unit two Flashcards
what is the cryosphere?
parts of the earths crust and atmosphere below 0 degrees for at least a part of each year
what does the cryosphere consist of?
ice sheets, glaciers, sea ice, lake ice, ground ice (permafrost) and snow cover
what is topography?
the natural shape of the land that controls glacier morphology
describe ice sheets and give an example of one
a gently sloping dome of ice several km thick in the centre. they are unconstrained and an example is the greenland ice sheet
describe ice caps and give an example
a smaller version of an ice sheet which is a gently sloping dome over several km thick that submerges reigonal topography. they are unconstrained and an example is greenland
describe an ice feild
ice covering an upland area that is not thick enough to bury the underlying topography, they are constrained
describe a valley glacier
a glacier confined between valley walls. they tend to form ice caps/sheets and may be terminated in the sea. they are constrained
describe piedmont glaciers
a valley glacier that extends beyond the end of a mountain valley into a flatter area. they are constrained
describe a cirque glacier
a smaller glacier occupying on the hollow of a mountain side. they are constrained. an example is cwm idal
describe an ice shelf
a large area of floating glacier ice extending from the coast where several glaciers have reached the sea. it is unconstrained
describe cold based glaciers
glaciers found at high latitude locations where the ice temperature is well below zero. the glacier is permanently frozen to the bedrock, so there is no meltwater
describe warm based/temperate glaciers
glaciers found in high altitude areas that have fluctuating temperatures. these glaciers are not frozen to the bedrock as there is meltwater present due to the pressure.
what is pressure melting?
where ice melts from the pressure of the overlying glacial ice.
what is the pressure melting point?
0 degrees
why do temperate/warm based glaciers get meltwater at the bottom?
during summer months, when the temperature rises the top of the ice melts and this percolates down into cracks in the glacier leaving meltwater at the bottom