Coastal processes involve erosion, mass movement and weathering that break down and remove material from the coast.
The material is moved along the coastline by the sea and deposited when there is energy loss.
Erosion, transportation, deposition, weathering, and mass movements are processes that occur in coastal areas.
Waves and wave types include constructive waves which help build up material on the beach, and destructive waves which remove material from the beach.
The characteristics of a destructive wave are: weak swash and strong backwash, and they occur in stormy conditions with strong winds.
The characteristics of a constructive wave are: small waves, with low wave height and long wavelength, and they occur in calm conditions without much wind.
The swash and backwash determine the type of wave.
Destructive waves remove sediment from the beach, while constructive waves add sediment to the beach.
Constructive waves are steep and close together, while destructive waves are tall and far apart.
Constructive waves arrive quickly and have a high frequency, while destructive waves come in a short period of time.
Types of weathering include: chemical, mechanical, and thermal weathering.
Types of mass movements include: rockfalls, landslides, and avalanches.