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earth interior - Red Hook Central Schools
earth interior - Red Hook Central Schools

... crust of the Earth rip and break apart, releasing tremendous energy in the form of seismic waves. What’s it like to be in an Earthquake? “Its like trying to stand up in an airplane during severe turbulence” ...
General Geology
General Geology

... the rocks and minerals which compose it, the processes which are constantly changing it, the concepts of relative and absolute time, the risks associated with geologic hazards, and the role of geology in shaping man’s environment. The course presents the tools, methods and approach employed by pract ...
Name: Date: Period: ______ Chapter 13 Study Guide 1. What is soil
Name: Date: Period: ______ Chapter 13 Study Guide 1. What is soil

... 1. What is soil? What do you call the layers that we see as we dig? Soil is the loose, weathered material in which plants grow. It is divided into layers that we call horizons. 2. How do scientists determine the density and the makeup of Earth’s inner layers? By analyzing earthquake waves 3. Define ...
Environmental Science
Environmental Science

... • Scientists use seismic waves to learn about Earth’s interior. • Seismic waves are the same waves that travel through Earth’s interior during an earthquake. • A similar process would be you tapping on a melon to see if it is ripe. ...
Development of geological processes on the Earth and their impact
Development of geological processes on the Earth and their impact

Unit 2
Unit 2

Life in the Universe - University of Georgia
Life in the Universe - University of Georgia

... Overall density versus surface rock ...
File
File

Grade Level - Research 2
Grade Level - Research 2

... Explain the purpose of using data and observations to create models Recognize that the interactions between the layers impact both the earth and its organisms Know that movement of lithospheric plates causes volcanoes and earthquakes ...
MS PowerPoint document, click here
MS PowerPoint document, click here

...  Shows the changes in elevation of the Earth’s surface  Contour lines ►A line on a map that connects points of equal elevation  Contour interval ►The distance between contour lines ►The closer the lines the steeper the surface ...
Earth Interior quest
Earth Interior quest

... 16. If the temperature of material is hotter than the melting point what should happen to it? 17. What is the outer core made of? What is the inner core made of? 18. What are the ranges of temperatures for the outer and inner cores? 19. Look at the answer for #10, why does the melting point cross th ...
Study Island
Study Island

... 2. Which is closer to the Earth—the Sun or the outer planets? A. The Sun is closer to the Earth than the outer planets are. B. They are the same distance from the Earth. C. The outer planets are closer to the Earth than the Sun is. D. The distance from the Earth to the Sun cannot be determined. 3. S ...
Chapter 1 Notes for Earth Science
Chapter 1 Notes for Earth Science

... -Inner planets are smaller and made of rock. -Outer planets are bigger and made of gasses. Day and Night -Earth rotates, or spins, on its axis. -It takes 24 hours for the Earth to rotate one time. -The Earth’s rotation causes day and night. -When we face the sun, it is day. -When we are not facing t ...
The Changing Earth
The Changing Earth

Plate tectonics - pams
Plate tectonics - pams

... plant) located in rocks about 250 million years old in South Africa, Australia, India and Antarctica. Seeds were too large to have been carried by wind and too fragile to have survived a trip by ocean waves. ...
Section 1 - Pelham City Schools
Section 1 - Pelham City Schools

... 3. Explain the main cause of earthquakes & their effects 4. Identify the relationship between volcanic eruptions & climate change 5. Describe how wind & water alter the Earth’s surface ...
6th Grade Science - Wichita Falls ISD
6th Grade Science - Wichita Falls ISD

Plate Tectonics Unit Assessment Study Guide Answers
Plate Tectonics Unit Assessment Study Guide Answers

The Layer`s Of The Earth!
The Layer`s Of The Earth!

Chapter 11: The Dynamic Planet I. Pace of Change A
Chapter 11: The Dynamic Planet I. Pace of Change A

view as pdf - KITP Online
view as pdf - KITP Online

Newtons laws
Newtons laws

... Every body in the universe attracts every other body with a force that is directly proportional to the product of the masses of the bodies and inversely proportional to the square of the distance between the bodies. The law of gravitation is universal and very fundamental. It can be used to understa ...
PowerPoint - Science A 2 Z
PowerPoint - Science A 2 Z

... nami/main.html Danger -Getting knocked about by debris -Being pulled out to sea ...
The Earth
The Earth

... Because water can dissolve CO2, the Earth was saved from a “runaway greenhouse effect.” (Compare with Venus.) • O2-rich atmosphere (21% O2 by volume) • Magnetic field that protects the planet from solar wind • Life! Living organisms cover the Earth. There is no definite evidence yet for any other bi ...
Plan for Living on a Restless Planet Sets NASA`s Solid Earth Agenda
Plan for Living on a Restless Planet Sets NASA`s Solid Earth Agenda

... of the South Atlantic Ocean.This pattern is connected to the growth of the South Atlantic Magnetic Anomaly, an area in which the field at the Earth’s surface is now about 35% weaker than would be expected.This hole in the field has serious implications for low-Earth-orbit satellite operations since ...
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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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