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Plate Tectonics

Published on Nov 18, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

The formation, movement, and subduction of Earth's plates.

CONVECTION CURRENTS

Heat is transferred from one part of the fluid to another.

SLAB PULL

Gravity pulling on the plates in the subduction zone.

RIDGE PUSH

The plates are pushed apart when new crust forms.

DIVERGENT PLATE BOUNDARY

The plates move apart from each other.

A rift valley forms on land as a result, such as this one near Quilotoa, Ecador.

Between oceanic plates, they exist as mid-ocean ridges. For instance, the East Pacific Rise is a mid-oceanic ridge.

CONVERGENT PLATE BOUNDARY

The plates move towards each other.

The Washington-Oregon coastline- Trench resulting from an oceanic and continental plate boundary.

The Aleutian Islands- Volcanic Arc resulting from an oceanic plate boundary.

The Appalachian Mountain Range- Mountain chain resulting from a continental plate boundary.

SUBDUCTION ZONE

Regions where the process of subduction occurs.

DEEP OCEAN TRENCH

A location where one tectonic plate subducts under another.

One example of a deep ocean trench is the Puerto Rico Trench.

TRANSFORM PLATE BOUNDARY

Two plates that move past each other.

A fault occurs as a result of a transform plate boundary.

New Zealand's Alpine fault is one example of a transform fault.