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Plate Tectonics

Published on Nov 18, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

THE EARTHS CRUST IS DIVIDED INTO PIECES THAT MOVE.

CONVECTION CURRENTS

THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID.

SLAB PULL

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUB-DUCTED.

RIDGE PUSH

NEW CRUST FORMING AND PUSHING OLDER CRUST OUT OF THE WAY.

DIVERGENT

PLATES MOVE AWAY FROM EACH OTHER.

RIFT VALLEY

LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY.

MID-OCEAN RIDGE

UNDERWATER LAND FORM CAUSED BY A DIVERGENT PLATE BOUNDARY.

CONVERGENT PLATE BOUNDARY

TWO PLATES COME TOGETHER.

Volcanic arc







A chain of active volcanos above a subduction zone caused by a convergent plate boundary.

ISLAND ARC

A TYPE OF ISLAND GROUP WITH VOLCANOS FROM CONVERGENT PLATES

Mountain Range



A mountain range or mountain belt is a geographic area containing numerous geologically related mountains.

SUBDUCTION ZONE

THE PROCESS IN WHICH ONE PLATE SLIDES BENEATH ANOTHER.

DEEP OCEAN TRENCH

A LONG DEEP DEPRESSION IN THE OCEAN FLOOR THAT FORMS

THE PERU-CHILE TRENCH

WHICH EXTENDS SOME 5,900 KM ALONG THE COAST OF SOUTH AMERICA.

TRANSFORM PLATE BOUNDARY

PLACES WHERE PLATES SLIDE PAST EACH OTHER.

Result of a transform plate boundary






At transform boundaries lithosphere is neither created nor destroyed. Many transform boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges.


The San Andreas Fault



The San Andreas Fault is a continental transform fault that extends roughly 810 miles through California in the United States.