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Plate Boundaries and Earth`s Land Features
Plate Boundaries and Earth`s Land Features

... to move across the top of it, carrying the continents and ocean basins with them as they move about. For example, North America and a good part of the Atlantic Ocean are on the North American Plate. The Theory of Plate Tectonics revolutionized geology because it finally provided an explanation for t ...
4.5 The Theory of Plate Tectonics
4.5 The Theory of Plate Tectonics

... • Demonstrate the boundaries using blocks. • Why do you think earthquakes occur frequently at transform boundaries? • Answer: The plates cannot move smoothly past one another because of the irregular nature of faults. • How fast do you think Earth’s plates are moving? ...
Dynamic Earth
Dynamic Earth

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... _____ 10. The type of mountain that forms when rock layers are squeezed together and pushed upward is a a. folded mountain. c. volcanic mountain. b. fault-block mountain. d. strike-slip mountain. _____ 11. Scientists’ knowledge of the Earth’s interior has come primarily from a. studying magnetic rev ...
GeomorphReview1 - University of Colorado Denver
GeomorphReview1 - University of Colorado Denver

... evidence...It is only by combing the information furnished by all the earth sciences that we can hope to determine ‘truth’ here, that is to say, to find the picture that sets out all the known facts in the best arrangement and that therefore has the highest degree of probability. Further, we have to ...
Name - oms6a
Name - oms6a

... Outer core - A layer of molten iron and nickel that surrounds the inner core of Earth. Inner core - A dense sphere of solid iron and nickel at the center of Earth. Ch 1-2 Radiation – The transfer of energy through space.(think of sun’s rays – sunshine) Conduction – The transfer of heat within a mate ...
Section 17.3 Theory of Plate Tectonics
Section 17.3 Theory of Plate Tectonics

... B. Rift Valley forms if the divergent boundary is _______________  As the continent is torn farther and farther apart, the rift valley gets deeper and ...
Chapter 6.1 Section Review
Chapter 6.1 Section Review

... theory that states that Earth’s lithosphere is divided into tectonic plates that move around. A tectonic plate is a piece of lithosphere that moves around on top of the asthenosphere. The theory of plate tectonics is the theory that explains how tectonic plates move and change shape. A tectonic plat ...
Plate Boundaries - CoconinoHighSchool
Plate Boundaries - CoconinoHighSchool

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Evaluating Evidence of Plate Tectonics

... • Explaining your evidence (back up each one of your pieces of evidence with reasoning for why it supports your claim) ...
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Unit 8 ~ Learning Guide Name

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Instructions: Earth`s Layers Questions
Instructions: Earth`s Layers Questions

... -Mountains and valleys mark the edge of a plate where the Earth’s crustal plates are moving apart Scientists also found evidence of long, narrow, deep depressions in the sea floor called trenches. Many trenches are found around the edges of the Pacific Ocean plate. What new evidence did scientists f ...
What is the crack in the ocean floor through which magma rises
What is the crack in the ocean floor through which magma rises

... Why do earthquakes usually occur at plate boundaries? a. The rock on the edges of tectonic plates is soft and gives in easily to various pressures. b. Rock in environments near tectonic plate boundaries experience great stress. c. The boundaries between tectonic plates have been seismically active ...
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Plate Tectonic Theory

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... 3. Tectonic plates forming a transform boundary may move only a few centimeters each year. Can even this small movement affect people and communities living near a transform boundary? Explain your answer. Answers will vary. Sample answer: When tectonic plates slide past each other, the movement may ...
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... lithosphere through a slow broad rise of rock throughout the mantle. The unequal distribution of heat within Earth causes the thermal convection in the mantle that ultimately drives plate ...
“Seeing” Continental Drift
“Seeing” Continental Drift

... boundary (transform plate boundary). However, 10 years ago, SLR measurements began to reveal that the San Andreas Fault was moving at only 3.5 cm/yr. This "San Andreas discrepancy" leaves about 2 cm/yr of movement that is taking place somewhere else. "We want to know where that movement is because t ...
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... A Glimpse of Earth’s Interior (p.16) Draw a simple sketch of the major layers that make up the Earth’s interior, show the locations of the Crust Mantle and Core and also label the position of the lithosphere, asthenosphere, outer core, and inner core. We will be referring to these different layers t ...
Earthquake BINGO
Earthquake BINGO

... Ring of Fire Plate Boundary Divergent Rupture (crack) at surface People hurt Streams/rivers diverted Modified Mercalli Intensity Scale Richter Scale Mountain ridges line up Shapes of continents match Mid Atlantic Ridge S-Wave Convergent ...
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... 1) _________________ boundaries are places where two tectonic plates move away from each other. There are 2 types based on the type of crust involved. (Draw arrows indicating plate directions in this box) a) ____-____: found on the seafloor where they form __________ ____________. It is in this rift ...
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Classzone webquest plate tectonics and Wegener

... 21. Those composed partly or entirely of ____________ lithosphere can _________ under another plate, usually a ____________, mostly ______________ plate and eventually _______________ completely. 22. The ___________________ Plate, formerly the _____________ Plate, will someday be entirely sunk under ...
Theory Development
Theory Development

... 1962 - Sea Floor Spreading Theory – idea that the seafloor itself moves and carries continents with it, as it expands from a central point. The theory is well-accepted now. It is caused by convection currents in the molten, very weak upper mantle, or asthenosphere. Hess described a geologic mechanis ...
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1 Plate Tectonics Review w

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Unit 07 Test Review

... line, divergent, subduction zone, San Andreas Fault, trench, mid-ocean ridge, transform, volcanic island, mountain, rift valley, convergent, MidAtlantic Ridge, Himalayan Mountains, earthquakes ...
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Plate tectonics



Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός ""pertaining to building"") is a scientific theory that describes the large-scale motion of Earth's lithosphere. This theoretical model builds on the concept of continental drift which was developed during the first few decades of the 20th century. The geoscientific community accepted the theory after the concepts of seafloor spreading were later developed in the late 1950s and early 1960s.The lithosphere, which is the rigid outermost shell of a planet (on Earth, the crust and upper mantle), is broken up into tectonic plates. On Earth, there are seven or eight major plates (depending on how they are defined) and many minor plates. Where plates meet, their relative motion determines the type of boundary; convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from zero to 100 mm annually.Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some supporters) propose gradual shrinking (contraction) or gradual expansion of the globe.Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
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