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Rocks and minerals
Rocks and minerals

... Physical properties of minerals include crystal structure, hardness (Mohs scale), (how it reflects light) and color, as well as more complicated properties such as streak, fracture, cleavage and density. ...
6 - Bal Bharati Public School
6 - Bal Bharati Public School

... Our lithosphere is broken into a number of plates called Lithospheric plates. The plates move because of molten magma inside the earth. Q7. What are minerals? How are they useful? Minerals are naturally occurring substances which have certain physical properties and definite chemical composition. So ...
GLOSSARY MINERAL – a naturally occurring inorganic element or
GLOSSARY MINERAL – a naturally occurring inorganic element or

... Batholith – a large pluton that has more than 100km2 of exposed surface and no known floor. Caldera – a large, basin-shaped depression formed by the inward collapse of a volcano after an eruption. Country Rock – pre-existing rocks into which plutonic rocks intrude. Desert Varnish – a thin, shiny blu ...
18.3 – Intrusive Activity
18.3 – Intrusive Activity

18.3 power point - Trimble County Schools
18.3 power point - Trimble County Schools

... • Intrusive igneous rock body, including batholiths, stocks,sills & dikes • Formed through mountain-building processes and oceanic-oceanic collisions • Can be exposed at Earth’s surface to uplift and erosion ...
Fulltext PDF
Fulltext PDF

... gradients between the Crust and the Core, like the convective flow of water when heated in a beaker (Figure 2). The energy for the above circulations is derived from the heat produced from the incessant decay of radioactive elements in the rocks throughout the Earth's interior. These convection curr ...
Layers of the Earth
Layers of the Earth

...  Where the two plates meet, one is usually subducted  Subducted means to go beneath  The plate that is subducted is destroyed in the mantle  This is why convergent plate boundaries are called destructive plate margins ...
Imaging continental collision and subduction in the Pamir mountain
Imaging continental collision and subduction in the Pamir mountain

... Subduction of continental crust is the mode of shortening in continental collision that is the least well understood. It is known to occur, as testified e.g., by now exhumed ultra-high-pressure rocks, despite the fact that continental crust is generally too buoyant to submerge into the mantle. Conti ...
Driving Forces- Plate Movement Transcript
Driving Forces- Plate Movement Transcript

... ..Convection is heat transfer by the movement of heated liquid. This method is the heat transfer method this lesson will focus on. Slide 5: Plate Movement ..Scientists still do not entirely understand the process of how tectonic plates move. ..However, most scientists agree that convection currents ...
Continental Drift and Seafloor Spreading
Continental Drift and Seafloor Spreading

... 3. Glossopteris- plant fossils found on different continents- Plant fossils 4. Tropical plant fossils that were found on an island in Artic Ocean! (Scratches in rocks made by glaciers in South Africa) The continental drift theory was NOT accepted because Wegener could not explain HOW the continents ...
Earth`s Systems and Resources Unit Test
Earth`s Systems and Resources Unit Test

... C. the outer core B. the inner core D. the crust 14. Due to extreme pressure, the inner core of Earth is A. solid. C. gas. B. liquid. D. plasma. 15. Which section of Earth is composed primarily of liquid metal? A. crust C. outer core B. mantle D. inner core 16. Which of these correctly lists Earth’s ...
plates - edl.io
plates - edl.io

... centimeters per year (≈ rate of fingernail growth). ...
Multiple Choice 3. ______ is a major dissolved volatile constituent in
Multiple Choice 3. ______ is a major dissolved volatile constituent in

... a. are generally fine-grained b. form at Earth’s surface c. are quite often vesicular d. none of the above 5. Granite and gabbro __________. a. have a similar mineral composition b. have a similar texture c. both a and b d. are in no way similar 6. Obsidian exhibits a(n) __________ texture. a. fine- ...
EARTH SCIENCE SOL REVIEW
EARTH SCIENCE SOL REVIEW

... Ocean crust is younger than continental crust. Youngest area of ocean floor is at midocean ridges Ocean crust is thinner than continental crust ...
Powerpoint Presentation Physical Geology, 10th ed.
Powerpoint Presentation Physical Geology, 10th ed.

... – Crust (~3-70 km thick) • Very thin outer rocky shell of Earth – Continental crust - thicker and less dense – Oceanic crust - thinner and more dense ...
10.3 Plate Tectonics and Igneous Activity
10.3 Plate Tectonics and Igneous Activity

... and volcanism is that plate motions provide the mechanisms by which mantle rocks melt to generate magma. At convergent plate boundaries, slabs of oceanic crust are pushed down into the mantle. As a slab sinks deeper into the mantle, the increase in temperature and pressure drives water from the ocea ...
Igneous Rock
Igneous Rock

... Igneous rocks are born in fire. There are two types of igneous rocks. The first type and most common are the intrusive igneous rocks. These rocks form when a pocket of magma (still underground) slowly cools down enough to form into solid rock. Great globs of molten rock rise toward the surface. Some ...
Volcanic Processes and Igneous Rocks
Volcanic Processes and Igneous Rocks

... Granite or diorite ...
Study Guide – Earth`s Changing Crust
Study Guide – Earth`s Changing Crust

... Physical or mechanical weathering: is the wearing away of rocks through wind, rain, ice or biological things (plants, animals, people) 18) What is erosion? Sediments or soil moving from one place to another through wind, water, or ice. 19) What are some causes of erosion? Wind, water, ice 20) What ...
CH 5 section 1
CH 5 section 1

... ______, twigs, litter, and small ______. Small particles of soil/rock are also found=sediment=sedimentary rock over time. 1. What would the Earth’s surface be like today if erosion were the only force acting upon it? What is erosion? 2. What are the four layers that the Earth is composed of? (Explai ...
Plate Tectonics
Plate Tectonics

... Six months later, on May 12, 1931, Wegener's body was found halfway between Eismitte and West camp. It had been buried (by Villumsen) with great care and a pair of skis marked the grave site. Wegener had been fifty years of age and a heavy smoker and it was believed that he had died of heart failure ...
lecture notes
lecture notes

... Subduction is the process at a trench whereby one part of the sea floor plunges below another and down into the asthenosphere  As the rocks scrape past each other, they generate earthquakes  In the asthenosphere the sea fl.oor melts and the molten material rises, melting through the overlying plat ...
Plate Tectonics Short Study Guide
Plate Tectonics Short Study Guide

... Scientists have studied the motions of Earth’s tectonic plates and recorded many of their findings as maps. Based on the assumption that the direction and rate of plate movement taking place today will continue for the next 50 million years, researchers have made predictions about the world’s future ...
earth-_ch_6_tectonic_plates_study_guide
earth-_ch_6_tectonic_plates_study_guide

Inside the Earth
Inside the Earth

... • With each eruption, gases, water vapor, ash and lava (molten material) were brought to the surface. • The water vapor and gases formed the atmosphere. • As the Earth cooled the water vapor turned to water and the rains started. • The oceans formed from runoff. This also supplied the ocean with the ...
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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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