Chapter 21 Flashcards
valley glaciers
rivers of ice
iceberg calving
when masses of ice break off glaciers at the ocean’s edge
continental glacier
ice sheet that covers a large part of a continent
ice shelves
thinner sheets of ice
ice caps
the masses of ice that cover the Earth’s North and South pole
what are the two types of glaciers?
valley glaciers and continental glaciers
snow line
the elevation above which snow does not completey melt in the summer
accumulation
the amount of ice added to a glacier annually
present and past distribution of glaciers
Today, 10%
20,000 years ago, 30%
700 million years ago, 100%
geologic record of ice sheets
40 Ma - Recent ice age
330-250 Ma - permian ice age
700 Ma - snowball earth
How do glaciers form? in terms of layers and density
snow - .05-.07
granular ice - .1-.4
firn - .4-.8
glacial ice - .8-.9
equilibrium line altitude
transition between snow and glacial ice
how fast do glaciers move on average?
3-300 m/yr
what is the record movement of a glacier?
100 ft/day
ablation
total amount of ice a glacier loses annually
mechanisms responsible for ablation (4)
melting
iceberg calving
sublimation
wind erosion
sublimation
H2O goes from ice to vapor, skipping liquid form
processes of glacial erosion
abrasion (~25%)
plucking (~75%)
other (kelleys island grooves)
abrasion
particles in the glacier “sand” the surface below
-can form striation
plucking
- ice plucks rock fragments, producing a rough surface
- increase pressure, ice melts to flow around obstruction and freezes on the other side, plucking rock with it
erosional landforms (3)
u-shaped valleys
cirques
fjords
u-shaped valleys
steep mountain sides with hanging valleys
cirque
nearly vertical walls with a flat base
fjord
u-shaped valley that is the arm of the sea
glacial deposits and landforms (5)
drift till drumlins esker nested moraine
drift
material of glacial origin found anywhere on land or beneath the ocean
till
unsorted glacial sediment
drumlins
sub-marine shaped hills that form from warm-based ice sheets
esker
stream channel
nested moraines
when glaciers remain still for a long time
warm-based glacier
not frozen to landmass
cold-based glacier
base frozen to landmass