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Higher Geography
Hydrosphere
Meander
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Created by
Kirsty Kitchin
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Hydraulic action is when water forces
air
into
rocks
,
dislodging
them.
Abrasion
is when rocks in the
water
are dragged along the river bed,
grinding
it down.
Solution is when
salts
and
acids
in the river
dissolve minerals
in the rock.
Attrition
is when rocks in the
water
hit off each other and
break
into
smaller
pieces.
Riffles and pools lead to changes in
speed
and
depths
in the river
channel
Pools are areas of
deeper
water whereas
riffles
are
shallower
with greater
turbulence.
River flows
fastest
on the outside bend increasing the
erosive
power.
River flows
slowest
on the inside bend, leading to
deposition.
Helicoidal
flow moves materials across the river
channel.
This leads to river
cliffs
and
beaches
developing.
Meanders migrate
downstream
as
erosion
continues.