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LESSON 2 EARTH`S MOVING CONTINENTS Chapter 5 Changes
LESSON 2 EARTH`S MOVING CONTINENTS Chapter 5 Changes

... • The split may one day form a new ocean. • Some divergent boundaries are less visible, occurring within a continental plate. ...
Unit Six Notes
Unit Six Notes

... (a pattern of volcanic islands created from a subduction zone that is located off the coast) ...
Chapter 21 Notes - Valdosta State University
Chapter 21 Notes - Valdosta State University

... In s waves, particles move at right angles to the direction of travel of the waves so they are transverse waves. s waves can only travel through solids. P waves can travel through solids, liquids, and gasses. P waves are called primary waves since they travel faster than s waves which are called se ...
Deadly quakes help renew the planet
Deadly quakes help renew the planet

... great benefits as well. "Nature is reborn with these kinds of terrible events," he says. "There are a lot of positive aspects even when we don't see them." Plate tectonics holds that the Earth's surface is made up of a dozen or so big crustal slabs that float on a sea of melted rock. Over ages, this ...
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Snack Tectonics

... Learning Objectives: What will students know and be able to do as a result of this lesson? Students will be able to identify the events that occur at plate boundaries as a result of Earth's tectonic activity. Student Content Statement: In the mantle there are convection currents that cause the plate ...
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Theory of Plate Tectonics III

... Convergent ...
Fire Quided _s KEY
Fire Quided _s KEY

... 1. What is convergent plate movement? What does it mean for Washington? Convergent plate movement is when two giant plates meet and one is forced under the other. This is the type of plate movement in WA, with the Juan de Fuca Plate moving under the North American Plate. 2. What is the major landfor ...
Plate Tectonics - GSHS Mrs. Francomb
Plate Tectonics - GSHS Mrs. Francomb

... 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 Earth's surface. • High pressure causes rock deformation during mountai ...
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... lava and magma). It is the only region of the planet that we can investigate directly by boring into it and taking samples. In continental areas, the crust's average thickness is 36 km but may be anything from 10 km to 80 km depending on the last movement of the tectonic plates in that area. The cru ...
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Seafloor spreading and plate tectonics are major concepts in geology

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... 4. Where and when is new crust made? ...
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3.3 Plates Move Apart

... Transform faults occur along divergent oceanic and continental plate boundaries Plates slide past each other building up tension until the tension is released during an earthquake ...
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A Review of the Earth Notes

...  Both types of crust can be found on a plate, but the denser ocean crust is found below sea level. Earth has 7 major plates and many minor plates.  The places where plates meet are called the plate boundaries.  Much of the geologic activity (earthquakes, volcanoes, mountain formation) takes place ...
CHAPTER 3
CHAPTER 3

... the north magnetic pole as a function of time, called polar wandering curves, can be made with different suites of rocks of varying ages from different continents. The polar wandering curves produced from suites of rocks in North America and Eurasia have the same shape but do not overlap (see fig. 3 ...
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Introduction to Plate Tectonic Theory, Geodesy, and VLBI

... km if incorporating continental crust. Plates move at different velocities The Earth's tectonic, seismic, and volcanic activity occurs at the boundaries of neighboring plates. The current theory is that the plates are moved around by convection currents caused by the cooling of the core and radioact ...
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... 8) What is the relationship between continental rifting and Pangaea? a) Continental rifting caused continents to come together to form Pangaea. b) Continental rifting tore Pangaea apart into separate continents. c) Continental rifting caused the land between the continents to drop down and form the ...
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Essentials of Oceanography, 10e (Trujillo/Keller)
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... 1) The four principle oceans of the Earth are the: A) Atlantic, Arctic, Mediterranean, and Pacific Oceans. B) Atlantic, Arctic, Indian, and Pacific Oceans. C) Atlantic, Antarctic, Mediterranean, and Pacific Oceans. D) Antarctic, Caspian, Indian, and Pacific Oceans. E) Antarctic, Arctic, Indian, and ...
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... What does the theory of continental drift state? Who came up the Continental Drift theory? ...
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Mrs

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File - Bruner science

...  Earthquakes often form from the ______________ between moving tectonic plates.  This accounts for _____ percent of all earthquakes.  The _________ _____ _________ convergent plate boundary west of Vancouver Island has many earthquakes. ...
Name: Doe Date: May 13, 2015 Directions: 1. Read the following
Name: Doe Date: May 13, 2015 Directions: 1. Read the following

... Earth looked like during the (looked, layer, first) 3.75 billion years. They do, however, know ...
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Powerpoint

... Earth’s outer layer is comprised of several large, rigid but mobile chunks called tectonic plates There are 12 tectonic plates that make up the crust Divided into: Continental plates Oceanic plates ...
Plate Tectonics The Earth`s tectonic plates. Three
Plate Tectonics The Earth`s tectonic plates. Three

... The existence of tectonic plates tells us that the Earth is a very active planet. In fact, many millions of years ago, the face of the Earth was vastly different than it is today! There are currently seven continents, but scientists believe that 225 million years ago there may have been only one! Th ...
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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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