Module 11 Flashcards

Periglacial Environments

1
Q

permafrost

A

rock or soil material that has remained below 0 degrees for two or more years. the upper surface thaws in the summer and is considered the active layer

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2
Q

why is permafrost important to canadians

A

40% land underlain by permafrost. 10-15% of Earths total land area

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3
Q

periglacial environments

A

areas/regions where landforms and geomorphic processes are influenced by seasonal thawing and freezing, often in areas of permafrost

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4
Q

distribution of permafrost in high latitude areas (arctic regions)

A

continuous permafrost, up to 700 m thick

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5
Q

temp required for continuous permafrost

A

annual air temps <-7 degrees

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6
Q

distribution of permafrost towards south (south of tree line)

A

discontinued, thins to only a few metres, patchy and sporadic

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7
Q

temp required for discontinuous permafrost

A

mean annual air temps >-7 degrees

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8
Q

ground ice

A

frozen moisture below earth’s surface. varies from small amount in pore spaces to large ice bodies

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9
Q

ways ground ice forms

A

pingo ice, ice wedges, polygonal ground

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10
Q

pingo ice

A

relatively clear permafrost, occurs horizontally or in lens-shaped masses. 3-54m in height and 30-450 in diameter.

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11
Q

largest pingo in NA

A

Ibyuk pingo of Tuktoyaktuk in Northwest Territories

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12
Q

ice wedges

A

permafrost formed in large ice wedges of masses with parallel or subparallel foliation. Foliated ice occurs as wedges, vertical or inclined sheets. 2.5cm-3m high, and 0.3 to 9m diameter.

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13
Q

polygonal ground

A

micro-relief pattern on the ground where ice wedges are below the polygons. they are indicative or periglacial environments. each mound is less than 1 m but they cover thousands of metres in the Arctic

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14
Q

causes of melting of the ice

A

erosion of stream banks, and the process thermokarst

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15
Q

thermokarst

A

erosional process unique to permafrost. process by which characteristics landforms results from the thawing of ice-rich permafrost and/or melting of massive ice

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16
Q

what does thermokarst cause

A

decreases the stability of the ground, landslides, thaw lakes, ground subsidence (road disturbance and house collapse), and freeze-thaw process

17
Q

freeze-thaw process

A

water expands by 9% when frozen which can fracture rocks. it produces frost-shattered screes.

18
Q

ice growth

A

occurs preferentially below stones in soil and forms pipraker. ice lifts stones/soil (frost heaving)

19
Q

pipraker

A

needle ice

20
Q

what does heaving produce

A

stone polygons and stone stripes

21
Q

slope processes

A

active layer has high water pressures, so it is prone to mass movement and solifluction lobes/terraces. there is a slow downslope movement of soil (couple cm/yr)

22
Q

creep

A

very slow rates of movement (<5mm/year) but can affect the stability of built structures such as pipes

23
Q

what gasses does permafrost release

A

carbon dioxide and methane