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A beach is any area of shoreline affected by winds or water.
A beach is any area of shoreline affected by ordinary waves that includes the nearshore sand bar and berm.
A beach is an area of the shoreline that includes the berm and is affected by ordinary waves.
A beach is only the large area near the berm of the shoreline affected by ordinary waves.
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Organisms need to be able to breathe water or hold their breath for long periods of time.
Organisms need to adapt to alternating between being exposed or submerged.
Organisms need to adapt to alternating between breathing or being submerged.
Organisms need to adapt to alternating between being submerged or holding their breath for long periods of time.
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Laborador/Virginia and the Gulf Stream currents
Gulf of Mexico and Laborador/Virginia currents
Canadian and Gulf of Mexico currents
Coast of Greenland and Gulf Stream currents
Between the swash zone (shoreface where waves break) and the dune
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A Barrier Island is a long, narrow body of sand separated from the mainland by a sound and from other islands by inlets at both ends.
A Barrier Island is a short, wide body of sand separated from the mainland by a sound and from other islands by inlets at both ends.
A Barrier Island is a long, narrow body of sand separated from other islands by a sound.
A Barrier Island is a body of sand separated from the mainland by an inlet.
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Estuary waters are a mixture of tidewater and longshore current.
Estuary waters are a mixture of soundwater and ocean water.
Estuary waters are a mixture of soundwater and littoral drift.
Estuary waters are a mixture of fresh and salt water.
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Estuary deposits
Tidal amplitude
Water turbulence
Coastal plain migration
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The back dune end of the supratidal zone
The movement of sand offshore during a storm
The supratidal ledge of sand at the high tide line
The edge of the swash (shoreface where waves break) zone
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35 ppt
55 ppt
15 ppt
25 ppt
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Fine silt
Loam
Coarse sand
Clay
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Silt
Gravel
Coarse sand
Clay
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The subtidal zone of crashing breakers with swirling sand and shallow water; the intertidal zone, alternately covered and exposed by tidal waters; and the dry, sandy supratidal zone extending to the base of the sand dunes.
The ocean zone of crashing breakers with swirling sand and shallow water; the salt marsh zone, alternately covered and exposed by tidal waters; and the dry, sandy sand dune zone extending to the base of the sand dunes.
The shoreface zone of crashing breakers with swirling sand and shallow water; the intertidal zone, alternately covered and exposed by tidal waters; and the dry, sandy subtidal zone extending to the base of the sand dunes.
The supratidal zone of crashing breakers with swirling sand and shallow water; the intertidal zone, alternately covered and exposed by tidal waters; and the dry, sandy subtidal zone extending to the base of the sand dunes.
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Wind coming off the ocean, the presence of water coming in with the tides and in the space between the sand sediment.
The presence of water coming in with the tides, salt spray and plants.
The wind coming off the ocean, salt spray and plants.
The wind coming off the ocean, the presence of water coming in with the tides and plants.
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At the high tide line.
At the shoreline.
Along the shoreface.
In the intertidal zone.
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Free floating microscopic plants that are the basis of the marine food chain.
Free floating microscopic animals that are the basis of the marine food chain.
Free floating microscopic scavengers that support the marine food chain.
Diatoms that cause red tide and are toxic to the marine food chain.
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Scavengers
Decomposers
Producers
Herbivores
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A gastropod is a mollusk that has one shell. It is a marine snail.
A gastropod is a mollusk that has two shells it is a bivalve or pelecypod with a strong muscular foot.
A gastropod is a mollusk that attaches itself to hard substrate to survive.
A gastropod is a mollusk that has an internal shell like a squid.
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Both organisms burrow rapidly into the sand. The coquina clam burrows as a wave recedes. The mole card burrows backward each time a wave advances.
Both organisms ride the surf to avoid the receding or advancing waves.
Both organisms hibernate to avoid the receding or advancing waves.
Though born on the ocean side of the barrier island, both organisms move to the sound to avoid the receding or advancing waves.
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Saltation.
Transpiration.
Ocean waves.
Mineralization.
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Moon and sun’s gravitational pull on Earth.
Moon's gravitational pull on Earth.
Sun’s gravitational pull on Earth.
The oceans wave energy.
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Ghost crabs breathe through gills which must be wet with ocean water daily.
Once ghost crabs come on land, they breathe air.
Ghost crabs breathe both air and water because they were born in the ocean and as adults live in the supratidal zone.
Ghost crabs breathe air only. As young in the ocean they came to the surface for air and continued to do so when moving to the supratidal zone.
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Waves
Tides
Longshore current
Winds
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Birth of an inlet
Nor'easter wind tide
Formation of a tidal delta
Spring tide
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Spring
Summer
Winter
Fall
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30 - 60 feet
10 - 20 feet
20 - 40 feet
40 - 70 feet
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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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This kind of hard stabilization is a groin.
This kind of hard stabilization is a jetty.
This kind of hard stabilization is a seawall.
This kind of hard stabilization is a breakwater.
Littoral current.
Seawall
Jetty
Groin
Breakers
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The movement of sand by the long shore current along the shoreline.
The tidal accumulation of sand parallel to the island.
The tidal flow of sand into the sound accumulating in a flood tidal delta.
The tidal movement of sand along the sound side of the island.
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Detritus and Rainfall
Rainfall and Nutrients
Nutrients and Salt
Detritus and Nutrients
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The seaward side.
The leeward side.
The sand shadow side.
The sound side.
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The island is wide.
It has a high dune.
It is migrating landward.
The island has been overwashed many times.
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Storm events that separated the spits from their sand supply and gradual sea level rise in the high latitudes that flooded the coastal lowlands behind the sand spit dune ridges.
Gradual sea level rise in the high latitudes that flooded the coastal lowlands behind the sand spit dune ridges and wave erosion caused the beach front to erode, the island to migrate quicker than the mainland retreated.
Wave erosion caused the beach front to erode, the island to migrate quicker than the mainland retreated and the longshore current added sand to the inlets, creating tidal deltas that added to the backside of the islands.
The longshore current added sand to the inlets, creating tidal deltas that added to the backside of the islands and storm events that separated the spits from their sand supply
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Predators and Evaporation
Transpiration and Predators
Dehydration and Evaporation
Transpiration and Evaporation
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Salt spray from wind kills back the tips of the tree and shrub branches causing them to look sheard and grow stunted and twisted.
Salt spray from wind nourishes the trees and shrubs causing their leaves to grow long and wide.
Salt spray from wind prevents trees and shrubs from growing on the back dune.
Dune plants: are evergreen plants with thin, needle like leaves tSalt spray from wind protects the trees and shrubs with a layer of salt covering.hat can tolerate wind, water and salt.
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Strong winds, whipping sands, glaring sun.
Strong winds, waves, and whipping sand.
Strong waves, glaring sun and whipping sands.
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There is little or no decaying plant and animal material to enrich the dunes.
There is too much Oxygen.
There is too much Hydrogen and Oxygen.
The organisms in a dune habitat consume more Nitrogen then they produce.
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Ocean breezes provide steady in flow of wind.
Dune plants provide Oxygen to the dune.
Ocean spray provides Oxygen in the water that mists the dunes.
All of these.
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Waves deposit the fine sand on to the dune.
Saltation carries only the finest of beach sand.
Saltation mixes salt with sand making it more fine.
Fine sand is more porous
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Surface creep occurs when saltating grains of sand strike heavier grains larger than one millimeter in diameter causing the heavier grains a slight forward movement along the surface.
Surface creep occurs when saltating grains of sand strike finer grains smaller than one millimeter in diameter causing the finer grains a slight forward movement along the surface.
Surface creep occurs when saltating grains of sand strike heavier grains larger than one millimeter in diameter causing the finer grains a slight forward movement along the surface.
Surface creep occurs when saltating grains of sand strike heavier grains larger than one millimeter in diameter causing the heavier grains to suspend in the air from their movement along the surface.
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Fluid threshold is the wind speed necessary for sand to start saltating under the direct pressure of the wind.
Fluid threshold is the wind speed necessary to maintain saltation once it has begun
Fluid threshold is how all the surfaces respond to each other as they move.
Fluid threshold is wind speeds above 20 mph that occur above the windy side of a dune.
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Sand tends to accumulate any place where there is a sufficient reduction of wind energy in the direction that sand drifts in and any obstacle, such as a rock outcrop or a stand of vegetation, forces sand accumulation by lowering the wind speed.
Sand tends to accumulate any place where there is a abundant wind velocity in the direction that sand drifts in and any obstacle, such as a rock outcrop or a stand of vegetation, forces sand accumulation by lowering the wind speed.
Sand tends to accumulate any place where there is a sufficient reduction of sand in the sand drifts in and any obstacle, such as a rock outcrop or a stand of vegetation, forces sand accumulation by sustaining the wind speed.
Sand tends to accumulate any place where there is a sufficient reduction of sand in the sand drifts in and any obstacle, such as a rock outcrop or a stand of vegetation, forces sand accumulation by lowering the wind speed.
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#1 Leeward and # 2 Windward
#1 Windward and # 2 Leeward
#1 Windward and # 2 Saltation
#1 Sand Shadow and # 2 Leeward
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A sand shadow is formed on the leeward side of the dune as that side is starved of sand and its steep shear cliff that creates a shadow.
A sand shadow is formed on the windward side of the dune as that side is starved of sand and its steep shear cliff that creates a shadow.
A sand shadow is formed on the leeward side of the dune as that side has a steep shear cliff that creates a shadow.
A sand shadow is formed on the ocean side of the dune during saltation when the scarp creates a shadow.
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Salt tolerant
Grows quickly
Predator tolerant
Wind and wave tolerant
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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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The diagram shows how sea level rise causes barrier islands to migration upslope toward the mainland on the continental shelf.
The diagram shows the formation of a barrier island on the continental slope.
The diagram rising sea level erosion of a barrier islands on the continental slope.
The diagram shows the migration of a barrier island.
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Bottom material ocean organisms live in or on.
Bottom material found in the ocean.
Bottom material organisms live in or on.
Subtidal nutrients.
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The intertidal zone is between the high and low tide lines.
The intertidal zone is above the high tide line.
The intertidal zone is below the high tide line.
The intertidal zone is between the sand bar and the berm.
The intertidal zone is between the swash zone (shoreface where waves break) and the dune.
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The subtidal zone is between the high and low tide lines.
The subtidal zone is above the high tide line.
The subtidal zone is always covered by water, below the low tide water line.
The subtidal zone is between the sand bar and the berm.
The subtidal zone is between the swash zone (shoreface where waves break) and the dune.
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The supratidal zone is between the high and low tide lines
The supratidal zone is above the high tide line.
The supratidal zone is below the high tide line.
The supratidal zone is between the sand bar and the berm.
The supratidal zone is between the swash zone (shoreface where waves break) and the dune.
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