Fluvioglacial landscapes Flashcards

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1
Q

What are the three main types of depositional landforms in fluvioglacial landscapes?

A

Kames, eskers, outwash plains

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2
Q

Describe what a kame is.

A

A hill or hummock composed of stratified sand and gravel deposited by glacial meltwater

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3
Q

Name the two different categories of kame.

A

Delta kame, terrace kame

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4
Q

Outline the two methods of formation of a delta kame.

A

Englacial streams emerge from the snout of a glacier, losing their energy at the base of the glacier and depositing their load OR supra glacial streams losing energy when meeting a static body of water in a ice-marginal lake

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5
Q

Where can kames be found?

A

East Lothian, Scotland

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6
Q

Where can terrace kames be located in relation to a glacial valley?

A

Along the edge of the valley floor

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7
Q

Outline how kame terraces are formed.

A

Supraglacial streams at the edge of a glacier transport lateral moraine, depositing it as the glacier retreats

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8
Q

What is the main difference between lateral moraine and kames?

A

The material is more rounded and sorted in a kame than in moraine

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9
Q

Where can kame terraces be found?

A

Kingsdale valley in the Yorkshire Dales

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10
Q

Describe a esker.

A

A long sinuous ridge composed of stratified sand and gravel deposited by glacial meltwater

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11
Q

How is material deposited in the formation of an esker?

A

It is deposited in sub-glacial tunnels as the supply of meltwater decreases at the end of the glacial period

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12
Q

What is the more controversial explanation for the formation of an esker?

A

That deposition occurs when the pressure is released and meltwater emerges at the glacial snout

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13
Q

What can cause beading in an esker?

A

When the retreat of the glacier slows or halts, eskers can be taller than at other points, giving the effect of beads

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14
Q

Give a named example of an esker, where it is and its approximate dimensions.

A

The Trim esker, near Dublin, 14.5km long, 4-15m high

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15
Q

What is the alternative name for an outwash plain?

A

A sandur

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16
Q

Describe a sandur.

A

A flat expanse of sediment in the pro-glacial area, with the largest material nearest the ice front and the finest further away

17
Q

How is an outwash plain formed?

A

As meltwater streams lose energy upon entering lowland areas beyond the ice front, they deposit their material

18
Q

What are braided streams?

A

Streams that drain outwash plains, they are river channels that are subdivided by numerous islets and channels

19
Q

How are braided streams formed?

A

Debris-laden streams lose water at the end of the glacial period, depositing it in the river channel causing it to divide. As flow decreases, the bar of sediment becomes exposed and vegetation grows making it more prominent

20
Q

Give a named example of a large sandur.

A

South coast of Iceland

21
Q

Why can fluvioglacial landforms be hard to identify?

A

Repeated advances and retreats modify the appearance of landforms, and are subject to weathering, erosion, vegetation and human activity