Module 11 Flashcards
Periglacial Environments
permafrost
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
why is permafrost important to canadians
40% land underlain by permafrost. 10-15% of Earths total land area
periglacial environments
areas/regions where landforms and geomorphic processes are influenced by seasonal thawing and freezing, often in areas of permafrost
distribution of permafrost in high latitude areas (arctic regions)
continuous permafrost, up to 700 m thick
temp required for continuous permafrost
annual air temps <-7 degrees
distribution of permafrost towards south (south of tree line)
discontinued, thins to only a few metres, patchy and sporadic
temp required for discontinuous permafrost
mean annual air temps >-7 degrees
ground ice
frozen moisture below earth’s surface. varies from small amount in pore spaces to large ice bodies
ways ground ice forms
pingo ice, ice wedges, polygonal ground
pingo ice
relatively clear permafrost, occurs horizontally or in lens-shaped masses. 3-54m in height and 30-450 in diameter.
largest pingo in NA
Ibyuk pingo of Tuktoyaktuk in Northwest Territories
ice wedges
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.
polygonal ground
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
causes of melting of the ice
erosion of stream banks, and the process thermokarst
thermokarst
erosional process unique to permafrost. process by which characteristics landforms results from the thawing of ice-rich permafrost and/or melting of massive ice
what does thermokarst cause
decreases the stability of the ground, landslides, thaw lakes, ground subsidence (road disturbance and house collapse), and freeze-thaw process
freeze-thaw process
water expands by 9% when frozen which can fracture rocks. it produces frost-shattered screes.
ice growth
occurs preferentially below stones in soil and forms pipraker. ice lifts stones/soil (frost heaving)
pipraker
needle ice
what does heaving produce
stone polygons and stone stripes
slope processes
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)
creep
very slow rates of movement (<5mm/year) but can affect the stability of built structures such as pipes
what gasses does permafrost release
carbon dioxide and methane