Plate Tectonics
Plate Boundaries and Landforms
Volcanoes
Earthquakes
Waves and Faults
100

This theory explains how Earth's plates move and interact over time.

Theory of Plate Tectonics


100

This landform forms when oceanic crust is pushed beneath continental crust.

Trench

100
Volcanoes are most commonly found in this location.

plate boundaries

100

The point underground where an earthquake starts...

the focus

100

The fastest seismic waves that can travel through solids and liquids

P waves

200

The layer beneath the lithosphere where convection currents occur.

The asthenosphere 

200

Mountains like the Himalayas form at this type of boundary...

C-C convergent boundary 
200

This type of volcano forms from slow, flowing lava and has gentle slopes.

Sheild volcano

200

The point on Earth's surface directly above the focus...

the epicenter 

200

These waves can only travel through solids

S waves 

300

The process where new ocean crust forms at mid-ocean ridges is called...

seafloor spreading

300

This boundary is responsible for earthquakes like those along the San Andreas Fault...

transform boundary

300

The measure of how thick lava is...

viscosity

300

The tool used to record earthquake waves...

a seismograph

300

This type of fault formed by compression at convergent boundaries.

a reverse fault

400

The main force that drives plate tectonics movement inside Earth is called...

convection currents

400

A chain of volcanic islands formed by subduction between oceanic plates are called...

an island arc

400

When magma reaches Earths surface, it is called...

lava

400

The total energy released from an earthquake is its...

magnitude

400

This type of stress pulls rocks apart.

tension

500

The type of boundary where two plates move apart is called..

divergent 

500

What landform is created when two continental plates pull apart?

A rift valley.

500

This process explains how the Hawaiian Islands formed...

a hot spot

500

This scale measures a scales intensity

Mercalli
500

The process where energy builds up and is suddenly released, causing earthquakes

elastic deformation