Transcript File

Erosion and Deposition
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Erosion
•Erosion – moving of rock material from one place
to a new location
– Three processes must take place:
• detachment of particles
• lifting them
• transporting them
– Agents of erosion:
• flowing water
• moving ice
• waves
• gravity
• wind
– Sand is composed of small pieces of rock that have been:
• weathered from a parent rock
• eroded
• deposited somewhere else
Erosion
•Wind – wears away rocks and is responsible for the
creation of deserts such as the Sahara and the Gobi
- Most effective in moving loose material
– Main effects:
1. Wind lifts small particles and moves them away.
2. Suspended particles may cause erosion on solid objects by abrasion
(rubbing).
– Occurs in areas where there is not enough rainfall to support vegetation
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Erosion
•Water – most influential force in erosion
–Moves materials
–Transports large objects with fast moving streams
–Wears away rocks:
• rivers
• lakes
• oceans
• Ground/sinkholes
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rosion_below_Scarsoch_Bheag__geograph.org.uk_-_1367808.jpg
Erosion
• Waves – relentless pounding
• Erodes:
• softer/weaker rock first
• harder/more resistant left behind
• Can take over 100 years to erode a rock to sand
• Energy of waves and chemicals contained in the water erode
the rock off the coastline.
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Erosion
•Mass Movement – downward movement of rock
and sediments, due primarily to the force of gravity
–Streams and glaciers
• move material from higher  to lower  elevation
– Occurs continuously on all slopes
» slow moving and sudden movement until equilibrium is reached
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Erosion
• Ice – moves and carries rocks, grinding the rocks
beneath the glacier
– Plucking occurs when water enters cracks under the glacier.
• freezing
• breaking off pieces of rock that are then carried by the glacier
– Abrade (abrasion)
• cuts into the rock under the glacier
• smoothing
• polishing the rock surface
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Deposition
•Deposition – laying down of sediment that has
been transported by a medium such as wind,
water, or ice
–Process of erosion stops:
• when the moving particles fall out of the transporting
medium and settle on a surface
–Speed of the medium slows or the resistance of the particles
increases, the balance changes and causes deposition
–Speed can be reduced by large rocks, hills, vegetation, etc.
Deposition
Wind speed can be related to variations in heating
and cooling.
 Transportation of particles in wind:
– Fine particles in suspension hundreds of km from its original source in
the desert
– Heavier material may be blown along the ground.
– Material is deposited when the wind changes direction or loses its
strength.
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Deposition
• Running water enters a large, fairly still body of water
and its speed decreases
• SPEED
• As the speed of the water decreases, the water's ability to carry
sediment also decreases.
• Deposited in streams, rivers, and oceans:
• Running water deposits sediments where the slowing water can no
longer move them.
• Largest particles are deposited near the shore.
• Increasingly smaller particles settle out farther from the shore where
the water is calmer.
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Deposition
• Glacial flows of ice
– become slower when the ice begins
melting
– Deposits left by glaciers:
– Outwashes are deposits similar to those left by rivers.
– Large chunks of broken rock deposited at the base and sides of the glacier as
it melts and recedes are called Moraines.
– When the glacial ice melts, smaller material is carried by the rivers.
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• WEATHERING – Think of weather wearing rock down.
• EROSION – Think of a road and traveling.
• DEPOSITION – Think of depositing money into a bank.
Running Water Deposits Well-Sorted Particles
Vertical Sorting – When
sediments are suddenly
deposited into water. The
particles separate by size with
the largest on the bottom and
smallest on top.
Horizontal Sorting – When rivers empty their sediments into
quiet bodies of water. Particles are sorted by size with larger
particles being found closer to the shore and smaller particles
being carried out into the body of water to be deposited.
Delta – A fan-shaped deposit of sediment
at the mouth of a river