| 1971 Bingöl earthquake | |
| Timestamp: | 1971-05-22 16:44:02 |
| Isc-Event: | 784837 |
| Anss-Url: | iscgem784837 |
| Local-Time: | 18:44:02 |
| Magnitude: | , |
| Depth: | NaNkm (-2,147,483,648miles) |
| Location: | 38.93°N 40.65°W |
| Damages: | $US 5 million |
| Foreshocks: | Yes |
| Aftershocks: | Yes |
| Casualties: | 755–1,000 killed, 1,200-1500 injured |
The 1971 Bingöl earthquake was a earthquake that occurred at on 22 May. It had a surface-wave magnitude of 6.9 and a maximum intensity of IX (Violent) on the Mercalli intensity scale, killing 755–1,000 people. Bingöl was largely destroyed, as well as many houses in the nearby Bingöl plain. Surface displacement of and various other surficial effects were directly caused by the earthquake.
Most of Turkey lies on the Anatolian Plate. Movement of the plate is accommodated through four main faults: the Aegean extensional system (AES), the Cyprus Arc, the North Anatolian Fault (NAF), the East Anatolian Fault (EAF). The AES accommodates extensional forces between the Anatolian and Aegean Sea Plates, and the Cyprus Arc accommodates convergence in the south between the African Plate and the Anatolian Plate. In the north, the NAF accommodates the faulting between the Eurasian Plate and the Anatolian plate and has produced prolific earthquakes such as the 1939 Erzincan earthquake. In the east, the Arabian Plate and the Eurasian Plate grind past each other, forming the EAF, the fault responsible for this earthquake. The EAF is a left-lateral strike slip fault which extends for and slips at a decreasing rate from east to west of per year.
The earthquake struck near the city of Bingöl, Turkey at 18:44:02 local time. It was assigned a maximum Mercalli intensity of IX. Various seismic observatories reported different focal depths but it is agreed to be very shallow. The estimates are between 3km (02miles) and 10km (10miles). The focal mechanism showed left lateral strike-slip faulting, consistent with faulting along the East Anatolian Fault. Small foreshocks were strongly felt locally, and two magnitude 5.1 aftershocks were felt on the day of the mainshock. Aftershocks continued to be felt for a couple months after the mainshock. The mainshock ruptured along a × area of the East Anatolian Fault. A second rupture area measuring × was detected to the northeast. The two rupture areas produced maximum slips of and, respectively. Minimal vertical displacement of was also found in parts of the southwestern portion of the rupture. Surface faulting was visible from Ormanardı in the southwest to Çobantaşı in the northeast over a distance of .
The earthquake killed at least 755 people and injured another 1,200–1500. Rubble masonry and reinforced concrete houses alike were severely damaged in the Bingöl plain. In Bingöl, 90 percent of buildings were destroyed, including the prison and hospital. Bridges crossing the Göynük and Murat rivers were closed to traffic due to damage caused by surficial effects of the earthquake. The total cost of damage was estimated at US$5 million. Sand boils formed at some ground cracks, and landslides and rockfalls were also observed. At least two people were killed in Palu, a town some west of Bingöl.[1] About half of the 800 reported deaths came from villages outside Bingöl.
In response to the disaster, officials deployed a field hospital and 10 medical personnel from Elazig. In Erzurum, 1,500 tents were sent to the affected area. On 23 May, the governor of Elazig said the Eighth Army Corps mobilised doctors and a convoy to Bingöl. Officials brought mobile kitchens, tents, food and water. The Turkish Red Crescent said it received offer for assistance from the League of Red Cross Societies and Iran to which they said was not needed. Prime minister Nihat Erim, who visited Bingöl with the health, construction and interior ministers, said most people in the area lived in sun-dried brick homes, incapable of withstanding earthquakes.