Boğaziçi University, also known as Bosphorus University, is a major research university in Istanbul, Turkey. Its main campus is located on the European side of the Bosphorus strait. It has six faculties and two schools offering undergraduate degrees, and six institutes offering graduate degrees. Traditionally, the language of instruction is English.
The 1855 Bursa earthquake occurred on 28 February, with an estimated magnitude of 7.02±0.64 A devastating precursor quake that took place in Kemalpaşa, a town of Bursa, Turkey caused severe destruction all over Bursa and other neighboring cities. 300 people died and thousands of homes and workplaces were wrecked, and some of the historical monuments and buildings including mosques collapsed. Subsequently, fire spread out in the city, which increased the death toll.
The 1966 Varto earthquake occurred on 19 August with a moment magnitude of 6.8 a maximum Mercalli intensity of IX (Violent). At least 2,394 were killed and up to 1,500 people were injured in the town of Varto in the Muş Province of eastern Turkey.
The 1926 Kars/Leninakan earthquake occurred at 21:59 local time on 22 October 1926 in the border area of Soviet Armenia and eastern Turkey. It had a surface wave magnitude of 6.0 and a maximum felt intensity of IX (Violent) on the Mercalli intensity scale, causing 360 casualties. Many buildings in Leninakan and surrounding villages were destroyed or damaged.
The 1935 Erdek–Marmara Islands earthquake occurred at 4 January on the islands of Marmara and Avşa off Erdek in the Sea of Marmara, Turkey. It had a moment magnitude of 6.4 and a maximum felt intensity of VIII (Severe) on the Mercalli intensity scale, causing 5 deaths and 30 injuries.
The 1938 Kırşehir earthquake occurred at 12:59 local time on 19 April. It had an estimated surface wave magnitude of 6.7 and a maximum intensity of IX (Violent) on the Mercalli intensity scale, causing 224 casualties.
The 1941 Van–Erciş earthquake occurred at 23:53 local time on 10 September. It had an estimated surface wave magnitude of 5.9 and a maximum intensity of VIII (Severe) on the Mercalli intensity scale. The earthquake has caused estimated casualties of between 190 and 430 people and also 600 buildings have collapsed.
The 1942 Niksar–Erbaa earthquake in Turkey occurred at 16:03 local time on 20 December. It had an estimated surface wave magnitude of 7.0 and a maximum felt intensity of IX (Violent) on the Mercalli intensity scale, causing 3,000 casualties.
The 1943 Adapazarı–Hendek earthquake occurred at 17:32 local time on 20 June in Sakarya Province, Turkey. It registered an estimated 6.6 on the surface wave magnitude scale with a maximum intensity of IX (Violent) on the Mercalli intensity scale.
The 1944 Bolu–Gerede earthquake occurred at 05:22 local time on 1 February. The earthquake had an estimated magnitude of 7.5 and a maximum felt intensity of IX–X (Violent–Extreme) on the Mercalli intensity scale. It ruptured part of the North Anatolian Fault, forming part of a progressive sequence of events that generally migrated westwards along the fault zone, starting with the 1939 Erzincan earthquake.
The 1946 Varto–Hınıs earthquake occurred at 05:12:46 local time on 31 May. The earthquake had an estimated moment magnitude of 5.9 and a maximum felt intensity of VIII (Severe) on the Mercalli intensity scale, causing between 800 and 1,300 casualties.
The 1949 Karlıova earthquake occurred at 18:44 UTC on 17 August with an epicenter near Karlıova in Bingöl Province, Eastern Anatolia Region of Turkey. It had an estimated magnitude of 6.7, a maximum felt intensity of X (Extreme) on the Mercalli intensity scale, and caused 320–450 casualties and destroyed 3,500 buildings.
The 1952 Hasankale earthquake occurred at 08:03 local time on 3 January in Hasankale in Erzurum Province, Eastern Anatolia Region of Turkey. The earthquake had an estimated magnitude of 5.8 and a maximum felt intensity of VIII (Severe) on the Mercalli intensity scale, causing 41 casualties. This spot has been the subject of studies due to the amount of earthquakes that occur in Turkey. 17% of earthquakes, globally, occur in this area. This is because the Alpide belt crosses through Turkey. The earthquakes are cause when the plates try to slide past each other on a transform boundary.
The 1957 Abant earthquake occurred at 8:33am on 26 May, in Turkey. The earthquake had an estimated surface wave magnitude of 7.1 and a maximum felt intensity of IX (Violent) on the Mercalli intensity scale, causing 52 fatalities and 101 injuries. Five thousand homes were damaged as a result of the earthquake.
The 1983 Erzurum earthquake occurred in northeastern Turkey on 30 October 1983 at 07:12 local time. It had a moment magnitude of 6.6 and a maximum Mercalli intensity of IX (Violent). Reuters reports that about 1340 people have died and 50 settlements in the provinces of Erzurum and Kars have been demolished by the earthquake.
The 1914 Burdur earthquake occurred at 00:07 local time on 4 October. It was estimated to be 7.0 on the surface wave magnitude scale with a maximum intensity of IX (Violent) on the Mercalli intensity scale. It was centered near Lake Burdur in southwestern Anatolia and the mainshock and subsequent fire destroyed more than 17,000 homes, and caused 2,344 casualties.
The 1912 Mürefte earthquake occurred at 03:29 local time on 9 August. It had an estimated magnitude of 7.4 and a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale, causing from 216–3000 casualties.
The 1859 Erzurum earthquake occurred at 10:30 on 2 June. It had a magnitude of 6.1 and a maximum intensity of IX on the Mercalli intensity scale, causing 15,000 casualties. The earthquake destroyed much of the city of Erzurum.
The 1688 Smyrna earthquake occurred at 11:45 on 10 July. It had an epicenter close to Izmir, Turkey. It had an estimated magnitude of 7.0 , with a maximum felt intensity of X (Extreme) on the Mercalli intensity scale, and caused about 16,000 casualties.
The 1951 Kurşunlu earthquake occurred at 18:33 GMT on 13 August near Kurşunlu, Çankırı Province, Central Anatolia Region, Turkey. The earthquake was one of a series of major and intermediate quakes that have occurred in modern times along the North Anatolian Fault since 1939.
