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Convergent Boundaries Places where plates crash or
Convergent Boundaries Places where plates crash or

... All that folding and bending makes rock in both plates break and slip, causing earthquakes. As the edge of the oceanic plate digs into Earth's hot interior, some of the rock in it melts. The melted rock rises up through the continental plate, causing more earthquakes on its way up, and can cause vol ...
Energy Rich, Coal is plentiful in US, Easy to transport
Energy Rich, Coal is plentiful in US, Easy to transport

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Impact on Landscape and Population

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Physical world of mountainss

... Mountains in tropical or subtropical regions can be snow-capped because the air temperature decreases with increasing height. Mountaineers climbing in the Himalayas or the central Andes set out in warm temperatures surrounded by lush vegetation. As they climb, the weather becomes steadily colder, an ...
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Unit 3:Tectonic Processes
Unit 3:Tectonic Processes

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Geohazards Name: Period: Date: _____

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Earth Science: Tectonic Plates Section 1-1

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Earthquakes, Volcanoes & The Ring of Fire

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Guided Notes on Erosion and Deposition—Section 7
Guided Notes on Erosion and Deposition—Section 7

... 8. Glaciers scrape and gouge out large sections of the Earth’s landscape. They have the capacity to carry large rocks over great distances. Glaciers create landscape features such as waterfalls, lakes, and valleys. 9. Wind is a major erosional agent in areas of the Earth that experience limited prec ...
The Theory of Plate Tectonics - Ouray School District R-1
The Theory of Plate Tectonics - Ouray School District R-1

... produce large mountains (hymliays) 3) Oceanic vs oceanic: One goes under the other and the subducted plate produces magma that forms and rises to form an island arc. ...
Plate Tectonics - GSHS Mrs. Francomb
Plate Tectonics - GSHS Mrs. Francomb

... Metamorphic Rocks • Metamorphic rocks were sedimentary or igneous rocks that have been transformed by heat and pressure. • The heat may come from nearby magma or hot, ion-rich water intruding into existing rock. It can also come from subduction, when tectonic forces draw rocks deep beneath the Eart ...
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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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