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Transcript: by marquel A sudden movement of the Earth's lithosphere (its crust and upper mantle). Earthquakes are caused by the release of built-up stress within rocks along geologic faults or by the movement of magma in volcanic areas. They are usually followed by aftershocks. See Note at fault. The layer of the Earth between the crust and the core. It is about 2,900 km (1,798 mi) thick and consists mainly of magnesium-iron silicate minerals, such as olivine and pyroxene. It has an upper, partially molten part, which is about 660 km (409 mi) thick, and a lower, solid part. The upper mantle is the source of magma and volcanic lava. The layer of soft tissue that covers the body of a clam, oyster, or other mollusk and secretes the material that forms the shell. In the theory of plate tectonics, the process by which new oceanic crust is formed by the convective upwelling of magma at mid-ocean ridges, resulting in the continuous lateral displacement of existing oceanic crust. See more at magnetic reversal. eathquakehttp: Sea floor spreading what happen when earth goes though these things MANTLE Plate tectoincs Theory that the Earth's lithosphere (the crust and upper portion of the mantle) is divided into about 12 large plates and several small ones that float on and travel independently over the asthenosphere. The theory revolutionized the geological sciences in the 1960s by combining the earlier idea of continental drift and the new concept of seafloor spreading into a coherent whole. Each plate consists of rigid rock created by upwelling magma at oceanic ridges, where plates diverge. Where two plates converge, a subduction zone forms, in which one plate is forced under another and into the Earth's mantle. The majority of the earthquakes and volcanoes on the Earth's surface occur along the margins of tectonic plates. EARTHQUAKE Mantle
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