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The Five Themes of Geography
The Five Themes of Geography

... ”How do people relate to the land?”  Use the environment to meet peoples needs  May use same land resource in different ways ►Ex. ...
Chapter 2
Chapter 2

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Physical Geology
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... Most scientists would argue that overpopulation is the greatest problem facing the world today. Increasingly large numbers of people must be fed, housed, and clothed, with a minimal impact on the environment. ...
Science Study Guide - Thomas C. Cario Middle School
Science Study Guide - Thomas C. Cario Middle School

... Energy released by an earthquake that travels through the earth 9. What is a seismograph? Tool used to measure the amount of energy released by an earthquake 10. Explain what seismic waves tell us about Earth’s interior Speed up in more dense substances and slow down in less dense. P waves can trave ...
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... 6.E.2 Understand the structure of the earth and how interactions of constructive and destructive forces have resulted in changes in the surface of the Earth over time and the effects of the lithosphere on humans. ...
#______ Parent Signature: Heading: The Earth`s Changing Surface
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... A. The temperature increases, the density decreases, and the composition increases B. The temperature decreases, the density increases, and the composition decreases C. The temperature increases, the density increases, and the composition changes D. The temperature decreases, the density decreases, ...
1 Plate Tectonics Post-Test
1 Plate Tectonics Post-Test

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File - Mr. Catt`s Class
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Earth Model Project
Earth Model Project

... The Earth's structure, scale and our place on it can be difficult to comprehend. Today we will use baker's clay to create a physical model of the planet. We will also use the idea of normalized data. At times it is difficult to visualize the relationships among numbers if they are in an inconvenient ...
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The Solid Earth - cloudfront.net
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Stanley
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The Solid Earth - Cloudfront.net
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... 1968 – Theory of Plate Tectonics- is a combination of two earlier ideas: continental drift and sea-floor spreading. This theory was formed as new information was learned about the nature of the ocean floor, Earth’s ancient magnetism patterns, the location of volcanoes and earthquakes, the flow of he ...
Inside Earth: Chapter 1
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... together form a rigid layer called the lithosphere. It averages about 100 km thick. • Heat and pressure continue to increase making the area just below the lithosphere less rigid and flows slowly. The material is like soft road tar and bends like plastic. This layer is called the ...
Unit Vocab
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... stated that continents were once one big supercontinent that drifted apart over many years to their present-day locations Pangaea: name given to the super-continent Mid-Atlantic Ridge: ridge in the Atlantic Ocean through which molten rock flows Sea-Floor Spreading: process where new crustal material ...
The Layer`s Of The Earth! - Mrs. V. Murphy`s Science Class
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... • The Earth’s crust is divided into 12 major plates which are moved in various directions. • This plate motion causes them to collide, pull apart, or scrape against each other. • The word, tectonic, refers to the deformation of the crust as a consequence of plate interaction. ...
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... Energy from the sun, or solar energy, is necessary for life on Earth. It helps plants grow and provides light and heat. Several factors affect the amount of solar energy Earth receives. These are rotation, revolution, tilt, and latitude. Earth’s axis is an imaginary rod running from the North Pole t ...
Document
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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 ...
Earth System Science: The Big Ideas
Earth System Science: The Big Ideas

... and rapid changes in the Earth system The Earth processes operating today, everything from local erosion to plate tectonics, are the same as those operating since they first arose in Earth history, and these processes are obedient to the laws of chemistry and physics. While the processes that consta ...
Continental Drift
Continental Drift

... divide the remaining clumps of Pangaea over time to form the positions of continents as we know them today. However, this movement is not complete. The continents will continue to flow adrift the asthenosphere, colliding and reforming new landmasses only to break up and drift apart again. Sediments ...
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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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