Geomophic Processes / Landscape Flashcards

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1
Q

Geomorphic

A

Relating to the form of landscape and other natural features

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2
Q

Three areas that have important impacts on Geomorphic processes

A
  • climate
  • geology
  • human activity
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3
Q

What is weathering?

A

The breaking down of rocks in situ (in one place)

this affects the surrounding area which in turn affects the process.

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4
Q

Mechanical (Physical) weathering

A

Freeze thaw weathering (Frost shattering)
- prominent in the UK
Exfoliation (onion skin weathering)
- from the heat so found more in desert areas.

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5
Q

Chemical weathering

A

Geology will affect it as some rocks are more susceptible and will be affected more.
Acid rain is often a cause for chemical weathering.

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6
Q

Biological weathering

A

This is, perhaps, less significant. Plant roots grow in rocks and break them up. Sometime burrowing animals can have an affect.

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7
Q

Solution/Corrosion

A

Acid water eroding coastlines

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8
Q

Hydraulic Action

A

Water forces into crack, gets pushed in, crack expands etc.

Can happen if air is forced in too.

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9
Q

Attrition

A

More for the sediment and load as they hit each other and this makes the peddles smooth.

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10
Q

Corrasion/Abrasion

A

Load and sediment in the water erodes the bed like sand paper.

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11
Q

Glacial erosion

A

Abrasion

Plucking (freeze thaw weathing weakens the rock then the glacier plucks it away.

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12
Q

Solution (Transportation)

A

Minerals are dissolved in the water and carried along.

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13
Q

Suspension

A

Fine material carried along in the water.

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14
Q

Saltation

A

Small pebbles and stones bounce along the river bed.

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15
Q

Traction

A

Large boulders and rocks are rolled along the river bed.

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16
Q

Constructive waves

A

Strong swash and weak backwash.
Low frequency.
Wave energy dissipates over a wide area.

17
Q

Destructive waves

A

Big, strong waves when the wind is powerful and has been blowing for a long time.
Energy is high and the wave has travelled over a long fetch.
Stronger backwash than swash.

18
Q

Longshore drift

A

Due to the wind the waves come in sideways, then go out straight. This causes the beach material to be pushed up the beach.
Demonstration of transportation. But leaves the coastal areas open to erosion.

19
Q

Supraglacial

A

Glacial transportation on top of the glacier.

20
Q

Englacial

A

Transportation inside the glacier.

21
Q

Subglacial

A

Transportation under the glacier.

22
Q

Deposition

A

Material that was being transported is dropped.

23
Q

Headlands and Bays

A

Formed based on rock types.
Hard rock is not eroded as easily as soft rock, which means they stick out into the sea causing cliff, whereas, soft rock is eroded faster and forms bays.

24
Q

Glacial landforms

A

Tend to form together.
Corries, Aretes and Pyramidal peaks.
Glaciers form and carve out the side (corries) leaving a jaged sticking up summit with little material around it (pyramidal peak).
Arete = sharp mountian ridge.

25
Q

Meanders

A

Happens in a lateral erosion period, with both erosion and deposition.
Rivers try to take the fastest route but if they hit an obstacle like hard rock, they will start to bend around it.
The outside bend will have the fastest flow so erode and the inside bend will be slower, leading to deposition.

26
Q

Jurassic Coast, Dorset examples

A

Old harrys rock

  • Headland of chalk
  • Cave - arch (less vulnerable to erosion but more vulnerable to weathering)
  • stack (old harry - vulnerable to sea on all sides)
  • stump (old harrys wife)

Lulworth cove
- Coastal and fluvial erosion

Durdle door

Chesil beach

  • Tombolo
  • Constructive waves
  • Deposited by size = sediment sorting process
27
Q

River Derwent, Cumbria examples

A

Meanders at cockermouth

Taylor gill force 
- Waterfall 
- Hard rock over soft rock 
- Erodes soft rock rapidly 
= overhang and plunge pool 
= overhang eventually drops off + causes more erosion 

Floodplains, Workington
- Usually fertile + flat