The Coastal System
- Created by: vicky.norton
- Created on: 29-03-14 22:17
Fullscreen
The Coastal System
Inputs:
- Marine: waves, tides
- People: human activities, economics, recreation/tourism, sea defences
- Atmospheric: weather/climate, climate change, colar energy
- Land: rock type/structure, tectonics
Processes:
- Erosion: hydraulic action, abrasion/corrasion, solution
- Transportation: sediment cells, longshore drift
- Deposition
- Weathering/mass movement: freeze thaw, salt weathering, carbonation
Outputs:
- Erosional landforms: cliffs, stacks, wave cut platforms, headlands
- Depositional landforms: beaches, spits, salt marshes, sand dunes
Coastal sediment cells (aka littoral cells) are lengths of coastline that are pretty much entirely self contained for the movement of sediment. Each one is a costal system, so processes going on in one sediment cell don't affect the movement of sediment in another cell.
Beaches
- Backshore: starts at the cliff and ends at the foreshore
- Foreshore: from the backshore to the nearshore
- Nearshore: from the foreshore to the offshore
- Offshore: from nearshore onwards
- Berms: ridges of pebbles about 1-2m high. They're formed vy waves throwing these materials up onto the beach (often associated with contrstuctive waves)
- Storm beaches: formed by storm waves. they're higher up the beach than the maximum high tide…
Comments
No comments have yet been made