Ice on the Land & Water on the Land Key Terms

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Hydraulic Action
The sheer force of the water hitting the bed and banks.
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Abrasion
The load of the river is carrying repeatedly hits the river bed and the banks, causing some of the material to break off.
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Attrition
The stones and boulders carried by the river knock against each other and over time are weakened, causing bits to fall off and reduce in size.
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Solution
Occurs only when the river flows on certain types of rock, such as chalk and limestone; these are soluble in rainwater and become part of the water as they are dissolved by it.
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Traction
The method used for moving the largest material. This is too heavy to lose contact with the bed so material such as boulders are moved along.
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Saltation
Moves the small stones and grains of sand by bouncing them along the bed. This lighter load leaves the river bed in a hopping motion.
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Suspension
A means of carrying very fine material within the water so that in floats in the river and is moved as it flows.
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Deposition
The river dumps or leaves behind material that it has been carrying.
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Long profile
This shows how the river changes in height along its course.
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Meander
A bend or curve in the river channel.
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Interception
Water being prevented from reaching the surface by trees or grass.
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Surface Storage
Water held on the ground surface eg. puddles.
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Infiltration
Water sinking into soil/rock from the ground surface.
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Soil moisture
Water held in the soil layer.
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Percolation
Water seeping deeper below the surface.
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Groundwater
Water stored in the rock.
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Transpiration
Water lost through pores in vegetation.
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Evaporation
Water lost from ground/vegetation surface.
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Surface run-off
Water flowing on top of the ground.
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Throughflow
Water flowing through the soil layer parallel to the surface.
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Groundwater flow
Water flowing through the rock layer parallel to the surface.
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Water table
Current upper level of saturated rock soil where no more water can be absorbed.
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Accumulation
Inputs to the glacier budget, such as snowfall and avalanches.
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Ablation
Outputs from the glacier budget such as melting.
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Snout
The front of a glacier.
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Glacier budget
The balance between the inputs and outputs of a glacier.
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Abrasion
A process of erosion involving the wearing away of the valley floor and sides.
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Plucking
A process of glacial erosion where individual rocks are plucked from the valley floor or sides as water freezes them to the glacier.
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Rotational Slip
Slippage of ice along a curved surface.
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Moraine
Sediment carried and deposited by ice.
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Bulldozing
The pushing of deposited sediment at the snout by the glacier as it advances.
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Hummock
A small area of raised ground, rather like a large molehill.
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Corrie
A deep depression on a hillside with a steep back wall, often containing a lake.
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Arete
A knife-edged ridge often formed between two corries.
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Pyramidal Peak
A sharp-edged mountain peak.
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Glacial Trough
A wide, steep-sided valley eroded by a glacier.
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Truncated Spur
An eroded interlocking spur characterised by having a very steep cliff.
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Hanging valley
A tributary glacial trough perched up on the side of a main valley, often marked by a waterfall.
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Ribbon Lake
A long narrow lake in the bottom of a glacial trough.
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Lateral Moraine
A ridge of frost-shattered sediment running along the edge of a glacier where it meets the valley side.
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Medial Moraine
A ridge of sediment running down the centre of a glacier formed when two lateral moraines merge.
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Terminal Moraine
A high ridge running across the valley representing the maximum advance of a glacier.
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Drumlin
An egg-shaped hill found on the floor of a glacial trough.
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Other cards in this set

Card 2

Front

The load of the river is carrying repeatedly hits the river bed and the banks, causing some of the material to break off.

Back

Abrasion

Card 3

Front

The stones and boulders carried by the river knock against each other and over time are weakened, causing bits to fall off and reduce in size.

Back

Preview of the back of card 3

Card 4

Front

Occurs only when the river flows on certain types of rock, such as chalk and limestone; these are soluble in rainwater and become part of the water as they are dissolved by it.

Back

Preview of the back of card 4

Card 5

Front

The method used for moving the largest material. This is too heavy to lose contact with the bed so material such as boulders are moved along.

Back

Preview of the back of card 5
View more cards

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