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Roundness and smoothness Lab
Roundness and smoothness Lab

... The ratio of the polar diameter to the equatorial diameter of a sphere is a measure of its roundness. We call this a roundness ratio. 1. Use the values given for the equatorial and polar diameters of the earth in the data chart on the report sheet to calculate the roundness-ratio of the earth. Recor ...
Physical Geography - Brogranoni-GEO1
Physical Geography - Brogranoni-GEO1

... reversed it's magnetic field, the north and south poles swapping over. It was also known that as volcanic rocks cool, all the minute particles of iron in them record the magnetic field around them, preserving the position of the north and south poles like a fossil. Scientists discovered that the roc ...
9 Geography Investigating Australia`s Physical Environments Term 1
9 Geography Investigating Australia`s Physical Environments Term 1

... down. This process forms both mountains and rift valleys. Rocks behave differently under pressure, depending on how brittle they are. Rocks close to the surface tend to be more brittle and will snap under pressure. Faults are formed when these rocks break. Evidence for Continental Drift and Plate Te ...
The Layer`s Of The Earth!
The Layer`s Of The Earth!

... 4) Now take the black cherry Jell-O and spoon it into the bowl that you have put the crust in. Form it so there is a pocket in the middle left open. 5) Take the lemon Jell-O and put it in the bowl where you left the pocket, but make sure you leave a hole in the middle for your raspberry Jell-O. 6) ...
Earth`s Interior Reading Packet 1
Earth`s Interior Reading Packet 1

Syllabus Danish International Geology 2014
Syllabus Danish International Geology 2014

... Minerals, the Rock Cycle, Plate Tectonics, and Mountain Building. We will also talk about the geology of Denmark. Before we get started, this website below is the one that your instrutors in Denmark expect you to study. The content here is the same as what you will study with me, but you may be more ...
The Layer's Of The Earth! - Waupun Area School District
The Layer's Of The Earth! - Waupun Area School District

plates
plates

... below Earth’s surface, scientists can study what the rocks are made of and make inferences about Earth’s interior. ...
Earth & Layers
Earth & Layers

... mixtures of elements. This means that the layers have different compositions. • Temperature, pressure, and density are the three things that increase as you go inside the Earth. ...
Plate Tectonics
Plate Tectonics

... crust – thin, outermost layer of the Earth divergent boundary – also called a spreading center; where two adjacent plates are moving away from each other earthquakes – vibrations caused by the sudden movement of Earth’s crust fault – a break or crack in Earth's crust along which movement has occurre ...
Science Study Guide - Thomas C. Cario Middle School
Science Study Guide - Thomas C. Cario Middle School

... The organisms that are better suited to the environment will survive and reproduce. 64.What defines the members of a species? Should be able to reproduce. 65.Marine fossils have been found in exposed rock layers in South Carolina. What would be a good interpretation of this discovery? South Carolina ...
Unit - MNPSSocialStudies
Unit - MNPSSocialStudies

... sources. Communication: demonstrate beliefs through multimedia projects; recognize beliefs through simulation and role play. Problem Solving and Analysis of Data: identify relevant factual material; critically examine data from a variety of sources; note cause/effect relationship and draw inferences ...
Sample High School Earth Science Unit Plan
Sample High School Earth Science Unit Plan

... o Some changes in the solid earth can be described as the "rock cycle." Old rocks at the earth's surface weather, forming sediments that are buried, then compacted, heated, and often recrystallized into new rock. Eventually, those new rocks may be brought to the surface by the forces that drive plat ...
Questions from the committee:
Questions from the committee:

... Era of OBSERVATORY Earth Science CZO: Critical Zone Observatories OOI: Ocean Observatory Initiative ...
Historical Geology
Historical Geology

... The Movie of Earth’s History • What kind of movie would we see – if it were possible to travel back in time – and film Earth’s History – from its beginning 4.6 billion years ago? ...
Exam review questions 2008 2
Exam review questions 2008 2

... With a characteristic streak-______________________________________ With a distinctive color-_________________________________________ 33. Why are diamonds used as gemstones? 34. Name the ore mined for aluminum. _____________________ Why is this mineral called an ore? 35. List Moh’s scale of hardnes ...
CRUSTAL EVOLUTION OF EARTH AND MARS E. Gazel1, H. Y.
CRUSTAL EVOLUTION OF EARTH AND MARS E. Gazel1, H. Y.

Practice Test – Geology 106, Chapter 17 from The Changing Earth
Practice Test – Geology 106, Chapter 17 from The Changing Earth

... _______________, by experimenting with the effects of high heat on lime, sand, and basalt; and _______________, by writing and publishing a book called _______________. 22. The two laws most used when determining the relative age of materials are the Law of _______________ and the Law of ___________ ...
pdf 4.5Mb
pdf 4.5Mb

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

... 1) What are the four layers of the Earth? 2) The Earth’s crust is very ______? 3) The mantle is the largest layer of the Earth? True or False 4) Is the Outer Core a liquid or a solid? ...
Review
Review

... 9.) Be able to explain/draw the Convection Cycle and how it causes plate movement. Also understand Seafloor Spreading and how it is evidence of Plate Tectonics. ...
Jeopardy
Jeopardy

... Geography Jeopardy Hosted by Mrs. Pulver ...
Paleozoic Plate Tectonics Quiz
Paleozoic Plate Tectonics Quiz

Journey to the Center of the Earth Project - Science
Journey to the Center of the Earth Project - Science

... Part 2 - Write a short story to go along with your model. The story is about a scientist (maybe you???) traveling to the center of the Earth. Begin at the crust and describe what you observe traveling through each layer. Although we don’t really have means to travel through the Earth, the descriptio ...
Veronica Flores – Laverty November 24, 2014 Layers of Earth There
Veronica Flores – Laverty November 24, 2014 Layers of Earth There

... names which are the crust, mantle, outer core, and inner core. Scientists use information gathered from seismographs after an earthquake to learn about Earths layers by studying the seismic waves. These waves travel differently through solids, liquids, and gases. The crust is Earth’s outermost layer ...
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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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