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Earth`s Surface:
Earth`s Surface:

...  Earth is a geologically active planet.  The continents, composed of less dense rock, move slowly upon the denser ...
CH. 7 Review WS #3 - Wachter Middle School
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... The earth's surface is built of material that comes from beneath the crust, or it is formed by the movement of the crust itself. The heat of the earth's interior creates convection currents in the mantle. These convection currents sometimes cause the magma in the mantle to break through the crust of ...
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...  A subduction zone occurs when one oceanic plate is forced down into the mantle beneath a second plate.  Oceanic-Continental - Denser oceanic slab sinks into the asthenosphere. - Pockets of magma develop and rise. - Continental volcanic arcs form in part by volcanic activity caused by the subducti ...
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...  Glomar Challenger 1968- drilled sediment core samples east and west of the Mid-Atlantic Ridge. o Evidence supported seafloor spreading- age of sediments were older further from the ridge and sediments were thicker further from the ridge  JOIDES Resolution 1996- drilled sediment core samples east ...
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... CAMP before or at the time of its emplacement (71). Simultaneously, rift basins farther north actually accelerated in subsidence. Sequentially, over the next 145 million years, the pattern of initial sea floor and seaward-dipping reflector formation and concomitant rift basin inversion seems to have ...
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... C. ______________________– steep walled depression around a volcano’s vent D. _______________________________ – areas where magma from deep in Earth’s mantle has melted through the crust to form several volcanoes 1. Ex. ___________________________________________ the Pacific Plate is moving over a s ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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