chapter 12: coasts classification (difficult task) tectonics active passive sea-level change may...

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Chapter 12: Coasts

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Page 1: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Chapter 12: Coasts

Page 2: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Classification (difficult task)tectonics

activepassive

sea-level changemay vary widelycauses

global (eustatic) from +6m to -125 m in the last 2 MYvolume of water available (can be tied up in ice)capacity of ocean basins (can be reduced by faster sea-

floor spreading)volume changes due to temp changes

local tectonics isostacy

Page 3: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Primary Coasts

characterisiticsyoungusually shaped by terrestrial processes

sea level change exposes new areas to erosionheavy deposition extends the land into the sea

Page 4: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Primary coastscut by land erosion, then flooded by sea-level

risedrowned river valleysfjords

cut by wave erosion, then sea-level fallswave-cut terraces

built out by land processesriver deltas - fig p 294

morainesvolcanicearth movement

upwarddownward

Page 5: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Secondary Coasts

oldshaped by waves

Page 6: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Secondary Coasts:Wave Erosion

methodsabrasionhydraulic pressuredissolution

effectssea cliffssea cavessea stacks and archeswave-cut platformshore straightening

caused by wave refractionwaves focus on headlands

Page 7: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Secondary Coasts:Beaches

deposits that accumulate in low energy areas sand is always being moved profile fig p 300

backshore - cliffs, dunes, seawall berm crest foreshore - intertidal zone off shore - longshore trough and bar

rip currents on-shore and off-shore

seasonal big waves - sand moves off-shore small waves - sand moves back on-shore effect of sea walls

Page 8: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Secondary Coasts:Transportation & Deposition

longshore drifttransportation

wave motion pushes in at an anglegravity pulls straight outsand moves along the shore

effectssand moves in the direction of the predominant wavesbarrier islandsspits, baymouth bars, & tomboloseffects of groins, piers, jetties, breakwaters

Page 9: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Secondary Coasts:Transportation & Depositioncoastal cells

sand movesentry point - cliffs, river, etclongshore driftexit point - submarine canyonhuman structures (dams, groins, jetties, piers,

breakwaters) can block flow of sand

Page 10: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Other Types of Coasts

reefsmangrove swampsestuaries

Page 11: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125

Estuaries

typesdrowned river mouthsfjordsbar-built (barrier

island lagoons)tectonic (grabens)

characterisiticssalt-wedgepartially mixedwell mixedfjordreverse

valueproductiveshelteredbrackishnurseries for the

oceanlagoons & wetlands

Page 12: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125
Page 13: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125
Page 14: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125
Page 15: Chapter 12: Coasts Classification (difficult task) tectonics active passive sea-level change may vary widely causes global (eustatic) from +6m to -125