Earth Systems & Resources

Transform

Divergent

Convergent

All of the above

Erosion

Deposition

Weathering

Decomposition

Stratosphere

Mesosphere

Thermosphere

Troposphere

Changes in the Earth's distance from the sun

The tilt of the Earth's axis

Variations in solar radiation output

The Earth's rotation speed

The daily temperature and precipitation

Short-term atmospheric conditions

Long-term patterns of weather conditions

A specific weather event

Unusually cold ocean temperatures in the eastern Pacific

Warmer-than-normal surface waters in the tropical Pacific Ocean

A decrease in global precipitation levels

An increase in the strength of the trade winds

Rift valleys

Mid-ocean ridges

Mountain ranges

Transform faults

Weathering moves soil, erosion breaks down rocks, deposition adds organic material, and decomposition transports materials.

Weathering breaks down rocks, erosion moves materials, deposition drops materials in a new location, and decomposition adds organic matter.

Weathering transports materials, erosion breaks down organic matter, deposition forms rocks, and decomposition moves soil.

Weathering adds organic matter, erosion forms rocks, deposition breaks down rocks, and decomposition moves materials.

CFCs increase greenhouse gases, leading to global warming.

CFCs deplete the ozone layer, leading to increased UV radiation.

CFCs cool the stratosphere, causing cloud formation.

CFCs thicken the ozone layer, reducing UV radiation.

Higher latitudes receive more direct sunlight than lower latitudes.

Latitude has no impact on the intensity of solar radiation.

Lower latitudes receive more direct sunlight than higher latitudes.

The intensity of solar radiation is consistent across all latitudes.