Grams of sodium per kilogram of dissolved ions.
Grams of solution per cubic kilometer of seawater.
Grams of dissolved ions in 1 kilogram of solution.
Grams of water in 1 kilogram of solution.
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Rainfall within subtropical regions has a higher salt content than along the equator.
Precipitation is greater in the subtropics than along the equatorial belt.
Evaporation exceeds precipitation in the subtropical region, whereas the reverse occurs along the equator.
More streams and rivers empty into the ocean within subtropical regions than along the equatorial belt.
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Motion of the surface layer is primarily driven by wind and deflected by the Coriollis force.
The surface layer is heated by the sun.
The temperature of surface water varies with latitude and the seasons.
Most surface water originates near Greenland and Antarctica and afterwards flows as surface water towards the equator.
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Coastlines are always in equilibrium with oceans and therefore never change.
The sea surface is everywhere smooth and flat.
Global sea level has risen and fallen many times throughout Earth history.
Ocean currents generate the tides.
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Neap tide
Ocean gyres
Spring tide
A lunar eclipse
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Global cooling during an ice age
Assembly of continents into a supercontinent.
Decrease in the volume of mid-ocean ridges
Global warming during an interglacial cycle
Removing fish from the oceans
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Crests
Swells
Surf
Breakers
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Wave crests bunch closer together when approaching the beach.
Approaching wave crests align parallel with the coastline in what is known as wave refraction.
Waves speed up when approaching the beach.
Wave crests increase in height when approaching the beach.
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A
B
C
D
E
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A
B
C
D
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Cove
Bay
Headlands
Coastal erosion is the same everywhere
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Beach drift causes beach sand to remain in place.
Longshore currents prevent waves from striking the beach.
Beach drift transports sediment in the same direction as does longshore current.
The zigzag motion of sand describes sediment transport by longshore currents.
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Coastal erosional features
Coastal depositonal features
Wetlands
Coral reefs
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Mangroves
Salt marshes
Bogs
Wave-cut platform
Flood plain
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U-shaped valley
Paternoster lakes
Horn
Lateral moraine
Cirque
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A
B
C
D
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Glacial meltwater
Glacial ice and snow
Terminal moraines
Drumlins
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Terminal moraine
Calving
Crevasses
Cirque
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Small hill or knob of poorly sorted gravel deposited by a melting glacier
Hole in the ground left behind after a large block of ice melts
Sinuous, narrow ridge of coarse sand and gravel formed by a meltwater stream that flowed beneath a glacier
Elongated deposit of till streamlined in the direction of ice movement by a continental glacier
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A
B
C
D
E or F (check explanation for the correct answer)
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Patterned ground forms due to frost action in the soil.
Expansion of water when freezing disrupts the soil and fractures rocks.
Melting of permafrost beneath a building constructed on the ground surface causes the structure to collapse.
Ice wedges develop in fractures below the ground surface.
Areas in subarctic and polar climates where the ground is cold but never freezes.
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Global sea level rose
Plants and animals characteristic of colder climates migrated southward to lower latitudes
Earth's crust in areas covered by glaciers rebounded to higher elevations
Land bridges and continental shelves became submerged under water
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The atmospheric concentration of greenhouse gases such as carbon dioxide and methane have actually decreased over the last 50 years.
Ice cores indicate that global temperatures have been fairly constant over the last few tens of thousands of years.
Atmospheric temperature has been steadily increasing over the last 12 thousand years and we are presently in an interglacial cycle
The concentrations of atmospheric greenhouse gases increase dramatically during periods of glaciation and global cooling.
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Higher sunspot activity pushes Earth's orbit further from the sun, thus cooling the planet
Lower sunspot activity allows more solar radiation to escape the Sun and reach Earth, thus warming the planet
Higher sunspot activity increases the solar wind, which in turn warms Earth's upper atmosphere
The amount of sunspot activity never changes and therefore cannot affect Earth's climate
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100,000
26,000
1
41,000
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Greater snow cover during climatic cooling reduces the activity of carbon dioxide sinks such as photosynthesis and formation of carbonate rocks, thus causing carbon dioxide to build up in the atmosphere
Warming of the climate increases evaporation in the oceans, leading to greater cloud cover such that more solar radiation is reflected back into space.
An increase in plant activity during global warming results in more carbon dioxide being removed from the atmosphere
Climate cooling increases the snow cover on land, thus increasing global albedo and causing more solar radiation to be reflected back into space
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Global climate was cold throughout the entire Cenozoic Era as evidenced by 60 million year old glaciers found today in Antarctica
Cenozoic climate started out cold, then warmed about 30 million years ago, and has since cooled again.
Cenozoic climate was warmest 60 million years ago and has gradually cooled since then, culminating in the Pleistocene Ice Age beginning 2 million years ago
Global climate today is the warmest it has ever been over the last 60 million years
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Plate tectonics
Milankovitch cycles
Changes in overall sunspot activity
Human activity such as burning of fossils fuels
Both C and D
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True
False
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B-horizon
C-horizon
A-horizon
O-horizon
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Consistency
Structure
Permeability
Texture
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Rich in humus
Available water
Good porosity
Presence of soil colloids
Leaching of cations
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Sand and clay only
Clay only
Sand, silt and clay
Humus and sand only
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Cold, dry climate and scarce vegetation
Temperate climate and flat to gently-rolling topography
Dry climate and steep slopes
Area of abundant rainfall but scarce vegetation
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Podzolization
Calcification
Cryoturbation
Laterization
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An O- and A-horizon rich in humus
A hardened layer in the B horizon called caliche
A leached soil high in iron and aluminum
A churned and mixed soil resulting from repeated freezing and thawing
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Surface horizon consists of acid-rich forest litter
Sandy-bleached layer occurs below the A-horizon
Oxides and clays brought down from higher horizons accumulate in the B-horizon
Common in northern coniferous forests
Form from young volcanic ash and cinders
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Ultisols
Histosols
Andisols
Gelisols
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Entisol
Histosol
Vertisol
Aridosol
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Calcification
Cryoturbation
Laterization
Podzolization
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Tundra
Broadleaf forest
Rain forest
Savanna
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Needleleaf forest
Tropical savanna
Mediterranean shrubland
Tropical rain forest
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Monsoonal rains
Stunted, woody shrubs
Southern California is an example
Dry summer climate
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Tropical savannas
Deserts
Temperate rain forest
Montane forest
Alpine tundra
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Tropical rain forest
Tropical savanna
Needleleaf forest
Temperate rain forest
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True
FALSE
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Niche
Habitat
Ecosystem
Web
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Use of fertilizers on crops
Construction of shells by marine organisms
Storage of oil, coal, and gas below Earth's surface
D. Plant photosynthesis E. Subduction of carbon-bearing oceanic sediments and rocks along a convergent plate boundary
F. Release of carbon dioxide into the atmosphere via volcanic eruptions G. Methane escape onto the seafloor via hydrothermal vents near mid-ocean ridges
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Atmospheric oxygen
Carbohydrates (sugars)
Atmospheric nitrogen
Water
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Soil type
Air and soil temperatures
Solar insolation
Amount of precipitation
E. Regional climate F. All of the above
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