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The Earth`s Interior
The Earth`s Interior

... In 1906, the center of the earth, the core, was discovered by a scientist named R. D. Oldham. To make this discovery, he studied earthquakes, and also the ideas of a scientist from earlier times, Isaac Newton. The core consists mainly of iron, along with smaller amounts of other elements. The iron a ...
Mena Pfest - Mrs. Pfest`s Science Place
Mena Pfest - Mrs. Pfest`s Science Place

... The dangers and importance of finding long term storage for nuclear waste. Volcanoes are both constructive and destructive earth processes. Lava released from volcanic eruptions is magma from beneath the earths surface. Geological time refers to time periods of thousands, millions and billions of ye ...
World Geography Facts PP
World Geography Facts PP

... Greenwich, England. Because the Earth's circumference is similar to circle, it was decided to measure longitude in degrees. The number of degrees found in a circle is 360. The Prime Meridian has a value of zero degrees. A line of longitude or meridian of 45° West has an angle that is 45° west of the ...
The 5 Themes of Geography
The 5 Themes of Geography

... – Tropic of Capricorn• 23 ½*S- the sun is directly overhead when it reaches the southern most point in the sky ...
Name
Name

... to the 1:10 million scale, one can simply move the decimal two places to the left and the number will be in cm. For example, 6371 km is 63.71 cm at the 1:10 million scale (see Table 1). 5. Label the boundaries and layers of the Earth and (optionally) color the various layers representing spherical s ...
Earth`s Structure - hrsbstaff.ednet.ns.ca
Earth`s Structure - hrsbstaff.ednet.ns.ca

... properties. They tell us how a certain material responds to force, how weak or strong it is and whether it is a liquid or a solid. The lithosphere (rock sphere) is the solid, strong and rigid outer layer of the Earth. It includes the crust and the upper most part of the mantle. It varies greatly in ...
The Earth-Mars-Moon System - Geophysical Journal International
The Earth-Mars-Moon System - Geophysical Journal International

... Fundy and the English Channel did not exist. The Behring Strait, which Jeffreys (1928) calculates accounts for two-thirds of the tidal friction, only came into being when America moved away from Europe. Lyttleton (1960) proposes that Mercury was once part of Venus. The mass of Mercury is only about ...
Land, Air, and Water • What forces shape the land? • What are the
Land, Air, and Water • What forces shape the land? • What are the

... • The thick layer of gases that surrounds the Earth is called the atmosphere. • It provides life-giving oxygen for people and animals and lifegiving carbon dioxide for plants. • It also acts as a blanket, holding in enough heat from the sun to make life possible. • Winds distribute this heat around ...
Study Guide Chapt 7: Solid Earth
Study Guide Chapt 7: Solid Earth

... Seismic waves Body waves P-wave (longitudinal)and travel faster. Can travel through both solid and liquid. P-wave shadow S-wave (transverse) slower than P waves . can only travel through solid. Surface waves Love waves and Rayleigh waves travel slower than Body waves (P and S waves) Difference in P- ...
Study Guide Chapt 7
Study Guide Chapt 7

... Seismic waves Body waves P-wave (longitudinal)and travel faster. Can travel through both solid and liquid. P-wave shadow S-wave (transverse) slower than P waves . can only travel through solid. Surface waves Love waves and Rayleigh waves travel slower than Body waves (P and S waves) Difference in P- ...
Lecture #1
Lecture #1

... • When an oceanic plate collides with a continental landmass, the continental plate will ride up over the seafloor and the oceanic plate will subduct down into the mantle where it melts. –Deep ocean trenches mark subduction zones. ...
Unit 1: Structure of the Earth
Unit 1: Structure of the Earth

... • Center of the Earth; under extreme pressure • Composition: iron and nickel • Relative Temperature: 2,000oC to 5,000oC • Density: 10 to 13 times denser than water ...
Introduction to Planet Earth
Introduction to Planet Earth

... what makes up the earth’s interior if we can’t actually dig a hole through the earth to see it directly? ...
Geologic Time Scale Study Guide
Geologic Time Scale Study Guide

...   lanets ___   in   the   solar   system   and   the   _s  un _____   were   formed   at   the   same  time.    The   planets   and   the   sun   _a   ccreted __   (came   together)   in   a  _ solar  nebula ________,   a  cloud   of   gas   and   dust.    _ Gravity _____   caused   bits   of   rock ...
Inside Earth Study Guide
Inside Earth Study Guide

... b. Which layer has the greatest pressure, density and temperature? c. Which layer makes up 70% of Earth’s mass? ...
Earth`s Surface and Layers Notes
Earth`s Surface and Layers Notes

... solid ball at the center of Earth ...
CSCOPE Unit 7 Forces That Change the Earth
CSCOPE Unit 7 Forces That Change the Earth

... CSCOPE Unit 7 Forces That Change the Earth Glossary Asthenosphere—layer in the upper part of Earth’s mantle that is made of material that can be reshaped and deformed, and on which the ...
Part I. The Layers of Earth - www .alexandria .k12 .mn .us
Part I. The Layers of Earth - www .alexandria .k12 .mn .us

... Use the following sites to help you understand the Earth’s interior-http://www.mnh.si.edu/earth/main_frames.html (Select the “Multi-Media Version” and then the “Plate Tectonics and Volcanoes” tab. Now, click on “Inner Earth” and read the Introduction (2 slides) and then click on words CRUST, MANTLE ...
Earth Structure Foldable Notes
Earth Structure Foldable Notes

... • Thickness: Approximately 2270 km thick – Composition: Consists mostly of the liquid metals iron and nickel – 16% of the Earth's total volume ...
Summary
Summary

... Seismic waves generated by earthquakes can be detected by seismographs all over the world and can reveal Earth’s internal structure. Pressure (P) waves can travel through a liquid, but shear (S) waves cannot. Observations show that S waves cannot pass through Earth’s core, and that is evidence that ...
The Earth*s Physical Geography
The Earth*s Physical Geography

... surface is water. Oceans hold 97% of Earth’s water. Fresh water is frozen in ice sheets near N and S Poles. ...
Today`s Objectives
Today`s Objectives

... • D. commensalism ...
8th Grade Science Units
8th Grade Science Units

... - This topic focuses on the physical features of Earth and how they formed. - This includes the interior of Earth, the rock record, plate tectonics and landforms. ...
Document
Document

... Pieces of Earth’s crust that “float” on mantle layer. ...
THE ATMOSPHERE
THE ATMOSPHERE

... temperatures and pressure – Troposphere- layer closest to the earth’s surface that provides earth’s weather – Stratosphere-layer where the sun’s ultra violet rays are absorbed in what is called the ozone layer – Mesosphere – coldest layer of the atmosphere at -93 C and located in the middle of the a ...
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Spherical Earth



The concept of a spherical Earth dates back to around the 6th century BC, when it was mentioned in ancient Greek philosophy, but remained a matter of philosophical speculation until the 3rd century BC, when Hellenistic astronomy established the spherical shape of the earth as a physical given. The paradigm was gradually adopted throughout the Old World during Late Antiquity and the Middle Ages. A practical demonstration of Earth's sphericity was achieved by Ferdinand Magellan and Juan Sebastián Elcano's expedition's circumnavigation (1519−1522).The concept of a spherical Earth displaced earlier beliefs in a flat Earth: In early Mesopotamian mythology, the world was portrayed as a flat disk floating in the ocean and surrounded by a spherical sky, and this forms the premise for early world maps like those of Anaximander and Hecataeus of Miletus. Other speculations on the shape of Earth include a seven-layered ziggurat or cosmic mountain, alluded to in the Avesta and ancient Persian writings (see seven climes).The realization that the figure of the Earth is more accurately described as an ellipsoid dates to the 18th century (Maupertuis).In the early 19th century, the flattening of the earth ellipsoid was determined to be of the order of 1/300 (Delambre, Everest). The modern value as determined by the US DoD World Geodetic System since the 1960s is close to 1/298.25.
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