Lithosphere Flashcards

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1
Q

Explain plucking?

A

Ice moulds itself to the walls and loose rocks are pulled out

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2
Q

Explain abrasion (glacial)

A

Rocks are embedded in ice and rubs against the ground like sandpaper, smoothing the land

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3
Q

Explain frost shattering

A

Water seeps into cracks in rocks and freezes, causing it to expand and crack the rocks further

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4
Q

How is a glacier formed?

A

Snow falls in a north facing hollow where it collects and compacts. Air is squeezed out over time and forms firn/neve

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5
Q

Explain the formation of a corrie

A

Explain glacier formation

Ice builds up and is pulled downslope due to gravity and its weight and leaves back wall steep and jagged due to plucking

Rotational flow pulls over lip creating possible deposition and a lip (weird right?)

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6
Q

Explain the formation of an arête

A

Explain formation of glacier and corrie

A sharp ridge where two corries form back to back or side to side when the back walls erode close together

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7
Q

Explain the formation of pyramidal peak

A

Explain formation of glacier and corrie

Left jagged by frost shattering. Where 3 or more corries form back to back.

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8
Q

Explain the formation of a U-shaped valley

A

Explain glacier formation

Glaciers flow from river valleys which deepens and widens them

V-shaped valley spurs are left as truncated

Valley streams return to over deepened valleys, forming misfit streams

Glaciers with less erosive power form hanging valleys, often with waterfalls. Found in Windermere

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9
Q

Explain formation of a drumlin

A

Drumlins are formed from glacial till.
Stoss end is steeper and used to face into ice flow. Lee slope is not as steep and becomes lower as you move away from source of ice.

Ice became overloaded with sediment and the glacier had less power. This meant material is deposited.

Drumlin shape moulded as ice was still moving over it, but it may have been eroded by more ice after

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10
Q

Explain terminal moraine

A

Marks furthest extent of ice. Ice melts at front end of glacier and the glacier loses power. Melting ice deposits till. Unsorted and angular rocks. Longer glacier is in the same place, larger terminal moraine is.

Meltwater flowing through through moraine carries smaller and rounder materials. Material is deposited beyond glacier and sorted. Bigger material is closer to moraine, smaller are far away. Forms outwash plans.

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11
Q

Lateral and medial moraines

A

Lateral develop along edges of an advancing glacier.

When two valleys meet a medial moraine is formed when the two lateral moraines meet.

Lateral moraines usually collapse when glacier retreats

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12
Q

Explain the formation of an Esker

A

Meltwater stream flows in a tunnel beneath a melting ice sheet.

Stream carries and deposits moraine, filling up tunnel.

When ice melts, ridge of moraine is left in the shape of stream’s tunnel

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13
Q

Explain longshore drift

A

Waves approach beach at an angle the same as the prevailing wind. Swash carries material up the beach at the angle of the prevailing wind and backwash carries the material back out to sea at a 90° angle due to gravity.

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14
Q

Explain the formation of a spit

A

Explain longshore drift
Spit forms when water deposits more material than it erodes. This causes sediment to be moved up the beach due to longshore drift. This continues until the land turns away, causing the sediment to be deposited out to sea, forming a spit.

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15
Q

Explain formation of bar

A

Explain longshore drift
Explain spit
Sediment continues to be deposited across the bay and eventually meets up with the other side, forming a bar and a lagoon behind it

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16
Q

Explain formation of a tombolo

A

Explain longshore drift
Explain spit
A tombolo forms if sediment is deposited out to sea and reaches an island