Archive for January, 2011

Mountain Formation

IDENTIFY THE TYPES OF PLATE COLLISIONS THAT BUILD MOUNTAINS.

COLLISIONS BETWEEN CONTINENTAL AND OCEANIC CRUST.

THE TWO PLATES COLLID AND USLY THE OCEANIC PLATE WELL SINK AND HEAT AND RISE AGEN UNDER THE LAND MASS PUSSING UPWORD AND MAKING A MOUNTAIN

COLLISIONS BETWEEN OCEANIC AND OCEANIC CRUSTS

ONE OCEANIC PLATE WELL SUBDUCTS BENEATH THE OTHER OCEANIC PLATEAS THE PLATE SUBUCTS WATER FROM THE SUBDUCTING LITHOSPHERE INDUCES PARTIAL MELTING AND MATERIAL TO FORM MAGMA THIS PUSSES UP AND MAKES A MOUNTAIN

COLLISIONS BETWEEN CONTINENTS

WHEN TWO LAND MASSES COLIDE THEY WELL FOLED AND CRUMPLE AND SQISH AND PUSH UPWORD MAKING SOM OF THE BIGIST MOUNTAINS FOUND TODAY

IDENTIFY FOUR TYPES OF MOUNTAINS AND DISUSS THE FORCES THAT SHAPED THEM.

FOLDED MOUNTAINS AND PLATEAUS-WHEN TWO LAND MASSES COLIDE THEY WELL FOLED AND CRUMPLE AND SQISH AND PUSH UPWORD MAKING SOM OF THE BIGIST MOUNTAINS FOUND TODAY

FAULT-BLOCK MOUNTAINS AND GRABENS- THIS IS WHEN A FAULT LINE BLOCKS AND PUSSES UP AND TURNS AND FOULDS UPWORD

DOME MOUNTAINS-WHEN LOVA PUSSES UP AND MAKES THE CRUST BOLJ BUT NOT BRACK

VOLCANIC MOUNTAINS. THIS IS WHEN MAGMA PUSSES THE CRUST UPWORD AND IT BREACKS AND MAKES A VALCANO

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