OCR A Level GL - 6 OCR A Level GL 2.2a Geomorphic and Glacial Processes Flashcards

1
Q

What is weathering?

A

the in situ breakdown of rocks exposed at, or near, the land surface by physical, chemical and biological processes.

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2
Q

What is physical weathering (Mechanical)?

A

the in situ breakdown of rock in which there is no chemical alteration. In glacial environments, these include “Freeze-thaw”, “Frost-shattering” and “Pressure Release”.

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3
Q

What is freeze-thaw weathering?

A

a form of physical weathering in which water enters cracks/joints in rocks then freezes, expanding by 10% in the process, and causing the rock to split or for pieces to break off. Particularly prevalent in areas where temperatures fluctuate around zero (i.e. areas of high altitude with diurnal changes in temperature).

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4
Q

What is frost shattering?

A

a form of physical weathering in which water trapped in rock pores freezes at extremely low temperatures, exerting stress and disintegrating the rock into small particles.

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5
Q

What is pressure release (dilatation)?

A

a form of physical weathering whereby rock underlying a glacier expands and fractures parallel to the surface when the weight of a glacier is removed when it melts.

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6
Q

What is chemical weathering?

A

the in situ breakdown of rock in which there is a chemical reaction between elements of the weather and some minerals within rocks. These type of weathering includes oxidation, carbonation, solution, hydrolysis and hydration.

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7
Q

What is oxidation?

A

a form of chemical weathering in which minerals in rocks react with the oxygen found in the air. This process particularly happens in rocks with high iron content (such as sandstone).

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8
Q

What is carbonation?

A

a form of chemical weathering in which carbonic acid (formed when rainwater combines with dissolved carbon dioxide) reacts with calcium carbonate, in particular found in limestone.

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9
Q

What is solution?

A

a form of chemical weathering whereby a mineral dissolves in water.

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10
Q

What is hydrolysis?

A

a form of chemical weathering in which water chemically reacts with rock minerals. Examples include: Silicate + Water = clay Feldspar (found in granite) + hydrogen (found in water) = kaolin (china clay)

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11
Q

What is hydration?

A

a form of chemical weathering in which water and rock minerals form new minerals of a larger volume. This process can cause surface flaking of rocks.

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12
Q

What is biological weathering?

A

the in situ breakdown of rock that is caused by the physical actions of plants and/or animals or by organic acids (chelation)

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13
Q

What is mass movement?

A

the movement of material down a slope when the forces acting on the slope (mainly gravity) exceed the forces keeping the material on the slope (friction).

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14
Q

What is rock fall?

A

when rocks dislodge from a steep slope (40 degrees or more) and fall to the foot of the slope under gravity. This mainly occurs in areas where bare rocks are exposed to physical weathering processes.

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15
Q

What are rock slides?

A

When a section of rock or soil moves downhill. This can be Linear - in which movement is along a straight line slip plane. This often occurs between bedding planes. Rotational - movement is along a curved slip plane (also known as slumps). This is a key process in the formation of corries.

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16
Q

What is glacial erosion?

A

The action of removing rock by a glacier

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17
Q

What is plucking (quarrying)?

A

a form of glacial erosion in which meltwater seeps into joints in rock on the valley floor or sides. This then refreezes and becomes reattached to the glacier. As the glacier advances, it pulls pieces of rock away. This mainly takes place at the base of a glacier where pressure melting can take place. If the bedrock is highly jointed then this process will be particularly effective.

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18
Q

What is abrasion?

A

a form of glacial erosion in which as a glacier moves across a surface, the debris that is embedded withing it scours the rock and wears them away. Larger or more coarse material will scrape, scratch and groove the rock - forming striations. Smaller and more fine material will smooth and polish the rock.

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19
Q

What factors affect the rate of abrasion?

A
  1. Presence of basal debris
  2. Debris size and shape
  3. Relative hardness of particles and bedrock
  4. Ice thickness.
  5. Basal water pressure
  6. . Basal sliding
  7. . Movement of debris to the base of the glacier
  8. . Removal of fine debris
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20
Q

How does basal debris affect the rate of abrasion?

A

more debris increases rate of abrasion, however, it also increases amount of friction, which slows down rate of movement

21
Q

How does debris size and shape affect the rate of abrasion?

A

Larger debris is more effective in abrasion because the amount of downward pressure of an object is proportional to its weight. More angular material creates more abrasion as pressure is concentrated onto a smaller area.

22
Q

How does relative hardness of particles and bedrock affect the rate of abrasion?

A

when the bedrock is more resistant than the debris = little abrasion when the bedrock is weak and softer than the debris = maximum abrasion

23
Q

How does ice thickness affect the rate of abrasion?

A

it is a complex relationship: In general - the thicker the ice, the more pressure and therefore the more abrasion However, if pressure becomes too great then there is too much friction and no movement and therefore little abrasion

24
Q

How does basal water pressure affect the rate of abrasion?

A

if basal water is under pressure, glacial debris may not be in as much contact with the bed and so abrasion is reduced

25
Q

How does basal sliding affect the rate of abrasion?

A

The presence of some water at the base of a glacier acts as a lubricating layer. This increases the rate of movement and therefore increases the rate of abrasion

26
Q

How does movement of debris to the base affect the rate of abrasion?

A

basal debris is worn away in the process of abrasion and so must be replenished if it is to remain effective

27
Q

How does the removal of fine debris affect the rate of abrasion?

A

rock flour (fine debris) needs to be removed in order that larger particles can abrade the bedrock.

28
Q

What is rock flour?

A

the product of glacial erosion where debris is worn down into fine particles (almost dust-like). This gives meltwater its milky white appearance.

29
Q

What is nivation?

A

a complex process believed to include a combination of freeze-thaw action, solifluction, transport by water and chemical weathering. It is understood to be the main process involved in initially enlarging hillside hollows in the formation of corries.

30
Q

What is solifluction?

A

the gradual movement of wet soil or other material down a slope, especially where frozen subsoil acts as a barrier to the percolation of water.

31
Q

What is transportation?

A

The process whereby material is moved from one location to another.

32
Q

What are aeolian deposits?

A

this is fine material that is carried by wind, often blowing across outwash deposits

33
Q

What is supraglacial material?

A

debris that is carried on the surface of a glacier. It mostly originates from weathering and rockfall of valley sides

34
Q

What is englacial material?

A

debris that is carried within a glacier. It often starts as supraglacial material but is then covered by further snowfall but can also include material that falls into creavasses or sinks into the ice due to localised pressure melting.

35
Q

What is subglacial material?

A

debris that is embedded in the base of a glacier. This material is often derived from plucking and abrasion but can be englacial material that has continued to move down through the ice to the base.

36
Q

What is drift?

A

All material that has been deposited during glaciation

37
Q

What is till?

A

a subcategory of drift. This is material that is directly deposited by ice.

38
Q

What characteristics do all forms of till have?

A
  1. Angular in shape
  2. Unsorted
  3. Unstratified
39
Q

Why is till angular?

A

material has been embedded in the ice and has not been subjected to further erosion processes, particularly not meltwater, which would make the material more rounded.

40
Q

Why is till unsorted?

A

when ice melts, all sizes of material are deposited together

41
Q

Why is till unstratified?

A

when ice melts it deposits material in mounds and ridges, rather than in layers.

42
Q

What is glacio-fluvial material?

A

a subcategory of drift. This is material that is directly deposited by glacial meltwater.

43
Q

What is lodgement till?

A

This is material that is deposited by advancing ice.

44
Q

What glacial landform is commonly associated with lodgement till?

A

drumlins

45
Q

How prevalent are glacial deposits at a global scale?

A

Estimated that 8% of the Earth’s surface is covered by glacial deposits

46
Q

What is ablation till?

A

This is material that is deposited by melting ice from glaciers that are stagnant (stationary) or retreating. Most glacial depositional landforms (such including kames, eskers and moraines) are made from ablation till.

47
Q

How prevalent are glacial deposits at a European scale?

A

nearly 30% of Europe is covered in glacial deposits

48
Q

How significant are glacial deposits in East Anglia?

A

East Anglia is completely covered by glacial deposits, some of which are 143m thick. They are the reason the region has fertile soils for farming.