Earth's Structure
Inside Earth
Rock Cycle
Earth's History
Changing Earth Surface
Human Impact
100

This theory explains how Earth's large crustal plates move and interact.

Plate Tectonics

100

This is Earth's thin, solid, outermost compositional layer.

Crust

100

Rock formed when molten rock cools and solidifies.

Igneous Rock

100

This principle states that in an undisturbed sequence of rock layers, the bottom layers are older than the layers above them.

Law of Superposition

100

The breakdown of rock into smaller pieces is called this.

Weathering

100

Removing large amounts of vegetation from an area is called this.

Deforestation

200

At this type of boundary, two plates move toward each other.

Convergent
200

This layer lies beneath the crust and contains hot material capable of convection.

Mantle

200

Rock formed from sediments that are compacted and cemented together.

Sedimentary Rock

200

This method uses the amount of radioactive elements and their decay to determine a rock's numerical age.

Radiometric Dating

200

The movement of sediment from one location to another is called this.

Erosion

200

When productive land becomes increasingly dry and loses its ability to support vegetation, this process is occurring.

Deserification

300

At this type of boundary, two plates move away from one another and new crust can form.

Divergent

300

This rigid outer portion of Earth includes the crust and uppermost mantle.

Lithosphere

300

Rock changed by heat and pressure without completely melting.

Metamorphic Rock

300

Scientists can use these preserved remains or traces of organisms as evidence of Earth's past.

Fossils

300

When transported sediment is dropped or settles in a new location, this process occurs.

Deposition

300

What variable is altered by the scientist in an experiment.

Independent

400

At this type of boundary, plates slide horizontally past one another, often producing earthquakes.

Transform Boundary


400

This type of heat transfer occurs when hot material rises and cooler material sinks.

Convection

400

Granite → sediment → sandstone → quartzite represents this sequence of rock types.

Describe How this would happen.

Mr. Jones will Approve

400

Identical fossils found on continents separated by an ocean provide evidence for this.

Continents were closer together.

400

These two processes can wear down young, jagged mountains and eventually produce older, more rounded mountains.

Weathering & Erosion

400

What variable is measured in an experiment

Dependent
500

The Andes Mountains contain many volcanoes because one crustal plate is doing this beneath another plate.

What is Subduction

500

This energy source drives plate tectonics, earthquakes, and volcanic activity according to the unit's test.

Heat Energy from Molten Layers

500

Wind, water, ice, and gravity can break down and move material, eventually providing sediment.

Weathering

500

If a scientist were to discover an old rock what would the scientist need to analyze about it to determine its ABSOLUTE AGE.

Amount of Radioactive Material

500

A coastline changes over time because waves and changing water levels can cause this process, moving sediment away from the coast.

Erosion

500

What process would be increased by humans removing trees and vegetation from a landscape?

Weathering and Erosion

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