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Skills Worksheet
Skills Worksheet

... a. uplift. c. faulting. b. folding. d. subsidence. _____ 9. The type of fault in which the hanging wall moves up relative to the footwall is called a a. strike-slip fault. c. normal fault. b. fault-block fault. d. reverse fault. _____ 10. The type of mountain that forms when rock layers are squeezed ...
Plate Tectonics Vocabulary Word Search
Plate Tectonics Vocabulary Word Search

... ______________ fault- In plate tectonics, a boundary between two plates that are sliding horizontally past one another. ...
Document
Document

... DIVERGENT - solid mantle upwells to replace lithospheric plates that are moving apart. In oceanic lithosphere, this is a Mid-ocean ridge (most common) In continental lithosphere, this is continental rift (much less common) ...
Document
Document

... liquid Lithosphere is the crust and rigid uppermost parts of upper mantle,at a depth of about ...
Pangaea (240 Myr ago) - University of Hawaii
Pangaea (240 Myr ago) - University of Hawaii

... Garrett Apuzen-Ito ...
2.13 Divergent Plate Boundaries
2.13 Divergent Plate Boundaries

...  As two oceanic plates move apart, the lithosphere is being extended, thinned and fractured.  Magma form the asthenosphere upwells into the rift valley. ...
Plate
Plate

... *The lava then cools & crystallizes to form new seafloor mountains (midocean ridges.) *Younger rock is at the midocean ridges & the older rock is at the continental margins. ...
Inside the Earth
Inside the Earth

... • Mantle (flows putty) – Oxygen – Silicon – Iron • Core (mostly iron) ...
Slide 1
Slide 1

... surface forms an Igneous Rock with a fine grained texture Instrusive – Magma that cools and solidifies inside the Earth’s surface forms Igneous Rock with a course grained texture ...
Chapter 10 study guide
Chapter 10 study guide

... Earth’s surface. Paleomagnetism – the study of the magnetic property of rocks. Magnetic stripes helped provide evidence for sea-floor spreading. Iron bearing minerals in igneous rocks can show the direction of Earth’s magnetic field at the time the rocks formed. Plate tectonics – theory that explain ...
Ancient crust rises from the deep
Ancient crust rises from the deep

... sulphur-33 is substantially lower than that typically found in Earth’s crust. Although biological processes can generate such an anomaly, they would simultaneously generate abnormally high concentrations of sulphur-34 — which are not present in the Mangaia samples. The most likely source of the sulp ...
File
File

... 27. What are the 2 types of crust, and where are they located? 28. Draw and label the layers of the Earth 29. Which core layer(s) are liquid, and which are solid and why? 30. Why is the mantle important to us and scientists? (what is it responsible for) ...
planetearthnotes - hrsbstaff.ednet.ns.ca
planetearthnotes - hrsbstaff.ednet.ns.ca

... ROTATION THROUGH THE CELL? 500,000,000years 16A) WHAT IS A “HOTSPOT”? – a plume of molten magma originating within the mantle – it is not associated with or generated by plate movements – hotspots create volcanoes and islands when magma spills onto the surface of the lithosphere – there are 120 on e ...
Desk Copy Changing Earth Common Assessment
Desk Copy Changing Earth Common Assessment

... b. The way the grains fit together c. shape of the rock’s clasts d. All of the above 20. When metamorphic rocks have foliation it means… a. They have been formed under extreme heat b. They have formed from igneous rock c. They have parallel bands of light and dark minerals d. They have a mixture of ...
Geology 101, Fall 2006  continental drift vs. plate tectonics
Geology 101, Fall 2006 continental drift vs. plate tectonics

... active contintental margin vs. passive continental margin ...
Splitting continents - Workspace
Splitting continents - Workspace

KEY -
KEY -

Sedimentary Igneous Metamorphic
Sedimentary Igneous Metamorphic

... ...
Chapter 5 Atoms to Minerals
Chapter 5 Atoms to Minerals

... At Divergent Boundaries Where plates move away from each other, pressure is lowered. This allows for magma to form, raise and create new crust. ...
Earth Science Honors
Earth Science Honors

... Some of the most convincing evidence confirming seafloor spreading Evidence from drilling directly into ocean-floor sediment  Age of deepest sediments - furthest away from boundary ...
sample 7 - msaldrichscience
sample 7 - msaldrichscience

... zones it happens at depths that are very shallow or near the trench. Hot spots originate the boundary between the mantle and the outer core, they are narrow plumes of unusually hot mantle material. Continental accretion is the growth of a continent along it’s edges. Continents grow as the igneous ro ...
Study Guide
Study Guide

BUGS Rocks Station 1 Plate Tectonics and the Rock Cycle
BUGS Rocks Station 1 Plate Tectonics and the Rock Cycle

... plates bump into each other (subduction, collision, seafloor spreading, and transform fault have the students do the hand motions as you define these terms). Explain how these plates bump into each other helps the earth to move the rock around. The earth is a great rock recycler. Using the rock cycl ...
10.1 Volcanoes and Plate Tectonics Lecture Outline Origin of
10.1 Volcanoes and Plate Tectonics Lecture Outline Origin of

Ch. 7 Plate Tectonics Section 1 Inside the Earth
Ch. 7 Plate Tectonics Section 1 Inside the Earth

... Wegner’s theory of continental drift explained many puzzling facts, including the fit of the Atlantic coastlines of South America and Africa. Today’s continents were originally joined together in the ancient continent Pangaea. ...
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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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