Zusammenfassung der Ressource
Coastal Zones
- WEATHERING
- Mechanical
- breakdown of rock without
changing its chemical
composition - freeze thaw
weathering
- 1. temperature alternates above
and below 0'C
- 2. Water gets into
cracks
- 3. When water freezes it
expands, puts pressure on the
rock
- 4. When water thaws it
contracts, releasing pressure
- 5. This process repeats and
widens the crack causes rock
to break up
- Chemical
- break down of rock by
changing chemical
composition - carbonation
weathering (warm and wet
conditions)
- 1. Rainwater has carbon dioxide
dissolved in it- makes it weak carbonic
acid
- 2. Carbonic acid reacts with rock that
contain calcium carbonate so rocks
dissolve by rainwater (limestone)
- MASS MOVEMENT
- shifting of rocks and loose
material down a slope.
- causes coasts to retreat rapidly
- more likely to happen when
material is full of water
- 2 types
- material shifts in a
straight line
- material shifts with a
rotation
- PROCESS OF EROSION
- Hydraulic Action - waves crash against rock,
compress air in crack. Pressure on rocks- process
repeats widens the crack, rocks fall off
- Abrasion - eroded particles in water scrape
and rub against rock, removing small pieces
- Attrition - particles smash into
eachother and break into smaller
fragments - edges round off
- Solution - particles dissolve in water
- WAVES
- Constructive
- carry and deposit
material
- low and long
- swash is more
powerful than the
backwash
- material is deposited instead
of taken away
- Destructive
- carry out
erosional process
- high and steep
- backwash is more
powerful than the swash
- material removed from
beach