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United States Coasts
 Atlantic coast
 Pacific coast
 Gulf coast
© 2011 Pearson Education, Inc.
1. Atlantic Coast
 Most coasts open to storm wave attack
 Barrier islands common from Massachusetts south
 Bedrock
 Florida bedrock is resistant limestone.
 Northward through New Jersey is comprised of easily
erodable recent deposits.
 New York through Maine has glacier-affected rocks.
© 2011 Pearson Education, Inc.
Atlantic Coast
 Strong storms called nor’easters can damage the coast
north of Cape Hatteras, NC.
 Nor’easters can generate storm waves
up to 6 meters (20 feet).
© 2011 Pearson Education, Inc.
Atlantic Coast
 Barrier islands
 Drowned river
valleys
© 2011 Pearson Education, Inc.
2. Gulf Coast
 Low tidal range
 Generally low wave energy
 Tectonically subsiding
 Mississippi delta dominates
 Locally sea level rises due to compaction of delta
sediments
 Average rate of erosion is 1.8 meters
(6 feet) per year
© 2011 Pearson Education, Inc.
3. Pacific Coast
 Tectonically rising
 Experiencing less erosion than Atlantic or Gulf
coasts
 Open exposure to high energy waves
 Average rate of erosion 0.005 meter
(0.016 feet) per year
© 2011 Pearson Education, Inc.
Stabilization
 Structures built to decrease coastal erosion and
interfere with sand movement
 Also called armoring of the shore
 Often results in unwanted outcomes
 Some structures may increase wave erosion
© 2011 Pearson Education, Inc.
Stabilization
 Four major types of stabilization structures:
1. Groins and groin fields
2. Jetties
3. Breakwaters
4. Seawalls
© 2011 Pearson Education, Inc.
1. Groins and Groin Fields
 Built perpendicular to
the beach
 Often made of rip rap, or
large blocky material
 Traps sand upcoast,
which can cause erosion
downstream of the
longshore current
 May necessitate a groin
field, or a series of groins
built along a beach
© 2011 Pearson Education, Inc.
2. Jetties
 Built perpendicular to shore
 Built in pairs
 Built to protect harbor entrances
© 2011 Pearson Education, Inc.
3. Breakwaters
 Built parallel to a shoreline
 Designed to protect harbors from waves
 Can cause excessive erosion, requiring dredging to
keep area stable
© 2011 Pearson Education, Inc.
Seawalls
 Destructive to environment
 Designed to armor coastline
and protect human
developments
 One large storm can remove
beach
 Wave activity eventually
undermines seawall
structure; need continual
repair or will collapse
© 2011 Pearson Education, Inc.
Alternatives to Hard Stabilization
Three major alternatives
1. Construction restrictions
2. Beach replenishment
3. Relocation
© 2011 Pearson Education, Inc.
Alternatives to Hard Stabilization
1. Construction restrictions
 Simplest alternative
 Limit building near shorelines
© 2011 Pearson Education, Inc.
Alternatives to Hard Stabilization
2. Beach replenishment
 Sand added to beach/longshore current
 Expensive; costs between $5 and $10 per
cubic yard
 Sand must be dredged from elsewhere.
© 2011 Pearson Education, Inc.
Alternatives to hard stabilization
 Relocation
 Move structures rather than protect them in areas
of erosion
© 2011 Pearson Education, Inc.

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Notes - United States Coasts & Stabilization

  • 1. United States Coasts  Atlantic coast  Pacific coast  Gulf coast © 2011 Pearson Education, Inc.
  • 2. 1. Atlantic Coast  Most coasts open to storm wave attack  Barrier islands common from Massachusetts south  Bedrock  Florida bedrock is resistant limestone.  Northward through New Jersey is comprised of easily erodable recent deposits.  New York through Maine has glacier-affected rocks. © 2011 Pearson Education, Inc.
  • 3. Atlantic Coast  Strong storms called nor’easters can damage the coast north of Cape Hatteras, NC.  Nor’easters can generate storm waves up to 6 meters (20 feet). © 2011 Pearson Education, Inc.
  • 4. Atlantic Coast  Barrier islands  Drowned river valleys © 2011 Pearson Education, Inc.
  • 5. 2. Gulf Coast  Low tidal range  Generally low wave energy  Tectonically subsiding  Mississippi delta dominates  Locally sea level rises due to compaction of delta sediments  Average rate of erosion is 1.8 meters (6 feet) per year © 2011 Pearson Education, Inc.
  • 6. 3. Pacific Coast  Tectonically rising  Experiencing less erosion than Atlantic or Gulf coasts  Open exposure to high energy waves  Average rate of erosion 0.005 meter (0.016 feet) per year © 2011 Pearson Education, Inc.
  • 7. Stabilization  Structures built to decrease coastal erosion and interfere with sand movement  Also called armoring of the shore  Often results in unwanted outcomes  Some structures may increase wave erosion © 2011 Pearson Education, Inc.
  • 8. Stabilization  Four major types of stabilization structures: 1. Groins and groin fields 2. Jetties 3. Breakwaters 4. Seawalls © 2011 Pearson Education, Inc.
  • 9. 1. Groins and Groin Fields  Built perpendicular to the beach  Often made of rip rap, or large blocky material  Traps sand upcoast, which can cause erosion downstream of the longshore current  May necessitate a groin field, or a series of groins built along a beach © 2011 Pearson Education, Inc.
  • 10. 2. Jetties  Built perpendicular to shore  Built in pairs  Built to protect harbor entrances © 2011 Pearson Education, Inc.
  • 11. 3. Breakwaters  Built parallel to a shoreline  Designed to protect harbors from waves  Can cause excessive erosion, requiring dredging to keep area stable © 2011 Pearson Education, Inc.
  • 12. Seawalls  Destructive to environment  Designed to armor coastline and protect human developments  One large storm can remove beach  Wave activity eventually undermines seawall structure; need continual repair or will collapse © 2011 Pearson Education, Inc.
  • 13. Alternatives to Hard Stabilization Three major alternatives 1. Construction restrictions 2. Beach replenishment 3. Relocation © 2011 Pearson Education, Inc.
  • 14. Alternatives to Hard Stabilization 1. Construction restrictions  Simplest alternative  Limit building near shorelines © 2011 Pearson Education, Inc.
  • 15. Alternatives to Hard Stabilization 2. Beach replenishment  Sand added to beach/longshore current  Expensive; costs between $5 and $10 per cubic yard  Sand must be dredged from elsewhere. © 2011 Pearson Education, Inc.
  • 16. Alternatives to hard stabilization  Relocation  Move structures rather than protect them in areas of erosion © 2011 Pearson Education, Inc.