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Volcanoes & Earthquakes
Volcanoes & Earthquakes

... chimney) of his furnace was an island named Volcano… this was a simple attempt by people to try to understand the complex processes that cause volcanic activity ...
View Sample - Popular Book Company
View Sample - Popular Book Company

... of South America seems to fit nicely with the west coast of Africa, like two puzzle pieces? This can be explained by the theory of plate tectonics in which we believe that, millions of years ago, all the continents of the world were one big landmass called Pangaea. Pangaea began breaking up 180 mill ...
Section 13
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... 1. broad volcano with gently sloping sides 2. long crack that forms as two tectonic plates move apart 3. magma that reaches Earth’s surface 4. point inside Earth where earthquake movement first occurs 5. small volcano formed from tephra 6. the surface of a break in a section of rock 8. steep-sided v ...
Name: Period:______ Date: Earth Science in Action: Rocks Video
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Read the following about the layers of the Earth and answer the
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HS Earth Standard 3.3 Plate Tectonics
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... not immediately cause a stampede, for they were new and uncertain and people doubted their reliability. Meanwhile, American scientists had been measuring the magnetism of rocks on the sea floor, partly out of curiosity, partly because the US Navy hoped these measurements might suggest new means to h ...
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... Terms to know prior to completing this lab: intrusive, extrusive, plutonic, volcanic, texture, composition, mafic, felsic, intermediate, aphanitic, phaneritic, vesicular, porphyritic, pegmatitic, glassy. These are the terms you needed to know for the pre-lab quiz. PART 1: Fill in the following table ...
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Created with Sketch. Tectonic sandwiches
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... The Earth’s crust is made up of large separate plates or areas that fit together rather like a huge jigsaw puzzle. They float on the partially molten mantle. Where the plates meet – the boundaries – movement happens. The plates can move apart, they can move horizontally past each other or they can m ...
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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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