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Chapter 6 Plate Tectonics
Chapter 6 Plate Tectonics

...  Most are found in the Pacific Ocean  The Mariana Trench is where the Pacific Plate is sinking under the Philippine Plate ...
Earthquakes: Tremors from Below – What Causes the Earth to Shake?
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... What Causes the Earth to Shake?  Tsunamis like the one in Samoa are triggered by large undersea earthquakes. To understand how  tsunamis form, let’s first take a look at what causes earthquakes. Most earthquakes happen at the  edges of tectonic plates, the big pieces of Earth’s crust that make up it ...
convection lab - Lauer Science
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... Convection takes place within a fluid. Large amounts of heat are transferred through Earth via convection currents. Some of these currents are in Earth’s liquid outer core. Other convection currents are present in the mantle. Convection currents in the mantle form and transfer heat as rock slowly ri ...
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Evolution of Australian Biota

... -There are three similar lung fish found in Australia, South America and Africa. ...
UNIT 1, Chapter 1, Lesson 2
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... 2. There are two types of crust, ____________________________ and ____________________. 3. ________________________ crust is thinner and denser than _________________________ crust because it has more __________________, __________________________, and _____________________ in its compounds. It more ...
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... Plate Tectonics Go through the slide show at your own pace, do more research if you need to ...
Convection Currents Lab
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Review material for Exam #3 in GLG 112 Natural Disasters

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Review material for Exam #3 in GLG 112 Natural Disasters
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... examples of each of these types of boundaries; examples of major plates on earth; where do volcanoes occur and what are their causes. What’s involved with hot spot volcanism and know examples; the similarities in spatial occurrence of earthquakes and volcanoes; two major types (central point and fis ...
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Lecture 3 Igneous Rocks
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... types of volcanoes due to the gas content in the magma.  Many famous eruptions are the  result, including Pompeii, Italy and Mt. St. Helens, Washington.  ...
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...  World’s youngest large igneous province (LIP).  Inundated by the largest documented flood in ...
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... (100 km) thick, resting upon a lower soft layer called the asthenosphere. Because the sides of a plate are either being created or destroyed, its size and shape are continually changing. Such active plate tectonics make studying global tectonic history, especially for the ocean plates, difficult for ...
PETROLOGY LAB 2: Nucleation and Crystal Growth in Mafic Lavas
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... transects of the associated Eocene plutons of the Coast Plutonic Belt. The Eocene magmatism of the northern Cordillera is particularly well suited to such an integrated study because uplift has exposed the deep core of the Coast Plutonic Belt (CPB), but shallow plutons and thick volcanic sequences a ...
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Unit 2 Review (CH 8, 10,11,12,13)
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... 48. True  or  False:  Most  mountains  form  as  a  result  of  collision  between  tectonic  plates.   49. Define  folded  mountain.   50. Define  fault-­‐block  mountain.   51. What  are  the  4  types  of  mountains?   52. What  happens  w ...
Collision-induced mantle flow during Tethyan closure: a link
Collision-induced mantle flow during Tethyan closure: a link

... represent lithospheric detritus accumulated at the core-mantle interface, they may be more plausibly explained by selective delamination of dispersed Gondwana cratonic roots in a context of shallow-level mantle convection. This type of model is supported by new thermobarometric and isotopic data for ...
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...  The thin outer layer of Earth.  There are 2 types of crust: continental and oceanic  The layer of rock beneath Earth’s crust  The inner part of the mantle is very hot, which makes it soft.  The liquid layer of melted iron and nickel beneath the mantle  The outer core is the source of Earth’s ...
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...  Because all of the oceans are connected, they are sometimes referred to as a single “world ocean”. ...
Late 20th Century Tests of the Continental Drift Hypothesis
Late 20th Century Tests of the Continental Drift Hypothesis

... • Like ridges and transform faults, the trenches are places where lithospheric plates move against each other. Benioff zones of earthquake foci tell us this. • The Benioff zones indicate that the movements are both deeper and occur in wider bands than at other plate margins, with one plate dipping b ...
NAME - Thomas C. Cario Middle School
NAME - Thomas C. Cario Middle School

... 23.) What happens to p-waves when they enter the liquid outer core? Bend and Slow down S-Waves? They don’t enter the Outer Core 24.) Which seismic waves are the fastest? Primary 25.) What is the name for the part of the Earth where no seismic waves are detected from a given earthquake? Shadow Zone 2 ...
The Four Layers
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... The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, plastic mantle which is located below the crust. These plates usually move along smoothly but sometimes they stick and build up pressure. The pressure builds and the rock bends until it snaps. When this ...
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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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