formed when two glaciers flow in parallel valley. The glaciers erode the sides of the valley, which shape end the mountain ridge in between them.

45
Q

What is a pyramidal peak?

A

It is a pointed mountain ridge with at least three sides. It forms where three or more corries form back to back as there back walls make the mountain peak.

46
Q

What is a glacial trough?

A

A glacial trough is a U shaped valley. It is a steep sided valley with a flat bottom formed by the erosion of V shaped river valley by glaciers. The glacier makes the V shaped valley deeper and wider.

47
Q

What is a tributary glacier and what does it form?

A

A tributary glacier is a smaller glacier that flows into the main valley. They form hanging valleys which erode the valley floor much less deeply because they’re smaller than the main glacier. When the glaciers melt, the valleys get left at a higher level than the glacial trough formed by the main glacier. You get waterfalls from hanging valleys into the main glacial trough.

48
Q

Describe a truncated spur.

A

A truncated spur occurs when ridges of land (Spurs) that stuck out into the main valley are chopped off (truncated) as the main valley glacier moves past.

49
Q

What are valley steps?

A

These are steps in the glacial trough. They are former when the glacier derided the valley floor more deeply. This happens when another glacier joins it or where there’s less resistant rock.

50
Q

What is tarn and where does it form?

A

A tarn is a lake that forms in corries after a glacier has retreated.

51
Q

What’s a ribbon lake?

A

Long, thin lakes that form after a glacier retreats. They form in dips caused by erosion of band of less resistant rock or behind dams of debris that have been left behind.

52
Q

What’s a fjord?

A

Long, deep inlets that form when a valley that’s been eroded by a glacier is flooded by sea level rise after the ice has melted.

53
Q

Describe a Roche moutonnée.

A

A Roche moutonnée is a resistant mass of rock on the valley floor. The stoss is smooth because it abrasion from the glacier travelling over it and the lee is steep and rough where the glacier plucked at it. It can be 8m long and 3m high.

54
Q

What’s a drumlin?

A

Drumlins are half egg shaped hills of till that can be 1500m long and 100m tall. The upstream is wife and tall and the downstream is narrow and low. Drumlin often form in groups e.g. Ribble Valley, Lancashire.

55
Q

What are erratics?

A

Erratics are boulders that have been picked up by a glacier or an ice sheet, carried along and dropped in an area of different geology e.g The Yorkshire Dales.