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 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.
Earthquake characteristics
Aftershocks affected the area for several years, probably including a damaging earthquake in western Khurasan.
Damage
The area of significant damage extended along the Alborz for about, including the towns of Ahevanu, Astan, Tash, Bastam and Shahrud, with almost all the villages in the area severely damaged. Hecatompylos, now called Šahr-e Qumis, the former capital of Parthian Empire, was destroyed. Half of Damghan and a third of the town of Bustam were also destroyed. The earthquake badly affected water supplies in the Qumis area, partly due to springs and qanats drying up, but also because of landslides damming streams. The total death toll for the earthquake is reported as 200,000, with 45,096 casualties in Damghan alone.
Aftermath
Šahr-e Qumis was so badly damaged that it appears to have been abandoned following the earthquake. The effects of the earthquake were still visible in the area between Bastam and Damghan many years later.
From the results of trenching at a single site along the Astaneh Fault a repeat period of about 3,700 years has been estimated and no large earthquakes have been recorded in the Damghan area since 856. However, further trenching studies are needed to establish whether the entire length of the fault is typically involved in a rupture event, or whether shorter segments may be responsible for smaller earthquakes with a shorter recurrence period.
