Earth Layers
Boundaries & Stress
Theories and Theorists
Volcanoes
Earthquakes
100

The outermost layer of Earth

Crust

100

Two plate colliding

Convergent Boundary

100

The landmass that existed when all continents were joined.

Pangaea

100

Located on the Pacific Plate

The Ring of Fire

100

Scale used to rate the San Francisco Earthquake

Richter Scale

200

Composed of the rigid crust and upper portion of the mantle.

Lithosphere

200

Two plates scraping past each other

Transform Boundary

200

The process of new oceanic crust forming as magma rises toward the surface and solidifies.

Sea-Floor Spreading

200

Have not erupted in recorded history and probably never will erupt again.

Extinct

200

More destructive seismic waves

Surface Waves

300

____________ of Earth's surface is composed primarily of water. 

75%

300

Stress that causes plates to thin in the middle due to the pull of a plate in opposite directions.

Tension

300

The theory that explains how large pieces of Earth’s outermost layer, called tectonic plates, move and change shape.

The Theory of Plate Tectonics

300

Volcanically active places on Earth’s surface that are far from tectonic plate boundaries

Hotspots

300

Fault responsible for many earthquakes in California.

San Andreas Fault

400

Under great pressure due to the weight and gravity of other layers. 

Inner core

400

Effects of an oceanic crust and continental crust colliding and causing crust to be DESTROYED

Subduction Zone

400

A professor of geology at Princeton University, was very influential in setting the stage for Sea-Floor Spreading.

Harry Hess

400

Gently sloping hillsides but can be HUGE!

Shield Volcano

400

A wave of energy that travels through the Earth, away from an earthquake in all directions

Seismic waves

500

Denser than the crust and mantle, about 2200km thick.

Outer Core

500

Rift valleys are an effect of this type of boundary.

Divergent Boundary

500

A German scientist born in 1880, noticed that the continents looked as if they all once fit together.

Alfred Wegener

500

“Resistance to flow”

Viscosity

500

90% of earthquakes occur at plate boundaries. 10% occur here. 

Middle of a plate/Fault Lines