This quiz prepares students for an exam on coastal environments, covering zones like intertidal and subtidal, and definitions relevant to coastal geology.
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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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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Saltation.
Transpiration.
Ocean waves.
Mineralization.
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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.
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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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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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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 suspension, #2 saltation, #3 creep
#1 saltation, #2 suspension, #3 creep
#1 suspension, #2 saltation, #3 impact threshold
#1 fluid threshold, #2 saltation, #3 impact threshold
Salt tolerant
Grows quickly
Predator tolerant
Wind and wave tolerant
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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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Longshore current
Currents and tides
Distance from shore and waves
Currents and gravitational pull of the moon
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When an organism dies, scavengers consume much of the organic debris, particularly animal debris. Decomposers are bacteria and fungi that complete the final step in the food web.
When an organism dies, decomposers scavenge the remains, there is no difference between decomposers and scavengers.
When an organism dies scavengers consisting of bacteria and fungi complete the process in the food web.
Both are detrital. When an organism dies uneaten debris is broken down by wave action, wind, heat, forming detritus
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The original source of energy is the sun.
The original source of energy is the ocean.
The original source of energy are the producers.
The original source of energy is the moon and tides.
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Six key shoreline environmental factors: climate, water level, salinity, water temperature, air temperature and substrate.
Six key shoreline environmental factors: currents, water level, salinity, water temperature, air temperature and substrate.
Six key shoreline environmental factors: climate, tides, salinity, water temperature, air temperature and substrate.
Six key shoreline environmental factors: climate, water level, salinity, water temperature, air temperature and sand supply.
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Energy is passed through the community through feeding relationships.
Energy is passed through the community as organisms move about their habitat.
Energy is passed through the community through organism decomposition.
Energy is passed through the community as organisms breed and grow.
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Water has a high specific heat causing it to take much energy for water to change 1º in temperature change. Air is less dense due to the movement of gas molecules.
Water has a low specific heat causing it to use much energy for water to change 1º in temperature change. Air is less dense than water.
Water has a high specific heat causing it to use much energy for water to change 1º in temperature change. Air is more dense than water due to the abundance of gas particles in air.
Water has a low specific heat causing it to use much energy for water to change 1º in temperature change. Air is more dense than water due to all the gas particles in air.
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Plankton, tides.
Zooplankton, waves.
Phytoplankton, waves.
Plankton, waves.
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Moon and sun’s gravitational pull on Earth.
Earth's rotation and its gravitational pull.
Sun’s gravitational pull on Earth.
The oceans wave energy.
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A radula is mouth device that looks like spiked tooth-like strap used to drill into a pelecypod (bivalve) which is its prey.
A radula is a large muscular foot used to pry open the shell of a pelecypod (bivalve) which is its prey.
A radula is a spiked foot like belt that wedges into a pelecypod (bivalve) which is its prey.
A radula is a chemosensitive mouth device that is used to poison a pelecypod (bivalve) which is its prey.
How far the tidal zones extend in a habitat.
How far the longshore current moves sand.
How far the overwash fan stretches into the sound.
How far the littoral drift carries and deposits sand.
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0.6 and 1.3 meters
0.1 and 2.0 meters
.01 and .002 meters
.5 and 2.0 meters
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Ocean, Ocean Beach, Sand Dune, Maritime Forest, Salt Marsh, Sound, Tidal Flat.
Ocean, Ocean Beach, Sand Dune, Maritime Forest, Salt Marsh, Sound, Rock Jetty.
Ocean Beach, Ocean, Sand Dune, Maritime Forest, Salt Marsh, Sound, Tidal Flat.
Ocean, Longshore Current, Sand Dune, Maritime Forest, Salt Marsh, Sound, Tidal Flat.
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