glacial systems Flashcards
over what time period did the Pleistocene last
1.8 million years ago until 11700 years ago
what was the name of the ice sheets which covered Briton in the last glacial maximum
Scandinavian ice sheets
what are the 4 types of glacial environment
polar - areas of permanent ice , Antarctica and Greenland
periglacial - on the edge of permanent ice . permanently frozen ground , Canada , Alaska
alpine - mountain areas- European alps
glacial - found in the edges of ice sheets and in mountainous regions , Himalayas and andes
what happens in the zone of accumulation
inputs exceed outputs
what are factors for the accumulation zone
higher altitude means increased snow fall
new snow means albedo effect which keeps it cooler reflecting the sunlight
strong winds means snow is blown into hollows and basins - accumulating
what is the albedo effect
ice and snow surfaced reflect more light keeping them cooler
what are the 3 factors keeping glaciers cold
latitude
albedo effect
altitude
what is the main input in the accumulation zone
snow.
turns to compacted ice over years
avalanches and mountain slides can be inputs
what happens in the ablation zone and what are its factors
output exceed inputs
lower altitude means less snowfall and higher temperatures
melting
sublimation
evaporation
calving
what are the 2 zones within a glacier
accumulation zone
ablation zone
what are the outputs in the ablation zone
calving
evaporation
sublimation
melting
what is the equilibrium line
the boundary where gains and loses are balanced
what is the glacial budget
considers the balance between inputs and outputs
what happens to the glaciers mass balance across a year
mass balance varies across a year
in summer ablation will be at its highest due to rapid melting of ice
in winter high snowfall and limited melting results in accumulation being higher than ablation
what are the characteristics of a warm based glacier
found at lower latitudes often in alpine environments
water present throughout the glacier which helps with movement
move much more than cold based glaciers . 20-200m per year
how far do cold base glaciers move a year
cms Per year
how far do warm based glaciers move per year
20-200 m
they erode and move large amounts of material
cold base glacier characteristics
found in polar regions in the arctic and Antartica
glacial ice remains frozen to the bedrock so limited movement
movement is cms per year
which glaciers can slide down mountains due to basal siding
warm based glaciers
what is basal sliding
siding of a glacier over bedrock due to meltwater at glaciers base
why does basal sliding occur
small obstacles create pressure points
increase of pressure causes melting - pressure melting point is reached
melting allows glacier to slide over the obstacle
meltwater refreezes on the downside of the obstacle and pressure reduces
this melting and freezing is called REGELATION
what is regelation
the melting and freezing which occurs in basal sliding
how do cold based glaciers move
internal deformation
which glaciers does internal deformation take place
warm and cold based glaciers