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planetesimals - Mestre a casa
planetesimals - Mestre a casa

... The rocky material formed the outer layers of the Earth. Of these, the lightest rock materials rose to the surface and formed the crust, while thicker materials remain in the intermediate layers and formed the mantle. ...
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FOSS Weather and Water Glossary FOSS Weather and

... the dew point. Dew point: The temperature at which a volume of air is saturated with water vapor; condensation occurs when the temperature drops below the dew point. Downburst: A severe localized downdraft from a thunderstorm, causing damaging winds at or near Earth’s surface. Drought: Less than nor ...
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Integrated Science Chapter 19 Name

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... molten rock and gases are erupted. There are, however, many kinds of volcanoes. Volcano does not have to be a beautiful snowcapped conical peak (Mt St Helens). It can be a hole in the ground, or a crack in the earth’s surface Most volcanoes occur at convergent boundaries ...
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chapter 11 Dynamic Planet

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Just how integrated is the Earth System

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Plate Tectonics and Weathering

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Plate Tectonics - THS Aquatic Science

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Tectonic Plate Theory PowerPoint Study Guide

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Earth PowerPoint

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Atmospheric Heating

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Planet Earth - Topic 4 (ANSWERS)
Planet Earth - Topic 4 (ANSWERS)

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Alfred Wegener - Colts Neck Township Schools

... America, Africa, India, and Australia –Coral reefs found in Northern Canada –Coal formation in North America ...
Four main kinds of changes affect the Earth`s surface: (1) weathering
Four main kinds of changes affect the Earth`s surface: (1) weathering

... In 1905, Thomas Chamberlin, an American geologist, and Forest Moulton, an American astronomer, proposed the planetesimal theory. According to this theory, a rapidly moving star passed close to the sun but did not collide with it. The gravity of the passing star pulled long, threadlike "arms" of gas ...
lesson-2-explore-page-115-shaping-earths-surface
lesson-2-explore-page-115-shaping-earths-surface

...  One place where a fault can exist is at a boundary plate.  Tectonic plates do not continually slide past each other along faults. But, because of the convection currents beneath the tectonic plates, forces build up along faults. Eventually, these forces become so great that the rocks on either si ...
Chapter 8 Test Review Notes
Chapter 8 Test Review Notes

... The lack of geologic activity is not a characteristic feature of at least one type of plate boundary. Plate boundaries are defined by: • Earthquake activity • Volcanic activity • High heat flow Click Here to See the Locations of these Activities. ...
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The Rock cycle

... world rock tour that began in Hawaii might end in east Greenland. Millions of years ago there, magma deep inside the Earth forced its way into another rock and solidified. This created an igneous rock. Then, intense pressure in the Earth caused the rock to up-heave, fold, and crumple, until it becam ...
Name
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... Destroy formations – weathering by gravity, wind, and water (breaks rocks apart), erosion (carries rock away), and tectonic activities (plates sliding under other plates to be consumed & melted by magma) ...
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Tectonic–climatic interaction



Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.
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