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EARTH`S INTERIOR
EARTH`S INTERIOR

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Magnetism Leaflet

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Magnetism Notes

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PowerPoint Presentation - The Interior of the Earth

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Earth`s Structure notes 5/26/15 • Crust

... • Mantle- 80 % 0f the volume of the earth. – Upper mantle is rigid, below is the asthenosphere which is a plastic like layer on which the tectonic plates float. – There is a huge difference in temperature between the outer mantle and the inner mantle. – This difference in temperature sets up a conve ...
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Take Home 12 Complete the following on your own paper. Do not

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F1 Notes.cwk

... Electrictiy and Magnetism Chapter F1 Notes Charge - measure of the extra charges that are on an object Series circuit - has only one path for the current to follow Parallel circuit - more than one path for current to follow Magnet -attracts objects made of iron or steel Magnetic pole - where a magne ...
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Magnetotellurics



Magnetotellurics (MT) is an electromagnetic geophysical method for inferring the earth's subsurface electrical conductivity from measurements of natural geomagnetic and geoelectric field variation at the Earth's surface. Investigation depth ranges from 300m below ground by recording higher frequencies down to 10,000m or deeper with long-period soundings. Developed in the USSR and France during the 1950s, MT is now an international academic discipline and is used in exploration surveys around the world. Commercial uses include hydrocarbon (oil and gas) exploration, geothermal exploration, mining exploration, as well as hydrocarbon and groundwater monitoring. Research applications include experimentation to further develop the MT technique, long-period deep crustal exploration, and earthquake precursor prediction research.
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