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Make a bar graph with the Tectonic Plate as the independent
Make a bar graph with the Tectonic Plate as the independent

... **Be sure to title your graph and label the x axis and the y axis as well as put in the units where it is appropriate. **Use different colors for different plates so that two colors are not next to each other. ...
Volcano and extrusive igneous rock notes
Volcano and extrusive igneous rock notes

... is the generation of fracture systems that isolate ~6-sided columns of cooling rock from one another, in a process that is quite similar to the development of shrinkage cracks in drying mud. Some effects of volcanoes • Volcanic activity can lead to the creation of new land area • source of geotherma ...
Crust
Crust

... • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. • The worlds deepest parts of the ocean are found along trenches. – ...
7.4 Forces that move plates.
7.4 Forces that move plates.

... Write a description of each example and suggest how each might have formed. ...
What is Plate Tectonics
What is Plate Tectonics

... A slab of continental lithosphere (continental crust + lithospheric mantle) stands higher than a slab of oceanic lithosphere (containing oceanic crust) of the same dimensions. Oceanic crust: 3.0 g/cm3 Lithospheric mantle ~ 3.3 g/cm3 ...
Exam #2 - MSU Billings
Exam #2 - MSU Billings

... d. An ancient strike-slip fault, like The San Andreas Fault 37. On what major island does the Mid-Atlantic Ridge appear above the surface of the ocean? a. Iceland b. Greenland c. Antarctica d. Baffin Island e. Great Britain 38. What is happening to lithospheric plates at divergent plate boundaries? ...
Processes
Processes

... 1. Metamorphism means "changed form." It is the process that changes sedimentary, igneous, and metamorphic rocks into new metamorphic rocks. 2. Weathering and Erosion is the process by which rocks are attacked by the environment3. Cementation and Compaction is a two step process. Rocks are constantl ...
Cornell Notes Topic/Objective: The Theory of Plate Tectonics Name
Cornell Notes Topic/Objective: The Theory of Plate Tectonics Name

... _______________suggests that Earth’s surface is divided into large ___________ of rigid rock and each plate ____________ over Earth’s hot and semi plastic mantle. In the 1940s scientists determined the depth of the ocean using an echo sounder. ...
Name:
Name:

... 8. Because less weight is exerted on the ____________ core, the pressure is less here, with the result that the iron and nickel are _________________. 9. The molten core flows at the low rate of several kilometers per ____________. 10. This flow is evident far outside the Earth’s surface as it gener ...
Pre/Post Test
Pre/Post Test

... B. weathering and erosion D. compaction and cementation ________4. Sedimentary rocks are formed by which earth process(es)? A. melting C. heat and pressure B. weathering and erosion D. compaction and cementation ________5. Igneous rocks are formed by which earth process(es)? A. melting C. heat and p ...
Earthquake in a Box
Earthquake in a Box

Dates and dynamics: Snowball Earth comes of age
Dates and dynamics: Snowball Earth comes of age

... sets and arguably the third are now strongly supported by observations unavailable when the hypothesis was proposed. At the same time, climate models suggest that the snowball atmosphere, cryosphere, ocean and lithosphere were more dynamic and unstable than initially assumed, consistent with geologi ...
Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

... • The rock cycle shows how one type of rocky material gets transformed into another – Representation of how rocks are formed, broken down, and processed in response to changing conditions – Processes may involve interactions of geosphere with hydrosphere, atmosphere and/or biosphere – Arrows indicat ...
PDF format - GEMOC - Macquarie University
PDF format - GEMOC - Macquarie University

... and/or rifting; its density also can be increased by infiltration of asthenospheric melts until the lower parts become unstable. 4-D Lithosphere Mapping in eastern China documents the Mesozoic extension of Archean SCLM and the upwelling of asthenospheric mantle; results included dramatic uplift foll ...
Plate Tectonics Study Guide: Answer key
Plate Tectonics Study Guide: Answer key

... Involves at least 1 oceanic crust and another crust in convergent boundary ...
Granitoid Rocks
Granitoid Rocks

... “Granitoids” (sensu lato): loosely applies to a wide range of felsic plutonic rocks This lecture focuses on non-continental arc intrusives Associated volcanics are common and have same origin, but are typically eroded away ...
Continental Margins
Continental Margins

... Continental shelf Continental slope Continental rise Submarine canyons ...
Preliminary geochemical data for dolerite dykes and sills of the
Preliminary geochemical data for dolerite dykes and sills of the

... of the Etendeka region and Karoo rocks occurring elsewhere in southern Africa, we propose to regard them as constituting a separate Etendeka Igneous Province which exhibits a close lithological, geochemical and temporal correlation with the Paraná Flood Basalt Province of South America. In previous ...
Quiz # 8
Quiz # 8

... C) a pattern of jumbled terrain diametrically opposite to the Basin, caused by the focused seismic waves from the original impact. D) a very thick dusty atmosphere that still obscures the planet's surface. ...
Laramide Orogeny - Major Tectonic event that formed the Rocky
Laramide Orogeny - Major Tectonic event that formed the Rocky

...           ‐ elevated levels of oxygen in the atmosphere (heavily oxidized)   ‐ Long record of sedimentary rocks (horizontal structure)             ‐ Upper Mesozoic Period =  shallow interior sea (easy to trace)  ...
The convergence of the Nazca and South American Plates has
The convergence of the Nazca and South American Plates has

... The oceanic Nazca Plate is being subducted under the continental part of the South American Plate. The South American Plate is being lifted up, creating the Andes mountains. Strong, destructive earthquakes and rapid uplift of mountain ranges are common in this region. These earthquakes are often acc ...
Who developed the theory that the continents were once joined
Who developed the theory that the continents were once joined

... Mid-Atlantic ridge 18. Give an example of a divergent plate boundary involving two continental plates. Great Rift Valley of Africa 19. Plates that move towards one another are called? convergent plate boundary 20. What is a subduction zone? A more dense oceanic plate is forced under a less dense con ...
Powerpoint Presentation Physical Geology, 10/e
Powerpoint Presentation Physical Geology, 10/e

... like the crust, is made of solid rock with only isolated pockets of magma • Higher seismic wave velocity (8 km/sec) of mantle vs. crustal rocks indicative of denser, ultramafic composition • Crust and upper mantle together form the lithosphere, the brittle outer shell of the Earth that makes up the ...
Plate Tectonics
Plate Tectonics

... 4. Fossils and evolution • Fossils of species on one side of the Atlantic found on the other side. • Today the species appear much different from each other due to evolution BUT they have a common ancestor ...
Large Igneous Provinces, Delamination, and Fertile Mantle
Large Igneous Provinces, Delamination, and Fertile Mantle

... delamination mechanism creates multiple pulses of magmatism, separated by tens of millions of years, a characteristic of some LIPs. If the crustal thickening is due to compressional tectonics, the time scales will be dictated by convergence rates. In a typical convergent belt, thickening and delamin ...
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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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