Topic 3- Cold Environments Flashcards

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1
Q

What is a cold environment?

A

Cold environments are areas of land permanently covered by ice. They are covered by glaciers, ice sheets and have frozen soil/rock. The temperature is constantly below freezing.

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2
Q

What are the three factors that increase the chance of cold environments in different areas.

A

Latitude (distance from the equator), Altitude (height above sea level), continentality (how far inland it is).

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3
Q

What is a glacier?

A

A slowly moving mass or river of ice formed by the collection and compaction of snow on mountains or near the poles.

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4
Q

What are the two zones that a glacier can be divided into?

A

The accumulation zone and the ablation zone.

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5
Q

What is the accumulation zone of a glacier?

A

The accumulation zone is where there are inputs into the glacier budget.

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6
Q

What is the ablation zone?

A

The ablation zone is where there are outputs from the glacial budget.

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7
Q

What are the inputs into the glacial system?

A

Input-the main input is snow. As it becomes increasingly compacted over many years, it gradually turns from powder snow to dense glacial blue ice. Avalanches from surrounding mountains sides also provide inputs to the glacial system.

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8
Q

What are the processes of the glacial system?

A

The weight of the compacted ice then combines with gravity to make the glacier move slowly downhill. As it does so, it transports sediment that has dropped onto it-and also erodes its valley (processes in the system)

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9
Q

What are the outputs of the glacial system?

A

The main outputs from the system include ice and meltwater- together with vast amounts of sediment.

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10
Q

What is the equilibrium line of a glacier?

A

The equilibrium line separates the ablation zone and the accumulation zone; it is the altitude where the amount of new snow gained by accumulation is equal to the amount of ice lost through ablation.

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11
Q

Why do glaciers advance and retreat?

A

If the inputs, accumulation zone, or the outputs, the ablation zone, are bigger than the other one than it will either retreat or advance, depending on which one is bigger.

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12
Q

If the inputs, accumulation zone, are bigger than the outputs, ablation zone, will the glacier advance or retreat?

A

Advance as the inputs outweigh the outputs.

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13
Q

If the outputs, ablation zone, are bigger than the inputs, accumulation zone, will the glacier advance or retreat?

A

Retreat as the outputs outweigh the inputs.

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14
Q

If the inputs and outputs of a glacier are the same, will it advance or retreat?

A

It will neither advance or retreat, only stay in the same position. This is because the inputs and outputs are equal.

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15
Q

What is a corrie?

A

A corrie- a rounded hollow on the side of a mountain with a steep wall at the back. They often contain a lake.

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16
Q

Wha is glacial erosion?

A

Glacial erosion- the process of breaking rock apart by a glacier.

17
Q

What is a moraine?

A

Moraine- piles of rock left behind when a glacier melts.

18
Q

What is freeze-thaw?

A

Freeze-thaw= water gets trapped into cracks in rock. When the temperature drops it freezes and expands. This helps crack open the rock. When the temperature rises, the ice will melt. This happens repeatedly and breaks off rock leaving a rough surface.

19
Q

What is plucking?

A

When a glacier moves, rock that is frozen to the base gets pulled from the ground, leaving behind a jagged landscape.

20
Q

What is abrasion?

A

Abrasion= when loose rocks become embedded in the base of a glacier and rub against the ground underneath, wearing it away.

21
Q

How does the glacial budget vary throughout the year?

A

The glacial budget varies during the course of a year. In the summer, ablation will be at its highest, because of rapid melting of ice. During winter, higher amounts of snowfall and limited melting will result in accumulation being greater than ablation.

22
Q

Give six key features of a corrie?

A

Arm chair shape (3 steep sides), steep back wall, shattered rock, deep tarn lake, rock lip-higher land, and a waterfall

23
Q

How many stages are there in the formation of a corrie?

A

Eight stages

24
Q

Expalin the formation of a corrie?

A

a) snow collects in hollows, b) snow compacts to ice, c) ice moves under gravity, softened by meltwater, d) ice rotates and leaves lip where less erosion has occurred, e) abrasion deepens corrie, f) plucking steepens back and sides, g)freeze-thaw makes the edges of the corrie rigid and rough h) ice melts and corrie lake/tarn may fill hollow.

25
Q

What is an arête?

A

Arêtes are knifed edged ridges formed between two corries.

26
Q

Explain the formation of an arête?

A

It is formed when two neighbouring corries run back to back. As each glacier erodes either side of the ridge, the edge becomes steeper and the ridge becomes narrower

27
Q

What is a pyramid peak?

A

A pyramidal peak can be a small peak on a mountain ridge, or a large mountain peak formed by glacier activity. A large pyramidal peak is sometimes called a horn.

28
Q

Explain the formation of a pyramid peak?

A

A pyramidal peak is formed where three or more corries and arêtes meet. The glaciers have carved away at the top of a mountain, creating a sharply pointed summit

29
Q

Why does a small glacier eventually form?

A

Snow accumulates in sheltered hollow and becomes compacted.

30
Q

Why is the back wall of a corrie very steep?

A

Due to plucking and freeze-thaw weathering.

31
Q

How does the glacier in a corrie move?

A

Under its own weight in a circular way called rotational movement/slip

32
Q

How is the hollow of a corrie deepened?

A

By plucking and abrasion.

33
Q

Why does a lip form at the front of a corrie?

A

There is less erosion at the front of the corrie.

34
Q

Once the ice has melted what often forms in the hollow?

A

A tarn/lake

35
Q

How is a U shaped valley formed?

A

U-shaped valleys are formed by the process of glaciation. Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring.

36
Q

How is a V shaped valley formed?

A

When a river is near its source, it often develops a V-shaped valley as the river erodes down (this is called vertical erosion).