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Ch 5 wo cycles
Ch 5 wo cycles

... air warms and rises again at ~60° N & S air sinks at poles ...
Chapter 1 powerpoint
Chapter 1 powerpoint

... • Historians look at events over time • Geographers look at: - use of space on Earth - interactions that take place there - patterns and connections between people and land • Geography is the study of the distribution and interaction of: - physical features on Earth - human features on Earth ...
Chapter 28: The Changing Earth
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Welcome to GEOLOGY

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Decision One: Concept Map and Learning Unit

... 2. What forces are involved in the changes of earth’s surface? Compare/contrast erosion and deposition. 3. How have wind and ice changed the shape of earth’s surface? 4. What forces cause earthquakes, volcanoes, and mountains? What is a fault? What effect do plate tectonics have on changes in earth’ ...
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sample test1 - this is only for questions style

... All of the following phrases below describe science: a) Science is the ability to formulate ideas. b) Science is the study of nature using observation and deductive reasoning c) Science is the method used to test an idea. d) Science will assume answers based on preconceived ideas. Science is: a) not ...
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Picture Review Name

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What’s inside the Earth? Is there really another world at

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Exam Study Guide

...  E3.1d Explain how the crystal sizes of igneous rocks indicate the rate of cooling and whether the rock is extrusive (small grained) or intrusive (large grained).  E3.1e Explain how the texture (foliated, nonfoliated) of metamorphic rock can indicate whether it ahs experienced regional or contact ...
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... Many things- some large, some small- influence climate • position and amount of land on planet • ocean-atmosphere-land dynamics • incoming solar radiation fluctuations • reflectance and absorption of solar energy • carbon cycle • water cycle • population of organisms (e.g., phytoplankton, humans) • ...
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... The rotation of the earth affects the movement of fluids. Energy transfer between the sun and earth's surface creates climate and weather patterns. The climate and weather on earth is affected by the composition of the ...
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... MOVES? The Earth’s crust is broken into several major plates, called “tectonic plates,” that float on the layer of magma underneath. These plates are usually very stable, but sometimes they bump or slide past each other, releasing a huge amount of energy called “seismic waves.” These waves cause the ...
Principles of Earth History
Principles of Earth History

... Mantle – It’s composed of Si, O, Mg and Fe. It extends to 2900km depth. Lithosphere - Outer, relatively rigid layer of the Earth, approximately 100 km thick, overlying the asthenosphere. It includes the entire crust plus the upper mantle. Asthenosphere - Layer within the upper mantle and below the l ...
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... In our model of sea-floor spreading, describe which type of plate boundary was found at each of the two areas of activity and tell which plate boundary was not represented in the model. ...
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... Suppose a magnetic reversal occurred today. How would new rocks at midocean ridges differ from the rocks that formed last year? The magnetic minerals in the new rocks would be aligned in the opposite direction. ...
This is - Welcome to St Paul Lutheran Church & School
This is - Welcome to St Paul Lutheran Church & School

... In our model of sea-floor spreading, describe which type of plate boundary was found at each of the two areas of activity and tell which plate boundary was not represented in the model. ...
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Final Review - Academic Computer Center
Final Review - Academic Computer Center

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The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics

... • The Earth’s crust is divided into _________major plates which are moved in various directions. • This plate motion causes them to _____________________________ • ________________ against each other. • Each type of interaction causes a characteristic set of Earth structures or “tectonic” features. ...
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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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