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Answers - Jenksps.org
Answers - Jenksps.org

... The Earth’s crust and part of the upper mantle are broken into sections. Plates move on plastic-like layers of mantle. 19. What evidence is used to support the Theory of plate Tectonics? Continental drift, seafloor spreading, fossil clues, rock clues, magnetic clues, puzzle-like fit of the continent ...
Document
Document

... responsible for movement of earth’s crust. MANTLE (MESOSPHERE) a semi-liquid plastic consistency which liquefies when pressure is reduced OUTER CORE liquid INNER CORE solid ...
ppt
ppt

... Figure 10-13b. Spider diagram for a typical alkaline ocean island basalt (OIB) and tholeiitic mid-ocean ridge basalt (MORB). From Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall. Data from Sun and McDonough (1989). ...
Document
Document

... Figure 10-13b. Spider diagram for a typical alkaline ocean island basalt (OIB) and tholeiitic mid-ocean ridge basalt (MORB). From Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall. Data from Sun and McDonough (1989). ...
a rock is - MR. TRAN @ JWG
a rock is - MR. TRAN @ JWG

... The sandstone was formed from sandy river deposits, a relatively high energy environment. After consolidation into rock these beds were gently uplifted, remaining almost horizontal. Cliff reveals layers which vary slightly in hardness and reflect variations in original conditions ...
Chapter 6 – Igneous rock
Chapter 6 – Igneous rock

... • Extrusive igneous rocks spill out on the surface as lava, which hardens to produce rocks such as rhyolite, andesite, basalt, obsidian, pumice, and different types of pyroclastic rocks. • Extrusive lava produce volcanoes and lava flows. • The Earth’s interior is not composed mostly of molten rock. ...
Tectonics of the Precambrian
Tectonics of the Precambrian

... produced by partial melting of oceanic crust in subduction zones • Tonalites are more felsic igneous rocks - abundant plagioclase, quartz, high in Ca,Na, Al ...
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5. Seismology and Plate Tectonics

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Plate Tectonics : Different Plate Boundaries Create Different
Plate Tectonics : Different Plate Boundaries Create Different

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ROCKS
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chap2 - LaffertysBiologyClass
chap2 - LaffertysBiologyClass

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Plate Tectonics : Different Plate Boundaries Create Different
Plate Tectonics : Different Plate Boundaries Create Different

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Plate Tectonics
Plate Tectonics

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Section 17.3 Theory of Plate Tectonics
Section 17.3 Theory of Plate Tectonics

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Rock Cycle notes
Rock Cycle notes

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Picture Review Name
Picture Review Name

... Two broken continents of Pangea Convection current in the asthenosphere Continents are drifting apart by Alfred Wegener What explains the continental drift theory. Plates move because of the convection current in the mantle. Plates separate or moves away from each other. Asthenosphere Convection Atl ...
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Obsidian Cooling Rate

Chapter 7 Section 1
Chapter 7 Section 1

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Chapter 8 Study Guide – Earthquakes 1. What is an
Chapter 8 Study Guide – Earthquakes 1. What is an

... 13 Why is the inner core a solid at a higher temperature than the outer core at a lower temperature? 14. Describe the characteristics of Earth’s mantle. 15. What is the boundary between the outermost layer of the earth and the mantle called? Who is it named after? 16. What are the two types of crust ...
Lab Partners: Period: Rock Cycle Review
Lab Partners: Period: Rock Cycle Review

... ____ 10. A rock is ____. a. always made of molten material b. a mixture of minerals, organic matter, volcanic glass, or other materials c. a pure mineral d. either igneous or sedimentary ____ 11. The crystals that form in slowly cooling magma are generally ____. a. nonexistent c. tiny b. invisible d ...
Movement of the Earth Theory of Plate Tectonics
Movement of the Earth Theory of Plate Tectonics

... • Plates moving apart at the mid-ocean ridges are examples of divergent plate boundaries. – In the Atlantic Ocean, the North American Plate is moving away from the Eurasian and the African Plates. – The Great Rift Valley in eastern Africa may become a divergent boundary. The continental plate is bei ...
Chapter 8
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Snack Tectonics - Doral Academy Preparatory
Snack Tectonics - Doral Academy Preparatory

... 1. What type of crust is represented by the graham crackers? 2. What type of crust is represented by the fruit roll-up? 3. What physical layer of the earth does the frosting represent? 4. Give one real –life example of each type of plate boundary: (geographic location and how it was formed) • Contin ...
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File - Islamic Center Of Northland

... The aforementioned hadith prohibits oppression in general, especially the taking of a piece of land belonging to others unjustly. What might the seven earths refer to? Studies in geology have proven that the earth is composed of seven zones, identified from the inner to the outer layers as follows: ...
Intrusive volcanism * a summary
Intrusive volcanism * a summary

... earth's crust (plate tectonics).The formation of mountain ranges occurs by means of lateral movements as opposed to vertical ones. Mountain formation is related to plate tectonics. Folding, faulting, volcanic activity, igneous intrusion and metamorphism are all parts of the orogenic process of mount ...
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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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