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Why no volcanoes? Why are there no active volcanoes in Britain?
Why no volcanoes? Why are there no active volcanoes in Britain?

... most volcanically active area in the world is around the edge of the Pacific Ocean, from Indonesia to Japan, Alaska, the USA, Central America and South America. These volcanoes all lie on the edges of the Pacific plate (or smaller plates close by). ...
InsidetheEarth
InsidetheEarth

... atoms of iron and nickel so much that they cannot spread out and become liquid. ...
Plate Tectonics
Plate Tectonics

... Evidence of Pangaea • Climate , as continents move toward the poles, its climate is colder. • As continents move toward the equator, its climate gets warmer. • Fossils of tropical plants were found in the ...
Rock and Roll
Rock and Roll

... 142.Rocks such as sandstone, which allow water to pass through them easily are: a. permeable b. impermeable c. cap rocks d. metamorphic 143.Siltstone is most likely to form: a. On the bottom of a still lagoon b. Near the end of a Raging river c. Close to the edges of a babbling brook d. At South Cou ...
Astronomy Test - The Summer Science Safari Summer Camp
Astronomy Test - The Summer Science Safari Summer Camp

... 2. According to the big bang theory, the age of the universe is about: 3. Astronomers often place telescopes on mountaintops because: 4. Describe the two types of telescopes. Include a description of the advantages and disadvantages of each 5. If you see a quasar that is 6 billion light-years away, ...
theory of plate tectonics
theory of plate tectonics

... a. thin outer shell of earth b. less dense than material below which causes movement of plates = broken into sections 1) have identified 30 so far 2) interact together to create major surface features a) move toward each other and collide b) moving apart c) slide past one another c. composed of gran ...
Geology (Chernicoff) - GEO
Geology (Chernicoff) - GEO

... C) Yukon River in Alaska. D) South America's Amazon River. 21) In which stage of the rifting process are plate edges considered to be passive continental margins? A) In the initial stages of continental rifting. B) When seawater from an adjacent ocean inundates a young rift. C) As basalts begin to f ...
Unit 10: Layers of the Earth
Unit 10: Layers of the Earth

... Element: A pure substance that cannot be separated into simpler substances by physical or chemical means Model: A limited representation of an object used to help us understand its structure or how it works Content Vocabulary Asthenosphere: The solid layer with plasticity in the upper mantle that is ...
Plate tectonics: Metamorphic myth
Plate tectonics: Metamorphic myth

... than at present — we may have been looking for rocks that simply could not have been generated. To preserve blueschist at the surface, the rocks must be rapidly exhumed to Earth’s surface without undergoing any further metamorphism8. Given this rather intricate scenario required for the surface expo ...
Pangaea
Pangaea

Document
Document

... FACT: Earthquakes induced by human activity have been documented in a few locations in the United States, Japan, and Canada. The cause was injection of fluids into deep wells for waste disposal and secondary recovery of oil, and the filling of large reservoirs for water supplies. Most of these earth ...
Why do you think Earth has layers?
Why do you think Earth has layers?

... - rocks are close to their melting points in this layer. (plastic-fluid like material) - the lithosphere floats on the ...
The surface of Earth is constantly being changed. Rocks are
The surface of Earth is constantly being changed. Rocks are

Geodynamics
Geodynamics

... Studies of the Earth's Deep Interior (CSEDI). Funding will support basic research on the character and dynamics of the Earth's mantle and core, their influence on the evolution of the Earth as a whole, and on processes operating within the deep interior that affect or are expressed on the Earth's su ...
Plate Tectonics
Plate Tectonics

... tectonic plates. They are moving very slowly, but constantly. (Most plates are moving about as fast as your fingernails are growing -- not very fast!) Currently Earth’s surface layers are divided into nine very large plates and several smaller ones. ...
1. Earth Science a. Branches i. Geology—study of rocks, minerals
1. Earth Science a. Branches i. Geology—study of rocks, minerals

... i. Most of Earth is mantle—rocky shell 2900 km thick ii. Crust has less iron, more silica—thin veneer iii. Core is mostly metal—iron and nickel, ~3500 km radius b. Physical properties of these zones change with depth, due to increase in pressure at greater distances from surface i. Lithosphere is th ...
Y8GeU4A Plate tectonicsPPwk14
Y8GeU4A Plate tectonicsPPwk14

... The Eurasian and North American plates moving away from each other – so very slowly Europe is getting further away from America. As the plates move apart (very slowly), magma rises from the mantle. The magma erupts to the surface of the earth. When the magma reaches the surface, it cools and solidif ...
What They Say in Hong Kong Geography Books and Exam
What They Say in Hong Kong Geography Books and Exam

... What they say (in a Geography exam marking scheme): The main cause of the transform faults is the results of the earth’s rotation. What we actually know: Earth’s rotation has nothing to do with transform faults. Transform faults are simply plate boundaries along which the plates on both sides of the ...
NSTA Geology Reading 1 • Plate Tectonics
NSTA Geology Reading 1 • Plate Tectonics

... ‣ Age of rocks from seafloor increased moving away from the ridges and toward the continents ‣ If seafloor is moving, then places and continents must also be moving ‣ When new oceanic crust from at mid-ocean ridges, both the older oceanic crust and the continents riding atop the plates move - Convec ...
Plate Tectonics Unit:
Plate Tectonics Unit:

... stretch as sections move past one another, but eventually so much pressure builds up that the rock breaks and snaps back (like a rubber band), which releases waves of energy. The sudden snapping back of rock is called elastic rebound. ...
No Slide Title
No Slide Title

... • Earthquake Seismic Waves => Physical state of crust, mantle, core. ...
Unit 3- Plate Tectonics - Thomas C. Cario Middle School
Unit 3- Plate Tectonics - Thomas C. Cario Middle School

... Lithosphere Mantle Mountains Valley/ Seas C ...
Earth Science Unit Review
Earth Science Unit Review

... (iv) No, there is no material that can flow in currents. 42. Slab pull occurs at subduction zones, where a part of a plate dives into the mantle, pulling the plate material behind down with it. Ridge push occurs at spreading ridges, where mantle material reaching the surface pushes plates apart. 43. ...
Layers of Earth Notes
Layers of Earth Notes

Questions For Review KEY
Questions For Review KEY

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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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