This 'End of Coastal Unit Exam Practice' assesses knowledge on coastal environments, focusing on definitions and ecological zones. It evaluates understanding of beach dynamics, substrate characteristics, and organism adaptations in various tidal zones.
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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Birth of an inlet
Nor'easter wind tide
Formation of a tidal delta
Spring tide
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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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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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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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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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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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Step 1: Sea level is low at the peak of glacial covering of the land.
Step 2: Glacial melt water floods coastal plain low land filling trenches and river valleys with fresh water and forming estuaries.
Step 3: Coastal plain lowland flooding continues to wash sediment to form barrier island spits form along the coastal headlands.
Step 4: Sea level rise and storms that breach the barrier spits separate the barrier spits from the mainland. Cutting them off from their original longshore sand supply. The gradual continued rise in sea level floods the low coastal plain on the mainland causing mainland shore retreat further separating and isolating the barrier island from the mainland.
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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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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.
Tidal current.
Ebb tidal delta.
Flood tidal delta.
Littoral current.
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Barrier island migration.
Barrier island rollover.
Barrier island formation
Barrier island shoreface erosion.
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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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Seawall
Jetty
Groin
Breakers
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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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Salt tolerant
Grows quickly
Predator tolerant
Wind and wave tolerant
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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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#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
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Fine silt
Loam
Coarse sand
Clay
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Silt
Gravel
Coarse sand
Clay
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Scavengers
Decomposers
Producers
Herbivores
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30 - 60 feet
10 - 20 feet
20 - 40 feet
40 - 70 feet
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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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A unit of life is an ecological community with plant and animal components acting together as an interdependent group.
A unit of life is an ecological community that looks at nature as complete.
A unit of life is an ecological community that is 15-25 ppt. in an estuary, 35 ppt. in the ocean.
A unit o life is an ecological community that is diverse.
#1 sand, #2 silt, #3 clay
#1 course sand, #2 fine sand , #3 silt
#1 rock, #2 sand, #3 silt
#1 mud, #2 silt, #3 clay
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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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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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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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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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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#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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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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Longshore current
Currents and tides
Distance from shore and waves
Currents and gravitational pull of the moon
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Three basic components of a food web are producers, consumers and decomposers.
Three basic components of a food web are producers, consumers, scavengers and decomposers.
Three basic components of a food web are producers, bacteria and fungi.
Three basic components of a food web are autotrophs, heterotrophs and heliotrophs.
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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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Fall.
Winter.
Spring.
Summer.
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Dinoflagellates cause 'red tides' when sudden blooms of certain species occur. Tiny whiplike tails enable them to swirl about in the water.
Diatoms cause 'red tides' when sudden blooms of certain species occur. Tiny whiplike tails enable them to swirl about in the water.
Zooplankton cause 'red tides' when sudden blooms of certain species occur. Tiny whiplike tails enable them to swirl about in the water.
Amphipods cause 'red tides' when sudden blooms of certain species occur. Tiny whiplike tails enable them to swirl about in the water.
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Spring
Summer
Winter
Fall
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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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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.
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With sea level rise, the mainland coastal plain receded faster than the islands had 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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35 ppt
55 ppt
15 ppt
25 ppt
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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.
Step 1: Sea level is low at the peak of glacial covering of the land.
Step 2: Glacial melt water floods coastal plain low land filling trenches and river valleys with fresh water and forming estuaries.
Step 3: Coastal plain lowland flooding continues to wash sediment to form barrier island spits form along the coastal headlands.
Step 4: Sea level rise and storms that breach the barrier spits separate the barrier spits from the mainland. Cutting them off from their original longshore sand supply. The gradual continued rise in sea level floods the low coastal plain on the mainland causing mainland shore retreat further separating and isolating the barrier island from the mainland.
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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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Spring
Winter
Summer
Fall
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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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