Glaciers Flashcards
Relict glacier
Area that used to be glacial
Periglacial
Permanently cold area near a glacier/ice sheet
Glacial alpine
Glacial due to its altitude
Glacial polar
Glacial due to its latitude
Closed system
There are changes/movement of energy but not mass
Open system
Where energy and matter can exchange in and out of the system. (E.g. Glaciers)
Zone of accumulation
Area towards the top of a glacier where snow accumulates
Zone of ablation
Area towards the bottom the glacier where snow/ice breaks up or melts
Firn/névé
snow that has been compressed into ice by layers above over many years
Mass balance
Accumulation - ablation
+ve value = glacier advancing
-ve value= glacier retreating
Dynamic equilibrium
amount of input=amount of output but glacier is still moving
lithology
physical and chemical composition of the rock
bedding planes
build up of sediment layers over time causing horizontal lines in the rock
joints
vertical cracks in rock
fault
large cracks caused by tectonic movement
Continentality
if a place is coastal or inland and the changes it brings
albedo effect
snow (white) reflects heat from the sun
relief
height of the land
aspect
which compass direction a slope is facing
pressure melting point
the melting point is reduced by applying pressure
laminar flow
type of internal deformation found in cold based glaciers. The top layer of ice moves furthest as the layers under it push it along. distance accumulates as you go up the layers.
slippage
type of basal sliding found in warm based glaciers
where the ice slides over bedrock as melt water reduces friction
creep/regelation
type of basal sliding found in warm based glaciers where ice deforms under pressure and flows like plastic
bed deformation
type of basal sliding found in warm based glaciers where ice is carried along by saturated sediments on gentle gradients.