Environmental geology is an applied science that pertains to the practical application of the factors in geology and the solving of environmental problems. It involves the application of the findings of geologic research and the difficulties of the utilization of land. In this quiz, you will be concerned with what is true of surface water in the oceans and which See morewaveforms closest to the beach. You clearly need to try this terrific quiz.
A
B
C
D
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Soil type / Regional climate
Air and soil temperatures
Solar insolation
Amount of precipitation
All of the above
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Plate tectonics
Milankovitch cycles
Changes in overall sunspot activity
Human activity such as burning of fossils fuels
Both C & D
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The sea surface is everywhere smooth and flat.
Global sea level has risen and fallen many times throughout Earth history.
Coastlines are always in equilibrium with oceans and therefore never change.
Ocean currents generate the tides.
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Ocean gyres
Spring tide
A lunar eclipse
Neap tide
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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
Lower sunspot activity allows more solar radiation to escape the Sun and reach Earth, thus warming the planet
Higher sunspot activity pushes Earth's orbit further from the sun, thus cooling the planet
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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.
Most surface water originates near Greenland and Antarctica and afterwards flows as surface water towards the equator.
The temperature of surface water varies with latitude and the seasons.
Surf
Crests
Breakers
Swells
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A
B
C
D
E
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A
B
C
D
E
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True
False
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Tropical rain forest
Tropical savanah
Needleleaf forest
Temperate rain forest
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Producers
Primary consumers
Secondary consumers
Tertiary consumers
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An ecosystem is a pathwork of habitats
Once an individual patch (habitat) arises, it will never fail
Adjoining patches may be at different stages of development
When existing organisms within a patch are disturbed or removed, a new community can emerge to fill the void
Cove
Bay
Headlands
Coastal erosion is the same everywhere
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Wetlands
Coral reefs
Coastal depositional features
Coastal erosion features
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Bogs
Salt marshes
Mangroves
Wave-cut platform
Flood plain
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Leaching of cations
Available water
Good porosity
Presence of soil colloids
Rich in humus
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Sand and clay only
Clay only
Sand, silt and clay
Humus and sand only
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Leaf
Caterpillar on the leaf
Bobolink bird ready to devour the caterpillar
Hawk attacking the bobolink bird
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Global cooling during an ice age
Assembly of continents into a supercontinent.
Decrease in the volume of mid-ocean ridges
Removing fish from the oceans
Global warming during an interglacial cycle
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A
B
C
D
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41,000
26,000
1
100,000
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Cold, dry climate and scarce vegetation
Area of abundant rainfall but scarce vegetation
Dry climate and steep slopes
Temperate climate and flat to gently-rolling topography
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Habitat
Web
Niche
Ecosystem
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Agricultural ecosystems with single crops like wheat generally do not require fertilizers or pesticides to remain vibrant
Ecosystems with large numbers of species are less likely to survive relative to ecosystems containing only a few species
Greater biodiversity in an ecosystem results in greater stability and greater productivity Agricultural ecosystems with single crops like wheat are more stable than ecosystems containing many different crops
Agricultural ecosystems with single crops like wheat are more stable than ecosystems containing many different crops
Rainfall within subtropical regions has a higher salt content than along the equator.
More streams and rivers empty into the ocean within subtropical regions than along the equatorial belt.
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.
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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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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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Savanna
Rain forest
Broadleaf forest
Tundra
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A natural disaster reduces the number of species within an ecosystem
Any new variant within a large population is quickly swamped by interbreeding with normal individuals
A small group is separated (isolated) from the larger (main) population and eventually evolves into a new species
Several different species eventually evolve into one common species
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Structure
Permeability
Consistency
Texture
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Tropical Savanna
Mediterranean shrubland
Needleleaf forest
Tropical rain forest
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Grams of solution per cubic kilometer of seawater.
Grams of water in 1 kilogram of solution.
Grams of dissolved ions in 1 kilogram of solution.
Grams of sodium per kilogram of dissolved ions.
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Calving
Cirque
Terminal moraine
Crevasses
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Hole in the ground left behind after a large block of ice melts
Small hill or knob of poorly sorted gravel deposited by a melting glacier
Elongated deposit of till streamlined in the direction of ice movement by a continental glacier
Sinuous, narrow ridge of coarse sand and gravel formed by a meltwater stream that flowed beneath a glacier
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Waves speed up when approaching the beach.
Wave crests bunch closer together when approaching the beach.
Wave crests increase in height when approaching the beach.
Approaching wave crests align parallel with the coastline in what is known as wave refraction.
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Ice cores indicate that global temperatures have been fairly constant over the last few tens of thousands of years.
The concentrations of atmospheric greenhouse gases increase dramatically during periods of glaciation and global cooling.
Atmospheric temperature has been steadily increasing over the last 12 thousand years and we are presently in an interglacial cycle
The atmospheric concentration of greenhouse gases such as carbon dioxide and methane have actually decreased over the last 50 years.
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Water
Atmospheric nitrogen
Carbohydrates (sugars)
Atmospheric oxygen
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Calcification
Cryoturbation
Laterization
Podzolization
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Tropical savannas
Deserts
Temperate rain forest
Montane forest
Alpine Tundra
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Release of carbon dioxide into the atmosphere via volcanic eruptions
Plant photosynthesis / Methane escape onto the seafloor via hydrothermal vents near mid-ocean ridges/ Construction of shells by marine organisms
Storage of oil, coal, and gas below Earth's surface
Subduction of carbon-bearing oceanic sediments and rocks along a convergent plate boundary
Use of fertilizers on crops
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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
Cenozoic climate started out cold, then warmed about 30 million years ago, and has since cooled again.
Global climate was cold throughout the entire Cenozoic Era as evidenced by 60 million year old glaciers found today in Antarctica
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O-horizon
A-horizon
B-horizon
C-horizon
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Stunted, woody shrubs
Southern California is an example
Dry summer climate
Monsoonal rains
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U-shaped valley
Horn
Paternoster lakes
Lateral moraine
Cirque
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Earth's crust in areas covered by glaciers rebounded to higher elevations
Land bridges and continental shelves became submerged under water
Global sea level rose
Plants and animals characteristic of colder climates migrated southward to lower latitudes
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Calcification
Cryoturbation
Laterization
Podzolization
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