Are you ready for this "End of coastal 8th grade quiz?" A coastal area is a part where the land meets the ocean. The quiz here deals with the end of the coastal area, and the questions here are about coastal areas and beaches. We will be testing how well you understand this part and whether you can answer these questions or not. So, do you think you are up to this challenge? If yes, then try your best and score the best.
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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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Not porous, densely packed, uniform grain size
Most porous, loosely packed large grain size
Low porosity, mixed grain sizes
Porous, mixed grain size
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Silt
Gravel
Coarse sand
Clay
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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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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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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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Barrier island migration.
Barrier island rollover.
Barrier island formation
Barrier island shoreface erosion.
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Rollover.
Littoral drift.
Longshore current.
Saltation
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Air & Water
Organic matter and minerals
Rocks and minerals
Organic matter and water
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Spongy, soft, earthy, twiggy
Small grained, light weight
Smooth, slippery, soft, not sticky
Gritty, grainy and coarse
Sticky, muddy, tiny grained
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Gritty, grainy and coarse
Smooth, slippery, soft, not sticky
Small grained, light weight
Spongy, soft, earthy, twiggy
Sticky, muddy, tiny grained
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Dinoflagellates
Diatoms
Gastropods
Pelecypods
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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. Salt spray from wind protects the trees and shrubs with a layer of salt covering it that can tolerate wind, water and salt.
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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.
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.
That the island is wide because 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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Small grained, light weight
Smooth, slippery, soft, not sticky
Gritty, grainy and coarse
Sticky, muddy, tiny grained
Spongy, soft, earthy, twiggy
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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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Birth of an inlet
Nor'easter wind tide
Formation of a tidal delta
Spring tide
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30 - 60 feet
10 - 20 feet
20 - 40 feet
40 - 70 feet
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Longshore current.
Tidal current.
Ebb tidal delta.
Flood tidal delta.
Littoral current.
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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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Estuary waters are a mixture of tidewater and longshore current.
Estuary waters are a mixture of groundwater and ocean water.
Estuary waters are a mixture of groundwater and littoral drift.
Estuary waters are a mixture of fresh and salt water.
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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.
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 is 15-25 ppt. in an estuary, 35 ppt. in the ocean.
How much salt is in the water
The movement of sand along the shoreline
The affect of salt spray on barrier island plants
Saltation is the movement of sand by 10 mph or greater winds that creates dune.
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For dune formation to occur the following is required: a large supply of sand, wind speeds capable of moving sand, and an ideal location for sand to accumulate.
For dune formation to occur the following is required: a large supply of sand, wind speeds capable of moving sand, and a shore face that extends from the near shoe sandbar to the berm.
For dune formation to occur the following is required: a large supply of sand, wind speeds greater than 20 mph, and a shore face that extends from the near shoe sandbar to the berm.
For dune formation to occur the following is required: a large supply of sand, wind speeds less than 10 mph, and a shore face that extends from the near shoe sandbar to the berm.
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Groin
Jetty
Seawall
Breakers
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Ocean
Ocean beach
Dune
Salt marsh
Tidal flat
Maritime forest
Sound
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Not porous, densely packed, uniform grain size
Porous, void space, packed large grain size
Low porosity, mixed grain sizes
Porous, mixed grain size
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Sticky, muddy, tiny grained
Spongy, soft, earthy, twiggy
Small grained, light weight
Smooth, slippery, soft, not sticky
Gritty, grainy and coarse
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Silt
Coarse Sand
Fine sand
Clay
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Clay
Coarse sand
Fine sand
Silt
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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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Between the high and low tide lines
Above the high tide line
Below the high tide line
Between the sand bar and the berm
Between the swash zone (shoreface where waves break) and the dune
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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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An organism with a hard shell that encases a soft muscle body
An organism with a soft shell and a hard interior skeleton
A bottom dwelling organism that breathes water and uses siphons to feed
A bottom dwelling organism that uses a muscular foot to dig and capture its prey
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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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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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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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Bogue Banks
Topsail
Oregon
Bald Head
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