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EARTH SCIENCE CHAPTER 6 – SECT. 1 LANDFORMS PLAINS COASTAL PLAINS – LOWLANDS; EXPOSED PORTION OF CONTINENTAL SHELF THAT EXTENDS INTO THE OCEAN o EXAMPLES – ATLANTIC COASTAL PLAINS, GULF COASTAL PLAINS INTERIOR PLAINS – FLAT, GRASSY DRY AREAS FOUND IN MIDDLE OF OUR COUNTRY BETWEEN THE ROCKY MTS., APPALACHIAN MTS., AND GULF COASTAL PLAINS; ALSO CALLED GREAT PLAINS PLATEAUS LARGE, RAISED FLAT AREAS; EDGES RISE STEEPLY; CUT THROUGH BY RIVER VALLEYS AND CANYONS o EXAMPLES – COLORADO PLATEAU FORMED THE GRAND CANYON MOUNTAINS TOWER HIGH ABOVE SURROUNDING LAND FOUR TYPES FOLDED MTS. – ROCK LAYERS ARE FOLDED LIKE A RUG THAT HAS BEEN PUSHED UP AGAINST A WALL. FORCES SQUEEZE HORIZONTAL ROCK LAYERS TOGETHER, CAUSING THEM TO FOLD EXAMPLE – APPALACHIAN MTS. UPWARPED MTS. – HAVE HIGH PEAKS AND SHARP RIDGES. FORM WHEN BLOCKS OF EARTH’S CRUST ARE PUSHED UP BY FORCES INSIDE EARTH. EXAMPLES – ADIRONDACK MTS., ROCKY MTS. BLACK HILLS FAULT-BLOCK MTS. – HUGE TILTED BLOCKS OF ROCK SEPARATED FROM SURROUNDING LAND BY FAULTS. ONE BLOCK IS PUSHED UP WHILE THE BLOCK NEXT TO IT DROPS DOWN. EXAMPLES – GRAND TETONS, SIERRA NEVADAS VOLCANIC MTS. – FORMED FROM MAGMA REACHING THE SURFACE, AND PILES UP LAVA LAYER UPON LAYER FORMING A CONE SHAPED STRUCTURE. EXAMPLES – MOUNT SAINT HELENS, MOUNT SHASTA, MAUNA LOA