Floods

Why The Flood Happened. The North sea, between Britain and northern nuclear number 63 has a long autobiography of fountain disasters. combined effect of coerce surge and high soars tide of 31 Jan 1953 was a full moon leaping tide, orgasm the equinox tide rooceante higher than expected because of atmospheric pressing and wind intense stamp moving from the Atlantic, turning southeasterly east to the North Sea i of the most vehement and prolonged northerly gales in British meteorological history tidal surge developed and moved take garbage down east coast tide 8-9 ft above predicted trains - fervor of clinical depression sucks the sea to its centre surge of 31 Jan 1953 took 11 hours to travel from Aberdeen to the Thames estuary, construct progressively It happened in the night or early morning, February 1st, 1953. A north-western storm was blowing and it was to be spring tide. At low tide the water system level at sea was as high as it is ordinarily when it is high tide.

Then the wind pushed the water up to organise even higher and the sea reached a disc round top of 4, 5 meter above mean sea level. In The Netherlands the dikes were breached at many places in the provinces along the south-western coast. Sea water covered large areas. Near the breaches houses were ruined by the take of the water rushing in. Many people were caught unawares, thither was no warning system and people were sleeping. In the send by there were 1.800 victims. About 72.000 people had to be evacuated. Roads were destruct and telephone lines were down. In large areas relief could on ly be brought by boat. Many cattle died, cro! ps failed, buildings were ruined.If you want to get a full essay, order it on our website: OrderCustomPaper.com

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