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Layers of the Earth - Atlanta Public Schools
Layers of the Earth - Atlanta Public Schools

... crust and core. • The mantle is the layer under the crust. • It is up to 2,897 kilometers(1,800 miles -from here to Arizona) thick. • The mantle is made up of rocks such as silicon, aluminum, iron, and magnesium. • Top layer - hot solid rock 1590 degrees Fahrenheit • Bottom layer - hot liquid rock 3 ...
Layers of the Earth Power Point
Layers of the Earth Power Point

Answer Key
Answer Key

... By definition, a mineral is any substance that forms from an inorganic source. Coal is the product of decayed vegetative plant life which is considered to be organic in origin. For this reason coal is not a mineral, but is classified as an organic sedimentary rock. ...
Geosphere - Written - Geological Society of India
Geosphere - Written - Geological Society of India

... d) The ring of fire around the Pacific Ocean reduces the rate of reversals of the Earth’s magnetic field. ...
Our Changing Earth
Our Changing Earth

... Sand dunes are large hills of sand often found in the desert. These huge features are made by wind erosion. The size and shape of dunes depend on the amount of sand, the number of plants in the area, and the strength of the winds. Winds can also blow sand dunes across the desert. The wind picks up s ...
Volcanoes
Volcanoes

... the lava piles up near the volcanic vent. The eruption of Mount St. Helens in 1980 was caused in part by a lava dome shifting to allow explosive gas and steam to escape from inside the mountain. ...
8-3 Unit HW Sheet Name: Date: Standard 8
8-3 Unit HW Sheet Name: Date: Standard 8

... 12. Which seismic wave is the fastest wave and which wave stops at the outer core-Explain why? P wave/ S wave stops at the outer core because it only travels through solids. 13. What is a fault? Crack in the Earth’s crust or rock 14. What is the process scientist use to locate the epicenter? Triangu ...
Earth Structure
Earth Structure

Chapter 29 - Physical Science 100
Chapter 29 - Physical Science 100

... Now that we have a basic understanding of chemistry and physics, as well as the earth’s internal structure and plate tectonics, we are ready to fully appreciate the significance of what the earth is made of. We intuitively appreciate that the earth is a rocky planet, but what are these things we cal ...
Volcanoes - Geography1000
Volcanoes - Geography1000

...  Sills– a long, thin intrusive body with its orientation determined by the structure of the preexisting rocks  Veins – least prominent- thin veins of igneous rock that are pushed up through small fractures of preexisting rocks  Batholiths -- a subterranean igneous body of indefinite depth and eno ...
CHAPTER 2 Plate Tectonics and the Sea Floor
CHAPTER 2 Plate Tectonics and the Sea Floor

... into fractures, is heated by hot rock or magma, and emerges as mineral-laden plumes of hot water. Tube worms and other unusual life forms utilize this energy source. See Box, p. 306-307 N. Lindsley-Griffin, 1999 ...
Q. What is the concept of plate tectonics theory?
Q. What is the concept of plate tectonics theory?

... Q. What is the concept of plate tectonics theory? - It is a scientific theory which describes the large scale motion of Earth’s lithosphere. The theory builds on the older concepts of continental drift developed by Alfred Wegner and seafloor spreading. Where the plates are relatively moving towards ...
Identifying Plate Tectonics Lab 1-34
Identifying Plate Tectonics Lab 1-34

... 33. Is the distance between the mainland of Mexico and Baja California getting larger, smaller, or staying the same? ...
Volcanoes: Fire Under the Surface
Volcanoes: Fire Under the Surface

... the tectonic plates shift, one volcano can become dormant while another volcano is formed. Whether volcanoes are creating new soil and beautiful islands like in Hawaii or causing damage to people’s homes, they are the earth’s way of reminding us that our planet is actually a hot, fiery ball of molte ...
Geomorphology
Geomorphology

... each other, one plate dips down into the magma (being distilled, in a Benioff zone), and the other plate overrides it. This is a destructive margin. Over it, volcanic island arcs will form. Japan is a volcanic island arc, as are the Philippines. Thermal convection produces slow moving currents in th ...
Document
Document

... melts should thus not be misinterpreted as indicating long melt residence times. In fact, we have seen above that mafic melts have the highest whole rock U-series disequilibria, and some make it to the surface quite rapidly (i.e. within hours to days in some cases!) • Many intermediate compositions ...
Ch. 9 Review - 8th Grade Science
Ch. 9 Review - 8th Grade Science

... • 4. Two plates collide with each other at: B – A convergent boundary • 5. A fault in which the hanging wall slides up and over the footwall is a: A – Reverse Fault ...
Effect of melt content and the melt texture on sound wave velocity
Effect of melt content and the melt texture on sound wave velocity

... have long been discussed in conjunctions with partial melting in the Earth’s asthenosphere. Alternative mechanisms based on solid state processes, such as anelastic relaxation and hydrogen diffusion in mantle minerals have also been proposed. However, the recent finding of young alkali basalt (< 10 ...
Continental Margins and Ocean Basins
Continental Margins and Ocean Basins

Intrusive and Extrusive Igneous Rocks
Intrusive and Extrusive Igneous Rocks

... The names “CK-12” and “CK12” and associated logos and the terms “FlexBook®” and “FlexBook Platform®” (collectively “CK-12 Marks”) are trademarks and service marks of CK-12 Foundation and are protected by federal, state, and international ...
The geology of Paka volcano, and its implication on geothermal
The geology of Paka volcano, and its implication on geothermal

... spar, augite and magnetite crystals as euhedral laths in a granular The most recent eruption produced basalt eruptions in the caldera, groundmass. The rock is vesicular, with the small rounded vesicles a flow from a cone low on the SW flanks, and basalt lava flows occasionally being in-filled with s ...
Plate Tectonics and volcanoes
Plate Tectonics and volcanoes

... • A zone of liquid rock inside of the earth? • If true, volcanoes would be scattered ...
Sample Lesson Plan - Desert Outdoor Center
Sample Lesson Plan - Desert Outdoor Center

... them have eroded away. Because these rocks cool very slowly they have observable crystals. • Extrusive rocks (also known as volcanic rocks) are formed when magma erupts from a volcano as lava, then cools at the surface. Because these rocks cool so quickly they have few or no observable crystals. • W ...
chapter 2 - Geophile.net
chapter 2 - Geophile.net

... * convergent (continent – ocean plate collision): Cascadia subduction zone (Pacific Ocean floor against North America) * convergent (continent- continent collision): Himalayas * divergent (rift or spreading, or extension): mid-oceanic ridge * transform (lateral motion): San Andreas Fault 15. Along w ...
chapter 2 - Geophile.net
chapter 2 - Geophile.net

... * convergent (continent – ocean plate collision): Cascadia subduction zone (Pacific Ocean floor against North America) * convergent (continent- continent collision): Himalayas * divergent (rift or spreading, or extension): mid-oceanic ridge * transform (lateral motion): San Andreas Fault 15. Along w ...
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Basalt



Basalt (pronounced /bəˈsɔːlt/, /ˈbæsɒlt/, /ˈbæsɔːlt/, or /ˈbeɪsɔːlt/)is a common extrusive igneous (volcanic) rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. Flood basalt describes the formation in a series of lava basalt flows.
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