1948 Ashgabat earthquake | |
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| Total costs | N/A |
| Deaths | 110000 |
The 1948 Ashgabat earthquake (Turkmen: 1948 Ашгабат ертитремеси, romanized: 1948 Aşgabat ýertitremesi; Russian: Ашхабадское землетрясение 1948 года, romanized: Ashkhabadskoye zemletryasenie 1948 goda) 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 USSR's 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 adequately respond. It was the strongest earthquake recorded in Turkmenistan.
Source: Wikipedia 1164 St. Juliana Flood | |
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| Total costs | N/A |
| Deaths | 10000 |
Storm tides of the North Sea are coastal floods associated with extratropical cyclones crossing over the North Sea, the severity of which are affected by the shallowness of the sea and the orientation of the shoreline relative to the storm's path, as well as the timing of tides. The water level can rise to more than 5 metres (17 ft) above the normal tide as a result of storm tides. Northern Germany and Denmark are particularly susceptible to storm tides. The coastline of the German Bight forms an L-shape facing northwest. Also vulnerable are the United Kingdom and the Netherlands, where the sea shallows and is funnelled toward the English Channel. Storm tides are a regular occurrence in the North Sea basin; several form each year. Although most do not cause significant damage, the impact of some has been devastating. During one, the February flood of 1825, the Danish coastline changed, as the North Jutlandic Island became separated from the Jutland Peninsula.
Source: WikipediaThe years before 1890 featured the pre-1890 North Indian Ocean cyclone seasons. Each season was...
The kamikaze (Japanese: 神風, lit. 'divine wind') were two winds or storms that are said to have...
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