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Rocks
Rocks

... This provides a list of Essential Knowledge and Skills that the student must master in order to be successful taking the Virginia SOL Test that will be administered at the end of the course. The student should check off each line item as their knowledge level is achieved. If at ANY TIME the student ...
Plate Boundaries and Plate Interactions
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13.7 plate tectonics MH - The University of Texas at Dallas
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... 2.7 billion years ago, these rocks were alive with volcanic fire. Today, they jut out of a mountainside like the spiny tail of a sleeping dragon. This rock, says Kevin Chamberlain, a geologist from the University of Wyoming in Laramie, could be a special kind — a lava called a komatiite. Today, Eart ...
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Wilson and Aster [2003
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... The Earthquake At 4:31 A.M. (local time) on Monday, January 17, 1994, a magnitude 6.8 earthquake woke nearly everyone in southern California. The earthquake epicenter was beneath the San Fernando Valley, 20 miles (32 km) west-northwest of downtown Los Angeles, near the community of Northridge (34° ...
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... •   If  the  trend  is  con8nued  back  to   about  80  million  years,  it  would   appear  that  the  hotspot  was   building  volcanoes  on  ocean  floor   of  the  same  age.   ...
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Microsoft PowerPoint - file.in [jen pro \350ten\355]

... In 1962, Harry Hess proposed the hypothesis that midocean ridges represent narrow zones where ocean crust forms. Seafloor spreading is a part of the theory of plate tectonics. At the Mid-Atlantic Ridge (and other places), material from the mantle rises through the faults between oceanic plates to f ...
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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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