Glaciers and ice ages Flashcards
What evidence was found for glaciation?
erratics: fine sediment of large boulders found 100s of km in local bedrock
unsorted sediments
what are glaciers?
thick masses of recrystallized ice. last all year long. flow via gravity. cover about 10% of the earth.
when did the most recent ice age end?
11000 years ago. ice sheets were hundreds to thousands of metres thick.
is ice a mineral?
yes
how is snow transformed into ice?
can form slowly (thousands of years) or quickly (tens of years)
Snow is buried by later falls. Compression reduces volume. Burial pressure causes melting
and recrystallization. Snow turns into granular firn.
Over time, firn becomes
interlocking crystals of ice.
what conditions are necessary for glacier formation?
cold local climate (polar latitudes or high elevations)
lots of snow in winter and can’t all melt in summer
what are the two types of glaciers?
mountain and continental
describe mountain glaciers
flow from high to low elev in mountain settings
name and describe 4 types of mountain glaciers
cirque: fill mountain top bowls
valley: flow like rivers down valleys
mountain ice caps cover peaks
piedmont: spread out at end of valley
descrive continental glaciers
Greenland and Antartica
Vast ice sheets covering large land areas. Ice flows outward from thickest part of sheet.
what is basal sliding?
meltwater forms at base of glacier, it decreases friction and ice slides along substrate
movement of glacier
what is plastic deformation?
movement of glacier
occurs below, about 60m depth. grains of ice change shape slowly. new grains form while old grain disappear. crevasses form at surface, upper zone too brittle to flow
why do glaciers move?
gravity is strong makes ice flow.
glacier moves in the direction of its surface slope.
ice base can flow up a local incline.
In continental glaciers, ice spreads away from center of
accumulation. because
ice sheet always thicker in the middle, so it spreads
toward the edges.
what control’s a glacier’s rate of flow?
The severity of slope angle: steeper = faster
Basal water: wet-bottom = faster
Location within glacier:
faster in ice center, slower due to Friction at margins.
what is zone of accumulation vs of ablation?
accumulation: net snow addition
colder temps prevent melting, snow remains in summer
ablation: net ice loss
zones meet at equilibrium line
what is toe?
leading edge of a glacier
what are toe positions based on accumulation and ablation?
accumulation = ablation: stays in the same place
accumulation > ablation: advances
accumulation < ablation: retreat upslope
what are tidewater glaciers?
valley glaciers entering the sea