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erosion

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Erosion

Cheddar Gorge in the Mendip Hills - Click to enlarge coastal erosion - Click to enlarge eroded sandstone - Click to enlarge Grand Canyon, South Rim - Click to enlarge
Hoodoos - Click to enlarge human impact on sand dunes - Click to enlarge rock erosion - Click to enlarge waterfall - Click to enlarge
weathering and erosion of limestone - Click to enlarge

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Wearing away of the Earth's surface by a moving agent, caused by the breakdown and transport of particles of rock or soil. Agents of erosion include the sea, rivers, glaciers, and wind. By contrast, weathering does not involve transportation.

The most powerful forms of erosion are water, consisting of sea waves and currents, rivers, and rain; ice, in the form of glaciers; and wind, hurling sand fragments against exposed rocks and moving dunes along. People also contribute to erosion by poor farming practices and the cutting down of forests, which can lead to increased overland water run-off.

There are several processes of river erosion including hydraulic action, corrasion, attrition, and solution.

© Research Machines plc 2008. All rights reserved. Helicon Publishing is a division of Research Machines plc.


 
 

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ablation
abrasion (earth science)
acid rain
aerosol
Agent Orange
air pollution
alluvium
arête
arch (earth science)
asymmetric valley
atmosphere (earth science)
attrition
bar (earth science)
basalt
bay (earth science)
beach
calcium carbonate
calcium hydroxide
carbon cycle
carbon dioxide
carbonate
catalytic converter
cave
cavitation (earth science)
cementation
chalk (rock)
channel efficiency
chemical weathering
chlorofluorocarbon
coast
coastal cliff
coastal deposition
coastal erosion
coastal protection
confluence
conglomerate (geology)
conservation
continental drift
core (earth science)
corrasion
corrie
corrosion
crust
dam
deforestation
delta
deposition (earth science)
desertification
drainage basin
drumlin
dry valley
dune
earthquake
environmental issues
erosion
erratic
esker
estuary
eutrophication
evaporation
exfoliation
extrusive rock
fault
fertilizer
fjord
flood plain
flooding
flue-gas desulphurization
fold
fossil
fossil fuel
freeze–thaw
geomorphology
glacial deposition
glacial erosion
glacial trough
glacier
glacier budget
global warming
gneiss
gorge
granite
gravel
green revolution
greenhouse effect
groyne
hanging valley
hazardous waste
headland
headward erosion
helium
Holocene epoch
hydraulic action
hydraulic radius
hydrograph
ice age
igneous rock
incised meander
interlocking spur
intrusive rock
irrigation
karst
krypton
lake
landform
landslide
lava
levee
limestone
lithosphere
longshore drift
magma
mantle
marble
meander
metamorphic rock
metamorphism
mineral
misfit valley
Montréal Protocol
moraine
mountain
neon
nitrate
nitrate pollution
nitrogen
nitrogen cycle
nivation
nuclear waste
ocean
oxbow lake
oxygen
ozone
ozone depleter
ozone layer
periglacial environment
pesticide
physical weathering
plain
plate
plate tectonics
playa
Pleistocene epoch
plutonic rock
PM10
pollution
Precambrian era
pyramidal peak
recycling
rejuvenation
ria
rift valley
river
river capture
river terrace
rock
rock cycle
salt marsh
saltation (earth science)
sandstone
schist
scree
seafloor spreading
seawater
sediment
sedimentary rock
sewage disposal
shale
silica
slate
soil
soil erosion
solution (earth science)
spit
stack (earth science)
storm surge
stump
suspension (earth science)
tide
till
truncated spur
V-shaped valley
valley
volcano
waste
water
water cycle
water pollution
water-borne disease
waterfall
wave (earth science)
wave-cut platform
weathering
weedkiller
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