Aug 17 Izmit Earthquake of The Izmit earthquake occurred at Previous aftershocks of this size were centered to the east of the mainshock, further from the cities of Bursa and Istanbul. Geological Society of America Today.
See Article History Alternative Titles: The hypocentre of the shock was at a depth of 17 km, approximately half way down to Moho. Seismic Record of the Izmit Earthquake with an unusually strong second shock.
Particularly in the last few decades, we have gained a much better understanding of earthquakes, chiefly owing to the concept of Plate Tectonics. The remarkable series of earthquakes along the North Anatolian fault, as well as the San Andreas fault, provide an ideal data set to further our understanding of earthquakes, with implications for forecasting and mitigating the effects of future ones.
Another large city badly affected by the earthquake is Adapazari, which is located North-East from the Sapanca Lake. The course of the fault between the Sapanca Lake and the Izmit Bay can also be easily identified in the center of the image. This location indicates that the earthquake occurred on the northernmost strand of the North Anatolian fault system.
See Article History Alternative Titles: Aircraft dropped chemical flame retardant on the blaze, which threatened to consume the entire facility. Note that the epicentre was very close to Izmit Bay. Because of their overwhelming power and the damage that they cause, men have been studying them for centuries.
The source of this shock is calculated to be equivalent to 7, Kilotons of TNT, which is close to of the atom bombs dropped over Hiroshima in Coruh, C. Turkey hit by huge earthquake The most powerful earthquake to hit Turkey has left at least 1, people dead.
It is remarkable that the epicentres of earthquakes during the 10th century were moving from west to east, while the direction appears to be reversed this century, from east to west Fig.
USGS ShakeMap showing the intensity of the event The following table shows the breakdown of rescue teams by country in the affected locations: The hypocentre of the shock was at a depth of 17 km, approximately half way down to Moho.
Note the two digit numbers annotated in the figure refer to the year of the earthquake. These motions are thought to be accommodated by lateral slips on the North and East Anatolian faults. Monitoring and studying GPS results is extremely important for earthquake prediction.
Rupture proceeded from west to east in two subevents.
The images show that in many of the areas that have been affected by the earthquake there were high levels of interferometric coherence.
Learn More in these related Britannica articles:Among these earlier earthquakes, the earthquake is perhaps most similar in magnitude and location to the earthquake, although it may have occurred closer to Istanbul.
The remaining two earthquakes, in andprobably occurred in the area between eastern part of the Gulf of Izmit. The August 17, Izmit (Kocaeli) earthquake is the largest earthquake of the 20th century that struck the Northwestern Turkey.
It hit a densely populated area while most of the people were asleep. The İzmit earthquake (also known as the Kocaeli, Gölcük, or Marmara earthquake) occurred on 17 August at local time in northwestern Turkey.
The shock had a moment magnitude of and a maximum Mercalli intensity of IX (Violent). Earthquake Kocaeli, Turkey, The moment magnitude (M W) Kocaeli, Turkey, earthquake struck the Kocaeli province of northwestern Turkey on Tuesday, August 17,at a.m.
local time. The cause of the earthquake was the sudden breakage, or rupture, of the Earth's crust along a western branch of the 1,km-long North Anatolian.
The August 17, Izmit (Kocaeli) earthquake is the largest earthquake of the 20th century that struck the Northwestern Turkey. It hit a densely populated area while most of the people were asleep. Aug 18, · Similar scenes played out in many places as the earthquake wielded a fearsome power across a wide swath of Turkey, including highly populated areas like Istanbul, with 12 million people, and Izmit.Download