Breaking down of sediment in situ
breaking down an transporting of sediment
the movement of sediment
Sediment broken down by living organisms
Sediment broken down by rain or acidity
Sediment broken down by water going into cracks and freezing over nightand expands. In the morning the ice melts.
water goes into cracks and forces the air out
rocks scrape each other away
Rocks hit each other chipping each other away slowly
water hits rocks and the acidity dissolves minerals
Boulders rolling along the river bed
pebbles bouncing along the river bed
silt flowing in water
dissolved oarticles flow in the river
cliffs slumping down due to gravity and erosion
sediment changed in postions
land higher than 600m in elevation
land less than 200m in elevation
land between 200m-600m in elevation
An ice sheet that covered the uk during the last ice age 10,000 years ago
period of time when the temperature was lower than average and allowed ice to form in the north parts of the world
the holocene
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wind that goes through the sea or ocean
wind that goes through land
polar maritime, arctic maritime, polar continental, tropical maritime, tropican continental
wet and cold
wet and cold
cold in winter, hot in summer
hot and dry
warm and moist
when a river flows overbands of rock which vary in their resistance to erosion. Areas of softer rock get eroded quicker and it creates a steep gradient of soft and hard rock. As the soft rock continues to be eroded an overhang of hard rock is created. a deep plunge pool is then formed at the base of the waterfall due to turbulant water.
when a waterfall retreats upwards because the overhang collapses.