chapter 16 Flashcards
GEOLOGY
STUDY OF DYNAIC PROCESSES OCCURRING ON THE EARTH’S SURFACE AND ITS INTERIOR
INTERNAL PROCESSES
GEOLOGIC CHANGES ORIGINATING FROM THE EARTH’S INTERIOR
CORE
EARTH’S MOST INNERMOST ZONE
-SURROUNDED BY A LIQUID CORE OF MOLTEN OR SEMISOLID MATERIAL
MANTLE
THICK SOLID ROCK ZONE THAT SURROUNDS THE CORE
-TWO TYPES OF MOVEMENT
CONVECTION CELLS/CURRENT
MANTLE PLUMES
CRUST
OUTERMOST AND THINNEST ZONE OF THE EARTH
-CONTINENTAL AND OCEAINC CRUST
ASTHENOSPHERE
OUTERMOST PART OF THE MANTLE
- VERY HOT
- MADE OF MELTED ROCK
- DEFORMED LIKE SOFT PLASTIC
TECTONIC PLATES
HUGE SOLID PLATES THAT MOVE SLOWLY ACROSS THE EARTH’S SURFACE DUE TO HEATED MATERIAL IN THE MANTLE CONVECTION SELLS
LITHOSPHERE
COMPOSED OF THE CONTINENTAL AND OCEANIC CRUST AND THE RIGID OUTERMOST PART OF THE MANTLE
PLATE TECTONICS
THE THEORY EXPLAINING THE MOVEMENTS OF THE PLATES AND THE PROCESSES THAT OCCUR AT THEIR BOUNDARIES
DIVERGENT PLATE BOUNDARIES
PLATES THAT MOVE APART IN OPPOSITE DIRECTIONS
CONVERGENT PLATE BOUNDARIES
PLATES ARE PUSHED TOGETHER BY INTERNAL FORCES
TRANSFORMING PLATE BOUNDARIES
PLATES SLIDE AND GRIND PAST ONE ANOTHER ALONG A FRACTURE IN THE LITHOSPHERE
SUBDUCTION
WHEN A OCEANIC PLATE COLLIDES WITH A CONTINENTAL PLATE, THE CONTINENTAL PLATE USALLY RIDES OVER THE DESNER OCEANIC PLATE AND PUSHES IT DOWN INTO THE MANTLE
EXTERNAL PROCESSES
GEOLOGIC CHANGES BASED ON DIRECTLY OR INDIRECTLY ON ENERGY FROM THE SUN AND ON GRAVITY (RATHER THAN ON THE HEAT FOUND IN THE INTERIOR)
EROSION
MAJOR EXTERNAL PROCESS
-MATERIAL IS DISSOLVED, LOOSENED, OR WORN AWAY FROM ONE PART OF THE EARTH’S SURFACE AND DEPOSITED ELSEWHERE