Glaciation Flashcards

1
Q

When was the last ice age in Europe and the British isles?

A

It ended about 18,000 years ago, ice sheets several metres thick spread down the north as the climate eroded and glaciers filled the eroded valleys. Today the ice sheets have retreated

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2
Q

What is a glacial period?

A

An interval in time within an ice age that is marked by colder temperatures and glacier advances.

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3
Q

What is an interglacial period?

A

During an ice age there are periods of colder and warmer average global temperatures. The warmer periods are called interglacial periods because they separate the colder periods during the ice age.

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4
Q

Talk about the Mer De Glace glacier

A

It is found in the Alps, NE or Mont Blanc, it’s 7km long, 1200m wide and 200m thick. It is the longest and largest glacier in France. It’s name means SEA OF ICE. It moves at a speed of 70m a year.
It’s fed by snow flakes at an altitude of 4000m

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5
Q

What is the glacier system?

A

Inputs; snow accumulates
Stores;over time snow turns to ice
Transfers;glacier moves downslope under the pull of gravity
Outputs;meltwater and some evaporation

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6
Q

What is accumulation?

A

In the winter, inputs usually exceed outputs near to the head of a glacier.

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7
Q

What is ablation?

A

In the summer and at lower altitudes outputs will exceed inputs.

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8
Q

What is plucking?

A

The water at the bottom of the glacier freezes onto rock on the valley base. As the glacier moves, the rock is pulled away from the valley base. Plucking mainly occurs when the rock is well jointed.

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9
Q

What is a cirque/Corrie?

A

Deep bowl shaped landform created by the glacier.

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10
Q

What is abrasion?

A

The moraine frozen into the glacier scours the valley sides and floor, this has a sandpapering effect similar to corrosion by a river but on a larger scale

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11
Q

What is the snout?

A

End of the glacier. Pushes huge amounts of material in front, moraine.

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12
Q

What are crevasses?

A

Cracks in the ice, they can be metres across and perhaps 5-10m deep. They form when the ice is shredded as it flows down a steep slope. Extremely dangerous because they open and close as glaciers move. They may be hidden under fresh snow

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13
Q

What is frost shattering?

A

Water that enters cracks in rocks freezes and when it does, it expands. Repeated freeze and thaw means cracks in the rock and expand until the rock is fractured. This leads to material falling off the sides of the mountain slopes on to glacier.

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14
Q

What are glacial striation marks?

A

Striation marks are marks left by glaciers as they travel across an area. These marks can tell us the direction of movement of the glacier.

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15
Q

How do you form a U shaped valley?

A

Formed by glacier in mountain valleys and have a characteristic U shape, with steep straight sides and a flat bottom. They are formed when a glacier travels across and down a slope, carving a valley. When the ice retreats or thaws the valley is often covered with small boulders that were transported within the ice as glacier till.

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16
Q

How to form a Corrie?

A

Snow accumulates in north and east facing hollows
Snow is compacted into ice and moves downhill
Frost shattering and plucking create a steep back wall
Abrasion deepens the hollow and forms a rock basin
A rock lip is left where the rate of erosion decreased
The height of the lip is increased by the deposition of moraine
The rock lip and moraine act as a dam.
The Corrie lake fills the rock basin after the ice age

17
Q

How do u form an arête?

A

Glaciers form on the mountain as snow accumulates in hollows and turns to ice. The weight creates corries. As the glacier starts to move plucking and abrasion occur. Much of the mountainside is removed by these processes creating a more angular shape. Continued erosion means the rounded mountain is replaced by an angular peak. As the climate warms the glacier retreats as melting occurs. The end result is steep ridge. If corries form on 3 or more sides of the mountain in pyramidal peak forms. Tarns form in the empty corries

18
Q

How is a pyramidal peak formed?

A

when three or more corries and aretes meet the glaciers have carved away at the top of a mountain creating a sharply pointed summit. Eg Mont Blanc, Matterhorn and Mount Everest.

19
Q

How is a drumlin formed?

A

They are formed by glacial till. They are elongated features that can reach a kilometre or more in length, 500m or 50 in width and 50m in height. Several drumlins are called a swarm.

20
Q

What is lateral moraine?

A

Occurs at the sides of the glacier. It is made of rocks that have been weathered from the valley sides by freeze thaw.

21
Q

What is medial moraine?

A

Occurs in the centre where two glaciers have joined

22
Q

What is ground moraine?

A

Moraine that was at the bottom of the glacier. It is found on the valley floor when ice melts. This is also called till.

23
Q

What is terminal moraine?

A

Material that is left piled up at the snout of the glacier.

24
Q

What is recessional moraine?

A

As the glacier recedes (moves backgrounds)it leaves piles of moraine behind.

25
Q

What is an erratic?

A

A boulder that is different to the bedrock upon which it is sitting. They have been transported and deposited by a glacier. Therefore erratics are useful indicators of patterns of former ice flow.

26
Q

Causes of an avalanche

A

Most avalanches are on steep slopes in spring when temperatures start to rise and melting occurs. Unstable layers can also slip because of skiers snow boarders or even small earthquakes.

27
Q

Impacts of an avalanche

A

People can be killed in avalanche, 90% of the people who die in avalanches trigger them themselves. They usually die of lack of oxygen when buried in snow rather than getting too cold but they may also suffer impact injuries and fractures. Many houses, roads and plantations are destroyed.

28
Q

How to protect against avalanches?

A

Wooden fences to hold back snow, avalanche sheds to protect railway lines, wedges to protect electricity pylons, walls on steep walls to hold the snow. Mounds to snow avalanches on flatter ground, plant trees to prevent avalanches from starting.