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50 Cards in this Set
- Front
- Back
density, 52
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property of a substance defined as mass per unit volume and usually expressed in grams per cubic centimeter or kilograms per cubic meter
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seismic wave, 52
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elestic disturbances, or vibrations, that are generated by earthquakes
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P-wave, 53
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a type of seismic wave in which material is alternately compressed and stretched in the direction of propagation of the wave
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S-wave, 53
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a type of seismic wave in which material is sheared from side to side, perpendiculater to the direction of propagation of the wave
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refract, 54
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change in direction, or bending, of a wave
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inner core, 54
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the innermost region of Earth. it is solid and consists primarily of iron with minor amounts of other elements that likely include nickel, sulfur, and oxygen
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outer core, 54
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a region surrounding the inner core. it is liquid and consists primarily of iron with minor amounts of other elements that likely include nickel, sulfur, and oxygen
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mantle, 55
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main bulk of earth between the crust and the core; increasing pressure and temperature with depth divide the mantle into concentric layers
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seismic tomography, 55
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the use of seismic data to produce computerized, detailed, three-dimensional maps of the boundaries between earth's layers
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Moho discontinuity, 55
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boundary between curst and mantle, marked by a rapid increase in seismic wave speed.
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Laurasia, 58
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an ancient landmass that fragmented to produce north america and eurasia
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granite, 55
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crustalline, coarse grained, igneous rock composed mainly of quartz and feldspar
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basalt, 55
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fine-grained, dark igneous rock, rich in iron and magnesium, characteristic of oceanic crust.
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lithosphere, 56
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outer, rigid portion of earth; includes the continental and oceanic cursts and the upper part of the mantle
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asthenosphere, 56
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upper, deformable portion of earths mantle, the layer below the lithosphere; probalby partially moltenl may be site of convection cells
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mesophere, 56
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either layer of the atmosphere above the stratosphere extending from about 50-90km, or the region of the mantle beneath the asthenosphere
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isostasy, 56
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mechanism by which areas of earths crust rise or subside until their masses are in balance, "floating" on the mantle
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Gondwanaland, 58
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an ancient land mass that fragmented to produce africa, south america, antartica, australia, and india
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continental drift, 58
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the movement of continenets; the name of Alfred Wegeners theory, preceding plate tectonics
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Pangaea, 58
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an ancient landmass that consisted of all of the present day continents; it fragmented into laurasia and gondwanaland
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ridge, 59
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long, narrow elevation of the sea floor, with steep sides and irregular topography
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rise, 59
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long, broad elecation that rises gently and genereally smoothly from the sea floor
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rift valley, 59
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trough formed by fualting along a zone in which plates move apart and new crust is created, such as along the crest of a ridge system
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trench
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long, deep, and narrow depression of the sea floor with relatively steep sides, associated with a subduction zone
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convection cell
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circulation in a fluid, or fluidlike material, caused by heating from below. heating the base of a fluid lowers its density, causing it to rise. the rising fluid cools, becomes denser and sinks creating circulation
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seafloor spreading
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movement of crustal plates away from the mid ocean ridges; process that creates the new crustal material at the mid ocean ridges
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spreading center
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region along which new crustal material is produced
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subduction zone
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plane descending away from a trench and defined by its seismic activity, interpreted as the convergence zone between a sinking plate and an overriding plate.
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epicenter
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point on earths surface directly above an earthquake location, specified by indentifying the latitude and longitude of the earthquake
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focus
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the location of an earthquake within earth. focus is specified by indentifying latitude, longitude, and depth of the earthquake
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sediment
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particulate organic and inorganic matter that accumulates in loose, unconsolidated form.
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core
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verticle, cyclindrical sample of bottom sediments, from which the nature of the bottom can be determined; also the central zone of earth, thought to be liquid or molten on the outside and solid on the inside
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diple
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a magnetic field like earths, with two opposite poles
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curie temperature
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temperature at which the magnetic signature is frozen into an igneous rock during cooling
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paleomagnetism
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study of ancient magnetism recorded in rocks; includes study of changes in location of earths magnetic poles through time and reversals in earths magnetic field
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polar reversal
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the periodic reversal of earths magnetic field where the north magnetic pole becomes the south magnetic pole and vice versa
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polar wandering curve
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a plot of the apparent location of earths north magnetic pole as a function of geologic time.
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inertia
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the property of matter that causes it to resist any change in its motion
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rift zone
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a region where the lithosphere splits and separates allowing new crustal material to intrude into the crack or rift
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graben
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a portion of earths crust that has been moved downward and is bounded by steep faults; a rift
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wadati-benioff zone
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dipping patterns of earthquake activity that descent into the mantle along convergent plate boundaries
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escarpment
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nearly continuos line of cliffs or steep slopes caused by erosion or faulting
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fracture zone
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long, linear zone of irregular bathymetry of the sea floor, characterized by asymmetric ridges and troughs; commonly associated with fault zones
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craton
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large peices of earths crust that form the centers of continents
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island arc
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chain of volcanic islands formed above the sinking plkate at a subduction zone
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terrane
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fragments of earths crust bounded by faults, each fragment with a history distinct from each other fragment
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spreading rate
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the rate at which two plates move apart. spreading rates are generally between about 2 and 10 cm a year
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hotspot
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surface expression of a persistent rising plume of hot mantle material
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guyot
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submerged, flat top seamount
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hydrothermal vent
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seafloor outlet for high temperature groundwater and associated mineral deposits; a hot spring
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