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  1. en.wikipedia.org › wiki › Gharm_OblastGharm Oblast - Wikipedia

    The Gharm Oblast (Russian: Гармская область; Tajik: Вилояти Ғарм, romanized: Viloyati Ğarm/Vilojati Ƣarm; Persian: ولایت غرم, Velâyate Qarm) was an oblast in the Tajik Soviet Socialist Republic in the Soviet Union from the 1920s to 1955. Its capital was Gharm.

  2. en.wikipedia.org › wiki › GharmGharm - Wikipedia

    Gharm (Tajik: Ғарм, tr. Gharm; Russian: Гарм, tr. Garm; Persian: غرم, tr. Gharm) is a city and jamoat in the Rasht Valley area of central Tajikistan. The population of the town is 9,800 (January 2020 estimate).

    • Tectonic Setting
    • Damage
    • Characteristics
    • See Also

    The earthquake occurred in a tectonically complex region at the southern edge of the Tien Shan. The southern margin of the Tien Shan is characterised by combination of dextral strike-slip faulting and southward thrusting over the Tajik Basin to the south along the Gissar-Kokshaal fault zone. At the same time the Tajik Basin is being shortened in re...

    In the area of maximum felt intensity (>IX) most kishlaks were completely destroyed. Most of the fatalities were caused by numerous landslides triggered by the earthquake. The town of Khait (modern spelling Hoit (Tajik: Ҳоит)) and the village of Khisorak were almost completely destroyed by the Khait landslide. Numerous kishlaks in the Yasman River ...

    Earthquake

    The main shock was preceded by two foreshocks (M5.1 and M5.6) on 8 July, just 12 minutes apart. The main shock had a magnitude of 7.4 calculated as the 'unified magnitude' using the 'Soviet Method'. The magnitude was recalculated as 7.5 on the moment magnitude scale in the ISC-GEM cataloguepublished in 2013.

    Landslides

    Most of the landslides triggered by the earthquake were loess flowslides, involving failure and flow of unconsolidated loess material. In the Yasman River valley, which lies almost entirely within the area of greatest felt intensity, a large number of such flowslides coalesced in tributary valleys before combining into one massive flowslide that travelled the length of the valley. The area covered by the Yasman valley slide is about 24.4 km2, with a total estimated volume of 245 MCM (million...

  3. The Khait or Hoit landslide occurred on July 10, 1949 in the Hoit district in the Gharm Oblast in the Tajikistan, then part of the Soviet Union. The landslide was triggered by the 1949 Khait earthquake and buried 33 villages and has by some estimates killed 28,000 people.

  4. Gharm is a city and jamoat in the Rasht Valley area of central Tajikistan. The population of the town is 9,800. From the 1920s until 1955 there was a Gharm Oblast in Tajikistan, which included the territory of the current Gharm Valley.

  5. The Gharm Oblast (Russian: Гармская область; Tajik: Вилояти Ғарм, romanized: Viloyati Ğarm/Vilojati Ƣarm; Persian: ولایت غرم, Velâyate Qarm) was an oblast in the Tajik Soviet Socialist Republic in the Soviet Union from the 1920s to 1955. Its capital was Gharm.

  6. The Gharm Oblast was an oblast in the Tajik Soviet Socialist Republic in the Soviet Union from the 1920s to 1955. Its capital was Gharm. The population of Gharm were known as Gharmis, a term still used in Tajikistan today. History