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Geography Edquadus > 1 > Flashcards

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1
Q
A
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2
Q

UNIT 3
What is weathering?

A

Breakdown of rock, in situ

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3
Q

UNIT 3
What are the two processes of weathering

A

Physical processes and chemical processes

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4
Q

UNIT 3
What is erosion

A

Removal of rock by ice, water, wind or gravity

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5
Q

UNIT 3
What are two types of weathering?

A

Freeze thaw / frost shattering, dilatation

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6
Q

UNIT 3
Explain freeze thaw weathering

A

Water enters a crack in a rock, the temperature fluctuates on either side of 0 degrees Celsius. Water freezes and expands by 9% in volume. Putting pressure on rock, after repeated cycles the rock splits

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7
Q

UNIT 3
What impacts freeze thaw weathering?

A

Geology of rock (more porous (absorption)/ bedding (gaps in formation)
Climate - temperature must be able to fluctuate between 0 degrees Celsius
Altitude - decrease in temp higher up
Aspect - Orientation of rock, North vs Southern hemisphere

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8
Q

UNIT 3
What is an example of freeze thaw?

A

Summit of Glyder Fawr

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9
Q

UNIT 3
Explain dilatation

A

Rocks fracture parralell to pressure when the pressure is released (glacier melts). Rocks expand and fracture fue to the pressure release. Called pressure relase or unloading.

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10
Q

UNIT 3
What are three erosional processes?

A

Abrasion, Plucking, Sub-glacial meltwater erosion.

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11
Q

UNIT 3
Explain abrasion

A

Weathered rocks are embedded as sub glacial debris (under glacier), this scrapes away at rock. Large pieces of rock cause scratches and striations, while fine particles cause smoothing an polishing (like sandpaper). When the debris gets worn away it turns into rock flour.

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12
Q

UNIT 3
What are the factors effecting abrasion?

A

Ice thickness - thicker ice causes more erosion due to higher pressure, but too thick and the glacier becomes hard to move
Subglacial meltwater - Increases speed of glacier, but too much lubricant means the glacier will not erode
Relative hardness/resistance of debris and bedrock - if bedrock is harder there will be less erosion, weak debris turns into rock flour
Shape of debris - angular debris causes striations and cracks, fine sand and clay smooth and polish
Supply of debris - More debris causes more erosion, but it depends on the type of debris. Too much causes lower speed
Speed of glacier - Fast movement causes more erosion up to a point - too fast causes less erosion

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13
Q

UNIT 3
Explain plucking

A

meltwater seeps into cracks in the rock, it refreezes, when the glacier moves to rock is plucked from the bedrock, causing the entrapment of rocks

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14
Q

UNIT 3
Plucking also occurs in what movement?

A

Regelation slip

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15
Q

UNIT 3
What is sub glacier meltwater erosion?

A

Meltwater channels under glacier, high velocity causes erosion at the glacier’s bed and the widening and deepening of channels

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16
Q

UNIT 3
What does plucking need to occour?

A

fractures in bedrock, resistant obstacles and meltwater

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17
Q

UNIT 3
What is an example of sub-glacial meltwater erosion?

A

Gwaun valley, North Pembrokeshire (South Wales)

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18
Q

UNIT 3
How does sub-glacial meltwater occour?

A

Increase of meltwater in summer, water flows into cracks and forces rocks out (hydraulic action).
Rocks grind and scrape rock (abrasion)
Ricks bounce around, making them rounder (attrition)
Chemicals in rock release minerals (corrosion)
Lateral erosion and vertical erosion find path of least resistance

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19
Q

UNIT 3
Why are sub-glacial meltwater channels powerful?

A

Ice adds pressure, increasing hydrostatic pressure and velocity

20
Q

UNIT 3
Why do sub-glacial meltwater channels have different discharge patterns to normal streams?

A

discharge comes from ablation in winter, movement is based on topography and movement of ice

21
Q

UNIT 3
What is a Macro landform?
What is a meso landform
What is a micro landform

A

Macro - big 1km+
Meso are often found in macro landforms
Micro are the smallest and often a few m

22
Q

UNIT 3
What is a cirque/cwm/corrie
Macro/Meso/Micro?
Case study

A

A large bowl shaped hollow, found at the head of a valley glacier.
Macro
Cwm coch

23
Q

UNIT 3
How are cirques/cwm/corrie formed

A

on North facing slopes in winter, small hollows freeze thaw weathering occurs. in summer meltwater removes the debris, enlarging the hollow, called nivation. Firn compacts into ice.

Accumulation results in rotational movement of ice, meltwater from pressure melting adds to this effects, this movement causes stage 2.
Ice rotates, removing fragments from the back wall via plucking, causing a steep, jagged backwall. Rock fragments cause ablation on the hollows floor, deepening the corrie. Crevasses, called bergschrunds add meltwater, causing more rotational movement. Pressure release causes dilation cracks to form, weakening the floor of the glacier, aiding erosion. Glacier begins to moves over the lip of the corrie and out of the rock basin. with abrasion on the stoss side and plucking on the lee side.

24
Q

UNIT 3
What orientations are cirques. Why?

A

Northern hemisphere corries face north east. Receives the least amount of insolation (lower temperatures), meaning firn can form

25
Q

UNIT 3
What is a rose diagram?

A

Circular histogram, showing directional data and frequency

26
Q

UNIT 3
What is a Arete? How are they formed?
Macro/Meso/Micro?
Case study

A

Sharp, knife edge ridge, produced by two corries eroding back to back towards each over (or two glacial troughs).
Macro
Gribin ridge

27
Q

UNIT 3
What is a Pyramidal Peak? How are they formed?
Macro/Meso/Micro?
Case study

A

Three or more corries erode, the remaining central area becomes sharp and steeper due to frost shattering.
Macro
Glyder Fawr - Snowdonia

28
Q

UNIT 3
What is a Glacial Trough? How are they formed?
Macro/Meso/Micro?
Case study

A

A U shaped valley, formed when glaciers flow into a pre-existing v shaped river valley. Home to a misfit river
Macro
Nant ffrancon Valley

29
Q

UNIT 3
What is a Truncated spur? How are they formed?
Macro/Meso/Micro?
Case study

A

steep cliff face in a glacial trough. In a pre existing river valley interlocking spurs occour, as the river erodes the path of least resistance. As the glaicer moves dont the valley these interlocking spurs are eroded.

30
Q

UNIT 3
What is a Hanging valley? How are they formed?
Macro/Meso/Micro?
Case study

A

A smaller U shaped valley joins a larger glacier. because the small glacier erodes less vertically it is hanging above the larger glacier. May have waterfalls.
Macro

31
Q

UNIT 3
What is a Ribbon lakes? How are they formed?
Macro/Meso/Micro?
Case study

A

Long, narrow lake found in glacial troughs. Glacier moves over alternating band of hard and soft rock. The glacier erodes the softer rock more then the hard rock. The outcrops of hard rock are called rock bars/steps. rainwater accumulates, creating a lake.
Macro
Llyn Ogwen - ribbon lake
Ogwen step - rock step

32
Q

UNIT 3
What is a Roche Moutonnees? How are they formed?
Macro/Meso/Micro?
Case study

A

Resistant rock that is smooth on one side and rigid on the other. Formed during regulation slip, with abrasion on the stoss side and plucking on the lee side.
Meso
Pen y Benglog - on Ogwen step

33
Q

UNIT 3
What is a Crag and tail? How are they formed?
Macro/Meso/Micro?
Case study

A

An steep wall of rock followed by a gentle slope. Resistant rock protects softer rock behind it, forming a gently sloping tail on lee side and a steep side, which has plucking and abrasion occur.
Meso
Edinburgh castle

34
Q

UNIT 3
What is a Striations? How are they formed?
Macro/Meso/Micro?
Case study

A

long scratches on bedrock, from abrasion
micro
Found on Roche Mountonees in Nant Ffrancon valley

35
Q

UNIT 3
What is a Chatter marks? How are they formed?
Macro/Meso/Micro?
Case study

A

small intermittent chips from abrasion, ice is not in continuous contact with rock.
Micro
Found on Roche Mountonees in Nant Ffrancon valley

36
Q

UNIT 3
What is a polished rock? How are they formed?
Macro/Meso/Micro?
Case study

A

sand, silt and clay (fine particles) polish rock surface, from abrasion.
Micro
Found on Roche Mountonees in Nant Ffrancon valley

37
Q

UNIT 3
How many cirques surround the Nant Ffrancon valley? What direction do they face?

A

7, North east

38
Q

UNIT 3
What does the Gribin Ridge (Arete) separate

A

Two cirques, cwm cneifion and cwm bochlwyd

39
Q

UNIT 3
How tall is Glyder Fawr? What type of weathering occurs at the top because of its height?

A

1001m, freeze thaw weathering

40
Q

UNIT 3
How long and deep is Nant Ffrancon Valley

A

700m deep and 5km long

41
Q

UNIT 3
What landforms also occour in Nant Ffrancon valley?

A

Roche Mountonees, truncated spurs, hanging valleys and misfit river (Afon Ogwen)

42
Q

UNIT 3
How long and wide is Llyn Ogwen? How was it formed?

A

1..5km long and 350m wide. Formed by Ogwen glacier

43
Q

UNIT 3
How tall is the Edinburgh Crag and Tail? What type of rock was it made from?

A

130m tall. Igneous rock

44
Q

UNIT 3
How is a rock step formed?
Case Study

A

a change in geology, band of hard rock and band of soft rock. Glacier does not erode hard rock but erodes soft rock, causing a drop in altitude.
Ogwen step

45
Q

UNIT 3
How much of a drop is Ogwen step?

A

170m

Geography Edquadus (4 decks)

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