Glacial Landscapes Flashcards

1
Q

What are the three types of glacial landform?

A
  1. Depositional
  2. Erosional
  3. Fluvioglacial
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2
Q

What are the erosional landforms?

A

Roche Moutonnée
U-shaped valley
Truncated Spur
Hanging Valley
Crag and Tail
Corrie
Arête
Ribbon Lake
Tarn
Pyramidal peak

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3
Q

How can we categorise erosional landforms?

A

Macro
Meso
Micro

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4
Q

What are the macro erosional landforms?

A

Corrie
Arête
Pyramidal Peak
U-shaped valley
Ribbon lake
Hanging valley
Truncated spurs

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5
Q

What are the meso erosional landforms?

A

Roche Moutonnée
Crag and Tail

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6
Q

What are the micro erosional landforms?

A

Striations

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7
Q

What are the depositional landforms?

A

Moraines
Drumlins
Erratics
Till Plains

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8
Q

What is moraine?

A

The accumulation of unsorted debris (till) deposited directly by a glacier as it advances and retreats

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9
Q

What is till?

A

Unstratified (no layers) and unsorted sediment containing a mix of rock particles (clay, sand, gravel, boulders) deposited by a glacier

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10
Q

What are the six different types of moraine?

A
  1. Lateral
  2. Medial
  3. Terminal
  4. Ground
  5. Recessional
  6. Push
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11
Q

Where are the different types of moraine found?

A
  1. LATERAL
    - sides
  2. MEDIAL
    - middle of two merging
  3. TERMINAL
    - end
  4. GROUND
    - underneath
  5. RECESSIONAL/PUSH
    - behind terminal moraine, marking stages of glacial retreat and/or readvancement
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12
Q

How is lateral moraine formed?

A

Debris falling from the cliffs at the side of the glacier due to freeze-thaw action gets trapped at the edges and transported as the glacier moves

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13
Q

How is medial moraine formed?

A

When the lateral moraines of two converging glaciers join together

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14
Q

How is terminal moraine formed?

A

When the debris pushed at the glaciers snout is deposited as a ridge when the glacier reaches its maximum extent and begins to retreat

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15
Q

How is ground moraine formed?

A

As the glacier moves it deposits a thin irregular layer of till at its base

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16
Q

How is recessional moraine formed?

A

When a retreating glacier temporarily stabilises, depositing a ridge of debris before continuing to melt back

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17
Q

How is push moraine formed?

A

If the glacier advances again after retreating then ridges of sediment previously deposited get shoved up into little hills

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18
Q

What does recessional/push moraine look like?

A

A series of ridges behind the terminal moraine, showing pauses in the glaciers retreat.

Can show folding/faulting/tilting due to the force of the glacier moving forward

Often curved and perpendicular to the direction of the glaciers advancement

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19
Q

What are drumlins?
Give an example

A

Elongated, egg-shaped hills made of till formed when a glacier moving over an obstruction deposits and shapes till over the to of it

e.g. The Drumlin Field beneath Cam Fell, Yorkshire Dales

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20
Q

What are eratics?
Give an example

A

large, random rocks transported by glaciers hundreds, sometimes thousands of km from where they originate. They do not fit with the size or type of rocks in the area in where they are deposited

e.g. The Great Stone of Fourstones, moors of Tatham Fell, England

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21
Q

What is a glacial outwash plain?
Give an example

A

Where till is carried and deposited by meltwater streams in layers further down the valley from the glacier snout

e.g. Lake Clarke National Monument, Alaska

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22
Q

What is another name for a glacial outwash plain?

A

Sandur

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23
Q

What is outwash?

A

Sediment that has been transported away from a glacier by meltwater

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24
Q

Why do you get layering in the outwash plain?

A

changing competence over time:
- bigger stuff is deposited in summer due to more meltwater = large sediment, high competence
- smaller stuff is deposited in winter due to less meltwater = small sediment, low competence

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25
Q

How do glacial outwash plains form?

A
  1. During summer, temps increase, melting increases, and sediment is deposited on the valley floor or sides of a moving glacier
  2. Meltwater will flow out of the glacier snout, forming meltwater rivers
  3. Meltwater rivers carry large amounts of glacial till, which undergoes erosion (attrition) to become outwash
  4. The finer till is then sorted, and when the energy of the river reduces, the outwash is sorted and deposited as layers further down the valley on the outwash plain
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26
Q

What and where are the different zones on a glacial outwash plain?

A

PROXIMAL ZONE
- close to the snout, just beyond the terminal moraine

MEDIAL ZONE
- the large middle majority of the outwash plain

DISTAL ZONE
- the end of the outwash plain, furthest away from the snout of the glacier

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27
Q

What is a Roche Moutonnée?
Give an example

A

A bedrock bump that has a steep and jagged face on the lee side due to plucking, and a smoothed/polished face on the stoss side due to abrasion

e.g. Dulnain Bridge, Cairngorms NP

28
Q

What is a U-shaped valley?
Give an example

A

A v-shaped valley that has been widened, deepened and straightened by the movement of a glacier. They have steep sides and a flat floor

e.g. Ullswater Valley

29
Q

What is a hanging valley?
Give an example

A

Where a tributary valley is left suspended above the main valley floor due to different rates of erosion between it and the main valley

e.g. Cwm Dyli, Eryri NP

30
Q

What is a truncated spur?
Give an example

A

A steep cliff face either side of a glacial trough caused by the glacier truncating/cutting off spurs as it moves down the valley. An inverted V shape

e.g. Nant Ffrancon Valley, Eryri NP

31
Q

What is a crag and tail?
Give an example

A

Where a glacier travelling over a piece of resistance rock with soft rock on both sides creates a small rocky hill from which there extends a tapering ridge of unconsolidated debris

e.g. Edinburgh - Castle is on the Crag, The Royal Mile is the Tail
e.g. North Berwick

32
Q

What is an arête?
Give an example

A

A knife edge ridge formed when two corries form back to back

e.g. Striding Edge, Helvellyn

33
Q

What is a pyramidal peak?
Give an example

A

An angular, sharply pointed mountain summit/peak formed when three or more corries form back to back

e.g. the Matterhorn

34
Q

What is a ribbon lake?
Give an example

A

When the glacier travels over softer rock is can carve a deeper trough in these areas, which will ill with water when the ice melts
The harder rock left behind are called rock steps

e.g. Windermere

35
Q

What is a tarn?
Give an example

A

When the hollow in the bottom of a corrie fills with water when the ice in the corrie melts which doesn’t flow out due to the corrie lip

e.g. Red Tarn, Helvellyn

36
Q

What factors affect the rate and amount of abrasion?

A
  • meltwater
  • debris
  • mass of glacier
  • ice thickness
  • velocity
  • gradient
  • thermal regime
    Geology:
  • relative hardness (type of rock)
  • jointing
  • permeability
37
Q

What are the two categories of fluvioglacial landforms?

A

Ice contact
Pro glacial

38
Q

What are the fluvioglacial ice contact landforms?

A

Eskers
Kames
Kame terraces

39
Q

What processes does glacial meltwater impact on?

A

movement
erosion
entrainment
transport
deposition

40
Q

Where does meltwater come from?

A

Surface
Basal (PMP)

41
Q

Where does glacial meltwater flow when it is on the glacier?

A

Subglacial
Englacial
Proglacial
Supraglacial - moulins and streams

42
Q

What is a moulin?

A

a roughly circular and vertical/near vertical well-like shaft in a glacier formed when surface meltwater exploits a weakness in the ice

43
Q

What are the fluvioglacial processes?

A

EROSION
- sub glacial, proglacial
TRANSPORT
- competence
DEPOSITION
- ice contact, pro glacial

44
Q

What is competence?

A

the ability of water to transport material

45
Q

What is high competence?
What is low competence?

A

high speed
high volume
high discharge

low speed
low volume
low discharge

46
Q

What are the characteristics of fluvioglacial deposits?

A

Rounded
Sorted
Stratified

47
Q

Why are fluvioglacial deposits rounded?

A

because of attrition in the water - rocks crash into each other and knock corner off

48
Q

Why are fluvioglacial deposits sorted?

A

because of the changing competence of the water - larger sediment is deposited first as the water flow slows

49
Q

Why are fluvioglacial deposits stratified?

A

because you get daily/seasonal changes on a regular basis, leading to layers on layers

50
Q

What is a kame?
Give an example

A

a mound of sorted/stratified sand and gravel found on the glacial valley floor or in the outwash plain

e.g. Holy Hill, Wisconsin

51
Q

What are the three different types of kame?

A

Kame delta
Crevasse kame
Kame terrace

52
Q

What is a kame delta?

A

Where the meltwater stream flowing round the sides of a glacier is dammed by a terminal moraine, and so the kame forms in a proglacial lake

53
Q

What is a crevasse kame?

A

small hummocks of glacial surface-deposited sediments that have been left behind

54
Q

What is a kame terrace?
Give an example

A

piles of debris left by meltwater channels that have been deposited between the sides of the valley and the glacier

e.g. Carstairs kames, Scotland

55
Q

What is the difference between a kame and moraine?

A

KAME:
- sorted
- stratified
(heaviest gravel at base, finer sediment on top)
- fluvioglacial deposition

MORAINE:
- unsorted
- unstratified
(no water competence involved)
- glacial deposition

BOTH:
- deposition
- form anywhere round the glacier

56
Q

What is an esker?
Give an example

A

a long, winding ridge composed of stratified sand and gravel (sediment) deposited by subglacial meltwater streams in tunnels, running parallel to the flow of the glacier

ONLY in a stagnant glacier/meltwater stream

e.g. Denali Highway Esker, Alaska

57
Q

Why does a glacier/meltwater stream have to be stagnant for an esker to form?

A

if it moved, it would transport material not deposit it

58
Q

Give some esker stats

A

20-30m high
a few (days/weeks formation) - 100s (100s-1000s year formation) km
50-500m wide
Can be:
- triangular
- semi circular
- multi crested
- flat topped

Types:
- single channel
- tributary channel
- continuous
- non continuous

59
Q

What is the difference between an esker and moraine?

A

ESKER:
- forms in outwash plain only
- stratified
- fluvioglacial deposition

MORAINE:
- forms all round the glacier
- unstratified
- glacial deposition

BOTH:
- deposition
- sand and gravel

60
Q

What is the importance of eskers?

A
  • sand and gravel used for construction
  • roads built on them e.g. Denali Highway
  • used in hunt for diamonds
  • ecology - plants grow on the e.g. cranberries
61
Q

What are the fluvioglacial pro glacial landforms?

A

Kettle holes/lakes
Varves
Glacial outwash plains

62
Q

What is a kettle hole?
What is a kettle lake?
Give an example

A

A depression or hole in an outwash plain formed by a retreating glacier

A kettle lake is when the ice melts and the kettle hole fills with water

e.g. Ellesmere, Shropshire

63
Q

What is a varve?
Give an example

A

stratified, distinct annual layers of sediment found in the deposits at the bottom of a pro glacial lake. 2 layers, one sandy, light coloured one, and one darker silt.

e.g. in Lake Suigetsu, Japan

64
Q

What forms the 2 distinct layers in a varve?

A

SEASONALITY: In summer, discharge is high so the coarse sediment is deposited, and in winter, discharge is low so the finer sediment is deposited

65
Q

Why are varves important to humans?

A

paleoclimatic indicators, radiocarbon dating, helps us understand climate change
e.g. in Lake Suigetsu, there are thousands of annual layers dating 50,000 years