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Chapter 7: Plate Tectonics
Chapter 7: Plate Tectonics

... 3 Types of Mountains  Folded Mountains ...
Unit 07 Test Review
Unit 07 Test Review

... of mountain worn down to broad shallow hill, 6-mountain completely weathered 5. A model of the process shown above is created, using a pipe that pumps mud up through a hole in a flat board, and a ruler that is used to scrape away the mud to represent weathering. What are some advantages and limitati ...
The History of the Earth
The History of the Earth

... • Says that Earth’s rigid outer shell (lithosphere) consists of 7 large and numerous smaller segments called plates that are in motion relative to each other • Most of Earth’s seismic activity, volcanism, and mountain building occur along the dynamic margins of these plates ...
Rocks Powerpoint Notes
Rocks Powerpoint Notes

... mantle that slowly change rocks from one kind to another Once a rock is formed, does it stay the same rock forever?_____________ Rocks are continually changed by many ___________________, such as weathering, _______________, compaction, ________________________, melting, and cooling Rocks can ______ ...
Geology Pre Test
Geology Pre Test

3. The Earth system
3. The Earth system

a type of rock that forms when sediments are
a type of rock that forms when sediments are

... from the cooling of lava. • Sedimentary – a type of rock that forms when sediments are compacted. • Metamorphic – forms when existing rocks are changed by heat and pressure. ...
Applying Concepts 33. a. Index fossils in each sequence can be
Applying Concepts 33. a. Index fossils in each sequence can be

General Geology
General Geology

... density gradient and results in flow - faster; generally associated with fluids (liquids and gases) • Advection - transfer of heat and mass - fluid flow through cracks; can be fast • Radiation - Direct heating via EM waves without any requirement of mass along path - fastest ...
Plate Tectonics, Topographic Maps, and Weather Study Guide KEY
Plate Tectonics, Topographic Maps, and Weather Study Guide KEY

... A topographic map shows elevations of land features using contour lines. 12. What are some specific features on a topographic map? Contour lines, compass, distance scale, symbols of land features 13. Why is it important to have compass directions on a topographic map? It is important to have a compa ...
Linking Asteroids and Meteorites through Reflectance
Linking Asteroids and Meteorites through Reflectance

... • Seafloor crust is created along mid-ocean ridges where magma upwells from the mantle • Ocean basins are generally younger than continents • Seaflloor spreads until it encounters a trench and descends back into the mantle ...
Theory of Plate Tectonics Cornell Notes Answers
Theory of Plate Tectonics Cornell Notes Answers

... A volcano is a weak spot in the crust where molten magma comes to the surface. Plate movements determine where volcanoes develop on Earth. Ex Ring of Fire on rim of Pacific Ocean. Most, but not all, occur along diverging plates such as mid-ocean ridge or subduction zones Ex: o/c convergence: Andes M ...
Plate Tectonics Notes
Plate Tectonics Notes

... core material - The release of heat (=energy) from the mantle causes volcanoes - Core heat causes the formation of hot spots, and is much more localized to one region—we can tell because the basalts formed have different mineral composition (core has more K, Ru, Cs, U, Th) - Hot spots include Icelan ...
Natural Disasters
Natural Disasters

... A tsunami is a series of ocean waves that sends surges of water, sometimes reaching heights of over 100 feet (30.5 meters), onto land. These walls of water can cause widespread destruction when they crash ashore. These awe-inspiring waves are typically caused by large, undersea earthquakes at tecton ...
Geography and Society – First Discussions
Geography and Society – First Discussions

... o Summarize the major points of the Theory of Plate Tectonics. o Explain how data collected on the magnetism, depth, and the age of oceanic crust support the Theory of Plate Tectonics. o Explain how the distribution of earthquakes, volcanoes, and the Hawaiian Island chain relate to plate tectonics. ...
Managing Earthquakes and Volcanoes
Managing Earthquakes and Volcanoes

... under the continental plate. The oceanic crust melts and creates new magma which then rises up through the continental crust to form a volcano. Earthquakes also happen here as friction builds up when the two plates move past each other. ...
EARTH SCIENCE FINAL EXAM REVIEW SHEET
EARTH SCIENCE FINAL EXAM REVIEW SHEET

... continental – continental convergencesubducion (ocean- continental) zonesdivergent boundaries2. Locate common earthquake zones and volcano zones 3. Describe the layers of the Earth and how we know about each layer layer ...
Plate Tectonics
Plate Tectonics

Theory of Plate Tectonics
Theory of Plate Tectonics

... plate bends underneath the  continental plate.   ...
The Restless Earth - Heathcote School & Science College
The Restless Earth - Heathcote School & Science College

... Help and aid provided to an area to prevent immediate loss of life because of shortages of basics, such as water, food and shelter. ...
Weather Lab Powerpoint Charts
Weather Lab Powerpoint Charts

Theory of Plate Tectonics Cornell Notes
Theory of Plate Tectonics Cornell Notes

... A volcano is a weak spot in the crust where molten magma comes to the surface. Plate movements determine where volcanoes develop on Earth. Ex Ring of Fire on rim of Pacific Ocean. Most, but not all, occur along diverging plates such as mid-ocean ridge or subduction zones Ex: o/c convergence: Andes M ...
Chapter 7, Section 4 Directed Reading A
Chapter 7, Section 4 Directed Reading A

... _____ 25. The rising of Earth’s crust to higher elevations is called a. uplift. c. subsidence. b. deformation. d. uprise. _____ 26. The sinking of regions of the Earth’s crust to lower elevations is called a. uplift. c. subsidence. b. rebound. d. uprise. _____ 27. When the Earth’s crust slowly sprin ...
Oceanic Crust
Oceanic Crust

... The first 50 miles (80km) of the mantle are believed to consist of very hard, rigid rock. The next 150 miles (241km) or so are believed to be super-heated solid rock that due to the heat energy is very weak. Below that for the next several hundred miles, the Earth's mantle is believed to once again ...
TECTONIC PLATES
TECTONIC PLATES

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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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