Moraines Flashcards

1
Q

What do end moraines mark?

A

The ice marginal position

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2
Q

When the moraines are at the side of the glacier they’re called

A

lateral moraines.

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3
Q

You can tell if a moraine has lots of ice in it because…

A

it’s covered in debris- ice is protected by debris so can last for a long time (can’t tell you of age therefore).

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4
Q

Glacier advance

A

Positive mass balance

Can advance over previous moraines

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5
Q

Glacier in balance

A

Glacier stay in one position and build up a large moraine

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6
Q

Glacier retreat

A

Leave a series of moraines marking it’s retreat.

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7
Q

End moraines general term for moraines that

A

Surround the glacier

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8
Q

End moraines are formed by…

A

Melt (dump)
Freezing on
Push

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9
Q

Melt-out Moraines

After a few years…

A

As a glacier melts out the debris will avalanche down the front, collecting, and forming an apron down the front (supra glacial source).
Subglacial/englacial source

they become vegetated and stablished- becomes harder for them to be washed away.

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10
Q

Freezing on

A

Underlying sediments are freezed on.

In summer this will be melted out, forming a moraine.

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11
Q

Push moraines

A

Another way in which moraines are formed is when there is some kind of subglacial source being pushed underneath towards the front, pushing up the sediment beneath it.
In this example the glacier is completely clean at the front (must have come from beneath).

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12
Q

Glaciotectonics

Proglacial deformation

A

Deformation in front of glacier

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13
Q

Compressed is…

Extended is…

A

Negative

Positive

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14
Q

Styles of deformation

A

Open folding and nappes (ductile deformation)- where something is pushed and ‘bends’

Listric thrust faulting (brittle deformation)

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15
Q

Faulting

A

Sometimes the sediment is too strong- instead of bending it snaps.

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16
Q

Push Moraine formation

A

Bulldozed push moraines- frontal pushing

Deforming bed push moraines- frontal pushing + lateral stresses transmitted through the deforming mass

17
Q

Landsystems

A

Facies = individual sedimentary deposits

Facies assemblage/sediment landform association = facies laid down next to each other or in a vertical sequence

Landsystem = Large scale groupings of facies deposited in same environment plus erosional landforms from same time

18
Q

Hard bed rock glacier

A

Low debris supply- alpine

19
Q

High debris supply - Ghulkin-type

A

They have so much debris because of being formed in new tectonic areas
Big contrast in summer and winter temperatures
Can dam

20
Q

Soft bed rock glacier

A

Marginal ice sheet

Typically a series of push moraines, stagnant ice till underneath the glacier

21
Q

Push moraines are only formed by glaciers that…

A

have retreated and then advance again.

22
Q

The existence of a push moraine is usually evidence of…

A

the climate becoming poorer after a relatively warm period.

23
Q

Why are there characteristic differences in the orientation of rocks within a push moraine?

A

Material that had already been deposited is shoved up into a pile as the ice advances, and because most moraine material was deposited by falling down not pushing up, there are characteristic differences in the orientation of rocks within a push moraine.