Glacier movement Flashcards

1
Q

What is a glacier system

A

It has interrelated components/ characteristics such as inputs/outputs

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2
Q

Define ablation

A

The output of snow/ice from a glacier by melting, sublimation or evaporation

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3
Q

Inputs of a glacier

A

Snow, ice
Precipitation, avalanches, wind deposition

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4
Q

Outputs of glacier

A

Melting, iceberg calving, sublimation, evaporation

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5
Q

What is the equilibrium line

A

The boundary between the two zones (accumulation and ablation)

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6
Q

How is glacier mass calculated

A

Year’s total accumulation - total ablation =Glacier mass balance

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7
Q

Factors that increase glacier movement

A

Ice temp
Pressure melting point is reached
Amount of meltwater

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8
Q

Types of movement for a temperate glacier x4

A

Basal slip
Creep and regelation
Extending and compressing flow
Surges

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9
Q

Types of movement for a polar glacier

A

Internal deformation- occurs when weight is ice and gravity cause the ice crystals to deform so glacier moves downhill

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10
Q

Define basal slip

A

Occurs at base of glacier when PMP is met and meltwater acts as lubricant causing glacier to Slide Over bedrock

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11
Q

Define creep and regelation

A

Basal slip is enhanced by obstacles
Creep- large obstacle causing increase in pressure. Ice deforms around obstacle
Regelation- smaller obstacle casing melting and more basal slip and re freezes further downslope.

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12
Q

Define extending and compressing flow

A

Extending flow- steep slopes causes basal slip to increase and the ice will accelerate and become thin
Compressional flow- shallower slopes basal slips slows and ice decelerated and thickens

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13
Q

Define surges

A

Short lived events where glacier dramatically advances caused by earthquakes or enhanced basal slip due to large amount of meltwater

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14
Q

Factors which accelerate glacier movement x6

A

Ice thickness- thicker more pressure/movement
Precipitation level- more accumulation/faster movement
Rate of ablation- more meltwater more movement
Bedrock permeability- bedrock permeable able to soak away slowing movement
Ice/slope gradient- steeper angle more movement
Ice temperature- warmer faster

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15
Q

Ñame glacial processes x4

A

Erosion
Entrainment- rock fragments trapped by basal ice causing them to be dragged
Transport- rock debris transported on ice surface
Deposition- till deposited by glacier ice

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16
Q

Size of glacial landforms

A

Micro scale- small
Meso scale- medium roches, drumlins
Macro scale- large troughs, pyramidal peaks

17
Q

Name glacial environments x4

A

Subglacial- environment beneath glacier
Ice marginal- environment edge of glacial
Pro glacial- environment at front of glacier
Periglacial- environment near glacier

18
Q

Name glacial landscapes x4

A

Upland
Lowland
Active
Relict