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Weathering is the breaking down of material in situ
the three types of
weathering
are biological, chemical or
freeze-thaw
biological weathering is caused by
plants
and
animals
biological weathering is when rocks are broken down by
plant roots
or
burrowing animals
chemical weathering
is the breaking down of rocks caused by a chemical change within that rock, this is caused by
salt water
or acid rain
freeze-thaw weathering is cased by water entering cracks in a rock,
freezing
, expanding and
breaking
rocks apart
the physical geography of the UK is caused by geological, fluvial,
glacial
or
tectonic
processes
geological
processes are
rocks
fluvial
is
water
glacial
is
ice
tectonic os earthquakes
and
volcanoes
The UK is made of
upland
and
lowland
areas
Upland areas are found in the
north
and west, particularly in
Scotland
, Wales and north england
lowland areas are in the
south
of the UK and are found in norfolk and
south
of the imaginary line between Flamborough head and the bristol channel
glaciers
are large masses of
ice
that move slowly downhill
upland regions of the UK like Snowdonia and the
lake district
used to be covered by
glaciers
explaining the U-shaped valleys and rocky geology
Igneous rocks are
hard
rocks formed by
cooled magma
that solidifies
igneous rocks are intrusive and form
underground
or are extrusive and form above
ground
examples of igneous rocks are
granite
and
basalt
Metamorphic rock are soft rocks that have been put under intense heat and pressure
examples of
metamorphic
rocks are marble from
limestone
, slate from clay and schist from shale
sedimentary rock is formed from sediment settled at the
bottom
of a
lake
, sea or ocean, compressed for millions of years
sedimentary rocks are
softer
, foliated and tend to create
fossils
examples of sedimentary rocks are limestone,
chalk
, sandstone,
shale
, and mudstone
erosion
is the
wearing away
of material
the types of erosion are
abrasion
, attrition, traction and
hydraulic
action
transportation
is the
movement
of material
the types of transportation are
saltation
,
traction
, solution, suspension
deposition
is the dropping of
sediment
mass movement occurs through
sliding
and
slumping
sliding
is when rocks slide or roll down the cliff of at the
coastline
slumping
is when the cliff collapses ina
rotational
movement due to a high force from a heavy object on a soft rock cliff
a
discordant
coastline is when the the types of rock are perpendicular to the shoreline
a
concordant
coastline is where the type of rock is
parallel
to the shore;ine
on
discordant
coastlines, headlands and bays are formed due to differential erosion
differential
erosion is when the rates of erosion a different due to different
resistances
a
headland
slowly erodes to create an crack cave arch stack stump
the
crack
of a headland is created through
weathering
a
crack
widens to create a
cave
the
back
cave wall is eroded through by abrasion and hydrolic action to form an
arch
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