basal sliding and internal deformation Flashcards

1
Q

what do warm based glaciers mainly move by

A

basal sliding

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2
Q

when will basal sliding occur

A

when basal temperatures are at or above the pressure melting point, generating a thin layer of meltwater between the glacier and the valley

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3
Q

what three mechanisms does basal sliding consist of

A

creep, slippage, or bed deformation

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4
Q

what is slippage

A

when the ice glides over the valley floor due to meltwater reducing friction

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5
Q

what is creep

A

when ice deforms, in a rather similar way to how plastic would, under increased pressure from an obstruction on the valley floor

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6
Q

what is bed deformation

A

when ice is carried by saturated sediments on the valley floor over a gentle gradient

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7
Q

what is an example of a glacier that moves frequently

A

the Franz Josef glacier in New Zealand moves around 300m per year

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8
Q

why do cold based glaciers never move by basal sliding

A

cold based glaciers never move by basal sliding because the basal temperature is always below pressure melting point

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9
Q

how does ice in a warm based glacier deform compared to ice in a cold based glacier

A

ice at 0 degrees deforms 100x faster than ice at -20 degrees

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10
Q

how do cold based glaciers move

A

internal deformation

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11
Q

what are the two aspects of internal deformation

A

intergranular flow

laminar flow

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12
Q

what is intergranular flow

A

when individual ice crystals move and reorientate around eachother

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13
Q

what is laminar flow

A

the movement of layers within an ice sheet- often layers of annual accumulation

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14
Q

what is fundamentally required for internal deformation

A

a gradient- internal deformation can only take place where there is at least some slope

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15
Q

give an example of an ice sheet that moves by internal deformation and how much does this move by every year

A

the merserve glacier in antarctica only moves by 3-4 m every year and this is entirely by internal deformation

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16
Q

what is another way in which ice can move

A

extending flow

17
Q

what is extending flow

A

when ice moves over a steep slope and is unable to deform quick enough and so fractures, forming crevasses