Reconstruction Of Past Glaciers Flashcards

1
Q

Types of linearity

A

Linear
Damped
Non-linear
Threshold

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2
Q

When was the Holocene?

A

12,000 years ago. Last interglacial. Experienced 10 degrees of cooling.

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3
Q

Potential causes of cooling?

A

Milankovitch
Formation of mountains causing feedback
Changing ocean circulation.

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4
Q

What is eccentricity?

A
100,000 year cycle. 
How eliptical earths orbit is. 
Maximum difference 30% more radiation. 
Matches with glacial/interglacial cycles 
- 10,000 interglacial. 90,000 glacial.
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5
Q

What is obliquity?

A
41,000 year cycle.
Tilt of the earth. 
Maximum tilt 24 degrees. 
Minimum 21 degrees. 
Influences seasons
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6
Q

What is Precession?

A

19/27,000 year cycle.

Earths wobble.

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7
Q

Geomorphological fingerprints show:

Landforms that can be used to reconstruct past glaciers are:

A

Ice extent
Ice flow
Thermal regime

Moraines - indicate ice volume and past extent.

Thermal regime showed through landscape unmodified landscape = cold based ice as slow moving.
Highly eroded landscape = warm based.

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8
Q

Case Study of unmodified landscape.

A

Gamburtsev mountains - East Antarctica.
2,500 meters of ice rumoured birth place of Antarctic ice sheet yet very young mountain range.
Cold based, slow moving ice preserved the landscape.

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9
Q

Small scale case Study for mapping past extent of glaciers.

A

Kea Point, New Zealand.

Mapping of past moraines shows extent of Mueller glacier. Contextualises retreat rates.

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10
Q

Case Study for reconstructing past glaciers.

A

Brit Ice Project (Clark 2004).
Reconstructed ice streams and ice sheet extent across UK.
Used ice cores to get precipitation data to see how the ice sheet responded to changes.

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11
Q

Thermal regime indicates how ice masses behave.

A

Cold based vs warm based

Cold based preserve landscapes. 
Case Study:
Gamburtsev mountains - East Antarctica. 
2,500 meters of ice rumoured birth place of Antarctic ice sheet yet very young mountain range. 
Cairngorms, Scotland. (Glasser, 2007). 
- unmodified.
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12
Q

2 Types of dating

A

Absolute - gives age in calendar years.

Relative - oldest at the bottom.

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13
Q

Dating techniques

A

Cosmogenic nuclides - cosmic rays absorbed in rocks when exposed to sunlight. More cosmic rays = longer exposure to sunlight.
Radiocarbon dating - reconstructs ice sheets in Antarctica. C14.

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