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Mini Lesson
Mini Lesson

Reasons for the Seasons Notes
Reasons for the Seasons Notes

... to revolve around Earth one time Year – the amount of time it takes for the Earth to revolve around the Sun one time ...
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... File for the TURTLE/Earth Science of the 5 pointed star* *Activities/Ideas like Stars-Ancestors-Descendants in the Tree/MilkyWay/River of Sky & Earth ...
200 300 400 500 100 200 300 400 500 100 200 300 400 500 100
200 300 400 500 100 200 300 400 500 100 200 300 400 500 100

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... Lava: Molten rock that flows from a volcano onto the earth’s surface. Sand Dune: A hill of sand made and shaped by the wind. Topography: Surface landforms of an area. Erosion: The process of moving sediment by wind, moving water, or ice. Delta: An area of new land at the mouth of a river formed from ...
Formation of the Crust and Continents
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... Radioactive decay produces heat as a by-product ...
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... Major geological events, such as earthquakes, volcanic eruptions, and mountain building, result from the motion of plates. Sea floor spreading, revealed in mapping of the Mid-Atlantic Ridge, and subduction zones are evidence for the theory of plate tectonics. ...
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... Mass movement – downhill movement of rock and soil because of gravity Lesson 2 Crust – other layer of Earth, made of rock Mantle – layer of rock beneath Earth’s crust Core – center layer of Earth Plates – rigid blocks of crust and upper mantle rock Magma – molten rock from Earth’s mantle Volcano – m ...
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... 1. The sun (1.98892 x 1030 kg) is the most massive object in our solar system and exerts a huge gravitational force. This is why all the planets stay in orbit around the sun. 2. The Earth (5.9742 x 1024 kg) is so massive that its gravitational force keeps us from falling off the planet. ...
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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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