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inertia Forces can change velocity!
inertia Forces can change velocity!

File
File

... o Magma rises and lowers, creating___________________________  3. Outer Core o ________________________________________  Flowing iron produces Earth’s _________________________  4. Inner Core – o Hottest Layer  Solid iron-nickel sphere  Solid due to ____________________________________ Lithosph ...
How The Earth Works
How The Earth Works

Inside the Earth
Inside the Earth

... • 2240 km thick (1400 mi) • 6093 C (11,000 ˚ F) • Movement is source of Earth’s magnetic field ...
Topic 6 and 10 TEST
Topic 6 and 10 TEST

... The Earth and the Moon may be considered to be two isolated point masses. The masses of the Earth and the Moon are 5.98  1024kg and 7.35  1022 kg respectively and their separation is 3.84  108 m, as shown below. The diagram is not to scale. Earth mass  5.98 1024kg ...
Science 4th Unit 2 4-ESS2-2
Science 4th Unit 2 4-ESS2-2

3A_Internal_Earth_Structure
3A_Internal_Earth_Structure

... • San Andreas fault: a transform plate boundary between the North American and the Pacific plates • Two major cities on the opposite sides of the fault: Los Angeles and San Francisco •Many major earthquakes related to the fault system •Loss of many lives and billions of property damages due to earth ...
Layers of the Earth
Layers of the Earth

... metallic sheen and has the smell of sulfur. This is because metals are partly composed of sulfur. - Present summarized background information provided about the 3 layers of the earth leaving out the mineral composition of each layer. - Ask students to think about the minerals they have just examined ...
Inside the Earth - ReedEarthScience
Inside the Earth - ReedEarthScience

Earth`s vital statistics Shape: almost spherical almost spherical Size
Earth`s vital statistics Shape: almost spherical almost spherical Size

EARTH LAYERS REVIEW Name the compositional layers of Earth in
EARTH LAYERS REVIEW Name the compositional layers of Earth in

... 1. Name the compositional layers of Earth in order, starting on the surface and moving to the center. CRUST, MANTLE, OUTER CORE, INNER CORE 2. Earth’s core (both inner and outer) is made of NICKEL AND IRON. 3. The hottest layer of Earth is the __INNER CORE_. The layer with the highest pressures is t ...
What Can Changes Inside Earth Communicate? Pre/Post Test 1
What Can Changes Inside Earth Communicate? Pre/Post Test 1

... They tell the absolute age of the rock in which they occur. They tell the ages of many different rock layers. They tell the age of the rock at one location only. They tell the relative age of the rock in which they occur. ...
Folleto-Guia ok ingles
Folleto-Guia ok ingles

Quiz # 6
Quiz # 6

... d. a piece of special clothing worn by astronomers after they get their PhD's e. a region where the ultraviolet light from the Sun is blocked from getting further down 5. The Moon is heavily cratered, but the Earth which "lives next door" is NOT. Why? a. the active geology and weather on Earth destr ...
Earth and Space Science Part 3
Earth and Space Science Part 3

Geol 201 - American University of Beirut
Geol 201 - American University of Beirut

... This course is designed to provide the basic principles, and fundamental concepts of the various aspects of geological sciences. Emphasis will be on the internal structure of the Earth, properties of minerals, mineral groups, formation and behaviour of earth materials, description, classification, a ...
U 8 Synopsis
U 8 Synopsis

... recorded in written documents. That meant that only events in human history after the invention of writing (about 5,000 years ago) could have absolute dates; and only a small number of them. Then, in the 1950s, a whole series of new techniques were developed for assigning absolute dates to events be ...
Science
Science

... silicon, oxygen, iron and ________________________. It is a solid that has the ability to flow. This is called ___________________. 6. The CORE is the ________________ part of the planet. It is made of hot, dense metals that sank, due to gravity, after the Earth formed. _______________ and _________ ...
a. asthenosphere b. lithosphere c. mesosphere d. outer core e. inner
a. asthenosphere b. lithosphere c. mesosphere d. outer core e. inner

Chapter_2_Section_2_NOTES
Chapter_2_Section_2_NOTES

... Landforms: _shapes or types of land a. Mountains: _landforms that rise more than 2,000 feet above the land it surrounds. They rise steeply and have a narrow peak or ridge. b. Hills: __ are landforms with rounded tops, which rise above the surrounding land but are less steep than mountains c. Plateau ...
Slide 1
Slide 1

6th Grade Earth Science – Inside Earth Vocabulary 1. crust – the
6th Grade Earth Science – Inside Earth Vocabulary 1. crust – the

Earth System - Earth`s Structure
Earth System - Earth`s Structure

... a. Core, mantle, and surface b. Core, mantle, and crust c. Inner core, outer core, and mantle d. Upper mantle, lower mantle, and crust 2. What do earthquake waves have in common with other waves? a. They travel at the same speed as light waves b. They carry the same amount of energy as sound waves c ...
Earth`s Layers Sort
Earth`s Layers Sort

Geology
Geology

... Warm-up 1/27/15 • Take out your Measurement lab from yesterday, the M & M lab if you fixed it and your Info sheet if you still have it. ...
< 1 ... 174 175 176 177 178 179 180 181 182 ... 212 >

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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