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Oceanic Overwash

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The washover fan is a fan-shaped accumulation of sand and shell that is ... Sediment may bury marshland on the lagoon side, building up the back side of the ... – PowerPoint PPT presentation

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Title: Oceanic Overwash


1
Oceanic Overwash
2
Beach Diagram
3
Oceanic Overwash
  • The washover fan is a fan-shaped accumulation of
    sand and shell that is deposited in a thin layer
    during intense storm conditions when part or all
    of the beach-dune system is overtopped or
    breached by incoming waves and storm surges
  • Fans may come together to form a washover apron
  • Sediment accumulations may be a few tens of
    centimeters or up to 1 meter thick
  • Sediment will cover vegetation on the back side
    of the island, but plants can grow up through the
    sediment, reworking the layering of the sediments

4
Overwash
5
Oceanic Overwash
6
Oceanic Overwash and Channels
7
Overwash and Storms
  • Strong wind and waves causes storm surges to wash
    over low dunes or create breaks in the dune
    system
  • New inlets can be formed in low lying areas on
    the island

8
Overwash
9
Overwash effects in Buxton, NC
10
Graph of changes after Dennis to Buxton, NC
11
Overwash after Hurricane Dennis
12
Washover After Dennis
13
Overwash and Transgression
  • Sediment is transferred to the back side of the
    island by overwash
  • Sediment may bury marshland on the lagoon side,
    building up the back side of the island
  • Overwash process erodes sediment from the front
    side and carries it to the back
  • The combination of erosion on the front and
    buildup on the back of the island are factors
    that lead to island transgression

14
Man-made Interventions
  • Groins-A shore protection structure built
    (usually perpendicular to the shoreline) to trap
    lateral drift or retard erosion of the shore
  • Jetties-structures intended to keep sand from
    flowing into a channel intended to protect an
    inlet
  • Sea walls-rock or concrete structures built
    parallel to the shoreline intended to protect
    buildings by repelling the sea
  • Beach replenishment-Building up the beach system
    by depositing sand

15
Beach Replenishment
  • Beach replenishment is used to add dredged sand
    or sediment from an inland source to the beach
    system.
  • Procedure is expensive and not a permanent
    solution
  • Some prefer this temporary fix to the more
    permanent structures that may cause more damage
    in the long run

16
Photos of Renourishment at Kure Beach
17
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19
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20
Groins
21
Groins
22
Jetty
23
Sea Wall
24
Effects of Sea Walls
25
Sea Wall at Shell Island
26
Sea Wall
27
Myrtle Beach
28
Disappearance of Islands
Long-term rates of change between 1855 and 1989
show both accretion and erosion for barrier
island shorelines facing Louisianas coast.
Between the late 1800s and the 1980s, deposits
left from washovers caused some of these
shorelines to migrate landward at rates up to
24.0 meters per year. Erosion, in contrast, has
caused loss on other shorelines at rates from 1
to 5 meters per year.
29
Disappearance of Islands
The timeline above shows anticipated years of
disappearance for several of Louisianas barrier
islands through 2110. Although these barrier
islands are in danger, other more stable barriers
exist. For example, Grand Isle has a life
expectancy about 900 years longer than that of
Timbalier Island
30
On-line References
  • http//books.nap.edu/books/030904806/html/70.html
    pagetop
  • http//coastal.er.usgs.gov/hurricanes/dennis/buxto
    n/
  • http//members.nbci.com/igorz/MIWO.html
  • http//www.beachbrowser.com/Archives/Environment/A
    /Barrier-Islands-Always-changing.ht
  • http//www.csc.noaa.gov/products/nchaz/htm/lidtopo
    .htmhttp//www.lacoast.gov/Programs/CWPPRA/Waterma
    rks/Fall99/barrier.fa99.htm

31
References
  • http//www.ncsu.edu/coast/shell/migration/migratio
    n.html
  • http//www.ncsu.edu/coast/shell/terms.html
  • http//www.salem.mass.edu/lhanson/gls214/gls214_t
    ec_clas.htm
  • http//www.seafriends.org.nz/oceano/beacheng.htms
    ea20walls
  • http//www.seashell.com/kbphotos.htm
  • http//www.vcrlter.virginia.edu/bph/NSFTalk/NSFTa
    lk.html

32
References
  • Davis, Richard, 1994, The Evolving Coast W.H.
    Freeman and Company, New York, pp 166-183.
  • Fox, William, 1983. At the Seas Edge,
    Prentice-Hall, Inc., pp. 151-175.
  • Pilkey, Orrin, 1990. The Beaches are moving
    (videorecording).
  • Schwartz, Maurice, 1973, Benchmark Papers in
    Geology Barrier Islands Dowden, Hutchinson and
    Ross, Inc., Stroudsburg, Pa.
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