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2. Manual plot of geographic coordinates on a stereographic
2. Manual plot of geographic coordinates on a stereographic

Internet Webquest
Internet Webquest

... The website contains information regarding each of the 3 types of plate boundaries we will be discussing in class. You will need to read the information to determine the definition and example locations. There are images for each of the three types, but there is also a link towards the top of the pa ...
Volcano Notes Viscosity is a property of fluids which describes the
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... have come from the continental rocks.  These sediments are high in  silica.  When the plate begins to melt, the silicates are some of the first  materials to melt. ...
Daily Questions
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...  What are the five major plutons?  Which type of crust would you find a basalt plateau on?  I have lava that is dark, ropy and very high in iron. What type of formational and compositional lava is this?  What type of magma did it originate from?  What type of volcano did it most likely originat ...
Chapter 10 Worksheet
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Geology Lab: "Edible Tectonics"
Geology Lab: "Edible Tectonics"

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Indicate the answer choice that best completes the statement or
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Chapter 2.pmd
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... the interior of the earth on its surface. When this molten word sedimentum lava comes on the earth’s surface, it rapidly cools down meaning settle down. and becomes solid. Rocks formed in such a way on the Metamorphic: Greek crust are called extrusive igneous rocks. They have a word metamorphose ver ...
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divergent plate boundary influenced by a hotspot

... The mid Atlantic ridge, separating the Eurasian and North American tectonic plates, is mostly buried below the Atlantic. There are, however, a few places where subaerial exposure of the mid-oceanic rift system allows geodetic observations of the deformation associated with the plate boundary. Icelan ...
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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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