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Changing Earth*s Surface
Changing Earth*s Surface

... sun and heat. Plants – roots Animals ...
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Earth - World Book Encyclopedia

... The Neptunists thought the entire earth had been covered by oceans at one time and had since evaporated, leaving dry land in some places.  In 2005, scientists of the American Geophysical Union reported that the earth’s north magnetic pole had been moving rapidly towards Siberia. Scientists believe ...
Earth Systems,Structures and Processes-Science Exam
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... The Earth is composed of five structural layers. The lithosphere is the layer that you live on, and it is the most widely studied and understood. The asthenosphere is much hotter and has the ability to flow, like oobleck. The mesosphere is even hotter than the asthenosphere! Finally, the inner and o ...
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Ch. 9 Study Sheet - Allen County Schools
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INTERIOR STRUCTURE OF THE EARTH

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Chapter 3 – The Dynamic Earth Section 1: The Geosphere

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... Convection: Transfer of heat within a liquid or gas. Conduction: Transfer of heat through matter by direct contact. Thermal Radiation: The energy radiated by solids, liquids, and gases in the form of electromagnetic waves as a result of their temperature. Deformation: Alteration of shape, as by pres ...
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7.1 Inside the Earth

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A Brief History of the Earth

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Eighth Grade ScienceEarth`s HistoryStudy Guide

... 6. What is subduction? When one plate goes under another plate and it is melted back into the mantle. 7. The Earth’s plates are made of what layer(s)? inner core, outer core, mantle (asthenosphere—upper mantle), crust (lithosphere) 8. Explain convection currents. Fluids when heated become less dense ...
earth space science review problem sheet
earth space science review problem sheet

... a. subduction zone b. divergent boundary c. convergent boundary d. transform boundary ___ 9. One major agent of erosion that has shaped Earth’s land surface is a. mass movement. b. moving water. c. chemical weathering. d. deposition ___ 10. Fossils of tropical plants found on an island in the Arctic ...
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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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