Decomposition uses much oxygen while releasing hydrogen sulfide. The reduced oxygen level combined with the release of hydrogen sulfide gives the marsh a rotten egg odor.
Decomposition uses much carbon dioxide while releasing hydrogen sulfide. The reduced carbon dioxide level combined with the release of hydrogen sulfide gives the marsh a rotten egg odor.
Decomposition uses much hydrogen while releasing carbon dioxide. The reduced hydrogen level combined with the release of carbon dioxide gives the marsh a rotten egg odor.
Decomposition uses much hydrogen while releasing sulfur. The reduced hydrogen level combined with the release of sulfur gives the marsh a rotten egg odor.
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It is a seawall. As as result of its presence, wave energy is redirected which enhances the erosion of both the front and sides of the wall.
It is a groin. As as result of its presence, wave energy is redirected which enhances the erosion of the front of the wall.
It is a jetty. As as result of its presence, wave energy is redirected which enhances the erosion of the front of the wall.
It is a breakwater.
Littoral current.
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Groin
Jetty
Seawall
Breakers
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40 miles.
30 miles.
60 miles.
1-2 miles.
Between the swash zone (shoreface where waves break) and the dune
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A microscopic plant that organisms feed on and move with tides and currents.
A microscopic animal that moves with currents and large aquatic organisms.
An organism that helps decompose detritus in the marsh.
An organism that scavengers feed on in the marsh.
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The marsh community supplies virtually all its own needs rather than being dependent on other communities.
The marsh community is able to provide the nutrients for all other barrier island habitats.
The marsh community is the basis of the barrier island community.
The marsh community is fragile and at risk.
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During high tide-incoming tides replenish ocean level salinity. During low tide areas of salt marsh are exposed and may have pools of water that when evaporated leave the salt behind creating salty substrate. Evaporation is a factor in intertidal areas. Heavy rains alter the salinity making the sound less salty.
During low tide-incoming tides replenish ocean level salinity. During low tide areas of salt marsh are exposed and may have pools of water that when evaporated leave the salt behind creating salty substrate. Transpiration is a factor in intertidal areas. Heavy rains alter the salinity making the sound less salty.
During high tide-incoming tides replenish ocean level salinity. During high tide areas of salt marsh are exposed and may have pools of water that when evaporated leave the salt behind creating salty substrate. Evaporation is a factor in intertidal areas. Heavy rains alter the salinity making the sound less salty.
During low tide-incoming tides replenish ocean level salinity. During high tide areas of salt marsh are exposed and may have pools of water that when evaporated leave the salt behind creating salty substrate. Evaporation is a factor in intertidal areas. Heavy rains alter the salinity making the sound less salty.
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Air
Tide pools
Tide line
Substrate
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Salt tolerant
Grows quickly
Predator tolerant
Wind and wave tolerant
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The installation of a jetty to stabilize the Ocean City Inlet in the 1930's has starved northern Assateague Island beaches of sand. This accelerated the landward migration of the island.
Assateague Island has migrated westward more than 1,148 feet (350 m) since 1933! The installation of a seawall to stabilize the Ocean City Inlet in the 1849 starved northern Assateague Island beaches of sand. This accelerated the landward migration of the island.
Assateague Island has migrated westward more than 1,148 feet (350 m) since 1933! The installation of a seawall to stabilize the Ocean City Inlet in the 1849 starved northern Assateague Island beaches of sand. This accelerated the landward migration of the island.The installation of a groin to stabilize the Ocean City Inlet in the 1849 starved northern Assateague Island beaches of sand. This accelerated the landward migration of the island.
In preparation for the Civil War, a seawall was installed to stabilize the Ocean City Inlet in 1849. Since then, Assateague Island has migrated south!
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Bogue Banks
Topsail
Oregon
Bald Head
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Bogue Banks
Topsail
Oregon
Bald Head
Bogue Banks
Topsail
Oregon
Bald Head
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Storm bars form as storm weather erodes the near shore sand bar and beach in preparation for a storm.
Storm bars form as storm weather erodes the berm and creates a sand bar during fair weather.
Storm bars form as the storm sediments overwash the island during a storm.
Storm bars form as wave strength, duration and fetch expand.
1 ft of sea level rise equals 2000 feet of shoreline retreat.
1 ft of sea level rise equals 6 feet of shoreline retreat.
1 ft of sea level rise equals 10,000 feet of shoreline retreat.
1 ft of sea level rise equals 4.6 feet of shoreline retreat.
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With sea level rise, the mainland coastal plain receded faster than the islands are migrated landward.
The Outer Banks are floating seaward due to migration.
The Outer Banks are returning to their original location further out on the continental shelf.
Sound waters in the basin behind the Outer Banks are filling with sand causing the islands to roll seaward.
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That a maritime forest is found in the middle of the widest part of an island.
That barrier islands are long and thin.
That a dune is not found on the sound side of an island.
That the island hasn't much shade from the sun.
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Jetties.
Groins.
Seawalls.
Breakwaters.
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A long shore current is formed as ordinary waves retreat from the shoreline slope causing them to angle towards the dunes creating a current.
A long shore current is formed as overwash waves hit the shoreline slope causing them to angle inward creating a current.
A long shore current is formed as parallel waves hit the beach causing a current to form along the shore.
A long shore current is formed as ordinary waves hit the shoreline slope causing them to angle away creating a current.
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Longshore current.
Tidal current.
Ebb tidal delta.
Flood tidal delta.
Littoral current.
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