GEOLOGY Flashcards
GEOLOGY
EARTH’S STRUCTURE, HISTORY, AND PROCESSES INVOLVED
CRUST
OUTERMOST LAYER
MANTLE
MIDDLE LAYER, MADE MOSTLY OF MOLTEN ROCK
CORE
INNER LAYER, MADE OF IRON AND NICKEL
TECTONIC PLATES
RIGID PIECES OF THE EARTH’S CRUST AND UPPER MANTLE
PLATE TECTONICS
THEORY DESCRIBING THE LARGE-SCALE MOTIONS OF THE EARTH’S LITHOSPHERE
CONTINENTAL DRIFT THEORY
THEORIZES THAT THE EARTH HAD A SINGLE CONTINENT
DIVERGENT BOUNDARY
PLATES MOVE AWAY FROM EACH OTHER
CONVERGENT BOUNDARY
PLATES MOVE TOWARDS EACH OTHER
TRANSFORM BOUNDARY
PLATES MOVE ALONG/SLIDE PAST EACH OTHER
EARTHQUAKE
SHAKING OF THE GROUND CAUSED BY TENSION OF PLATES
FOCUS
POINT BENEATH EARTH’S SURFACE WHERE ROCKS BREAK UNDER STRESS
EPICENTER
CENTER OF THE QUAKE ABOVE THE FOCUS
BODY WAVES
ENERGY WAVES THAT TRAVEL UNDERGROUND
PRIMARY WAVES
COMPRESSIONAL, FAST, AND TRAVELS THROUGH ALL MEDIUMS
SECONDARY WAVES
SHEAR, SLOWER THAN PRIMARY WAVES, AND TRAVELS THROUGH SOLID ROCK
SURFACE WAVES
ENERGY WAVES THAT TRAVEL ALONG THE SURFACE OF THE EARTH
RAYLEIGH WAVE
DISSIPATES AS IT TRAVELS FARTHER FROM THE CENTER
LOVE WAVE
SIDEWAY MOVEMENT THAT OCCUR WHEN THE GROUND IS MADE OF MULTIPLE LAYERS
TSUNAMI
SERIES OF ENORMOUS WAVES IN THE OCEAN OR LARGE WAVES
RICHTER SCALE
NUMERICAL SCALE EXPRESSING THE MAGNITUDE OF AN EARTHQUAKE
MERCALLI SCALE
USES THE OBSERVATIONS OF PEOPLE AND IS LESS SCIENTIFIC THAN THE RICHTER SCALE
VOLCANO
OPENING OR RUPTURE IN THE EARTH’S SURFACE
CINDER CONE VOLCANO
BUILT FROM PARTICLES AND LAVA EJECTED FROM A SINGLE VENT
STRATOVOLCANO
STEEP-SIDED, SYMMETRICAL, BUILT OF ALTERNATING LAYERS OF LAVA, LOOKS LIKE PERFECT CONES, AND HAS A SLOWER LAVA FLOW
SHIELD VOLCANO
BUILT FROM FLUID LAVA FLOWS AND HAS FASTER LAVA FLOWS
IGNEOUS ROCKS
FORMED WHEN MAGMA OR LAVA SOLIDIFIES
INTRUSIVE ROCKS
CRYSTALLIZES BELOW THE EARTH’S SURFACE AND COOLS SLOWLY FORMING CRYSTALS
EXTRUSIVE ROCKS
ERUPT ONTO THE SURFACE AND COOLS QUICKLY FORMING GLASS
SEDIMENTARY ROCKS
FROM ROCK RESIDUES THAT ACCUMULATE OVER TIME AND HARDEN
METAMORPHIC ROCKS
ROCKS THAT UNDERGO PHYSICAL AND CHEMICAL CHANGES DUE TO INTENSE PRESSURE AND TEMPERATURE
MINERALS
NATURALLY OCCURRING INORGANIC SOLIDS
HARDNESS
ABILITY OF THE MINERAL TO RESIST BEING SCRATCHED; 1 IS THE SOFTEST AND 10 IS THE HARDEST
COLOR
MOST OBVIOUS PROPERTY BUT THE LEAST DIAGNOSTIC
STREAK
COLOR OF A MINERAL IN ITS POWDERED FORM; SHOWS THE TRUE COLOR OF THE MINERAL
DENSITY
REFERS TO THE MINERAL’S COMPOSITION AND PATTERN IN WHICH THE MINERAL’S ATOMS ARE ARRANGED
CRYSTALLINE STRUCTURE
MINERALS OCCUR IN SHAPES DETERMINED BY THE ARRANGEMENT OF THEIR ATOMS, MOLECULES, OR IONS
CLEAVAGE
TENDENCY OF A MINERAL TO BREAK ALONG A PLANE
LUSTER
THE WAY A MINERAL REFLECTS THE LIGHT
SOIL
FINE FRAGMENTS BROUGHT ABOUT BY WEATHERING THAT MAKE UP THE GROUND
EROSION
TERM USED TO REFER TO THE TRANSFER OF GROUND MATERIALS TO ANOTHER LOCATION; CAN BE CAUSED BY NATURAL OR MAN-MADE EVENTS
ANGLE OF REPOSE
STEEPEST SLOPE OF UNCONFINED MATERIAL ON WHICH THE MATERIAL CAN BE HEAPED WITHOUT COLLAPSING
HYDROSPHERE
97% OF ALL WATER ON EARTH IS OCEANIC WATER
OCEANIC WATER
COVERS 70% OF EARTHS SURFACE
GROUND WATER
SEEPS UNDERGROUND THROUGH PERMEABLE ROCKS AND ACCUMULATES DIFFERENTLY
ZONE OF SATURATION
REGION WHERE WATER IS ALWAYS PRESENT
WATER TABLE
REGION ABOVE THE ZONE OF SATURATION WHERE WATER LEVEL CHANGES BASED ON THE ENVIRONMENTAL CONDITIONS
UNSATURATED ZONE
REGION ABOVE WATER TABLE WHERE WATER ONLY PASSES THROUGH BUT DOES NOT ACCUMULATE
EVAPORATION
HEAT FROM THE SUN EVAPORATES WATER FROM OCEANS, LAKES, MOIST SOIL, LEAVES, AND BODIES OF ANIMALS AND HUMANS
CONDENSATION
WATER MOLECULES LIQUIFY AND CLING TO DUST PARTICLES IN THE HIGH AIR TO FORM CLOUDS
PRECIPITATION
MOISTURE IN THE AIR BECOMES TOO HEAVY AND FALLS BACK ON EARTH; IT CAN BE IN THE FORM OF RAIN, HAIL, OR SNOW
ATMOSPHERE
MADE OF LAYERS OF GASSES ENVELOPING THE EARTH; COMPOSED OF NITROGEN (78%), OXYGEN (21%), AND ETC.
TROPOSPHERE
LAYER WHERE WEATHER CONDITIONS OCCUR
STRATOSPHERE
LAYER WHERE THE OZONE LAYER IS FOUND
MESOSPHERE
LAYER WITH LOW TEMPERATURES AND STRONG WINDS; CAN SLOW DOWN METEORS
THERMOSPHERE
VERY HOT LAYER DUE TO THE SUN’S RADIATION; GASES ARE NOT UNIFORMLY MIXED
EXOSPHERE
THIN OUTER LAYER MADE OF GASES
IONOSPHERE
LAYER WHERE IONIZED PARTICLES EXIST; EXIST WITHIN THE THERMOSPHERE AND EXOSPHERE