1 of 8

Slide Notes

DownloadGo Live

Plate Tectonics

Published on Nov 24, 2015

No Description

PRESENTATION OUTLINE

Plate tectonics is the theory that the crust is split into pieces that float on the mantle.

CONVECTION CURRENTS

CURRENTS CAUSED BY DIFFERENT DENSITIES IN THE MANTLE

SLAB PULL

THE PULL OF GRAVITY ON A SUBDUCTED PLATE

RIDGE PUSH

NEW LESS DENCE CRUST AT A DIVERGENT BOUNDRY PUSHES OLD CRUST AWAY AT Y

DIVERGENT PLATE BOUNDRY

OCCURS WHEN TWO PLATES PULL AWAY FROM EACHOTHER OR DIVERGE

RIFT VALLEY

  • A divergent boundry on land creats a
  • A large rift valley in africa is lake rukwa.

MID OCEAN RIDGE

  • Divergent plates under water creates a mid ocean ridge.
  • Mid ocean ridges are underwater land forms that creat new crust at divergent plates
Photo by wockerjabby

CONVERGENT PLATE BOUNDRIES