WebThe lithosphere is the more or less stable crust of the earth, which may have been, to begin with, about fifty miles in thickness. The accompanying figure shows the boundaries of lithosphere plates that are presently active. These igneous rocks were consolidated either upon the surface of the lithosphere or in its interior. WebCHARACTERISTICS OF PLATE BOUNDARIES divergent transform convergent boundaries lithosphere created neither created subduction or collision nor destroyed sites of orogenesis and metamorphism volcanoes basaltic none subduction ! andesitic stresses tensional shear complex, mainly compressional earthquakesyshallow shallow shallow, …
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Web8 jul. 2010 · A convergent boundary neither creates nor destroys crust. What happens when a plate carrying continental crust and a plate carrying continental crust collide? No lithosphere is formed or... Weblithosphere is neither destroyed nor produced new continetal crust is formed Question 14 30 seconds Q. According to the property of paleomagnetism ___________. answer choices Iron rich rocks show the location of the magnetic poles at the time of their formation All rocks, regardless of when they are formed, have the same polarity irony definition literature simple
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Web30 mrt. 2024 · Transform boundaries: where crust is neither produced nor destroyed as the plates slide horizontally past each other. Plate boundary zones: broad belts in which boundaries are not well defined and the effects of plate interaction are unclear. Plate Boundary Types Divergent boundary (Constructive) Webseafloor is neither formed nor destroyed but spreads apart at ridges. new seafloor is formed at ridges and destroyed at trenches. new seafloor is formed at trenches and … WebSince neither plate is stronger than the other, they crumple and are pushed up. 6.Mid-ocean ridges occur along divergent plate boundaries, where new ocean floor is created as the Earth's tectonic plates spread apart. 7.Subduction zones are where the cold oceanic lithosphere sinks back into the mantle and is recycled. portability iso