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50 Cards in this Set

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