Fluvioglacial Landforms Flashcards

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1
Q

Formation of outwash plains

A

Formed from outwash sediment carried by meltwater streams. Made up of materials brought down by the glacier which is then picked up and sorted and dropped by running water beyond position of ice front, deposition

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2
Q

What are eskers

A

Long sinuous, winding ridges of sorted material that run in direction of ice advance. Often stratified(layered).
Meandering hills

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3
Q

Formation of eskers

A

Formed by subglacial river deposition when ice was melting away.
Mark the course of streams that once carried subglacial meltwater beneath glacier

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4
Q

Why do some eskers run up gentle gradients

A

Channel of streams would be restricted by ice walls so there would be considerable hydrostatic pressure.
Allow large load to be carried

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5
Q

What are kames

A

Deposits of sorted and often stratified sand and gravel left by meltwater along front of melting ice sheets.
Irregular undulating mounds
Can collapse when ice supporting them melts

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6
Q

What are outwash plains

A

Extensive, gently sloping areas of sands and gravel that form in front of a glaciers snout.

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7
Q

Formation of kames

A

When cracks in ice fill with sediments and the ice melts and sediments fall to form a mound

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8
Q

What are braided streams

A

When a stream splits off into little streams and material is deposited in the centre of them

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9
Q

Formation of a braided stream

A

Channel becomes choked with coarse material because of marked seasonal variations in discharge . When discharge is low excess sediment is deposited, discharge is variable

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10
Q

What are kettle holes/lakes

A

Series of small depressions filled with lakes/marshes

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11
Q

Formation of kettle holes/lakes

A

When blocks of ice buried beneath flubioglacial material melts causing surface layer of debris above buried ice to slump. The hollow can then fill with water to from a kettle Lake

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12
Q

What are varves

A

Layered deposits which reflect the seasonal flow of meltwater into lakes

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13
Q

Formation of varves

A

Sediment carried by meltwater streams is deposited when water enters a proglacial lake as the energy of the stream is lost.
They vary in thickness and this shows how much melting happens

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