Paternoster lakes
Horn
U-shaped valley
Cirque
Lateral moraine
A
B
C
D
Drumlins
Glacial meltwater
Glacial ice and snow
Terminal moraines
Calving
Cirque
Crevasses
Terminal moraine
Elongated deposit of till streamlined in the direction of ice movement by a continental glacier
Small hill or knob of poorly sorted gravel deposited by a melting glacier
Sinuous, narrow ridge of coarse sand and gravel formed by a meltwater stream that flowed beneath a glacier
Hole in the ground left behind after a large block of ice melts
A
B
C
D
E
Melting of permafrost beneath a building constructed on the ground surface causes the structure to collapse.
Areas in subarctic and polar climates where the ground is cold but never freezes.
Expansion of water when freezing disrupts the soil and fractures rocks.
Patterned ground forms due to frost action in the soil.
Ice wedges develop in fractures below the ground surface.
Plants and animals characteristic of colder climates migrated southward to lower latitudes
Land bridges and continental shelves became submerged under water
Global sea level rose
Earth's crust in areas covered by glaciers rebounded to higher elevations
Ice cores indicate that global temperatures have been fairly constant over the last few tens of thousands of years.
The atmospheric concentration of greenhouse gases such as carbon dioxide and methane have actually decreased over the last 50 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.
Higher sunspot activity increases the solar wind, which in turn warms Earth's upper atmosphere
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
The amount of sunspot activity never changes and therefore cannot affect Earth's climate
1
26,000
41,000
100,000
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
Global climate was cold throughout the entire Cenozoic Era as evidenced by 60 million year old glaciers found today in Antarctica
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.
Plate tectonics
Milankovitch cycles
Changes in overall sunspot activity
Human activity such as burning of fossils fuels
Both C and D
True
False
Grams of sodium per kilogram of dissolved ions.
Grams of dissolved ions in 1 kilogram of solution.
Grams of water in 1 kilogram of solution.
Grams of solution per cubic kilometer of seawater.
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.
Evaporation exceeds precipitation in the subtropical region, whereas the reverse occurs along the equator.
Precipitation is greater in the subtropics than along the equatorial belt.
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.
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 sea surface is everywhere smooth and flat.
Coastlines are always in equilibrium with oceans and therefore never change.
Ocean currents generate the tides.
Global sea level has risen and fallen many times throughout Earth history.
Spring tide
A lunar eclipse
Ocean gyres
Neap tide
Assembly of continents into a supercontinent.
Global warming during an interglacial cycle
Removing fish from the oceans
Global cooling during an ice age
Decrease in the volume of mid-ocean ridges
Surf
Crests
Breakers
Swells
Wave crests increase in height when approaching the beach.
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.
A
B
C
D
E
A
B
C
D
E