Glaciers Flashcards
Champlain Sea
clay deposits dating from that time
Laurentide Ice sheet = melted = Champlain Sea
Isolatic rebound = Champlain Sea Basin
Leda clay = quick clay –> clay particles are bonded together by salt irons
Ice sheet
cover continents
2 remaining: Greenland and Antarctica
ice shelves = extensions of ice sheet into the ocean
glacial formations created by ice sheet
roches moutonnes
= pattern of stress on a bedrock surface beneath a sliding glacier
striations:
= long + narrow scratch
= on surface of rocks
= glaciers flow over land = reveal direction
Eratics:
Glaciers retreat creations
= When the glacier advances it plucks and abrades the bedrock below
Glacier Till = deposited assorted rock debris
End Moraines = named for their size (smaller) and location
Recessional Moraines = that record a stepwise retreat of the glaciers
Kettles lakes = water filled bowl shape lakes
Fjords = located on the coasts of continents
Eskers = a long sinuous deposit due to the retreat of a glacier
Alpine Glaciers
alpine glaciers = go through the same processes as Continental glaciers, but because of the folding and high Mountains, some of the formations are different.
Alpine glaciers or Valley Glaciers provide most of the world with fresh clean water.
Glaciers form on land when more snow falls in the winter than melts in the summer.
= This happens in the zone of accumulation.
The six-sided snowflakes change to firn (aka corn snow) and continued accumulation causes the trapped air to be expelled from the firn and flue glacial ice is then formed
= Zone of firm glacial ice
Once the ice attains a thickness of about 30 m,
it begins to deform as a viscous fluid, and flows
guided by its own weight. (plastic flow)
= Zone of flowage.
Glaciers finally ablate, or waste away, by
melting when the temperature conditions
become warmer.
= Zone of Ablation
isostatic rebound
the rise of land masses that were depressed by the huge weight of ice sheets during the last ice age
alpine glaciers
valley glaciers
zones:
// snowffall = accumulation
// snow melt = ablation
1) accumulation zone
–more snow fall (winter) than snow melt (summer)
2) zone of firm glacial ice
–firn = corn snow
–trapped air expelled = flue glacial ice
3) zone of flowage = plastic flow
–thickness of ice = deformation = viscous fluid + flow guided by own weight
4) ablation zone
= wastage
+ calving = icebergs (water)
formation
burial and metamorphosis of snow
two main mechanisms of subglacial erosion
Glacial abrasion, the wearing down of bedrock surfaces
Glacial plucking or quarrying, the removal of rock fragments and blocks from the bed
quick clay / leda clay
Clay particles that are bonded together with salt ions
// water