periglacial processes Flashcards

1
Q

What is a periglacial environment?

A

exist at the edges of glacial / polar environments and cover 20% of earth’s land surface

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2
Q

what are the three characteristics of periglacial environments?

A

1) Found on the edges of glacial / polar environments - alaska / russia / Northern Europe
2) No permanent covering of ice - do experience cold for most of year (frost) with periodic snow
3) Permafrost is one key feature of periglacial environments

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3
Q

Whats the permafrost?

A

Where a layer of sediment, soil or rock below the ground remains frozen for 1 year+

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4
Q

Whats the active layer?

A

The layer above the permafrost that thaws in summer and refreezes again in winter.

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5
Q

What is a talik?

A

A layer of unfrozen ground that is surrounded by permafrost due to anomaly in thermal conditions.

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6
Q

What is continuous permafrost?

A

A continuous sheet of frozen material which extends without any breaks→ found in Siberia Russia - higher latitudes

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7
Q

What is discontinuous permafrost?

A

Is permafrost that is broken up into separate areas → Hudson bay Canada - warmer regions

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8
Q

What is sporadic permafrost?

A
  • Found when mean annual temperature is just below 0

the summer temperatures reach several degrees above

isolated pockets of permanently frozen ground remain below the surface.
Lower latitudes - prevent complete thawing

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9
Q

What is frost action ?

A
  • Leads to the accumulation of angular rocks at the foot of a mountain slopes or a boulder strewn landscapes
  • Cracks in the ground formed by winter contraction become filled with water during the day
  • Water freezes and expands - enlarges the crack
  • Over many years an ice wedge is formed up to 3m x 10m
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10
Q

What is a soliflucation?

A
  • The water in the upper active layer melts leading to soil becoming saturated
  • If on a slope causes the downhill movement of top layer of soil under force of gravityAKA Gelifluction
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11
Q

rockfalls

A
  • Result from freeze thaw action
  • Scree slopes are a common feature of periglacial environments
  • On flat land extensive areas of angular boulders can be left known as block fields
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12
Q

Nivation

A

Snow collects in hollows especially on north facing slopes

With increase amount of weight if the ice begins to disintegrate the underlying rock

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13
Q

Frost Heave

A

A subsurface process that leads to vertical sorting of material in the active layer.

  • Stones within finer material heat up and cool down faster than their surroundings as have lower heat capacity
  • Temperatures fall water beneath the stones freeze and expand pushing the stones upwards to the surface
  • Ground ice also pushes up finer material
  • Warm season → thawing causes ice to convert back to water and the contracting surface drops particles in elevation → this is influenced by gravity causing for particles to move downslope
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