glacio fluvial landforms Flashcards

1
Q

what are glacio fluvial landforms

A

landforms produced by the meltwater from glaciers

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2
Q

what is the deposit produced by glacio-fluvial streams known as

A

outwash

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3
Q

what are three key characteristics of outwash

A
  • smooth and rounded due to attrition
  • sorted horizontally with the largest furthest up the stream
  • stratified vertically with distinctive seasonal layers of annual sediment accumulation
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4
Q

how do seasons impact the discharge of glacio fluvial rivers

A
  • in winter months there is minimal discharge so the river will only have energy to carry small material
  • in the summer melting season there will be extremely high discharge enabling glacio fluvial rivers to carry large sediment and even boulders
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5
Q

give a specific example of a glacier with discharge significantly influenced by season

A

-the glacier d’Angentiere, lying perpendicular to Chamonix in france has a winter discharge of 0.1-0.5 cumecs but summer discharge of 10-11 cumecs.

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6
Q

what is a kame

A

a hill or hummock composed of stratified gravel and sand laid down by glacial meltwater

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7
Q

what are the two types of kames

A
  • delta kames

- kame terraces

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8
Q

describe the two ways in which delta kames can be formed

A
  • some formed by en-glacial streams when the stream exists the glacier at its snout, losing energy and depositing the material
  • some are formed by supra glacial streams entering a lake, losing their energy as they enter the static body of water
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9
Q

what are kame terraces

A

ridges of material running along the valley floor

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10
Q

how are kame terraces formed

A

supra glacial rivers running along the side of the glacier collect material which is deposited when the glacier retreats

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11
Q

how are kame terraces different from lateral moraines

A

although they appear simiar, kame terraces are composed of outwash which is smaller, rounder and smoother than material deposited directly from a glacier

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12
Q

give a specific example of kame terraces

A

kames are widespread in lothian, scotland

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13
Q

what is an esker

A

-a long sinuous ridge composed of stratified sand and gravel laid down by glacial meltwater

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14
Q

how do eskers form

A

material is deposited in sub glacial tunnels as meltwater is decreased

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15
Q

what is a secondary theory to the formation of eskers

A

scientist argue that deposition occurs as material emerges from the glacial snout. as the glacier retreats the snout moves further back resulting in the long ridge.

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16
Q

give a specific example of an esker

A

the trim esker in dublin is 14.5km long

17
Q

what are the three types of depositional glacio fluvial landforms

A

kames, eskers, outwash planes

18
Q

describe four ways in which modification can occur with glacio fluvial landforms

A
  • repeated advance and retreat
  • weathering an rockfall
  • rising temperatures lead to excessive meltwater thus excessive outwash
  • -rising temperatures also lead to ideal conditions for vegetation growth therefore outwash can be overcome by moss, grasses, flowers and shrubs