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Coastal processes and landforms geography.ppt
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- 9. Wavelength Distance from onewave crest to the next Wave height The distance between trough and crest Wave period The time taken for two crests to pass a given point (remains almost constant) = V * P The wavelength, , is the product of its velocity and period.
- 10. Wave Properties The energysource for both coastal erosion and sediment transport are the ocean waves generated by the frictional effect of the winds ncident on the ocean surface 1) Kinetic Energy: The motion of the water within the wave. 2) Potential Energy: Due to the position of water above the wave trough. Wave energy increases with wind speed and fetch
- 11. Wave motion a)Ocean depth> ½ wavelength - waves not affected by ocean floor b) Ocean depth < ½ wavelength - wave height increases and wavelength decreases he wave becomes more peaked Breakers” form reaking of waves: conversion f potential to kinetic energy Work done on the shoreline
- 12. Transport of Sedimentsby Wave Action Rock particles are eroded from one area and deposited elsewhere. Wave refraction affects this process. Beach Drift: Swash and backwash rarely occur in exactly opposite directions Upward movement occurs at some oblique angle Backward movement occurs at right angles to the beach. This creates lateral movement of particles (beach drift)
- 13. Decrease in wavelength as wavesapproach a shoreline
- 14. Wave Refraction Straight shoreline -drag exerted by the ocean floor causes waves to break parallel with the shoreline. The direction of travel of a wave varies as it approaches an indented coast. Crests approaching the headlands experience the drag of the ocean floor first, which causes: 1. Increase in wave height 2. Decrease in wavelength 3. Decrease in velocity
- 16. Longshore Current andBeach Drift
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- 19. Rip currents formwhen waves are pushed over sandbars. The weight of excess water near the shore can ‘rip’ an opening in the sandbar, causing water to rush seaward. Rip Currents Source: NOAA
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- 25. Tidal forces Tides enhancedduring full Moon and new Moon Sun-Moon-Earth closely aligned
- 26. Influence of Perigee,Apogee, Perihelion and Aphelion on the Earth’s Tides Stronger for perigee and perihelion
- 27. Annapolis Tidal PowerGenerating Station
- 28. Hopewell Rocks, NewBrunswick “flower pot rocks”
- 29. Coastal Processes and Landforms Erosionaland depositional landforms of coastal areas are the result of the action of ocean waves. Erosional Landforms Depositional landforms Sea Cliffs Beaches Wave-cut Notches Barrier Spit Caves Baymouth Bar Sea stacks Lagoon Sea arches Tombolo
- 30. Erosional Coastal Landforms Alongrugged, high-relief, tectonically-active coastlines Sea cliffs A tall, steep rock face, formed by the undercutting action of the sea Wave-cut notches A rock recess at the foot of a sea cliff where the energy of waves is concentrated Sea Caves Caves form in more erosive sediment when the rock does not fully collapse in a deeply-notched environment
- 33. Wave-cut platform Horizontal benchesin the tidal zone extending from the sea cliff out into the sea If the sea level relative to the land changes over time (becoming lower with respect to the land due to uplift), multiple wave cut platforms (terraces) result 1 3 2 5 4 6 http://www.rgs.edu.sg/events/geotrip/cliff.html
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- 37. Barrier Spit Material transportedby littoral drift deposited along ridge, extending outward from a coast in an area with weak offshore currents If the spit grows to completely block an embayment, it is called a bay barrier or baymouth bar A lagoon is a body of water behind the barrier
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- 42. Coastal Straightening Figure 13.8 Copyright© 2010 Pearson Education, Inc. Christopherson, Elemental Geosystems, Sixth Edition
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- 45. A tombolo occurswhen sediment deposits connect the shoreline with an offshore sea stack or island
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- 51. Coral Reef Formationand Forms
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