3.1.4.4 Glacial Deposition Landforms Flashcards

1
Q

2 ways debris transported by a glacier will eventually be deposited

A
  • when it’s released by ice melting at snout

- when ice becomes overloaded with material

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2
Q

What’s the most common till

A

Ablation till at snout

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3
Q

What’s the name for subglacial debris till

A

Lodgement till

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4
Q

What are the 4 landforms formed by glacial deposition

A

Drumlins
Erratics
Moraines
Till plains

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5
Q

What’s a drumlin

A

Smooth egg-shaped hill up to 1.5km length + 50-60m in height

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6
Q

What are the 2 ends of drumlins like

What do they show

A

Steeper ‘upstream’ end + gently sloping ‘downstream’ end

Show direction of ice advance

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7
Q

Where are drumlins formed

A

Beneath glaciers

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8
Q

What’s the most popular theory of how a drumlin forms

A

The glacier being overloaded by moraine compared to the energy it has, so struggled to cope with transporting the amount in the lower parts of the course and so deposits it

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9
Q

What end of the drumlins means what

A

Blunt end - facing oncoming in

Tapered end - is the lee

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10
Q

2 other theories of how drumlins form

A

Obstacles (resistant rock) in glaciers path encourage deposited material to be moulded into the drumlin shape

Glacial meltwater is responsible for eroding large hollows beneath ice and then infilling causing drumlins

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11
Q

What are erratics

A

Rocks picked up + carried by ice, often for many kilometres and then deposited in areas of completely different lithology (rock type)

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12
Q

What can you track by erratics

A

Track ice movements, by determining where rocks originated from

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13
Q

What are moraines

A

Lines/series of mounds of material mainly running across glacial valleys

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14
Q

What moraine is found at the snout

A

Terminal/end moraine

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15
Q

Describe terminal moraine

A

Steep-sided
Can reach up to 50-60m high
Often moulded to the form of the snout

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16
Q

When do terminal moraines form

A

When ice melts during snout standstill, when its reached its furthest point down a valley + material has been deposited

17
Q

When can recessional moraines be formed along the length of the valley

A

As the glacier retreats

18
Q

What are till plains

A

Wide areas of flat relief created by a till sheet (thick glacial till, sand + gravel)

19
Q

Where are rill plains often found

A

Behind a terminal moraine/towards former ice sheet margins

20
Q

Why are till plains usually poorly drained with bigs, lakes and slow moving meandering streams

A

As depth can vary and a lot of material tends to be compacted

21
Q

When are till plains formed

A

When ice melts leaving a layer of till behind

22
Q

What’s drift

A

All glacial deposits (subdivided into till + glacifluvial material)

23
Q

What’s till

A

Unsorted mixture of rocks,clay and sand mainly transported as supraglacial + englacial debris and then deposited

(all material deposited by glacier itself)

24
Q

What’s glacifluvial material

A

All material deposited by meltwater streams