UTC time | 1914-10-03 22:07:07 |
---|---|
ISC event | 914008 |
USGS-ANSS | ComCat |
Local date | October 4, 1914 |
Local time | 00:07 |
Magnitude | 7.0 Ms [1] |
Epicenter | 37°49′N30°16′E / 37.82°N 30.27°E |
Areas affected | Ottoman Empire |
Max. intensity | MMI IX (Violent) [2] |
Casualties | 2,344 [3] |
The 1914 Burdur earthquake (also called the Afyon-Bolvadin earthquake) occurred at 00:07 local time (22:07 UTC) 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, [1] and caused 2,344 casualties.
The earthquake, along with several others in 1959 and 1971, occurred along the Fethiye-Burdur fault zone, a parallel and discontinuous series of fault segments. [4] No unambiguous fault displacement has been found that is related to the event, but a 23 km (14 mi) portion of the southeast coast of Lake Burdur experienced subsidence of up to 150 centimeters (59 in) and this may indicate that the event was due to normal faulting with a strike of N45°E. [1]
In Burdur nearly all homes were destroyed along with other significant and historical monuments. Kilinc was destroyed and in Keciborlu around 85 percent of the houses were lost. In the city of Isparta the great Mosque was destroyed along with more than half of the homes. Other villages were also impacted as far as 60 kilometers (37 mi) from the epicenter. [1]
The 1857 Fort Tejon earthquake occurred at about 8:20 a.m. on January 9 in central and Southern California. One of the largest recorded earthquakes in the United States, with an estimated moment magnitude of 7.9, it ruptured the southern part of the San Andreas Fault for a length of about 225 miles, between Parkfield and Wrightwood.
The 1953 Yenice–Gönen earthquake occurred at 21:06 local time (19:06 UTC on 18 March in the province of Çanakkale and Balıkesir in the Marmara Region at western Turkey. It had a surface-wave magnitude of 7.5 and a maximum felt intensity of IX on the Mercalli intensity scale. It caused widespread damage, killing 1,070 and causing damage that was estimated at US$3,570,000 repair value.
The 1918 Shantou earthquake occurred in Shantou, Guangdong, Republic of China. Serious damage and high casualty numbers were reported in Guangdong and the surrounding provinces. It also caused some damage in British Hong Kong.
The 1930 Salmas earthquake occurred on May 7 at 01:34:26 IRST in West Azerbaijan Province, Iran. The earthquake, which was among Iran's largest, measured 7.1 on the moment magnitude scale and had a maximum Mercalli intensity of IX (Violent). A damaging foreshock occurred fifteen hours prior to the main event and served as a warning to the people that felt it strongly. Reports from seismologists and seismological organizations indicate that up to 3,000 fatalities may have occurred in northwest Iran and southeast Turkey.
The 1975 Lice earthquake struck the Turkish district of Lice at 12:20 local time on 6 September. The epicenter of the Ms 6.7 shock was located near the town of Lice and the maximum felt intensity was VIII (Severe) on the Mercalli intensity scale. More than 2,300 people were killed.
The 1944 Bolu–Gerede earthquake occurred at 05:22 local time on 1 February. The earthquake had an estimated magnitude of 7.5 Mw 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 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 1967 Mudurnu earthquake or more correctly, the 1967 Mudurnu Valley earthquake occurred at about 18:57 local time on 22 July near Mudurnu, Bolu Province, north-western Turkey. The magnitude 7.4 Mw earthquake was one of a series of major and intermediate quakes that have occurred in modern times along the North Anatolian Fault since 1939.
The 1971 Bingöl earthquake was a Mw6.6–6.7 earthquake that occurred at 18:44:02 local time 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 38 km (24 mi) and various other surficial effects were directly caused by 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 1,340 people have died and 50 settlements in the provinces of Erzurum and Kars have been demolished by the earthquake.
The 1912 Mürefte earthquake occurred at 03:29 local time on 9 August. It had an estimated magnitude of 7.4 Mw and a maximum intensity of X (Extreme) on the Modified Mercalli intensity scale, causing from 216 to 3,000 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.
The 1901 Black Sea earthquakewas a 7.2 magnitude earthquake, the most powerful earthquake ever recorded in the Black Sea. The earthquake epicenter was located in the east of Cape Kaliakra, 30 kilometres (19 mi) off northeast coast of Bulgaria. The mainshock occurred at a depth of 15 km (9.3 mi) and generated a 4–5-metre (13–16 ft) high tsunami that devastated the coastal areas of Romania and Bulgaria. In Romania, the earthquake was felt not only throughout Northern Dobruja, but also in Oltenia and Muntenia, and even in southern Moldova.
The first of the 1957 Fethiye earthquakes occurred on April 24, 1957, with the second and larger event about seven hours later on the following day. Both earthquakes had epicentres in the eastern Mediterranean between Rhodes and the coastal city of Fethiye in Muğla Province, southwestern Turkey.
The Afyon Province of western Turkey was struck by an earthquake measuring 6.5 Mw on 3 February 2002 at 10:11 local time. It had a maximum felt intensity of VIII (Severe) on the Modified Mercalli intensity scale. It damaged hundreds of buildings and caused the deaths of 44 people and a further 318 injuries.
Northern Anatolia was struck by a large earthquake on 17 August 1668 in the late morning. It had an estimated magnitude in the range 7.8–8.0 Ms and the maximum felt intensity was IX on the Modified Mercalli intensity scale. The epicenter of the earthquake was on the southern shore of Ladik Lake. It caused widespread damage from as far west as Bolu and as far east as Erzincan, resulting in about 8,000 deaths. It is thought to be the most powerful earthquake in Turkey.
The 1695 Linfen earthquake struck Shanxi Province in North China, Qing dynasty on May 18. Occurring at a shallow depth within the continental crust, the surface-wave magnitude 7.8 earthquake had a maximum intensity of XI on the China seismic intensity scale and Mercalli intensity scale. This devastating earthquake affected over 120 counties across eight provinces of modern-day China. An estimated 52,600 people died in the earthquake, although the death toll may have been 176,365.
The 1872 Amik (Antakya) earthquake occurred on April 3 with an epicenter within the Amik Valley in the Ottoman Empire. Earthquake had an estimated magnitude of Mw 7.0–7.2 or Ms 7.2 and maximum MSK 64 rating of XI (Catastrophic). Turkey and Syria were devastated by this earthquake, and the region lost at least 1,800 residents.
The 1944 Gulf of Edremit–Ayvacik earthquake occurred on October 6 at 05:34:48 local time in Balıkesir Province, Turkey. It measured 6.7 on the moment magnitude scale (Mw ) and occurred at a depth of 15 km (9 mi). The normal-faulting event had a maximum MSK-64 intensity of IX. A total of 73 people died and 275 others were injured.
The 1893 Malatya earthquake occurred at 02:30 local time on 3 March in Malatya, Eastern Anatolia Region of Turkey. It had a surface wave magnitude of 7.1 and maximum felt intensity of X (Extreme) on the Mercalli intensity scale. This destructive earthquake caused 885 deaths and 164 injuries.