1. CHAPTER 10 The Coast: Beaches and Shoreline Processes

2. Overview Coastal region constantly changes Coastal region constantly changes Primarily due to waves Primarily due to waves Erosion Erosion Deposition Deposition Many people live in coastal regions Many people live in coastal regions 80% of people in U.S. live within easy access of coast 80% of people in U.S. live within easy access of coast

3. Coastal regions Coast and coastline Coast and coastline Beach Beach Shore, foreshore, backshore Shore, foreshore, backshore Nearshore, offshore Nearshore, offshore

4. Fig. 10-1

5. Beach profile Beach Wave-worked sediments Wave-cut bench Recreational beach Berm Beach face Longshore bars Longshore trough

6. Composition of beaches Locally available material Locally available material May be coarse or fine May be coarse or fine Boulders from local cliffs Boulders from local cliffs Sand from rivers Sand from rivers Mud from rivers Mud from rivers Significant biologic material at tropical beaches Significant biologic material at tropical beaches Example, Coral reef material Example, Coral reef material

7. Sand movement along beach Perpendicular to shoreline (toward and away) Perpendicular to shoreline (toward and away) Swash and backwash Swash and backwash Parallel to shoreline (up-coast or down-coast) Parallel to shoreline (up-coast or down-coast) Longshore current Longshore current

8. Swash and backwash After wave breaks, uprush of water (swash) on beach After wave breaks, uprush of water (swash) on beach Sediment moved toward land Sediment moved toward land Backwash Backwash Water returns to ocean Water returns to ocean Sediment moved away from shore Sediment moved away from shore Light wave activity Light wave activity Swash dominates Swash dominates Sediment moved toward shore Sediment moved toward shore Wider beach Wider beach Fair weather Fair weather Summertime beach Summertime beach

9. Fig. 10.3b

10. Swash and backwash Fig. 10.2a

11. Swash and backwash Heavy wave activity Heavy wave activity Backwash dominates Backwash dominates Sediment moved away from shore Sediment moved away from shore Narrower beach Narrower beach Sand forms offshore sand bars Sand forms offshore sand bars Stormy weather Stormy weather Wintertime beach Wintertime beach

12. Fig. 10.2b

13. Longshore current Wave refraction causes water and sand to move parallel to shore Wave refraction causes water and sand to move parallel to shore Zigzag motion in surf zone Zigzag motion in surf zone Longshore current Longshore current Longshore transport Longshore transport

14. Longshore transport Millions of tons of sediment moved yearly Millions of tons of sediment moved yearly Direction of transport changes due to wave approach Direction of transport changes due to wave approach In general, sediment transported southward along Atlantic and Pacific coasts of U.S. In general, sediment transported southward along Atlantic and Pacific coasts of U.S.

15. Erosional shorelines Well-developed cliffs Well-developed cliffs Recent tectonic activity Recent tectonic activity Headlands Headlands Wave-cut cliff with sea cave Wave-cut cliff with sea cave Sea arches Sea arches Sea stacks Sea stacks Marine terrace Marine terrace Wave erosion increases with Wave erosion increases with More shore exposed to open ocean More shore exposed to open ocean Smaller tidal range Smaller tidal range Weaker bedrock Weaker bedrock

16. Fig. 10.4

17. Depositional shorelines Primarily deposited by longshore drift Primarily deposited by longshore drift Beach Beach Spit Spit Bay barrier Bay barrier Tombolo Tombolo Barrier island Barrier island Delta Delta Beach compartment Beach compartment Fig. 10.7

18. Depositional shorelines Fig. 10.8a

19. Barrier islands Long, narrow offshore deposits parallel to shore Long, narrow offshore deposits parallel to shore Most developed due to rise of sea level about 18,000 years ago Most developed due to rise of sea level about 18,000 years ago Common East and Gulf coasts of U.S. Common East and Gulf coasts of U.S. Protect mainland from high wave activity Protect mainland from high wave activity

20. Barrier island Ocean beach Ocean beach Dunes Dunes Barrier flat Barrier flat High salt marsh High salt marsh Low salt marsh Low salt marsh Lagoon Lagoon Fig. 10.10a

21. Barrier island Fig. 10.10b Movement landward over time Movement landward over time Associated with rising sea levels Associated with rising sea levels Older peat deposits found on ocean beach Older peat deposits found on ocean beach

22. Deltas River sediments reworked by ocean processes: waves, tides River sediments reworked by ocean processes: waves, tides Distributaries carry sediment to ocean Distributaries carry sediment to ocean Fig. 10-11b

23. Beach compartments Rivers supply sediment Rivers supply sediment Beach Beach Offshore submarine canyons “drain” sediments from beach Offshore submarine canyons “drain” sediments from beach Beach starvation Beach starvation

24. Fig. 10.12

25. Emerging shorelines Shorelines above current sea level Shorelines above current sea level Marine terraces Marine terraces Fig. 10.13

26. Submerging shorelines Shoreline below current sea level Shoreline below current sea level Drowned beaches Drowned beaches Submerged dune topography Submerged dune topography Drowned river valleys (estuaries) Drowned river valleys (estuaries)

27. Changing sea level Local tectonic processes Local tectonic processes Example, Pacific Coast of U.S. and active plate margin Example, Pacific Coast of U.S. and active plate margin Isostatic adjustments Isostatic adjustments Ice-loading Ice-loading Global (eustatic) changes in sea level Global (eustatic) changes in sea level Changes in seafloor spreading rates Changes in seafloor spreading rates Lake buildup or destruction Lake buildup or destruction Ice volume changes Ice volume changes

28. Eustatic changes in sea level Ice build up (glaciation) Ice build up (glaciation) Ice melting (deglaciation) Ice melting (deglaciation) Thermal contraction and expansion of seawater Thermal contraction and expansion of seawater About 120 m (400 ft) change in sea level About 120 m (400 ft) change in sea level

29. Fig. 10.14

30. Global warming and changing sea level About 0.6 o C (1.1 o F) warmer over last 130 years About 0.6 o C (1.1 o F) warmer over last 130 years Sea level rose 10-15 cm (4-10 in) over past 100 years Sea level rose 10-15 cm (4-10 in) over past 100 years If global warming continues, higher sea level If global warming continues, higher sea level Fig. 10.15

31. U.S. coasts Erosion or deposition dominates Erosion or deposition dominates Type of bedrock Type of bedrock Tidal range and wave exposure Tidal range and wave exposure Active tectonics Active tectonics Eustatic changes in sea level Eustatic changes in sea level Fig. 10.17

32. Atlantic coast Most coasts open to wave attack Most coasts open to wave attack Barrier islands common Barrier islands common Varied bedrock from resistant rocks to non-resistant sedimentary rocks Varied bedrock from resistant rocks to non-resistant sedimentary rocks Sea level rising about 0.3 m (1 ft) per century Sea level rising about 0.3 m (1 ft) per century Drowned river valleys common Drowned river valleys common Average erosion 0.8 m (2.6 ft) per year Average erosion 0.8 m (2.6 ft) per year

33. Atlantic coast Barrier islands Barrier islands Drowned river valleys Drowned river valleys Fig. 10.18

34. Gulf coast Low tidal range Low tidal range Generally low wave energy Generally low wave energy Tectonic subsidence Tectonic subsidence Mississippi delta dominates Mississippi delta dominates Locally sea level rises due to compaction of delta sediments Locally sea level rises due to compaction of delta sediments Average rate of erosion 1.8 m (6 ft) per year Average rate of erosion 1.8 m (6 ft) per year

35. Pacific coast Tectonically rising Tectonically rising Bedrock typically non-resistant sedimentary rocks Bedrock typically non-resistant sedimentary rocks Open exposure to high energy waves Open exposure to high energy waves Average rate of erosion 0.005 m (0.016 ft) per year Average rate of erosion 0.005 m (0.016 ft) per year

36. Hard stabilization Structures built to decrease coastal erosion and Structures built to decrease coastal erosion and Interfere with sand movement Interfere with sand movement Often results in unwanted outcomes Often results in unwanted outcomes Some structures may increase wave erosion Some structures may increase wave erosion Groins and groin fields Groins and groin fields Jetties Jetties Breakwaters Breakwaters Seawalls Seawalls

37. Groins and groin fields Fig. 10.20

38. Jetties Fig. 10.22

39. Breakwaters Fig. 10.24

40. Seawalls Fig. 10.26

41. Alternatives to hard stabilization Construction restrictions Construction restrictions Limit building near shorelines Limit building near shorelines National Flood Insurance Program encouraged construction National Flood Insurance Program encouraged construction Beach replenishment Beach replenishment Sand added to beach/longshore current Sand added to beach/longshore current

42. Alternatives to hard stabilization Relocation Relocation Move structures rather than protect them in areas of erosion Move structures rather than protect them in areas of erosion Fig. 10B

43. End of CHAPTER 10 The Coast: Beaches and Shoreline Processes