glacial landforms Flashcards

(42 cards)

1
Q

what landforms are found in upper glacial valleys and mountain tops

A

corries
pyramidal peaks
aretes

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2
Q

what landforms are found in lower glacial valleys

A

glacial troughs
ribbon lakes
truncated spurs
hanging valley

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3
Q

what landform is found in the lower valley

A

roche moutonnees

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4
Q

what is a corrie

A

arm chair shaped hollow with a steep back wall. often contains a small lake called a tarn

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5
Q

where do corries normally form , facing which way

A

corries often face north because in the uk cold winds and the least sun comes from the north. north facing has more accumulation and less ablation

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6
Q

what process help corries form

A

niviation - early stages

frost-shattering
plucking
freeze thaw process

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7
Q

what is on the back wall of the corrie

A

scree

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8
Q

what process causes rocks to shatter and produce scree on the steep back wall

A

freeze thawing

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9
Q

what is formed by 2 corries

A

an arete

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10
Q

how is a arete formed

A

2 glaciers travel in parallel valleys which sharpens the mountain ridge between them

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11
Q

how is a pyramidal peak formed

A

a peak with at least 3 side
when 3 or more corries form back to back

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12
Q

what are the characteristics of a glacial troughs

A

steep sided valleys
several hundred metres in depth
may contain ribbon lakes
tend to be straight
Erosion landform

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13
Q

what is a ribbon lake

A

deep narrow lake

caused by enhanced erosion caused by weaker bedrock which allows for increase vertical erosion

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14
Q

what is a truncated spur

A

formed when ridges of land stick out into the main valley are chopped off as the glacier moves past it

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15
Q

what is a hanging valley

A

formed by smaller glaciers (Tributary glaciers ) they erode the valley much less deeply because they aren’t as big as the main glacier . when the ice melts the smaller valley will be left hanging

Erosional landform

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16
Q

what are the 8 erosional landscapes

A

arete
pyramidal peak
corrie
ribbon lake
glacial troughs
truncated spurs
hanging valley
roche moutonnée

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17
Q

what is a rouche moutonnee

A

small rock feature determining the direction of past glacial flow within a valley

18
Q

how have Roche moutonnees been shaped

A

by abrasion, plucking , basal sliding

jagged end - plucking
ice slides over the obstacle due to pressure melting point and melts

abrasion - steep polished end. smoothed by abrasion as the glacier went over it

19
Q

what are striations

A

on the surface of Roche moutonnees

they are scratch marks left by abrasion as ice moved over the bedrock

the marks are made by the rock the glacier carries

20
Q

what is till

A

unsorted material deposited directly by the ice

21
Q

what are the characteristics of till

A

the stuff the glacier leaves behind

unsorted boulders, stones and clay

22
Q

what are the characteristics of erratics

A

rocks that have been picked up and transported by glacial ice and deposited in a area with different geology

debris is out of place compared to its surroundings

23
Q

what is a moraine

A

name given to particular forms of till

24
Q

what are the types of moraines

A

lateral - deposited where the sides of the glacier were

medial - deposited in the centre of the valley - where 2 lateral moraines join together in the middle

terminal - build up at the end of the glacier

25
what is a till plain
large expanse of till formed when a ice sheet melts where it is
26
what are drumlins
drumlins are smooth elongated mounds of till half egg shaped hills up to 100m long and 100m high drumlins often form in groups / swarms the pointier end points the direction of the ice flow
27
what are the fluvioglacial landforms
eskers kames outwash plains kettle holes
28
what plays a important role in forming eskers and kames
meltwater
29
what is a esker
fluvioglacial landform long ridges on sand and gravel which run the same direction as a glacier they are deposited by meltwater streams flowing in tunnels under the glacier when the glacier retreats and the streams dry up esker is left
30
what are kame mounds
mounds of sand and gravel found on the valley floor meltwater streams onto of glaciers collect debris in crevasses debris is dropped to valley floor when the glacier melts
31
what are kame terraces
mounds of deposits left against the valley wall by meltwater that runs between the glacier and valley sides martial is sorted into layers meltwater deposits the heaviest loads first. kame terraces have gravel at the bottom with sand and finer sediments at the top
32
kame deltas
found in the front of glaciers the flow from the meltwater stream gets damned by moraines when the meltwater flows into the lake it deposits its sediments on the ice these deposits are deltas when ice melts the deltas drop to the valley floor forming kame deltas
33
kettle holes
34
fluvioglacial process and landforms
Meltwater streams erode the land Out wash plains Eskers Kames - mounds, terrace , deltas
35
what is a meltwater channel
36
what is permafrost
permanently frozen ground soil tempter must remain below 0 for two years or more
37
characteristics of continuous permafrost
found in the coldest regions
38
discontinuous permafrost
occurs in regions which are slightly Warmer 20-20 m
39
sporadic permafrost
mean annual temps around freezing
40
blockfields
periglacial landform thy are expanses of loose rock formed by repeated cycles of freezing and thawing frost chattered bedrock
41
terracettes
periglacial landform formed by solifluction lobes
42
how are drumlins formed
debate about how drumlins are formed one view : result from from the ice becomes overloaded with debris the ice reduces the capacity to carry material and deposition occurs at the base of the ice the material is shaped by glacier advance