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An expert panel chaired by senior geoscientist John Matthai of the National Centre for Geosciences (NCG) appointed by the State Disaster Management Authority (SDMA) visited the villages in the impacted area and reported that an uphill heavy rainfall–induced "Dam burst effect" caused the landslide that destroyed the three villages.
A slide is the movement of a body of material that generally remains intact while moving over one or several inclined surfaces or thin layers of material (also called shear zones) in which large deformations are concentrated. Slides are also sub-classified by the form of the surface(s) or shear zone(s) on which movement happens.
The FEMA Photo Library (now FEMA Media Library) was an online gallery of photos compiled by the Federal Emergency Management Agency (FEMA) of the United States, containing more than 52,000 disaster related photographs taken since 1980. [1]
Some Wikipedians have formed a project to better organize information in articles related to Disaster Management (a.k.a. Emergency management). We have three main work areas: Theoretical and background information, including the phrases: Mitigation, Preparedness, Response, and Recovery. This section also covers methods for managing disasters.
The disaster was characterized by over 29 cm of rainfall in a single day, which overwhelmed the Krishna River and Budameru Rivulet. The flooding caused extensive damage to infrastructure, homes, and agricultural land. [2] The extreme rainfall caused catastrophic flooding, severely damaging infrastructure, homes, and agricultural land.
The three Storegga Slides (Norwegian: Storeggaraset) are amongst the largest known submarine landslides. They occurred at the edge of Norway's continental shelf in the Norwegian Sea , approximately 6225–6170 BCE .
The government of Sikkim declared the flood a disaster, and the Indian central government released ₹48 crore ($5.76 million) in disaster relief funds. [a] [10] [13] Additionally, the state government announced an ex-gratia compensation of ₹4 lakh ($4804) to the families of those who died, as well as an immediate payment of ₹2,000 ($24) to those in relief camps. [14]
Although the initial slide lasted only about three minutes, [3] a second debris flow occurred on top of the initial slide, followed by a further collapse of the downslope face of the slide. [6] Smaller landslides and slope failures continued for several weeks after the disaster, bringing the total volume of collapsed material to 71.2 million yd ...
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