Periglacial Shite Flashcards

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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
Q

How is an ice wedge created?

A

AL freezes in winter
Soil contracts
Surface cracks
Cracks fill with water
Freeze thaw