Title: Coastal Environmental Geology
1Coastal Environmental Geology
2Environmental Issues and Coastal Geology
- Excessive Sedimentation
- Shoreline Erosion
- Coastal Subsidence
- Sea Level Rise
- Storm Surges
- Tsunamis
3Wave Motions
- Particles in a wave travel circular paths
- The water in a deep-water wave does not move
forward - Below wave base, wave effects are negligible
4The Highest Recorded Ocean Wave
5When Waves Meet the Shore
- When the bottom interferes with wave motion, the
wave steepens and the top overtakes the bottom.
6Wave Refraction
- Waves change path when they reach shallow water
- Wave energy is concentrated on headlands and
spread out in bays
7Rips
- When waves break parallel to a beach, rips occur
8Rips, Lake Superior
9Excessive Sedimentation
- Natural Sedimentation
- Rarely an issue Nobody complains about too much
beach - Siltation of harbors and channels
- Artificial Sedimentation
- Smothering of Marine Communities and Wetlands
10Shoreline Retreat
- Shoreline Erosion
- Sediment Starvation
- Coastal Subsidence
- Compaction
- Sediment Starvation
- Sea Level Rise
- Thermal Expansion
- Glacial Melting
11Shoreline Retreat, Wisconsin
12Beach Erosion, Surfside, Texas
13Beach Erosion, Surfside, Texas
14Beach Erosion, Surfside, Texas
15In the long run, nothing is as futile as trying
to resist shoreline change.
- Change can be resisted for a while, but when the
water wants something badly enough, it will come
in and take it.
16Property Values and Shoreline Erosion
- If more than half the original lot is left, its
Location, Location, Location - After that, it becomes obvious there soon wont
be any location left
17Longshore and Beach Drift
- Most Beach Sand Is Created by Weathering and
Carried to Coasts by Rivers - Beach Sand Moves along the Coast by Longshore and
Beach Drift
18Beach Drift
19Beach Drift, New Jersey
20Catastrophic Waves
- Storm Surges
- Galveston 1900 (6000-8000 dead)
- Bangladesh 1970 (300,000 dead)
- Bangladesh 1991 (140,000 dead)
- Operation Sea Angel
- Katrina 2005 (1300 dead)
- Tsunamis
- Indian Ocean 2004 (250,000 dead)
21Bangladesh Annual Flooding
22Bangladesh Cyclone Hazard
23Hurricane Evacuation Marker
24Storm Waves Galveston, Texas, September 8, 1900
- 6000-8000 dead
- 3600 houses destroyed
25Raising Galveston 6 in. to 17 ft.
26A rickety maze such as Dr. Seuss might have
drawn
27The Lift in Progress
28Pumping in the Sand
29The Galveston Seawall
30Seawall, Galveston, Texas
31Seawall, Galveston, Texas
32Centennial Monument
33Seawall Model, Galveston, Texas
34Raised Hotel, Galveston, Texas
35Seawall Buffer, Galveston, Texas
36Seawall, Galveston, Texas
37Beach Growth, Galveston, Texas
38Any Port in a Storm?
39The Decline of Galveston
- In 1900, Houston and Galveston were comparable in
size - It took years for Galveston to recover
- The East Texas oil boom happened during the
recovery and bypassed Galveston - Business and shipping relocated to Houston
- Galveston 60,000
- Houston 1.6 million
40Katrina, 2005
41Coastal Wetland, Louisiana
42Mississippi River Levee
43Mississippi River Levee
44Levee and French Quarter
45New Orleans
46Katrina Flooding
47Katrina Flooding
48The Katrina Disaster
- Could have been much worse
- Storm weakened before landfall (5 to 3)
- Eye passed east of New Orleans
- Many levees failed after peak of storm
- Predictable Disaster
- Poor Individual Preparedness
- Unrealistic Expectations
- Media Sensationalism
- Insufficient FEMA Authority
49Coastal Subsidence in Louisiana
- Compaction of sediment
- Formerly offset by new sediment
- Interception of sediment by dams
- Delta buildup far offshore
- Atchafalaya diversion?
- Sea Level Rise
- Oil drilling?
50Neglected Factors in Louisiana
- Atchafalaya sedimentation
- 6.5 km2 per year
- Channel dredging needed
- Concern over loss of wetlands
- Mississippi is long overdue to shift to the
Atchafalaya - Before locks, 1/3 of Mississippi being diverted
- Diversion will starve other areas of coast
naturally - No amount of sediment will raise New Orleans
51The Great Tsunami
52(No Transcript)
53Banda Aceh
54(No Transcript)
55Waves Approaching Sri Lanka
56Waves Hitting Sri Lanka
57Wave Height and Travel Time