Periglacial Shite Flashcards

(25 cards)

1
Q

What are the 3 types of permafrost?

A

Continuous
Discontinuous
Sporadic

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2
Q

What is continuous permafrost?

A

Found in coldest regions
Little thawing in Summer
-5 to -50 degrees
Up to 700m in Canada

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3
Q

What is discontinuous permafrost?

A

Slightly warmer conditions
Breaks in permafrost under lakes, rivers, sea etc
20-30m avg
-1.5 to -5 degrees

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4
Q

What is sporadic permafrost?

A

Mean annual temp. just below freezing
Permafrost occurs in isolated spots
Local climate cold enough to prevent complete thawing
0 to -1.5 degrees

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5
Q

What is permafrost?

A

Layer of soil, sediment, or rock below surface remains permanently frozen

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6
Q

What is the active layer?

A

Topsoil in permafrost environments
Thaws in summer
Freezes in winter

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7
Q

Which factors influence prescence of permafrost?

A

Rock + soil types (Depth)
Vegetation (Insulation)
Snow cover
Slope angle (Solar radiation)
Proximity to water bodies

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8
Q

List periglacial processes

A

Freeze thaw
Nivation
Frost heave
Groundwater freezing
Solifluction
Meltwater erosion

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9
Q

List periglacial landforms

A

Nivation hollows
Patterned ground
Ice wedges
Pingos
Solifluction lobes
Braiding
Scree
Loess

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10
Q

Which landform does freeze thaw create?

A

Scree

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11
Q

Which landform does nivation create?

A

Nivation Hollow

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12
Q

Which landform does frost heave create?

A

Patterned ground
Some pingos

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13
Q

Which landform does groundwater freezing create?

A

Pingos

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14
Q

Which landform does solifluction create?

A

Solifluction lobes

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15
Q

Which landform does meltwater erosion create?

A

Braiding

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16
Q

How is a nivation hollow created?

A

Snow falls into hollow/depression
Protected from wind + sun
Compaction by further snowfall
Underlying rocks weakened + eroded

17
Q

How is a solifluction lobe created?

A

Active layer thaws
Meltwater reduces friction between soil particles
AL moves downslope
Rounded tongue like features form terraces in valley

17
Q

What is gelifluction?

A

Combination of solifluction with frost heave and permafrost

18
Q

How is patterned ground created?

A

AL freezes, ice lenses develop
Soil volume rises + forced upwards
Frost heave - fine grain soil expands unevenly
Stones heat up faster than ground, cool + expand when ground freezes
Freeze thaw, crystals heave rocks upwards

19
Q

How is an ice lens created?

A

Soil moisture becomes free
Lens develops
Fed by water from capillary action + movement through frost susceptible soil
Lens expands, land lifts + heaves

20
Q

What are the 2 types of pingo?

A

Open system
Closed system

21
Q

How is a pingo formed?

A

Groundwater freezes into ice lens
Lens trapped within layers of land
Lens forces overlying land + sediments upwards

22
Q

What is the difference between the 2 types of pingo?

A

OS - Water able to seep through permafrost
CS - Water unable to seep through frozen ground

23
Q

How is an ognip created?

A

Pingo grows overly large
Lens exposed
Lens melts
Pingo collapses

24
How is an ice wedge created?
AL freezes in winter Soil contracts Surface cracks Cracks fill with water Freeze thaw