what are the different types of glaciers and glacier movement Flashcards
what are the densities of fresh snow, firn and glacier ice
- fresh snow= 0.05g/cm3
- firn= 0.4g/cm3
- glacier= 0.91cm3
what is the process of snow turning to glacier ice called
diagnesis= snow to firn to glacier ice
how long could it take for diagnesis to happen
30-40 years (valley) and 1000 (ice sheets)
what depth will true glacier ice be discovered at and what is it characterised by
100m, blueish colour
what defines ice sheet glaciers
expands over 50,000km2, high latitude locations
what are the two current ice sheets glaciers and how much of the worlds ice do these possess
antarctica and greenland, 96%
what are the typical rates of movement for valley glaciers
20-200m per year
what are two locations where valley glaciers are rife
alps and rockeys
what is the main difference between cold and warm based glaciers
- cold based glaciers have basal temperature below pressure melting point
- warm based glaciers basal temperature is above PMP
what is the pressure melting point
the PMP is the temperature at which the ice is on the verge of melting
-at the surface of a glacier this is 0 degrees, but within the ice mass it will be lowered by increased pressure
why is the basal temperatures relationship with PMP so important
glacial movement is catalysed by the presence of meltwater. Where basal temp is below PMP there will be a lack of meltwater.
what is an example of a warm based glacier and four characteristics of it
the Athabasca glacier Canada
- moves 2-3 metres per year
- approx 6km long
- basal temp at PMP
- moves mainly by basal slippage
give an example of a cold based glacier and four characteristics of it
the merserve glacier antarctica
- average temperature all year is -17 degrees
- PMP is not reached so no meltwater
- limited precipitation, less than 250mm
- moves mainly by intergranular flow or laminar flow
what are the two key types of glacier movement and which type of glaciers do these apply to
- basal sliding, warm based
- internal deformation, cold based
explain the three types of basal sliding are there
- slippage, ice slides over the valley surface due to meltwater
- creep, ice deforms under pressure do to obstructions on the valley surface
- bed deformation, ice is carried by the downslope movement of sediment on a gentle gradient