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The Structure of the Earth*s Interior
The Structure of the Earth*s Interior

... • The Earth's Crust is like the skin of an apple. It is very thin in comparison to the other three layers. The crust is only about 3-5 miles (8 kilometers) thick under the oceans (oceanic crust) the distance of here to Cosmopolis, and about 2530 miles (32 kilometers) thick under the continents (cont ...
notes for geologofe - sciencepowerpoint.com
notes for geologofe - sciencepowerpoint.com

...  Fold – Collision of crust bends rock layers “stress” Normal Fault – Pulling apart tension causes crust to drop down. Reverse / Thrust Fault – Compression forces cause crust to move up. Lateral or Strike Slip Fault – Crust moves alongside each other in opposite directions. ...
Structure of the Earth Study Guide with Answers
Structure of the Earth Study Guide with Answers

... 22) List the order of seismic waves as they reach a site from fastest to slowest. P WAVE, S WAVE, SURFACE WAVES 23) How fast do body waves move through the Earth? 11 KM/SEC 24) What are the layers of the Earth from inside out? INNER CORE, OUTER CORE, MANTLE, CRUST 25) What layer of the Earth is the ...
Layers of the Earth
Layers of the Earth

... • It is cool on the surface but very _________ deep inside the planet. • The center, or core, is as hot as ____________________ which is ...
Plate Tectonics Notes
Plate Tectonics Notes

...  Scientists can match up the bands on either side of the mid-ocean ridge to prove that the seafloor is spreading.  Scientists have also found that the bands alternate between pointing north and pointing south. This indicates that the Earth’s magnetic poles have reversed many times. ...
Plate Tectonics
Plate Tectonics

...  Scientists can match up the bands on either side of the mid-ocean ridge to prove that the seafloor is spreading.  Scientists have also found that the bands alternate between pointing north and pointing south. This indicates that the Earth’s magnetic poles have reversed many times. ...
Geology Pre Test
Geology Pre Test

... 5. The theory that explains how the large blocks of the Earth’s outermost layer move and change shape is called (6.E.2.1): a. Plate Tectonics. b. Convergent Boundary. c. Pangaea. d. Lithosphere. 6. Tectonic plates are (6.E.2.1): a. the theory of how continents drift apart. b. blocks of lithosphere t ...
ES Unit 3 standards - Springfield Public Schools
ES Unit 3 standards - Springfield Public Schools

... eruptions that occur and describe the various types of materials that are ejected from volcanoes. Describe the major intrusive igneous features and the ...
The Layer`s Of The Earth!
The Layer`s Of The Earth!

... over 1km long. It is a line of lava escaping at a major fault line in Iceland. It will eventually make the cone shape of a volcano. ...
Ch. 7 - Department of Physics and Astronomy
Ch. 7 - Department of Physics and Astronomy

... tidal power like this to generate electricity ...
Earth`s Layers Online Activity http://homepage.mac.com/cohora/ext
Earth`s Layers Online Activity http://homepage.mac.com/cohora/ext

... 8. The Inner core is under so much pressure it does not move like a liquid, it Write the temperature of the center of the Earth. 9. A scientist who studies rocks is called a ____________________________________. What does a Geomorphologist study? ...
Plate Tectonics
Plate Tectonics

... Pacific Ocean Plate…high area of nd S-Waves arrive 2 & travel through earthquake/volcano activity solids only…inner core of Earth is solid Outer Core is Liquid Epicenter (911) happens on the surface of the earth ...
Captain Curiosity - Curiosity Zone of Ashburn VA
Captain Curiosity - Curiosity Zone of Ashburn VA

Practice Questions: Earth`s Interior
Practice Questions: Earth`s Interior

... range in the Atlantic Ocean. The oceanic bedrock is composed mainly of basalt. Points X and Y are locations in the bedrock that have been diverging at the same rate. The movement of the North American Plate and Eurasian Plate is shown by the two arrows. ...
Reinforcing Key Concepts
Reinforcing Key Concepts

... each layer is made of and how thick the layers are. In the diagram below, label each of Earth’s layers. In the space provided, explain what each layer is made of. ...
What Causes Earthquakes?
What Causes Earthquakes?

Inside the Earth Study Guide The format on tests and quizzes is a
Inside the Earth Study Guide The format on tests and quizzes is a

... 4. What do the particles in each look like? 5. What is the difference between a solid and a plastic solid? 6. What are the 5 physical layers and how are they different in their physical properties? 7. Even though it is the hottest in the center of the earth, why is the inner core solid, while the ou ...
Earth structure
Earth structure

... The crust is made of about twelve plates. These are like big rafts floating on the semi-molten mantle. Convection currents within the mantle cause the plates to move. Although they only move about 2 cm/year this can have huge effects over long periods of time. ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... supported theory of continental drift. Wegener’s hypothesis lacked a geological mechanism to explain how the continents could drift across the Earth’s surface. ...
Introduction to Atmospheric Science, PHSC 3223
Introduction to Atmospheric Science, PHSC 3223

... • The Rock Cycle gives rise to three main types of rocks, based on their origins or means of formation – Igneous rocks originate from cooling and crystallization of magma from inside the Earth: Extrusive or volcanic igneous rocks form when magma is forced to the surface; Intrusive or plutonic igneo ...
EDWARD J. GARNERO 2. Employer - AGU Elections
EDWARD J. GARNERO 2. Employer - AGU Elections

... My discipline of research is seismology, and my research focus is the interior of Earth and the Moon. I am interested in seismic imaging of structures that relate to the chemistry, dynamics, and evolution of interiors, especially as it relates to observables at Earth’s surfaces (hotspots, LIPs, subd ...
Plate Tectonics
Plate Tectonics

... It takes S waves 13 minutes to travel from an epicenter to a seismic station. How long will it take P waves to reach the same station? ...
The Layer`s Of The Earth!
The Layer`s Of The Earth!

... 4. Is the Outer Core a liquid or a solid? 5. The Earth Bowl graham cracker or Rice Krispies layer represents the Earth’s ________, which is 20 ______ deep. 6. Although the Earth Bowl is made of cool gelatin, the center of the earth is actually extremely ...
Pangea Location of different fossils, location of different types of
Pangea Location of different fossils, location of different types of

... These sound waves show features on the ocean floor. The mid­ocean ridge and trenches The plates moving apart along the mid­ocean ridge have different  ages of rocks.  The newest rocks are along the mid­ocean ridge  where lava comes out.  The oldest rocks are next to the continents.   ...
plate tectonics - mfischerscience
plate tectonics - mfischerscience

... • This is because mountains and other rock formations split apart. • Ex. Similar rocks in the Appalachian Mountains in the U.S. and in Greenland & Europe. ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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