GEOL 240 Final Exam – Flashcards

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single most important concept in earth sciences idea that the outermost part of the earth (lithosphere) is made up of twelve large plates that move past each other
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theory of plate tectonics
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strong, rigid outer shell of earth that contains the crust and the uppermost part of the mantle
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lithosphere
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weak, partially molten part of the earth in the upper mantle
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asthenosphere
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region of the earth between the crust and the core and includes the lower lithosphere and asthenosphere
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mantle
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continental crust and oceanic crust
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outermost part of the earth's composition
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average thickness of continental crust
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40 km
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average thickness of oceanic crust
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7 km
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a crack with displacement in it; a fracture or discrete surface separating two bodies of rock which have moved relative to one another
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fault
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occur where plates move away from each other; this type of plate boundary is the result of tensional stress and is characterized by normal faults
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divergent plate boundaries
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volcanism and normal faulting are associated with topographic highs in the ocean basins in areas known as ________. New crust is continuously being formed at ___________ therefore the age of the crust is essentially 0, and as you move away the age of the seafloor becomes progressively older
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mid-ocean ridges
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plate boundaries where two plates collide with one another
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convergent plate boundaries
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compressional stresses and reverse faults
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convergent plate boundaries
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denser crust sinks below less dense crust in a ________.
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subduction zone
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older, cooler, and denser oceanic crust is subducted beneath younger, warmer, and more buoyant oceanic crust
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ocean-ocean
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minerals that compose oceanic rocks are more dense than those that make up continental rocks so this occurs
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ocean-continent
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deep depression forms parallel to the subduction zone, deepest parts of the ocean floor
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trench
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earthquakes will occur from the earth's surface down to a depth of 700 km in the boundary between the subducting and overriding plate
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wadati-benioff zone
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as oceanic plates subduct, heat is produced by friction and the minerals in the crust change form and release water. as a result, a portion of the material in the downgoing slab and in the overlying mantle melts and _____ is produced.
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magma
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molten rock inside the earth, less dense than the surrounding rock and will rise towards the earth's surgace
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magma
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arcuate chains of volcanoes in the ocean basins
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island arc
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chains of volcanoes on the continents will form if this process occurs beneath continental crust
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continental arcs
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really big mountains will be formed at the plate boundary. one plate won't be large enough to cause one plate to subduct beneath the other
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continent-continent
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two plates move past each other horizontally - large shear stresses result in strike-slip faults, link segments of divergent plate boundaries at mid-ocean ridges
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transform plate boundary
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regions of volcanic activity in the interior of a lithospheric plate away from the plate boundaries or major faults
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hot spots
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formed above hot plumes of magma from the mantle that rise toward the earth's surface because of their decreased buoyancy
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hot spots
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1km=1000m=100,000cm=1,000,000mm 1 in = 2.54cm 1.6 km = 1 mile
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metric system
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the study of the earth's past magnetic field as it is recorded in the rocks
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paleomagnetism
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a rock sample can acquire and hold the direction of the magnetic field that existed at the time and place the rock was formed
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fossil magnetic remanence of the rock
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about 600ºC
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curie point
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magnetite crystals in the rock cannot be magnetized
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above the curie point
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magnetite crystals will acquire a direction of magnetization parallel to the surrounding earth's field
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below the curie point
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earth's magnetic field is generated as if there were a giant bar magnet placed at the earth's interior and slightly inclined from the rotational axis
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dipole
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angle between the magnetic field vector and the surface of the earth
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inclination
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angle between the horizontal component of the magnetic field vector and geographic north
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declination
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force per unit area
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stress
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newtons per square meter
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earth's stress is measured in
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stress that acts perpendicular or 90º to that plane
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normal stress acting on a plane
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the stress acting parallel to a plane
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shear stress
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direction of maximum compressive normal stress, zero shear stress
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sigma 1 (maximum principle stress direction)
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smallest normal stress value, still a direction of zero shear stress
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sigma 3 (minimum principle stress direction)
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perpendicular to both sigma 1 and sigma 3
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sigma 2 (intermediate stress direction)
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large earthquakes always occur on pre-existing planes called ______.
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faults
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line where the fault plane intersects the earth's surface
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fault trace
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orientation of the fault trace with respect to the north i.e. the angle between the fault trace and the north
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strike
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angle between the earth's surface and the fault plane measured at right angles to the strike
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dip
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relative movement across the fault is in the direction of the dip i.e. up and down the plane
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dip slip
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hanging wall moves down relative to the footwall; extend crust
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normal faulting
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hanging wall moves up relative to the footwall; shorten crust
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reverse (thrust) faulting
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tensional forces stretch a rock and tend to pull it apart, such as at a rift zone or mid-ocean ridge
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normal faulting causes
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compressive forces squeeze and shorten a rock, such as at a continent continent collision or a subduction zone
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reverse faulting causes
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form from shear stresses and cause blocks of rock to move past each other horizontally, SA fault
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strike slip faults causes
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when one plate moves to the right relative to the other
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right lateral strike slip faults
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when one plate moves to the left relative to the other
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left lateral strike slip faults
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theres a relationship between the orientations of the principle stress directions near the surface of the Earth and the type of faulting we observe
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anderson's theory of faulting
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a subduction zone formed off the west coast of the north american plate
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sierra nevada mts
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28 million years ago, the collision of the pacific plate and north american plate cause the suduction zone along the coast to cease and the two plates began to slide past each other - right lateral fault
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San Andreas transform fault system
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cliffs commonly associated with dip slip faults where vertical offset has occured
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fault scarp
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faults can develop branches and sub-parallel fractures adjacent to the main fracture that have lesser amounts of displacement
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fault zone
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closed depressions of internal drainage are often found in fault zones, occur where faults bend or sidestep forming echelon fractures
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sag ponds
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where failure of rocks occurs
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rupture surface
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fault that has had surface displacement within holocene time
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active fault
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about the last 11,000 years
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holocene time
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San Andreas, San Jacinto, Hayward, Garlock, Newport-Inglewood, Raymond Hill, and Whittier
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active faults in CA
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followed 1971 San Fernando EQ - required compiling of maps delineating active fault zones, local governments can regulate construction for human occupancy across an active fault trace, perspective buyers must be notified that their property is on an active fault
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SSZ Act
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study of ancient earthquakes
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paleoseismology
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paleoseismologists dig trenches across recent fault traces and then study the walls of the trenches for evidence of earlier fault ruptures
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how to study ancient earthquakes
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if a layer is cut by a fault, that layer must be older than the fault
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cross cutting relations
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how to yield absolute ages of layers involved
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carbon-14 dating
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average time between each earthquake
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recurrence interval
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the velocities of the different frequencies in the glass are different
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snells law
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record the travel time of the waves which return to the surface and since the distance from the sources is known the velocity of the reflected and refracted waves can be determined
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seismometers
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faults that only rupture in the subsurface
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blind faults
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a recording of ground motion at a seismic station during some time period
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seismogram
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the place at which the earthquake rupture begins; underground focus point of an earthquake
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hypocenter
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time at which the earthquake rupture begins
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origin time
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a measure of the degree of shaking at a certain location during an earthquake
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intensity
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closed intensity scale measured from I to XII, depends on location relative to hypocenter
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MMI Scale
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contoured map showing regions of equal intensity of shaking
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isoseismal map
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measures the size or the total energy release of an earthquake, open scale (-infinity, infinity)
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magnitude
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a logarithmic scale that assesses the sizes of earthquakes by powers of 10
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Richter scale
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the logarithm of the maximum seismic body wave amplitude recorded on a standard type of seismograph at a distance of 100 km from the epicenter
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local magnitude Ml
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the duration of perceptible oscillation as recorded on a seismogram from a local earthquake can be conveniently converted to a ___________.
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duration magnitude Md
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the number of cycles the wave goes through in a certain amount of time
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frequency
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when the passing seismic waves have a frequency that matches the natural frequency of the building
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resonance
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the condition of soil and unconsolidated sediments losing their resistance to shearing; a situation when water that is located in pore spaces between sand grains is mobilized due to shaking and essentially turns the sediment into a fluid
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liquefaction
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supported by a series of bearing pads which are placed between the building and the building's foundation
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base isolation
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made from layers of rubber sandwiched together with layers of steel
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lead-rubber bearings
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piles of rubble - brick, stone, adobe
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unreinforced masonry
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not enough steel especially confinement steel (steel rebar wrapped around vertical rebar)
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non-ductile steel-reinforced concrete
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optimal building type
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steel frame
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when properly built will ride out the earthquake, more of the damage comes from flying objects
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wood frame
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Mw 6.4; arguably the most important eq in history because it mandated schools in LA be earthquake resistant - field act
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1933 Long Beach
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Mw 6.9; first eq to be recorded by strong ground motion seismometers, showed 0.3g
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1940 Imperial Valley
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increase of 1 second in frequency for every _______.
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10 stories
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Mw 6.9, used soviet style buildings with L brackets connecting beams to walls
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1988 Spitak Armenia
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Mw 8.5, 10-20 story buildings collapsing, matched resonance frequency, sedimentary basin
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1985 Mexico City
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Mw 6.5, most buildings were non-ductile steel reinforced concrete buildings
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1971 San Fernando
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most important in dictating whether or not a building will hold
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90 degree column to beam connection
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ideal crimping angle for confinement rebar
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135 degrees
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if a column exceeds _____, it is unable to resist gravity
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10 degrees
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philosophy of earthquake prediction based on previous history
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statistics and probabilities
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philosophy of earthquake prediction based on looking for precursors
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deterministic/physical
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Mw 9.4, largest earthquake ever recorded
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1960 Chile
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Mw 7.8
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1857 Fort Tejon
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Mw 6.9
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1995 Kobe
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Mw 7.9, epicenter in the heart of the city
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1906 San Francisco
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Mw 6.9, during the world series
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1989 Loma Prieta
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Mw 6.7, destructive eq in LA area
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1994 Northridge
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____ of oceanic lithosphere is mantle
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95%
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____ of oceanic lithosphere is crust
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5%
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what is the outer core made of
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iron and nickel
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what is the inner core made of
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iron and nickel
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outer core is
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liquid
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inner core is
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solid
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most damage from an earthquake a few tens of miles away comes from ______
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s waves
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body waves have a ________
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high frequency
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in partially molten material, p waves __________
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slow down
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most effective way to measure earthquakes
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moment magnitude scale
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the lithosphere/asthenosphere boundary is ______
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mechanical
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results from S waves being stopped entirely by the liquid core and P waves being bent by the liquid core
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s-wave shadow zone
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deepest San Andreas ruptures are ____ depth
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15 km
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how long do tsunami periods last?
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15 minutes
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fault displacement has a factor of _____
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3.2
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relative motion between the Pacific and North American plates is ______
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5 cm
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closest fault to USC
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Puente Hills blind thrust fault
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most important control of tectonic plates
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slab pull
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magma on convergent boundaries forms through _______
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dehydration melting
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magma on oceanic spreading centers forms through ______
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decompression melting
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isotropic stress is the __________
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same in all directions
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oceanic plates are rich in _______
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iron and magnesium
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reason for large hills in LA
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East West striking reverse faults
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_____ of plate boundary motion is caused by the Eastern California shear zone
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20%
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in normal faults _____ is vertical
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sigma 1
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1 mile = ____ km
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1.6
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_____ of total seismic energy occurs on the Pacific Rim
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90%
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how old is the earth?
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4.6 billion
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depth of the moho
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30-70 km
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depth of asthenosphere lithosphere boundary
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100 km
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depth of deepest earthquakes
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700 km
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depth of olivine to spinel boundary
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400 km
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earth's radius
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6371 km
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how thick is the earth's mantle
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2900 km
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earth's core radius
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3458 km
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order of polymorphic phase change
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olivine, spinel, perovskite
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locating EQ with s-p travel time: 1 sec
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4 km
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locating EQ with s-p travel time: 2 sec
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10 km
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locating EQ with s-p travel time: 10 sec
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80 km
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locating EQ with s-p travel time: 18 sec
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150 km
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Mw 7.6 manifestation of the release pressure that built up in the CA shear zone
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1872 Owens Valley
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the first time that a law had been passed to require buildings that had to be built to withstand earthquakes
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field act
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Mw 9.0 earthquake and tsunami killed 16,000
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2011 Tohohku
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Mw 7.3 only earthquake "ever" predicted by people
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1975 Haicheng
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Mw 7.8 no foreshocks, flattened the city
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1976 Tangshan
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Mw 6.1 foreshock of Landers earthquake
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1992 Joshua Tree
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Mw 7.1 west of Christchurch, occurred out in farm country
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2010 Darfield
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Mw 6.3 worst case scenario, occurred directly beneath the city
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2011 Christchurch
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original great San Francisco earthquake
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1868 Hayward
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earthquake that destroyed San Juan Capistrano mission
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1812 Wrightwood
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Mw 9.2 killed 250,000
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2004 Sumatra
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