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Earth Science - Issaquah Connect
Earth Science - Issaquah Connect

... Plate Tectonics • Plate tectonics is the concept that the outer surface of the Earth is made of large plates of crust and outer mantle that are slowly moving over the surface of the liquid outer mantle. – Heat from the Earth causes the slow movement. – Plates are pulling apart in some areas, and co ...
Structure of Earth Student Notes
Structure of Earth Student Notes

... As you go deeper into the mantle, __________ and ____________________ increase. This makes the rock ________ rigid. It has the consistency of _________ and can bend much like plastic (_______________________). This plastic-like layer of the mantle is called the _____________________________. The lit ...
Layers of the Earth
Layers of the Earth

... • Thinnest layer of the Earth that ranges from only 2 miles in some areas of the ocean floor to 75 miles deep ...
Layers of the Earth ppt
Layers of the Earth ppt

... • Thinnest layer of the Earth that ranges from only 2 miles in some areas of the ocean floor to 75 miles deep ...
Name
Name

... Word Bank provided. Hypothesis for Divergent Boundary: ...
Unit 1 - Earth`s Dimensions Review Powerpoint
Unit 1 - Earth`s Dimensions Review Powerpoint

Physical Geography Geomorphology
Physical Geography Geomorphology

... dominant scientific beliefs in Europe founded on the biblical narratives of Creation and flood of Noah Anglican Archbishop James Ussher published a widely-accepted chronology in 1648 based on the Bible and historical texts ...
Geology_101_Homework_2
Geology_101_Homework_2

... Quiz on this material will be Thursday, March 13 Show me completed work for credit on or before Thursday, March 20 Write your answers on a separate piece of paper. Interlude C, pages 318-329 1) Explain the evidence for the theory that the outer core of Earth is liquid. 2) Explain the factors that af ...
L1: Continental Drift and Layers of the Earth Goals: to describe the
L1: Continental Drift and Layers of the Earth Goals: to describe the

... 1. a) How do scientists know what Earth’s inner layers look like when they can’t see them or use tools to probe that deep? ...
RESTLESS EARTH
RESTLESS EARTH

File
File

To demonstrate how Young Fold Mountains are
To demonstrate how Young Fold Mountains are

Supporting Content Web Sites
Supporting Content Web Sites

... rocks were formed and what has happened to them since their formation. They also study the evolution of life by analyzing plant and animal fossils. Volcanologists study the remains of either dead or dormant volcanoes, or monitor volcanoes that are dormant, but may become active or "reawaken.” A sign ...
Describe the composition and structure of Earth.
Describe the composition and structure of Earth.

Get out your pieces for Tectonicland Have your HOMEWORK out
Get out your pieces for Tectonicland Have your HOMEWORK out

... the continents once fit together? ii. What was one of Wegener’s forms of evidence for continental drift? iii. What were the two flaws of Wegener’s continental drift hypothesis? ...
Powerpoint - Physics and Astronomy
Powerpoint - Physics and Astronomy

... 1) "Fission": The material that would be the Moon was thrown off the Earth and coalesced into a single body. Problem: Earth not spinning fast enough to eject large amount of material. 2) "Coformation": The Moon and Earth formed out of the same material at the beginning of the Solar System. Problem: ...
Layers of the Earth Notes
Layers of the Earth Notes

... Earth’s Layers by Composition • Crust – Outermost layer – Thinnest layer – Composed mostly of oxygen, silicon, and aluminum – Two types • Oceanic (found under oceans; more dense) – Twice as much iron, calcium, and magnesium which are more dense minerals ...
Plate Tectonics - Department of Physics and Astronomy
Plate Tectonics - Department of Physics and Astronomy

... formation of the three major categories of rocks – Igneous Rock ...
Plate Tectonics - Awtrey Middle School
Plate Tectonics - Awtrey Middle School

... 1. Continents fit together like puzzle pieces (mountain ranges lined up) 2. Mesosaurus – Reptile fossil found on South America and Africa – It couldn’t swim! 3. Glossopteris – Tropical plant fossil that was found in Antarctica! ...
Layers of Earth - Skyline R2 School
Layers of Earth - Skyline R2 School

... The crust is made up of many kinds of rock, such as granite, sandstone, and ...
Earth`s Composition and Structure
Earth`s Composition and Structure

... give a whole earth density of ~5.5 g/cm3 • Typical rocks at the surface of the Earth have a density of 2.0-2.5 g/cm3 • What does this require of the density of material in the Earth’s interior? ...
PDF file of Lecture 4a - Earth`s Interior and Tectonics
PDF file of Lecture 4a - Earth`s Interior and Tectonics

the File
the File

... Continental Drift Theory but it was not accepted by the scientific community. In the 1960's, scientists began to realize that there might be a connection between continental drift, earthquakes and volcanoes. When the ship The Glomar Challenger completed studies of the ocean floor, scientists had a m ...
Directed Reading A
Directed Reading A

Study Guide Questions – Earth Structure and Plate Tectonics What
Study Guide Questions – Earth Structure and Plate Tectonics What

... mid-ocean ridge, and the thickness of sediments and structure of bedrock below the seafloor Broader application of radiometric dating revealed some really old (billions of years) pieces of continents, but the ocean basins were no older than about 200 million years The expanding field of paleomagneti ...
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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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