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Earth Dynamics
Earth Dynamics

PHY2100 Physics Practical II
PHY2100 Physics Practical II

... To do this, a search coil is used. It can be shown that the maximum deflection of a heavily-damped (ballistic) galvanometer is proportional to the change of flux through the search coil. Thus, to measure the magnetic field, all that is required is to set the galvo to zero with the search coil far fr ...
Earth`s Layers
Earth`s Layers

... currents. • Convection currents are caused by the very hot material at the deepest part of the mantle rising, then cooling and sinking again • The cycle repeats over and over. • The molten rock below Earth’s surface is known as magma ...
Unit 5_Lesson 109_Review
Unit 5_Lesson 109_Review

... Impacts from asteroids, comets, and meteors are an important part of Earth’s history. They are responsible for the creation of the Moon, the delivery of water to Earth, and the extinction of the dinosaurs. An impact from any of these objects creates a crater. Comets are balls of ice and rock (dirty ...
Chapter 2 Whole Notes
Chapter 2 Whole Notes

... turns into kinetic energy. Second law of thermodynamics The second law of thermodynamics states that when energy transfer occurs, matter becomes less organized with time. Thus, the universe’s energy is spread out more uniformly over time. As the disorder in the universe increases, the energy is tran ...
Compilation of activites
Compilation of activites

... Explain that students will choose 1 planet and write a 2 page report on it their specific plant. Next the teacher will divide the class into 2 or more groups and explain the rules for an in class jeopardy game. Management Concerns: When working with younger children it is better to have a variety of ...
Plate Tectonics
Plate Tectonics

3.1 Notes
3.1 Notes

Volcanoes and Igneous Activity Earth
Volcanoes and Igneous Activity Earth

Circular Motion Lab
Circular Motion Lab

Earth Layers Foldable
Earth Layers Foldable

... Extra points awarded for additional and correct information ...
Geography - English Language Support Programme
Geography - English Language Support Programme

... Bring the relevant subject textbooks to learning/language support class. It does not matter if they have different textbooks as the activities in these units refer to vocabulary and other items that will be found in all subject textbooks. These units are based on curriculum materials. Take some resp ...
Grade Seven Outline - Toms River Regional Schools
Grade Seven Outline - Toms River Regional Schools

... Unbalanced forces acting on an object result in a net force and cause a change in the object’s motion. (MS-PS2-2) Balanced forces acting on an object do not change the object’s motion. (MS-PS2-2) Two factors affect the gravitational attraction between objects: mass and distance. (MSPS2-4) An object ...
Chapter 3: Earth Structure and Plate Tectonics
Chapter 3: Earth Structure and Plate Tectonics

... until it has displaced a volume of asthenosphere equal to the mass of the mountain’s mass. Very slow process – if it goes too fast for some reason then the rock will crack (fracture) and a fault occurs, and cause earthquakes ...
Earth Egg Model
Earth Egg Model

... 1. The crust is a very thin solid outer layer of the Earth. Continental crust lies above denser oceanic crust. Continental crust can be 25-90km thick and consists of silica and aluminium rich rocks such as granite and sediment. Underlying oceanic crust is darker and denser because it contains rocks ...
5.1-.5
5.1-.5

Outer Core Facts - New York Science Teacher
Outer Core Facts - New York Science Teacher

handbook - Tinybop
handbook - Tinybop

... Why do you think scientists call Earth a ”living planet”? ...
Short course program: Earth and planetary materials and dynamics
Short course program: Earth and planetary materials and dynamics

Chapter 20
Chapter 20

... As high-energy particles leak into the lower magnetosphere, they excite molecules near the Earth’s magnetic poles, causing the aurora ...
The Milky Way - Department of Physics
The Milky Way - Department of Physics

Standard 1a
Standard 1a

Chapter 8 Study Guide
Chapter 8 Study Guide

II. Millikan Oil Drop Experiment
II. Millikan Oil Drop Experiment

... sphere by an external electric field Eext is then: Fe = (σ4πR2 ) · Eext = 0 Eb Eext · 4πR2 ...
The Dynamic Earth
The Dynamic Earth

... atmosphere. The amount of sunlight that reached the Earth’s surface was estimated to have decreased by 2 to 4 percent. As a result, the average global temperature dropped by several tenths of a degree Celsius over a period of several years. Copyright© by Holt, Rinehart and Winston. All rights reserv ...
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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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