Deposition along high energy coastlines
- large heavier material is deposited, forming single beaches
Deposition along low energy coastlines
Even the smallest matter is deposited firming mudflats and salt marshes
Hydraulic action
- can exert enormous pressure on a rock surface, weakening it
Wave quarrying
Abrasion/corrosion
Attrition
-rocks which are carrying out abrasion are worn down into smaller rounder particles
Solution (corrosion)
- but wheee sea water interacts with freshwater supplies, carbon based rocks (eg. limestone) may be dissolved
Traction
The rolling of coarse sediment along the sea bed that is too heavy to be picked up and carried by the sea
Saltation
Sediment ‘bounced’ along the seabed, light enough to be picked up or dislodged but too heavy to remain with the flow of water
Suspension
Smaller (lighter) sediment picked up and carried within the flow of the water
Suspension
Chemicals dissolved in the water, transported and precipitated elsewhere. This plays an important role in the carbon cycle, transferring and redepositing carbon in the oceans