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How Does Earth Work?
How Does Earth Work?

... Continental margins above subduction zones Island arc volcanic chains above subduction zones Divergent boundaries: mid-ocean ridges, continental rifts ...
Tectonic Processes
Tectonic Processes

... thinning. Because the lithosphere is thinned, there is upwelling of the mantle below the necked crust. Decompression of the mantle results in partial melting, and basaltic magma is injected into the fissures or extruded as fissure eruptions. Basaltic magmatism at the axis of a ridge creates new ocea ...
C:\Users\jmhemzac\Desktop\2016 Fall\121rev1f16.wpd
C:\Users\jmhemzac\Desktop\2016 Fall\121rev1f16.wpd

... Be able to give examples (geographic locations, like our study sites) for each Describe and explain the differences in convergent boundaries with 2 continental plates, vs. those involving one or more oceanic plates. Give examples (geographic locations) for each type. Describe how transform boundary ...
Flynt - ______ Name: Fill in the Blank Fill in the blank with the
Flynt - ______ Name: Fill in the Blank Fill in the blank with the

... d. a volcanic island arc. ____ 29. Which of the following is NOT true of transform boundaries. a. Transform boundaries are places where two plates slip past each other moving in opposite directions. b. At a transform boundary, crust is neither created nor destroyed. c. Earthquakes frequently occur a ...
Igneous Activity and Volcanism Homework
Igneous Activity and Volcanism Homework

... 107. A ________ texture refers to rocks composed mainly of visible crystals greater than 1-inch. 108. A ________ texture refers to rocks composed mainly of uniform crystals that can only be seen with the aid of a microscope. 109. What term(s) denotes the smaller mineral grains in a porphyritic igneo ...
Plate Tectonic Theory
Plate Tectonic Theory

... material rises toward the mid-ocean ridges Some material solidifies. Some flows sideways and drags the seafloor along with it in both directions As the seafloor spreads apart, new seafloor is created Older seafloor moves away in opposite ...
VOLCANOES
VOLCANOES

... relative to the surrounding rocks causes it to rise. It will rise to the surface or to a depth that is determined by the density of the magma and the weight of the rocks above it. As the magma rises, bubbles start to form from the gas dissolved in the magma. The gas bubbles exert ...
Igneous Activity and Volcanism Homework
Igneous Activity and Volcanism Homework

... 107. A ________ texture refers to rocks composed mainly of visible crystals greater than 1-inch. 108. A ________ texture refers to rocks composed mainly of uniform crystals that can only be seen with the aid of a microscope. 109. What term(s) denotes the smaller mineral grains in a porphyritic igneo ...
loeclosednotes
loeclosednotes

... - ______, rigid, brittle, broken into _______ that move slowly and independently of one another. - This plate movement causes _________, volcanic eruptions, mountain shaping and _________ spreading. - This section floats on top of the ________________ ...
Volcanoes Webquest Wkst
Volcanoes Webquest Wkst

... Visit the following website: http://pubs.usgs.gov/fs/2005/3024/ Write a report about the Yellowstone regions volcanic activity, and its future. This should be two typed paragraphs ( minimum of 5 sentences each ...
Lecture 13.
Lecture 13.

... This process explains recent changes in the height of sea-level in coastal areas of eastern and northern Canada and Scandinavia. Some locations in these regions of the world have seen sea-level fall by as much as one meter over the last one hundred years. This fall is caused by isostatic rebound. Bo ...
crust, mantle, outer core, inner core
crust, mantle, outer core, inner core

... Bowl-shaped part of a volcano; lava often collects here before flowing down the slope ( vent, crater, magma chamber, pipe) ...
Glencoe Chapter 9
Glencoe Chapter 9

... measurements they use a _____________ and plot the distance as a radius out from each seismic station. ...
Pre-visit Lesson: Grades 3-5 - Washington State Parks and
Pre-visit Lesson: Grades 3-5 - Washington State Parks and

... point where the crust can break apart, earthquakes can occur, and the crust can crumple forming mountains. This theory can be shown through a simple demonstration. Using a few colors of play dough or craft foam you can demonstrate the various movements of tectonic plates and the layering of the eart ...
Inside the Earth
Inside the Earth

... Layer of the Earth that extends from below the mantle to the center of the Earth.  Outer core – liquid, inner core - solid  33% of Earth’s mass  Radius of 3,420 km  Temp. ranges from 3,700°C to 7,000°C (sun’s surface temp – 5500°C  Composed mainly of iron and contains smaller amounts of nickel ...
Volcano World Computer Activity
Volcano World Computer Activity

The Active Earth
The Active Earth

... convection currents in the Asthenosphere on the continental plates causing them to move small distances over long periods of time in relation to each other. ...
3 Cool , ρ = 3400 kg m
3 Cool , ρ = 3400 kg m

... 2. Transform faults and fracture zones (adjacent transform faults are parallel). 3. Continuous plate boundaries 4. Volcanic Island chains - plates moving over fixed mantle plume (melt source) 5. Topography variations consistent with aging plates. ...
Inside Earth
Inside Earth

... – Many volcanoes occur due to the many plate boundaries that exist in this region – Plate boundaries provide a weak spot in the crust that is necessary for volcano formation ...
it is a series of steps used to help solve a problem
it is a series of steps used to help solve a problem

The Rock Cycle and the three rock types File
The Rock Cycle and the three rock types File

... and more magma is introduced from below, the plate is forced away from the spreading ridge, and acquires a sediment cover. As shown in the figure, in this case, the oceanic plate eventually "dives" under the adjacent continental plate. As the oceanic plate travels deeper, high temperature conditions ...
Locate the plate boundaries
Locate the plate boundaries

... 3. Students will be able to make inferences about possible location of plate boundaries based upon seismic data obtained from various sources on the internet. Concept: Earth’s Oceans and continents are embedded in several large, flat plates that are moving slowly (about 5 cm/year). These lithospheri ...
The Edible Earth: Plate Movements
The Edible Earth: Plate Movements

... twenty separate plates that “float” on the hot plastic mantle of the inner Earth. The theory also states that the motion of these plates creates a variety of interactions at the plate boundaries. The boundaries of these crust plates collide, diverge, or slip past each other. Some crust plate boundar ...
Volcanoes
Volcanoes

... • Area where magma from deep within the mantle melts through the crust like a blow torch – Example: Hawaiian Islands ...
ALFRED WEGENER AND PANGAEA In 1915, the German geologist
ALFRED WEGENER AND PANGAEA In 1915, the German geologist

... Continental Drift The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle. The plates are made of rock and drift all over the globe; they move bot ...
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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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