1948 Ashgabat earthquake in the context of Surface-wave magnitude


1948 Ashgabat earthquake in the context of Surface-wave magnitude

⭐ Core Definition: 1948 Ashgabat earthquake

The 1948 Ashgabat earthquake was on 6 October with a surface-wave magnitude of 7.3 and a maximum Mercalli intensity of X (Extreme), in Turkmenistan near Ashgabat. Due to censorship by the Soviet government, the event was not widely reported in the Soviet media. Historians tend to agree that the ban on reporting the extent of the casualties and damage did not allow the Soviet government to allocate enough financial resources to respond adequately. It was the strongest earthquake recorded in Turkmenistan.

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1948 Ashgabat earthquake in the context of Ashgabat

Ashgabat is the capital and largest city of Turkmenistan. It lies between the Karakum Desert and the Kopetdag mountain range in Central Asia, approximately 50 km (30 mi) away from the Iran-Turkmenistan border. The city has a population of 1,030,063 (2022 census).

The city was founded in 1881 on the basis of an Ahal Teke tribal village, and made the capital of the Turkmen Soviet Socialist Republic in 1924 when it was known as Poltoratsk. Much of the city was destroyed by the 1948 Ashgabat earthquake, but has since been extensively rebuilt under the rule of Saparmurat Niyazov's "White City" urban renewal project, resulting in monumental projects sheathed in costly white marble. The Soviet-era Karakum Canal runs through the city, carrying waters from the Amu Darya from east to west.

View the full Wikipedia page for Ashgabat
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