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Published byMatthew Ferguson Modified over 9 years ago
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Barrier Islands are Geologically Temporary
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Chandeleur Islands Before (above) and after (below) Hurricane Katrina
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10) Sea Cliff Erosion Headlands erode from wave action Creates caves, arches, sea stacks
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Sea Cave
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Arches
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Sea Stacks
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Sea Cliff Erosion
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Coastal Erosion
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1) Hurricanes and Coastal Erosion
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Ivan: 2004 Dennis: 2005
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Charley: 2004
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Rita: 2005
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Ivan: 2004
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Katrina: 2005
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Sea Cliff Erosion
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Coastal erosion rates:Cape Cod, Massachusetts Average 0.5 ft/yr, 50 ft/century Not constant 15 feet in 5 years, then stable for 40 yrs Leads to false sense of security Erosion is episodic, not gradual
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Local Erosion Rates Vary Depends on geology Storm frequency Louisiana: Several meters/year Rocky coasts: a few cm/yr Erosion is episodic, not gradual
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Factors Leading to Erosion Depends on geology Storm frequency Wave height Tidal range Sea-level changes
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Preventing Beach Erosion Structural: Sea walls and groins Non-structural: adding sand, land-use planning
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Preventing Beach Erosion
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