Orogenic belt
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An orogenic belt, orogen, or mobile belt is a zone of Earth's crust affected by orogeny. An orogenic belt develops when a continental plate crumples and is uplifted to form one or more mountain ranges; this involves a series of geological processes collectively called orogenesis.
An orogenic belt, orogen, or mobile belt is a zone of Earth's crust affected by orogeny. An orogenic belt develops when a continental plate crumples and is uplifted to form one or more mountain ranges; this involves a series of geological processes collectively called orogenesis. File:Active Margin.svg|Subduction of an oceanic plate beneath a continental plate to form an accretionary orogen. (example: the Andes) File:Continental-continental convergence Fig21contcont.gif|Continental collision of two continental plates to form a collisional orogen. Typically, continental crust is subducted to lithospheric depths for blueschist to eclogite facies metamorphism, and then exhumed along the same subduction channel. (example: the Himalayas) Orogenic belts are associated with subduction zones, which consume crust, thicken lithosphere, produce earthquake and volcanoes, and often build island arcs. These island arcs may be added to a continental margin during an accretionary orogeny. The orogeny may culminate with continental crust from the opposite side of the subducting oceanic plate arriving at the subduction zone. This ends subduction and transforms the accretional orogeny into a collisional orogeny. The collisional orogeny may produce extremely high mountains, as has been taking place in the Himalayas for the last 65 million years. File:Pacific Ring of Fire.png|Circum-Pacific orogenic belt (Pacific Ring of Fire) File:Alpiner Gebirgsgürtel.png|Alpine-Himalayan orogenic belt Prominent orogenic belts on the Earth are the circum-Pacific orogenic belt (the Pacific Ring of Fire) and the Alpine-Himalayan orogenic belt. Since these orogenic belts are young, they form large mountain ranges; crustal activity is active and accompanied by volcanic belts and seismic belts. ==External links==
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