Coastal Processes Flashcards
Attrition
A process of erosion. The pebbles are reduced in size as they hit off of one another. Smaller pebbles are easier to transport away
Corrasion
A process of erosion caused by waves throwing pebbles against the cliff face; this can also be called abrasion
Corrosion
A process of erosion by which some rocks dissolve by chemical action
Hydraulic Action
Hydraulic action is erosion that occurs when the motion of water against a rock surface produces mechanical weathering.
Destructive Wave
A high wave, with strong backwash, which breaks frequently causing erosion
Constructive Wave
A low wave, with a strong swash, which breaks gently encouraging deposition of beach materials
Backwash
The motion of receding waves.
Beach Morphology
Interaction and adjustment of the seafloor topography
Climate Change
A change in global or regional climate patterns
Eustatic Change
When the sea level changes due to an alteration in the volume of water in the oceans or, alternatively, a change in the shape of an ocean basin and hence a change in the amount of water the sea can hold. Eustatic change is always a global effect.
Isostatic Change
Isostatic sea level change is the result of an increase or decrease in the height of the land. When the height of the land increases, the sea level falls and when the height of the land decreases the sea level rises. Isostatic change is a local sea level change
Saltation
Small pebbles and stones are bounced along the sea floor/river bed
Salt Crystalisation
This is when salt crystals are deposited in cracks and over time the salt accumulates and applies pressure to the crack (similar to freeze-thaw weathering)
Suspension
Fine light material is carried along in the water
Traction
Large boulders and rocks are rolled along the river bed.