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Physical
Glaciers
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Siena Edhem
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glaciers
alter landscapes through
abrasion
deposition
transportation
entrainment
glaciers
can develop at different scales
micro
meso
macro
different morphology means
different
shape
, structure and
size
of things
glacial
landforms can impact environments through sub-glacial process...
marginal
proglacial
periglacial
landforms
in the system create distinctive
landscapes
in
upland and lowland areas that can be used to measure the
extent
of
ice cover
glacial
landforms are not formed by a definitive process because
glaciers have been subject to sub-areal, mass movement, fluvial actions, mechanical and
chemical weathering
since the
last ice age
this is called
equifinality
change will have occurred due to a
number of cycles
which would have made
modifications
in their own right
inversion
modelling
mapping relict
landscapes
and measuring current deposits to model
past ice extent
the ice can transport
sediment
horizontally
or
vertically
glacier
landform systems can highlight ice
extent
because
look at where the
landform originated
+ how
landforms
go to be where they are today
deposition occurs where?
at
margins
Fluvioglacial processes dominate what
pro-glacial
morphologies
marginal
morphologies
side
and
front
of glacier
there are long term factors leading to climate change
Milankovitch
cycles
tectonic
movement
there are short term factors that lead to climate change
sun spots
volcanic eruptions
the
Little Ice Age was caused by
Sun spot activity
sun spots are
variations
in
solar output
the
little ice age lasted from
1400-1600
increased
the price of food
famine
thames
freeze over
the
Loch
Lomand
stadial
during an interglacial period in the Pleistocene
caused by increase in freshwater in the
ocean
because of glacial melt that disrupted the
thermohaline
circulation
thermohaline circulation brought
colder
weather to the UK - an ice field was
re-established
in the Scottish Highlands
the shape of the orbit changes every
100,000
years
the tilt of the axis changes every
41,000
years
when there is no tilt of the axis there is
no seasons
elliptical
there are seasons
interglacial
circular
consistently further
glacial
the Little Ice Age lasted from
1400
-
1600
The year without summer was caused by
Tambora
exploding
In
1991 Mt
Pinatubo
erupted and caused
short
term climate variation
decreased temperatures by
0.6C
lasted for
3
years
stadial
shorter periods of intense colder within
glacial-interglacial
periods
the
earth currently has a tilt of
24.44
degrees
when the angle increases there is
seasonal variability
within climate systems
The
quaternary
most recent period of geological time - it is split into
two
epochs
Pleistocene
Holocene