1 of 16

Slide Notes

DownloadGo Live

Plate Tectonics

No Description

PRESENTATION OUTLINE

PLATE TECTONICS

Convection currents in the asthenosphere move plates in the lithosphere.

CONVECTION CURRENTS

The movement of a fluid caused by differences in temperature and density.
Photo by wockerjabby

SLAB PULL

The pull of gravity on a plate causing the plate to sink back into the mantle.

RIDGE PUSH

When new rock forms it pushes old rock further from the ridge.

DIVERGENT PLATE BOUNDARY

A plate boundary were plates pull apart from each other.

RIFT VALLEY

A rift formed on land caused by a divergent boundary underneath.

MID-OCEAN RIDGE

A ridge at the bottom of the ocean where new ocean crust is formed.

CONVERGENT PLATE BOUNDARY

A plate boundary where the plates crash into each other.

VOLCANIC ARC

Volcanoes formed by oceanic crust and continental crust crashing into each other.

ISLAND ARC

Islands formed from two oceanic crust plates crash into each other.

MOUNTAIN RANGE

Mountains formed when two continental crust plates crush into each other.

SUBDUCTION ZONE

Occurs when one plate goes under another plate and goes back into the mantle.

DEEP OCEAN TRENCH

Forms at subduction zones where one plate goes under another plate.

TRANSFORM PLATE BOUNDARY

A plate boundary where two plates slide past each other.

EARTHQUAKES

Earthquakes are caused when two plates slide past each other.

SAN ANDREAS FAULT, CALIFORNIA

A fault caused by two plates sliding past each other in California.