Lesson 9: Glacial Processes and Landforms Flashcards

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1
Q

4 glacial processes

A

Erosion
Transportation
Entrainment
Sedimentation/deposition

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2
Q

Define erosion

A

Weathering of a glacial valley floor and sides by processes of freeze-thaw, weakens the rock, allowing the moving glacier to erode and remove more rock debris, which may be transported over longer distances

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3
Q

3 types of transportation

A

Supraglacial
Englacial
Subglacial

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4
Q

Define supraglacial

A

Mainly weathered material carried on top of the ice. Includes material falling from hillsides being washed or blown down, plus atmospheric fallout such as volcanic ash

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5
Q

Define englacial

A

Formally supraglacial material, but now buried by fresh snow and carried with the ice

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6
Q

Define subglacial

A

Material carried below the ice. Includes material eroded from the glacier bed and valley walls, material frozen to the base from subglacial streams, as well as englacial material that has worked its way down through the glacier or ice sheet

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7
Q

Define entrainment

A

Surface sediment is incorporated into a fluid flow (air, ice, water) as part of the process of erosion

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8
Q

Define deposition

A

Deposition of sediment transported by the ice occurs when it melts - mainly in the ablation zone close to he glaciers snout. Here the sediment in and on the ice melts. Water may then carry the sediment further away from the ice

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9
Q

Define plucking

A

Freeze thaw weathering with basal melt water

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10
Q

Define abrasion

A

Rocks being transported scratch bedrock, breaking more rock away from the base and valley walls of the glacier

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11
Q

Define crushing

A

Direct fracturing of weak bedrock by the weight of the glacier, producing large angular rocks

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12
Q

Define basal melting

A

Meltwater causes fluvial erosion processes such as abrasion, hydraulic action, attrition and corrosion

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13
Q

Describe cirque glacier

A

Amphitheatre shaped depression with a steep back wall and rock lip

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14
Q

Process of formation of cirque glacier

A

Large rounded hollow high on a mountainside is eroded and deepened by plucking and abrasion due to the rotational movement of ice

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15
Q

Example of a cirque glacier

A

Cwm Idwal, Snowdonia

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16
Q

Describe arete

A

Narrow, knife-edge ridge between 2 cirques

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17
Q

Process of formation of arete

A

Plucking and abrasion on the back wall of 2 cirques on a mountainside mean they erode backwards towards one another. Freeze-thaw important

18
Q

Example of arete

A

Striding edge, Lake District

19
Q

Describe pyramidal peak

A

Pointed mountain peak with 3 or more cirques

20
Q

Process of formation pyramidal peak

A

Erosional processes within cirques erode backwards into each other. Plucking important

21
Q

Example pyramidal peak

A

Matterhorn, Alps

22
Q

Describe glacial trough

A

U-shaped valley with step sides and a wide, flat floor

23
Q

Process of formation of glacial trough

A

V-shaped river valley widened and deepened from plucking and abrasion by a valley glacier which goes through the landscape rather than around

24
Q

Example of glacial trough

A

Nant Ffrancon Valley, Snowdonia

25
Q

Describe truncated spur

A

Steep rocky valley side where spurs of a river valley used to interlock before glaciation

26
Q

Process of formation of truncated spurs

A

Valley glaciers less flexible than rivers and remove the ends of interlocking spurs by plucking and abrasion as they move down the river valley

27
Q

Example of truncated spurs

A

Mer de Glace, Alps

28
Q

Describe hanging valley

A

Small tributary V-shaped or small U-shaped valley high above the main glacial trough floor, often with a waterfall as the river flows over the edge

29
Q

Process of formation of hanging valley

A

Thicker glacial ice is the main glacial trough eroded downwards more rapidly than thinner ice or river tributary valleys. The floor of the tributary valleys are left high above the main valley floor

30
Q

Example of hanging valley

A

Berwyn Mountains, Wales

31
Q

Describe ribbon lake

A

Long, narrow lake along the floor of a glacial trough

32
Q

Process of formation of ribbon lake

A

Increased plucking and abrasion by the valley glacier deepen part of the valley floor, causing the confluence of glaciers or weaker rocks

33
Q

Example of ribbon lake

A

Llyn Ogwen, Wales

34
Q

Describe roche moutonnee

A

Mass of bare rock on the valley floor with a smooth stoss and a steep jagged lee

35
Q

Process of formation of roche moutonnee

A

More resistant rock outcrop causes ice movement by creep and regelation. Ice slide over rock, smooths the stoss while refreezing on the lee causes plucking

36
Q

Example of roche moutonnee

A

Lembert Dome, Yosemite NP, California

37
Q

Describe knock and lochan

A

Lowland areas with alternating small rock hills (knock) and hollows, often containing small lakes (lochan)

38
Q

Process of formation of knock and lochan

A

Scouring at the base of the glacier excavates areas of weaker rock, forming hollows of meltwater and precipitation following ice retreat

39
Q

Example of knock and lochan

A

Shetland Islands, Scotland

40
Q

Describe crag and tail

A

Very large mass of hard rock forms a steep stoss with a gently sloping tail of deposited material

41
Q

Process of formation of crag and tail

A

Large mass of hard rock is resistant to ice scouring and creates a steep stoss. Reduced glacier velocity on the lee protects softer rock and allows deposition - sheltering diminishes with distance - sloping tail

42
Q

Example of crag and tail

A

Castle Rock, Edinburgh