week 7 ~ glacial

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45 Terms

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glacial trough/U-shaped valley
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hanging valley
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fjord → U-shaped valley with sea level high enough to fill
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grooves
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plastically moulded forms (p-forms)

diff lithology causing diff levels of abrasion
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striations
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glacial polish
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how are partly streamlined landforms produced?
combination of abrasion and rock fracturing
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roche moutonnee
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how are roche moutonnees formed?
stoss - striated surface due to abrasion from moraine at glacier base

lee - materials plucked from lee side
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crag and tail
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how is crag and tail formed?
stoss - plucking and abrasion erode side

lee - less resistant moraines deposited giving it a tail
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cirque and tarn
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horn → pyramidal peak
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arete → saw tooth like ridges
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nunatak (glacial islands) → high elevated bed rock that has not been glaciated
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what is the low lying area between horns and aretes?
col
col
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erratics → pieces of material transported from glacier, vary in size
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what is a moraine?
mound of till
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what are the types of moraines?
lateral → formed along edge of valley

medial → joining of 2 lateral moraines

end → formed at end of glacier

terminal → type of end glacier, furthest one formed

recessional → end moraine marking times of temp pauses
lateral → formed along edge of valley

medial → joining of 2 lateral moraines

end → formed at end of glacier 

terminal → type of end glacier, furthest one formed

recessional → end moraine marking times of temp pauses
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drumlin → stream lined, formed through subglacial deposition
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what are the types of glacial sediment?
glacial till → from ice directly

glaciofluvial → from melted glacial water rivers

glaciolacustrine → from melted glacial water lakes
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eskers
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how are eskers formed?
when rivers/lakes are formed under or right at the edge of a glacier and leave behind a pile of material when the ice melts
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kames
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kettle lakes
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how are kames formed?
formed when supraglacial sediment is deposited on top and the ice melts leaving a mound of debris
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how are kettle lakes formed?
formed when you have a block of ice that eventually melts surrounded by outwash material or tills
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what is permafrost?
zones of permanently frozen ground (more than 2 years)
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what is continuous vs discontinuous ground ice?
cont → entire thing frozen

discont → pockets of frozen/unfrozen
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what is an active layer?
seasonally thaws/freezes
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what is a permafrost table?
line where permanent ice begins
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frost cracking
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what is frost heave?
when ice lens layers thickens and the frozen zone experiences volume expansion/shrinkage due to frost heaving/thawing
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frost wedges
frost wedges
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melted ice wedges

formed when series of ice wedges are formed in the same area
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frost mounds. → pockets of soil filled with icea
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pingos
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how are pingos formed?
giant ice mounds

formed when there is a pocket of water underneath which pushes the ground upwards as it freezes
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thermokarst → irregular terrain with depressions and hummocks between them
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how is thermokarst formed?
thawing of ground ice and material collapsing
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stone circles
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polygons
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stone stripes
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hummocks