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Plate Tectonic Unit Test Review
Plate Tectonic Unit Test Review

... 40. Figure 6F-1A is a(n) __composite volcano_____. It is made of __alternating layers of lava & tephra_. 41. Figure 6F-1B is a(n) ___Cinder cone volcano__. It is made of _ loosely packed layers of tephra__. 42. Figure 6F-1C is a(n) ___Shield Volcano_____. It is made of __flat layers of silica-poor l ...
The Restless Earth - Whitworth Community High School
The Restless Earth - Whitworth Community High School

... margins new land is neither created not destroyed. Landforms found at plate margins/boundaries ...
this and open it
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Plate Tectonics Reading
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... ocean floor, oceanographers have discovered mountainous ridges along the bottom of the ocean. These ridges appear to be where two plates have started to move apart. Molten rock from the underlying mantle oozes out and fills the space that has been created by the plates’ movement. The theory of plate ...
The Rock Cycle - Science A 2 Z
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... Sedimentary rock is the only place where we ...
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... East African Rift rift valley Example: _____________ Creates a __________. ...
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... 120ºE ...
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... Heat and pressure cause the plates to move – pressure pushes the asthenosphere to move plates Outer core because it’s made of liquid metal Fe and Ni Solid? Must be inner core Outer core is liquid Outer core is hottest – hotter than the surface of the sun Lithosphere True, we have convection currents ...
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Volcanoes - SchoolRack

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Plate Tectonics What is it and what makes it work?

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3.4 * Igneous and Metamorphic Rocks
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RM 1 Snack Tectonics Lab Sheet

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Name: June Proficiency Exam Study Guide 7th Grade Science
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... down 6. What was Wegener’s initial hypothesis? Why didn’t scientists accept it? What eventually caused them to change their minds? What is the Theory of Plate Tectonics? Wegener’s hypothesis stated that the continents have slowly moved to their current locations. Wegener’s hypothesis was rejected be ...
Activity: A Plate Tectonic Puzzle - American Museum of Natural History
Activity: A Plate Tectonic Puzzle - American Museum of Natural History

... Activity: A Plate Tectonic Puzzle Introduction The Earth’s crust is not a solid shell. It is made up of thick, interconnecting pieces called tectonic plates that fit together like a puzzle. They move atop the underlying mantle, a really thick layer of hot flowing rock. By examining evidence such as ...
No Slide Title
No Slide Title

... too low, – although one continent may partly slide under the other ...
Seismic Waves
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Rock cycle - Evaeducation
Rock cycle - Evaeducation

... which is typical of a group of rocks or rock-forming minerals, though usually more than one of these alterations will be found in progress in the same rock. Silicification, the replacement of the minerals by crystalline or crypto-crystalline silica, is most common in felsic rocks, such as rhyolite, ...
Plate tect - jenniferwells-lewis
Plate tect - jenniferwells-lewis

... Principles of plate tectonics Lithosphere - The outermost portion of Earth is composed of a mosaic of thin rigid plates that move horizontally with respect to one another Asthenosphere – middle of the mantle lithosphere ‘floats on top’ zone where magma is formed easily deformed, can be pushed down ...
Earth - World Book Encyclopedia
Earth - World Book Encyclopedia

... Plutonists believed rock was formed by the cooling of igneous rock after volcanic eruptions. The Neptunists thought the entire earth had been covered by oceans at one time and had since evaporated, leaving dry land in some places.  In 2005, scientists of the American Geophysical Union reported that ...
Powerpoint
Powerpoint

... marine sandstone and mudstone grade westward into the paleoPacific. Deposits were thin on the continental platform east of the hingeline, and thicken rapidly to the west of the hingeline. ...
Geology of the Hawaiian Islands
Geology of the Hawaiian Islands

... At shallow depths, rocks are brittle and deform elastically When subjected to sufficient stress, they fracture forming a fault  When the fault is locked, stress builds ...
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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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