Marine Processes
- types of waves
- component of waves
- erosional processes: corrasion, corrosion, hydraulic action, attrition
- onshore and offshore movement
- longshore drift
- wind actions and dunes
Waves
- energy transmitted through matter
- the medium (solid liquid gas) does not actually travel as the energy passes, but its particles vibrate as the energy passes through
- Progressive waves
- Size of wave depends on fetch= distance a wave travels
- The greater the fetch, the larger the wave
- The stronger the wind, the larger the wave
- As the wave approaches the beach, it slows down due to friction between water and beach, and this causes the wave to break.
- terms: break, swash, backwash
- If swash is bigger than backwash, more deposition occurs so beach is created. If backwash is bigger than swash, beach is destroyed

- Destructive waves destroy beaches. Back wash has less time to soak into sand. So it carries a lot of sand with it. As waves continue to hit the beach, more running water carry material to the sea.
- Wind generated waves originate in windy places of the ocean
- They keep on moving along large areas without the aid of wind
- As wind blows over ocean surface, it creates pressure that deform the surface of the ocean
- If power increases, it becomes gravity waves

