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Plate Movement
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After Wilson s description of plate tectonics, geologists began comparing plate measurements and found that most plates aren t even close to their original positions! Fossils of tropical plants, once at the equator, were found in Antarctica Deep rock in the Sahara desert, sliced by glacier travel, was frosty long before arriving at its current hot and dry retreat Most importantly, plates slide along at rates of up to 8 inches per year in some areas The Pacific and Nazca plates are separating as fast as 16 centimeters (cm) per year, while the Australian continental plate is moving northward at a rate of nearly 11 cm per year In the Atlantic, plates crawl along at only 1 to 2 cm per year When enough new material from within the Earth is deposited, plates slant, slide, collide, and push over, under, and alongside their neighbors Continental and ocean plates ride over or dive under each other, forcing movement down into the mantle and liquid core A subduction zone is an area where two crustal plates collide and one plate is forced under the other into the mantle Figure 52 illustrates the subduction zone between plates The lithospheric plate causes volcanism on the overriding plate, while the crustal plate is forced deep into the mantle
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Lithosphere Crust
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Mountain building occurs at subduction zones between plate margins
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Convection
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Material circulation caused by heat is called convection In the Earth s system, convection is affected by gravitational forces within the planet, as well as heat and radioactive recycling of elements in the molten core Convection is the process of heat transfer that causes hot, less dense matter to rise and cool matter to sink All tectonic processes within the Earth involve movement of solid or malleable matter Mantle convection, driven by the thermal gradient between the core and crust, takes place by the extremely slow deformation (creep) of the rocks and minerals in the upper and lower mantle and the transition zone Flaws in mineral crystalline structures provide gaps The application of extreme pressure causes atoms in the structure to creep, one atom at a time, into a new position Magma movement depends on temperature and density differences within large pockets of molten matter Depending on conditions, magma rises in hotter pockets and sinks in cooler pockets The Earth s molten core keeps thermal activity and tectonic processes going
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Plate Boundaries
There are three main types of plate boundaries that form when convection drives plates together and apart These boundaries include Convergent boundaries Plates clash, and one is forced below the other, pulling older lithosphere into the depths of the mantle (See the Trenches section that follows) Divergent boundaries Plates pull apart and move in opposite directions making room for new lithosphere to form from outpouring magma (See the Ridges section that follows) Transform fault boundaries Plates slide past each other parallel to their shared boundaries The Earth s core is roughly 6,000 C, and its heat production keeps the convection cycle going Heat transfer from rising and sinking convection currents provides the power to move plates around the globe
Trenches
An ocean trench is formed along the convergent boundary of two colliding plates The Pacific Ocean is ringed by these trenches (called the Ring of Fire) because of the constant action of the Pacific oceanic plates against the North American, Eurasian, IndianAustralian, Philippine, and Antarctic plates Some of the deepest points on the Earth are found within ocean trenches The Java trench in the West Indies, and the Mariana Trench (five times as deep as the Grand Canyon) in the Pacific, average between 7,450 meters (m) and 11,200 m, respectively
Ridges
Ridges are formed along divergent boundaries where plates slowly edge apart from each other When plates separate, magma rises into the crack, filling it and hardening into rock Most magma exiting the mantle today is found at ocean floor ridges and along plate margins Nearly all ridges are at the bottom of oceans, but the Mid-Atlantic Ridge, which bisects the Atlantic, emerges in a few places (eg, Iceland) where geologists can measure its growth and movement
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