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what is an estuary?
where the tide meets the stream
what is a drainage basin?
ana rea of land drained by a river and its tributaries
features of upper course?
low volume of water
v-shaped valley
interlocking spurs
gorges
high level of percepitation
features of the middle coarse
wide valley
flood plains
meander
oxbow lake
more suspended sedement
what kind of erosion occurs on the upper coarse
vertica; erosion
what kind of erosion occurs on the middle coarse?
lateral erosion
features of the lower coarse
levees
deep and wide channels
lots of deposition
what is hydraulic action
force of water foces air into crack which break the rock on the river bank away
requires high energy water
what is abrasion
eroding the river bed as big angular boulder roll across the river bed
what is attrition
when small sediment hit eachother as they are carriend in the river
what is solution
soluble material has been dissolved in the river by the mildly acidic river water
what is traction?
the moving of large rocks being rolled along the river bed
what is saltation?
small stones bouncing along the bed in a hopping motion
what is suspension?
carrying find river material within the water so it floats in the river and is moved as it flows
what is solution and an example
carrying dissolved soluble rocks e.g. limestone
how are v - shaped valleys formed?
formed in the upper coarse where the river channel is narrow and fast-flowing
abrasion cuts into the landscape
over time the side of the valley are weekend by weathering
mass movement causes material from the valley sides to fall into the river
this material is transported downstream
how do interlocking spurs form?>
the river cuts down into the valley
if there are areas of hard rock the river will bend around it.
creating interlocking spurs
how are waterfalls formed?
when hard rock lays on top of soft rock
the soft rock erodes faster
this results in an overhand and undercut
overtime the overhand collapses and the process repeats
forming steep sided gorge
how do meanders form?
a meander is a bend in the river
mater moves faster on the outer backs due to obstacles
the high velocity water has more energy to erode the rocks through hydraulic action
this forms a river cliff
water moves slowly on the inside of the bend and the river deposits load forming slip off slopes
a meander will change over time
formation of an oxbow lake
a meander forms on the river
the neck joins.
in times of flood the river takes the shortest path
the river now uses the new path
over time deposition occurs cutting of the neck of meander
creating an oxbow lake
characteristics of flood plain?
lots of vegetation
arable farming
fertile soil
formation of a flood plain
wide flat area casued by meanders shifting along the valley
formation of a levee
before the flood the water is base leve
during the flood the water overflows, loosing velocity and dropping heavier sediment
further along the finnner sediment is deposited.
after many floods a natural levee is built up
feature sof eastuariers
large amount of deposition of muddle silt
salt marshes and mudflats formed
uses of the estuariers
oil industries,
steel, cast iron factories
physical factors increase flood risk
percipitation
geology
the shape of the land