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-complex motion -slowest velocity |
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-push/pull motion -travels through solids, liquids, gases -greatest velocity of all earthquake waves |
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'shake' motion -travels only through solids -slower velocity of all earthquake waves |
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study of earthquake waves |
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earthquake recording instrument -records movement of Earth |
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the record that comes from a seismograph |
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the place within Earth where earthquake waves originate |
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the point above the focus where the earthquake waves originate |
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-introduced by Charles Richter in 1935 -based on amplitude of the largest seismic wave -each unit of Richter magnitude equates to roughly a 32-fold energy increase -does not estimate adequately the size of very large earthquakes |
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-saturated material turns fluid -underground objects may float to surface |
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-thin, rocky outer layer -varies in thickness -roughly 5 miles in oceanic regions -upper crust made up of granite -ocean crust made up of basalt -crust average is 25 miles |
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composition of uppermost mantle is the igneous rock peridotite (changes at greater depth) |
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-a sphere having a radius of 3486 km -composed of an iron-nickel alloy |
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-crust and uppermost mantle -cool,rigid,solid |
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-beneath lithosphere -play dough material -soft, weak, easily deformed -upper mantle |
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-lower mantle -more rigid layer -very hot rocks and capable of gradual flow |
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-liquid layer -2270 km thick -convective flow of metallic iron within generates Earth's magnetic field -S waves stop when they hit outer core |
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-sphere with a radius of 1216 km -behaves like a solid |
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three station recordings are needed to locate an epicenter -circle equal to the epicenter distance is drawn around each station -point where three circles intersect is the epicenter |
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continental drift hypothesis |
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super continent drifted apart 200 million years ago -continents drifted to present positions -continents broke through oceans crust |
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-first proposed hypothesis, 1915 -published The Origin of Continents and Oceans |
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a super continent that broke apart 200 million years ago. |
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(constructive margins) -two plates move apart -mantle material up-wells to create new seafloor |
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convergent plate boundaries |
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(destructive margins) -plates collide, and ocean trench forms and lithosphere is subducted into the mantle |
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oceanic-continental convergence |
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-denser oceanic slab sinks into the athenosphere -pockets of magma develop and rise -continental volcanic arcs form -examples include the Andes mountains |
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oceanic-oceanic convergence |
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-two oceanic slabs converge and one descends beneath the other -often forms volcanoes on the ocean floor -volcanic islands arcs forms as volcanoes emerge from the sea -examples include Japan |
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continental-continental convergence |
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when subducting plates contain continental material, two continents collide -can produce new mountain ranges such as the Himalayas |
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types of divergent plate boundaries |
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-ocean ridges -seafloor speading |
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transform fault boundaries |
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-plates slide past each other -no new crust is made or destroyed -examples include San Andreas fault |
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bid, almost all lava that comes out, broad, quietest eruption, flat mountain-like |
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almost all pyroclastic,tiny,quiet eruption, steep sides |
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stratovolcano (composite) |
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mix of lava/pyroclastic, pretty bif, violent eruptions, steep sides |
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200 times more eruption debris than any other volcano -Toba, Yosemite -underground. weather changing, demographics changing |
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molten rock originating deep within the planet rises to the surface to produce 'hot spot' volcanoes |
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Fluid basaltic lava extruded from crustal fractures called fissures e.g., Columbia Plateau |
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An underground igneous body |
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Types of igneous intrusive features:Dike |
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Types of igneous intrusive features:Sill |
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parallel to features such as sedimentary strata |
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cuts across existing structures |
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Steep walled depression at the summit Formed by collapse Nearly circular Size exceeds one kilometer in diameter |
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is a measure of a material's resistance to flow |
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High viscosity means more resistant to flow Slower movement |
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Thicker liquid High silica – high viscosity (e.g., rhyolitic lava) aa lava |
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Low viscosity means less resistance to flow Faster movement |
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Thinner liquid Low silica – more fluid (e.g., basaltic lava) pahoehoe lava |
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