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Full-Wave Simulation of High-Frequency Electromagnetic

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... Talkeetna, the two best-exposed oceanic arc sections (see Methods for geological setting). Previous studies have suggested that the Talkeetna arc crust is generally less dense than the underlying upper mantle peridotites (‘density stable’)13,14, whereas in Kohistan lower-crustal rocks denser than th ...
Classical Mechanics
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... Does your solution give the correct result for t → ∞? What is the physical meaning of this asymptotic value? Would you expect the time during which the ball rises to be longer or shorter than the time during which it falls back to the ground? Problem 6. 1983-Spring-CM-U-3. ID:CM-U-42 Two metal balls ...
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... and is similar to the 8.11 km.s-1 measured on a north/ south line in the southwest Yilgarn Craton, where the east!west Pn velocity is 8.39 km.s-1 (Mathur, 1974). This gives a somewhat tenuous average for the upper mantle velocity under the Yilgarn Craton of 8.25 kms!, which is greater than under the ...
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Rheology of the mantle

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Schiehallion experiment



The Schiehallion experiment was an 18th-century experiment to determine the mean density of the Earth. Funded by a grant from the Royal Society, it was conducted in the summer of 1774 around the Scottish mountain of Schiehallion, Perthshire. The experiment involved measuring the tiny deflection of a pendulum due to the gravitational attraction of a nearby mountain. Schiehallion was considered the ideal location after a search for candidate mountains, thanks to its isolation and almost symmetrical shape. One of the triggers for the experiment were anomalies noted during the survey of the Mason–Dixon Line.The experiment had previously been considered, but rejected, by Isaac Newton as a practical demonstration of his theory of gravitation. However, a team of scientists, notably Nevil Maskelyne, the Astronomer Royal, were convinced that the effect would be detectable and undertook to conduct the experiment. The deflection angle depended on the relative densities and volumes of the Earth and the mountain: if the density and volume of Schiehallion could be ascertained, then so could the density of the Earth. Once this was known, then this would in turn yield approximate values for those of the other planets, their moons, and the Sun, previously known only in terms of their relative ratios. As an additional benefit, the concept of contour lines, devised to simplify the process of surveying the mountain, later became a standard technique in cartography.
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