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cryosphere
the frozen part of the earth’s surface (e.g. polar ice caps, continental ice sheets, glaciers, sea ice, permafrost)
glacial landscape areas
Andes - located on the West coast of South America
Rockies - North West coast of North America
Himalayas - Central Asia, North of India
glacial periods temp fluctuations
global temperature fluctuates between 5°C and 6°C between glacials (cold periods, e.g. the Pleistocene) and interglacials (warmer periods, e.g. Holocene)
the different types of glaciers
ice sheets
ice caps
ice shelf
valley glacier
types of valley glacier
niche
corrie
piedmont
outlet
glacier
it is a permanent body of ice (on a human timescale), consisting largely of recrystalised snow which shows evidence of downslope or outwards movement due to the pull of gravity
what are ice sheets?
they are the largest glaciers
they are continental glaciers, with a large flat appearance
covers large areas of land
e.g. Greenland and Antarctica which cover 96% of all glacial ice on earth
what are ice caps?
they sit across mountains and mountain ranges
they have exposed summits of high mountains (called nunataks)
what is a valley glacier?
the most common glacier
it is a flowing stream or tongue of ice
it is restricted by surrounding relief mountains
carves out landscapes
what is a niche?
a small version of a corrie which occupies hollows on North facing slopes in the Northern Hemisphere
what is a corrie?
masses of ice which fills armchair shaped hollows in mountains. they can overspill and fill valley glaciers.
aspect
the direction something faces in
piedmont
can make up the bottom stretches of a valley glacier.
the ice becomes broader and shallower as it spreads out onto the land.
it looks like a spoon
outlet
is a valley glacier that has its source from a icesheets
e.g. the Beardmore on Antarctica (extends over 200km and is up to 20km wide)
what is a glacial environment?
an environment which contains snow and ice all year round
active glacial environments
means the environment is currently covered in ice
relict glacial environments
old, no longer covered in ice
process of diagenesis
glaciers form when snowfall in 1 year remains frozen throughout the year
fresh snow falls on top of last years snow
snow that survives a summer is called névé/ firn ice which has a density of 0.4g/cm3
fresh snow has low density
each layer of fresh snowfall compresses and compacts the layer beneath, squeezing out air
low density snow becomes higher density ice
glacial ice has a density of 0.83 - 0.94g/cm3