5. Periglacial landscapes, processes and deposits Flashcards

1
Q

What does periglacial mean?

A

Domain of frost climate

● Strict sense: effects of ground frost
● Broader sense: also other processes influenced by frost climate (e.g. loess formation)

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2
Q

What is permafrost?

A

Rock or soil frozen for at least 2 years.

Dry permafrost → little geomorphic effect; e.g. cold bedrock.

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3
Q

What is the active layer of the permafrost?

A

freezing/thawing cycles

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4
Q

What is cryoplanation?

A

Formation of flat land surfaces under the influence of periglacial processes

Disintegration of solid rock into coarse congelifracts → boulder fields (e.g. Scottish Highland) without erratics (the boulders
are formed in situ and not brought here by glaciers!)

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5
Q

What is a rock glacier?

A
  • In high mountains
  • Tongue-shaped frozen debris masses
  • Ice inside, but not glacier ice
  • Movement due to slow deformation of ice core, up to 3 m/a.
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6
Q

What is cryoturbation?

A

Cryo = ice, turbation = deformation

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7
Q

What does different grain sizes and different water content mean?

A

different rates of freezing

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8
Q

What is solifluction?

A

Downslope (2º enough!), slow creep of soil over permafrost

High water saturation of the active layer → reduction in shear strength → flow

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9
Q

What are frost fissures and ice wedges?

A

Ice wedges:

rapid freezing of dry soil
→ soil contraction, cracks in polygonal pattern
→ water enters in thaw period and may re-freeze
→ cracks cannot close

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10
Q

What is an epigenetic ice wedge?

A

In already existing permafrost;
Younger than the surrounding material;
Crack in the centre, do not grow downward

New wedges down in cracks in the centre of older wedges

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11
Q

What is a syngenetic ice wedge?

A

Grow parallel with sediment accumulation
Oldest ice at the bottom

Looks like a reverse Christmas tree where triangles haven’t been erased

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12
Q

What is an anti-syngenetic ice wedge?

A

When erosion removes sediment
They grow downward
Oldest ice is on the outside

Gets deeper each time, but also thinner

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13
Q

What can cause patterned ground?

Polygons and/or sorted polygons (stone rings)

A

Development of ice wedges (they develop in a certain geometric way)

Periglacial freeze-thaw processes

Stone rings by ice lenses

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14
Q

What is a pingo?

A

Eskimos for “small hill”

Single ice-cored hillocks with a round base up to 1200 m diameter, height up to 100 m, steep slopes.
Ice core with soil around.
Typically occur on flat surfaces.

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15
Q

What is a talik?

A

Unfrozen soil

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16
Q

What are the two types of pingos?

A

Mackenzie-type (closed hydrological system)
East Greenland type (open hydrological system)

17
Q

What is a palsa?

A

Local frost heaving on mires
Much smaller than pingos
Caused by differential snow cover in winter

18
Q

What is thufur?

Icelandic word

A

Small earth hummocks up to 0.5 m high, in fine-grained sediment.
Contain cryoturbations.
Origin unclear, possibly differential frost penetration due to vegetation.

19
Q

What is “growing” stones?

A

Stone movement during freeze-thaw

As soon as the stone is grasped by freezing soil, it’s lifted up.
The ice melts and the soil collapses a bit - but softer material (sand, silt) has moved into the depression where the stone used to be