Английская Википедия:1946 Chatkal earthquake
Шаблон:Short description Шаблон:Infobox earthquake On November 2 of 1946, west Kyrgyzstan (then the Kirghiz Soviet Socialist Republic in the Soviet Union) was struck by a magnitude 7.5–7.6 earthquake, the largest in the republic since 1911.[1] The earthquake's hypocenter is probably located beneath the Tian Shan Mountains, near the border with Uzbekistan and north of Namangan.
The earthquake had a maximum intensity of X (Extreme) on the Mercalli intensity scale, and IX on the MSK scale. This shock rocked the entire country and Tian Shan range. Severe property damage was reported in its aftermath, but the number of deaths and injuries remains unknown. It has been considered one of the most devastating earthquakes in Central Asia.
Two days later, a magnitude 6.9 earthquake struck nearby Turkmenistan, killing 400 people.[2]
Tectonic setting
The Talas-Fergana Fault is a massive Шаблон:Convert intracontinental strike-slip fault running through the Tian Shan Mountains, the largest in Central Asia.[3][4] It has produced several significant earthquakes with magnitude 7.0 or greater in the past 6000 years with recurrence intervals on segments of the fault between 145 and 850 years, and an average of 375 years.[3] Earlier studies and research on this event concluded that the earthquake occurred on a secondary branch of this fault known as the Atoinok Thrust Fault.[5][6]
Effects
Man-made structures within a Шаблон:Convert area around the epicenter were completely destroyed. The villages of Shuduger, Kichitovar, and Chontovar were severely damaged or totally destroyed. Intensity X to VIII was evaluated to occupy an area perpendicular to the Chatkal Range, and parallel to the fault.[7][8] The meizoseismal area, however, was parallel to the Talas-Fergana Fault, indicating most of the seismic energy was released parallel to the fault instead.
Landslides, loams and rockfalls dammed rivers. A rockfall dammed the Naryn river, forming a quake lake. This threatened the small community of Toktogul with a possibility of the rockfall dam breaching, causing a surge.
Surface ruptures up to Шаблон:Convert long and Шаблон:Convert wide fissured the landscape.
The earthquake's strength was also felt in Osh and Tashkent, Uzbekistan where the shaking intensity was VI (Strong) to IV (Light), causing substantial damage to buildings.
Aftershocks
Numerous aftershocks continued throughout the region. The largest included a magnitude 5.5 and 5.4 in 1955 and 1959.[9][10] Another magnitude 5.6 struck near Toktogul Reservoir on October 28, 1971.[11]
See also
References
Шаблон:Reflist Шаблон:Earthquakes in 1946 Шаблон:Earthquakes in Kyrgyzstan
- Английская Википедия
- Страницы с неработающими файловыми ссылками
- 1946 earthquakes
- Earthquakes in Kyrgyzstan
- Earthquakes in Kazakhstan
- Earthquakes in Uzbekistan
- Earthquakes in the Soviet Union
- Earthquakes in Russia
- 1946 in the Soviet Union
- 1946 in Russia
- 1946 disasters in the Soviet Union
- Страницы, где используется шаблон "Навигационная таблица/Телепорт"
- Страницы с телепортом
- Википедия
- Статья из Википедии
- Статья из Английской Википедии
.png){kind=link}