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the process involving uplife and erosion that returns deeply buried rocks to the surface |
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layering formed as a consequence of the alighment of mineral grains, or of compositional banding in a metamorphic rock |
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a compositionally banded metamorphic rock typically composed of alternating dark and light colored layers |
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a metamorphic rock composed of calcite and transformed from a protolith of limestone |
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The intensity or rank of metamorphism, measured by the amount or degree of difference between the original parent rock and the metamorphic rock. It indicates in a general way the pressure-temperature environment or facies in which the metamorphism took place |
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rock that forms when existing rock changes into new rock as a result of an increase in pressure and temperature and or shearing under elebated termperature
-metmorphism occurs without the rock first becoming a melt or a sediment |
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the process by which one kind of rock transforms into a different kind of rock |
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the original from which a metamorphic rock formed |
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a medium to coarse grained metamorphic rock that possesses schistosity |
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fine grained, low grade metamorphic rock formed by metamophism of shale |
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the series of smaller earthquakes that follow a major earthquake |
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the amount of movement or slip across a fault plane |
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a vibration caused by the sudden breaking or frictional slifing of rock in the earth |
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the point on the surgace of the earth directly aboe the focus of an earthquake |
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a fracture on which one body of rock slides past another |
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a smell step in the ground surface where one side of a fault has moved vertically with respect to the other |
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resistance to sliding on a surface |
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the point of an earthquak beneath the surface |
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a measure of the relative size of an earthquake at a location, as determined by examining the amount of damage caused |
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the size of the earthquake |
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the average time between successive geologic events |
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the record of an earthquake |
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compressional seismic waves that move through the body of the earth |
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seismic shear waves that pass through the body of the earth |
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a fault in which one block slides horizontally past another so there is no realtive vertical motion |
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the push, pull, or shear that a material feels when subejcted to a force |
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seismic waves that travel along the earth's surface |
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a large wave along the sea surface triggered by an earthquak or large submarine slump |
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a fold with an arch-like shape in which the limbs dip away from the hinge |
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the cracking and fracturing of a material subjected to stress |
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a change in the shampe, position, or orientation of a material by bending, breaking, or flowing |
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a fault in which sliding occurs up or down the slope |
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the bending and flowing of a material without cracking and breaking subjected to stress |
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he rocks on the lower side of an inclined fault plane |
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the rock or sediment above an inclined fault plane |
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the condition that exists when the buotancy force pushing lithosphere up equals the gravitational force pulling lithosphere down |
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naturally formed cracks in rocks |
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a trough shaped fold whose limbs dip toward the hinge |
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a fauly in which the hanging wall block moves down the slope of the fault |
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a steeply dipping fault on which the hanging wall block slides up |
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a fault marking a transform plate boundary
-along mid ocean ridges, are actively slipping segment of a fracture zone between two ridge segments |
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Tectonic uplift is the portion of the total geologic uplift of the mean earth surface that is not attributable to an isostatic |
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a broad relatively flat region of ocean that lies at least 4.5 km below sea level |
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a continental margine that coincides with a plate boundary |
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a broad, shallowly submerged fringe of a continent
-the widest continental shelves occur over passive margins |
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the deflection of objectsm winds, and currents on the surface of the earth owing to the planet's rotation |
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a large circular flow pattern of ocean surface currents |
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passive continental margin |
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a continental margin that is not a plate boundary |
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the rising and sinking of water driven by contrasts in water ensity, which is due in turn to differences in temp and salinity
-circulation involved both surface and deep water currents |
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the process of reducing heat through a change in air pressure caused by volume expansion |
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A change in the temperature of a material without addition of heat that happens when the pressure of a gas is increased. |
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the mixture of gases that make up the earth's atmosphere |
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the push that air exerts on its surroundings |
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a layer of gases that surrounds a planet |
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the average weather conditions along with the range of conditions of a region over a year |
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a mist of tiny water droplets in the sky |
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a place where two surface air flows meet so that air has to rise |
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a place where sinking air separates into two flows that move in opposite directions |
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the temp at which air becomes satuared so that dew can form |
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the flow of warm water eastward form the pacific ocean that reverses the upselling of cold water along the western coast of south america and causes significant global changes in weather patterns |
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the name given to the low altitude convection cells in the atmosphere |
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exposure to the sun's rays |
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a fast moving current of air that flowa at high elevation |
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the cooler layer of atmosphere overlying the stratosphere |
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o3
-protects
-absorbs ultraviolet |
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the stable stratified layer of atmosphere directly above the troposphere |
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the outermost layer of the atmopshere conaining very little gas |
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a wind blowing steadily toward the equator from the northeast in the northern hemisphere or the southeast in the southern hemisphere, esp. at sea |
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the lowest layer of the atmosphere where air undergoes convection and where most wind and clouds develop |
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local scale conditions as defined by temperature air pressure relative humidity and wind speed |
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natural movement of the air, esp. in the form of a current of air blowing from a particular direction. |
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typical p wave velocities in crust |
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typical s wave velocity in crust |
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magnesium
calicum
potassium
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-more saline as temp increases |
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typical depth of abyssal plains |
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depends on the angle at which sunbeams strike the earth
-poles are cooler |
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