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Profile Documents Logout
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06SC_TEST7 - Secondary Science Wiki
06SC_TEST7 - Secondary Science Wiki

... continental crust. B. The oceanic crust will push the continental crust so that a separation occurs between the two crusts. C. Uplift of the continental crust will occur as the result of pressure applied by the oceanic crust. D. As the two crusts slide past each other, the routes of rivers and strea ...
6th Grade Science Formative Assessment 5 Multiple Choice
6th Grade Science Formative Assessment 5 Multiple Choice

... continental crust. B. The oceanic crust will push the continental crust so that a separation occurs between the two crusts. C. Uplift of the continental crust will occur as the result of pressure applied by the oceanic crust. D. As the two crusts slide past each other, the routes of rivers and strea ...
Plate Tectonics - East Hanover Township School District
Plate Tectonics - East Hanover Township School District

... outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle. ...
Earthquake Test Study Guide
Earthquake Test Study Guide

... 5) Name the three types of earthquake waves. 6) Which seismic wave has a push-pull movement? 7) Which seismic wave has a wriggling side to side motion? 8) Which seismic wave causes the most damage during an earthquake? 9) Which seismic wave does not travel through liquids? 10) Which seismic wave tra ...
© NCERT not to be republished
© NCERT not to be republished

... Consider the set up shown in Fig. E 8.1. Here a roller of mass M1 has been placed on an inclined plane making an angle θ with the horizontal. An upward force, along the inclined plane, could be applied on the mass M1 by adjusting the weights on the pan suspended with a string while its other end is ...
(b) examine the chemical, physical, and thermal structure of Earth`s
(b) examine the chemical, physical, and thermal structure of Earth`s

Words of the Day
Words of the Day

... 14). Density: The amount of matter an object contains compared to the space it takes up. ...
The Sea Floor - Mrs. Gallegos Website
The Sea Floor - Mrs. Gallegos Website

chapter 12
chapter 12

Layers of the Earth - Endeavor Charter School
Layers of the Earth - Endeavor Charter School

Layers of Earth Notes
Layers of Earth Notes

Chapter Pages... 4 ..... 21 landform patterns and processes
Chapter Pages... 4 ..... 21 landform patterns and processes

GRAVITY AND MAGNETIC METHODS
GRAVITY AND MAGNETIC METHODS

... igneous and metamorphic rocks generally have a higher magnetic susceptibility than sedimentary rocks. An igneous intrusion or pluton is detectable in a magnetic survey due to the contrast in magnetic susceptibility with the surrounding rock. Where the rocks have high magnetic susceptibility, the loc ...
Introduction to Earthquakes EASA
Introduction to Earthquakes EASA

... in general metals are good conductors and rocks are poor conductors of heat. ...
3 Explanation - Earth`s Layers
3 Explanation - Earth`s Layers

chapter1
chapter1

Midterm I Physics 231
Midterm I Physics 231

force
force

... a. Gravity attracts objects toward each other. b. The more mass an object has, the greater its force of gravity is. c. The force of gravity is stronger when two objects are farther apart. 5. Is the following sentence true or false? Gravity is a force that pushes all objects away from each other. ...
Flash Cards - tclauset.org
Flash Cards - tclauset.org

Physiography of the Seafloor
Physiography of the Seafloor

Abstract - Institute for Nuclear Theory
Abstract - Institute for Nuclear Theory

... surface of the metallic pendulum. These eddy currents are, in turn, interact with the magnetic field; this provides the desired torque. A drawback of the current design is that it can only provide rotation in one direction, but there is a plan for alterations that would change the torque to be a re ...
Earth`s Crust in Motion
Earth`s Crust in Motion

... 36. State Alfred Wegener’s hypothesis about how Earth’s continents have moved. Wegener’s hypothesis was that all the continents had once been joined together in a single landmass and have since drifted apart, to their current locations. 37. Wegener named his supercontinent Pangaea. ...
A density model of the Andean subduction zone
A density model of the Andean subduction zone

... The upper crust is shaped like a lens, thickening up to 20-25 km beneath the Cordillera mountain belt and thinning at the edges near the coast and the Subandean thrust. The marine sediments which have been affected by tectonic deformation are seen in the Eastern Cordillera and Subandean ranges with ...
Name:__________________ Date: Pre
Name:__________________ Date: Pre

... 14. The diagram below shows four positions of the Earth in its orbit around the Sun. The diagram indicates relative positions of the Earth to the Sun, but the diagram has not been drawn to scale In which position would New York State receive the maximum insolation? (1) D (2) C (3) A (4) B ...
Reminders: * 1st HW due Sep 16 * 1st Midterm moved to Oct 4
Reminders: * 1st HW due Sep 16 * 1st Midterm moved to Oct 4

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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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