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Plate Tectonics Notes
Plate Tectonics Notes

How the Earth was Made
How the Earth was Made

... 1. Who was a Scottish farmer and known as the father of modern geology? ...
The formation of mountains 1) Fold mountains Complete
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Earth-Science-Test-Week-9
Earth-Science-Test-Week-9

... Scientists know about the center of the Earth because they have made a tunnel to the center. ...
Chapter 13 Earth`s Interior and Tectonics
Chapter 13 Earth`s Interior and Tectonics

... Bedrock: solid rock that underlies the surface material of the Earth. Regolith: the layer above the bedrock, usually composed of weathered down bedrock. Outcrop: exposure of rock at the Earth’s surface. Mineral Classification What does it take to be a mineral? ...
Earth as a System
Earth as a System

... Consists of the __________________ and Upper ________________________. The upper part of the mantle is _______________ and _________________________ The lithosphere is very narrow and is __________and ____________. It ______________ on the asthenosphere. It is less ______________________. ...
MYSTERIES OF PLANET EARTH
MYSTERIES OF PLANET EARTH

... Force of attraction that an object (A) exerts on another object (B), i.e. Force of gravity is proportional to mass of A x mass of B distance 2  Gravimeter- measures variation in Earth’s gravity.  Gravity depends on the altitude of the land, latitude, and distance ...
Spheres of the Earth
Spheres of the Earth

... • The hydrosphere includes all water on Earth. • 71% of the Earth is covered by water and only 29% is land. • Earth called “Blue Planet” • Water to exist in all three states: solid (ice), liquid (water), and gas (water vapor). • Water is the universal solvent and the basis of all life on our Planet. ...
Professor Bruce Watson
Professor Bruce Watson

... The first 700 million years of Earth’s existence (the Hadean Eon) are widely regarded as the most geodynamically vigorous period in the history of our planet. It has been variously inferred that during this time the Earth: 1) collided with a Mars-sized-object; 2) formed a deep magma ocean; 3) grew t ...
the junior version pdf file
the junior version pdf file

Place on the Earth where seismic waves are first felt
Place on the Earth where seismic waves are first felt

... circulatory movement in a liquid or gas, resulting from regions of different temperatures and different densities rising and falling in response to gravity ...
TERM 1 Final Exam – Study Guide
TERM 1 Final Exam – Study Guide

section 1 - image identification
section 1 - image identification

...  Is the Chesapeake Bay only 10,000-15,000 years old or is it a much older feature?  The Chesapeake Bay was carved out by the ________ River and its tributaries.  The muddy appearance of rivers and streams – which provides their “color” – is evidence that a form of sediment transport known as ____ ...
Chapter 26: Earth`s Interior
Chapter 26: Earth`s Interior

Week 30 CCA - Net Start Class
Week 30 CCA - Net Start Class

... Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune 12. What 2 forces work together to keep the planets in orbit around the sun? Gravity and Inertia 13. Where is the asteroid belt located? Between Mars and Jupiter 14. Explain how a planet could be “eaten” by a star? The force of gravity of ...
7-1 Inside the Earth RG
7-1 Inside the Earth RG

... 5. Oceanic crust is denser than the continental crust because it contains more of which three elements? ...
Oceanography Notes - Intro (Day 1-3)
Oceanography Notes - Intro (Day 1-3)

... 5. No ____________________  Earth’s surface was too hot, Earth’s rotation & orbit was still too unstable, Moon that was much closer caused huge changes in Earth’s surface D. 4.5 - 4 BYA  Earth Began to cool w/ little to no atmosphere 1. Intense ____________________ /____________________ Bombardmen ...
Section 8-4
Section 8-4

Earth Science Chap 1.2
Earth Science Chap 1.2

... glaciers, as well as that found underground. ...
Inside Earth Worksheet
Inside Earth Worksheet

The Geosphere
The Geosphere

... Scientists use special terms to describe the different parts of the Earth • Geosphere – consists of all the rock, soils and sediments on the Earth • Atmosphere – consists of the air that surrounds the Earth • Hydrosphere – consists of all water, fresh or ...
The Geosphere
The Geosphere

1.3, 1.4
1.3, 1.4

Variation of g (acceleration due to gravity) - cal
Variation of g (acceleration due to gravity) - cal

... be attributed to several factors:First, Earth is not homogeneous. Second, the Earth is not a perfect sphere. Third, the choice of a value for the radius of the Earth.( This calculated value of g does not include the centrifugal force effects that are found in practice due to the rotation of the Eart ...
Review Worksheet
Review Worksheet

... 1. ______ This variable doesn’t change 2. ______ The steps you follow to do an experiment. 3. ______ A prediction of the results 4. ______ This variable is what you measure 5. ______ The question you try to answer using an experiment ...
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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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