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yr12-pt-lesson-7-hmwk-ws
yr12-pt-lesson-7-hmwk-ws

... b. Import and annotate a diagram to explain what happens at this boundary c. Describe and explain the processes that occur at this boundary e.g. rifting d. Name the landforms that are produced e. Give a named example (Include the plate names) NB: Causes of plate movement at a divergent/constructive ...
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Invited Review Gillian R. Foulger Dept. Earth Sciences, Science
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GCSE Geography Revision Pack: Key Themes Paper Natural
GCSE Geography Revision Pack: Key Themes Paper Natural

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Igneous rocks form from molten rock.

... crack, the lava may erupt in different ways. Some lava can build huge plateaus when it erupts from long cracks in Earth’s surface. Lava that is low in silica, such as basalt lava, flows easily and spreads out in thin sheets over great distances. The Columbia Plateau in Oregon and Washington is made ...
Igneous rocks form from molten rock.
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... such as rhyolite and pumice (PUHM-ihs). Basalt (buh-SAWLT) is an extrusive igneous rock that forms the ocean floor. Gabbro is an intrusive rock that has the same composition as basalt. ...
Geology * Part II - Hatboro
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... 4. Satellite Monitors – uses GPS from outer space to monitor changes in elevation as well as horizontal movement along a fault 5. Seismographs – collects data (seismic waves) from earthquakes ...
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SENIOR SCIENCE SUPPLEMENTARY QUESTIONS Physics (22
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... In correct order from the center outward, Earth includes which layers? a. core, inner mantle, outer mantle, crust b. inner core, outer core, mantle, crust c. inner core, crust, mantle, hydrosphere d. core, crust, mantle, hydrosphere ...
Cenozoic 1 - E. R. Greenman
Cenozoic 1 - E. R. Greenman

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The Earth`s Layers Foldable
The Earth`s Layers Foldable

... 4. Set a piece of 8 by 11 blue paper in front of you. Closely trim the title. Paste The Earth's Layers title in the top left corner of the paper (or bottom right corner after you have folded and stapled the pages together--see Image). 5. Paste the Crust on the top of the first blue paper, to the lef ...
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Earth has several layers.

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oceanic crust

... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Earthquake-Volcano Research Project Rubric
Earthquake-Volcano Research Project Rubric

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our Chocolate Geology outdoor learning resource
our Chocolate Geology outdoor learning resource

... SEDIMENTARY rocks are made up from fragments of rocks and the remains of animals and plants. Rain, wind and ice wear away and erode tiny pieces of exposed surfaces like mountains. These fragments are called sediment. Rain washes the sediment into rivers and streams where they tumble and knock into e ...
Rapid lithification masks the Venus sedimentary cycle
Rapid lithification masks the Venus sedimentary cycle

... material throughout the highland regions. In some areas, this material is deposited on adjacent plains where, under the extreme Venus surface conditions, lithification is an apparently rapid process. Thus the largely featureless plains may not be igneous at all but sedimentary in origin. The settlin ...
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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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