This quiz evaluates knowledge on coastal environments, covering beach definitions, substrate, and organism adaptations in different zones, plus regional climatic influences.
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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Moon and sun’s gravitational pull on Earth.
The gravitational pull of the tilt of the Earth on its axis.
Sun’s gravitational pull on Earth.
The oceans wave energy.
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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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Overwash fan
Berm
Shoreface
Dune
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Rollover.
Littoral drift.
Longshore current.
Saltation
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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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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.
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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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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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30 - 60 feet
10 - 20 feet
20 - 40 feet
40 - 70 feet
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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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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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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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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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Estuary deposits
Tidal amplitude
Water turbulence
Coastal plain migration
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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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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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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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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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Spring
Winter
Summer
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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Birth of an inlet
Nor'easter wind tide
Formation of a tidal delta
Spring tide
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Longshore current.
Tidal current.
Ebb tidal delta.
Flood tidal delta.
Littoral current.
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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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Scavengers
Decomposers
Producers
Herbivores
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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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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.
1Estuary waters are a mixture of fresh and salt water.
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Salt spray
Oxygen
Plant nitrogen
Water (Hydrogen + Oxygen)
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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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The higher the dune the larger the vegetation behind it.
The higher the dune the smaller the vegetation behind it.
The dune height does not affect the vegetation behind it.
The lower the dune the larger the vegetation behind it.
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Eastern Oyster.
Blue or ribbed mussel.
Mud snail.
Scallop
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This crab lives inside the shells of oysters and other bivalves and at times may eat the muscle tissue of the "host" oyster.
This crab moves into the shell of a dead oyster and inhabits its shell for protection.
The oyster crab is a host organism for oysters to feed upon.
The oyster crab hides within a bed of oysters to protect itself.
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25-35 ppt.
10-25 ppt.
15-25 ppt.
10-30 ppt
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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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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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Dune plants: some have thick, waxy leaves, some that close curl inward and turn in a vertical position to reduce sun expose.
Dune plants: can tolerate changes in salinity and can withstand different levels of salinity.
Dune plants: are made up of brown and red marine leaft grasses that tolerate water, wind, and salt.
Dune plants: are evergreen plants with thin, needle like leaves that can tolerate wind, water and salt.
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Groin
Jetty
Seawall
Breakers
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Salt tolerant
Grows quickly
Predator tolerant
Wind and wave tolerant
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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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