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856 Damghan earthquake
The 856 Damghan earthquake or the 856 Qumis earthquake occurred on 22 December, 856 AD (242 A.H.). The earthquake had an estimated magnitude of 7.9, and a maximum intensity of X (''Extreme'') on the Mercalli intensity scale. The meizoseismal area (area of maximum damage) extended for about along the southern edge of the eastern Alborz mountains of present-day Iran including parts of Tabaristan and Gorgan. The earthquake's epicenter is estimated to be close to the city of Damghan, which was then the capital of the Persian province of Qumis. It caused approximately 200,000 deaths and is listed by the USGS as the sixth deadliest earthquake in recorded history.
==Tectonic setting==
Iran lies within the complex zone of continental collision between the Arabian Plate and the Eurasian Plate, which extends from the Bitlis-Zagros belt in the south to the Greater Caucasus mountains, the Apsheron-Balkan Sill and the Kopet Dag mountains in the north. The epicentral area is located in the Alborz mountain range, in which oblique north-south shortening is accommodated by a combination of thrusting and sinistral (left-lateral) strike-slip faulting.
The main active structure in the Qumis region is the Shahrud fault system, which extends for several hundred km. This zone of overall sinistral strike-slip consists of several fault strands, including the Damghan Fault, Northern Damghan Fault and the Astaneh Fault System, all of which lie within the epicentral area and show evidence of displacement during the Quaternary. The longest of these possible candidates for the source of the 856 earthquake is the 150 km long Astaneh Fault System. Trenching along one of the segments of the Astaneh Fault System has provided evidence of a significant earthquake along the fault that occurred well after 600 BC and before 1300 AD, consistent with the 856 event.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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