Ice Sheets
-Only found in Antarctica
and Greenland
-Huge mass of ice
and snow (50,000sq km)
-When an ice sheet
extents over the sea and floats on water
-100-1000 metres
thick
-Mainly around
Antarctica
-When they retreat,
this is an indication of climate change
-Larsen Ice Shelf
has been retreating since 1998
-Mini ice sheets
(less than 50,000sq km)
-Usually in polar and sub-polar regions
-Flat and tall
-Usually in polar and sub-polar regions
-Flat and tall
-Channelled
glaciers that flow rapidly compared to the rest of the ice
-Similar to ice
caps
-Flow is determined
by underlying topography
-Smaller than ice
caps
-In high mountain
regions
-Flow out of an ice
field
-Can be seen in
Canada, the Andres, Alaska
-Originate from
mountain glaciers or ice fields
-Flow down valleys
-Can be long and
flow beyond the snow line
-When steep valley glaciers
flow to flat plains
-Malaspina glacier
in Alaska prime example
-Occupy blow-like
holes
-Usually found in
high mountainside.
-Tend to be wide
and long
-Cling to steep
mountainsides
-Wider and long
-Common on the Alps
where they cause avalanches
-Reach the sea
-Carve icebergs
(Adapted from http://nsidc.org/cryosphere/glaciers/questions/types.html)
Try having a look at a different way of classifying glaciers: warm and cold based glaciers.
ReplyDeleteI will do. Thank you
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