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Geodynamic basis of heat transport in the Earth
Geodynamic basis of heat transport in the Earth

Chapter 15 - Spring Branch ISD
Chapter 15 - Spring Branch ISD

... The Composition of the Earth, continued • The Mantle the layer of the Earth between the crust and the core. •much thicker than the crust (2,900 km) •67% of the mass •more magnesium, less aluminum and silicon than crust •more dense than crust • The crust is too thick to drill through, so scientists m ...
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... m = 1 mode in a cylindrical geometry with a uniform plasma pressure (Naitou et al., 1995, 1996). They showed that the magnetic reconnection is triggered by the electron inertia in a much faster time scale than that caused by the resistivity, and the magnetic configuration with qmin < 1 can be recons ...
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... These activities cause displacements and deformations of the Earth’s surface, landslides and subsidence, mud-rock flow, and other phenomena. In the past, plate motion was inferred from marine magnetic anomalies located on both sides of the mid-ocean ridges and from the azimuth of transform-faults (at ...
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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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