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C:\Users\jmhemzac\Desktop\2017 spring\121 final rev S17f.wpd
C:\Users\jmhemzac\Desktop\2017 spring\121 final rev S17f.wpd

... general topographic characteristics of an area, such as determining high vs. low areas. e.g., Recognize how drainage patterns of streams are related to differences in topography: radial (Mt. Rainier) vs. dendritic (“tree-like”) vs. right-angle tributaries (Grand Canyon); What are some ways to tell, ...
Magnetic Field of Earth
Magnetic Field of Earth

... The phenomenon of magnetic properties of the matter was known around the VIII. century. In 1750 John Michell used a torsion balance to show that magnetic poles exert attractive or repulsive forces on each other and that these forces vary the inverse square of their separation. Although the force bet ...
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Powerpoint Presentation Physical Geology, 10/e

... Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. ...
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Hall of Planet Earth Educator`s Guide

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File - Ms. D. Science CGPA

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Chapter 19 Option H: RELATIVITY

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Surfaces and features of the Earth 4th.notebook

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5th grade plate tectonics and mountain building

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... would show three distinct layers: the crust, mantle, and core. 2 The first layer is called the crust. This is the surface we live on. The continents and the ocean basins make up the crust. It is Earth's thinnest layer. It is 35-70 km thick under the continents. The crust is only 5-10 km thick under ...
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... – Underwater mountain chain that runs through the Earth’s oceans. • Sea-floor spreading – Process in which new lithosphere forms • Magma rises to the surface through the mid-ocean ridge forming new oceanic crust • Tectonic plates spread apart and magma fills the gap. • As new crust forms older crust ...
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Volcanoes and Igneous Activity Earth - Chapter 4

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Millikan - SharedCurriculum

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Lesson 2 | Shaping Earth`s Surface

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... Turn down all the voltages to their minimum, then turn on the power supplies. Let the heater voltage (marked “amplitude” on the Pasco supply) warm up a few minutes and then apply about +150 V accelerating voltage (on the Heathkit supply). Adjust the heater voltage so that you obtain a fairly sharp b ...
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... Explain why the stars must be diametrically opposite to travel in the circular orbit. ……For circular motion there must be centripetal force ……This force is toward the centre of the circle – in this case the attraction due to gravity and so must be along the diameter of the circle making the planets ...
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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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