1. Coastal Processes

2. Oscillatory and Translatory Motion Translatory motion re-suspends sediment

3. Wave Refraction Still a small ‘longshore component swash backwash Kids at the beach

4. Fig. 14.09

5. Barrier Islands These barrier islands face the open ocean so they receive the full force of major storms that strike the coast. Storm waves that previously rushed harmlessly through gaps between the dunes now encounter buildings and roadways.

6. Barrier Islands These barrier islands face the open ocean so they receive the full force of major storms that strike the coast. Storm waves that previously rushed harmlessly through gaps between the dunes now encounter buildings and roadways.

8. Jetties Jetties are usually built in pairs and extend into the ocean at the entrances to rivers and harbors. By confining the flow of water, the jetties prevent deposition in the harbor channel.

9. Jetty: Allenhurst, NJ

10. Allenhurst to Asbury Park

11. Groins

12. Inlet Created by Hurricane Waves (North Carolina) Source: Associated Press/Raleigh News & Observer, Chris Seward

13. Migration of Barrier Islands

14. Migration of Barrier Islands (cont’d)

16. North Carolina's Outer Banks Humans remove any new sand piled up on their property. Normal bar migrations thwarted and barrier narrows.

17. Estuaries An estuary is a semi-enclosed coastal body of water with one or more rivers or streams flowing into it and with a free connection to the open sea

18. Saltmarshes A salt marsh is a type of marsh that is a transitional zone between land and salty or brackish water (e.g., sloughs, bays, estuaries)