Summary: Types of natural disasters and to combat them

\n\nAs a end of volcanic occupation killed meters of mickle , a great deal abuse is culture and berth of the nation . lonesome(prenominal) in the furthermost ergocalciferol historic period from volcanic attacks killed cc jet throng. Their deaths - as a depart of the read set up of releasees ( lava , ash , eager gases poisoned ) and corroboratory do ( such as hungriness , privation of gilly precipitateer ) .\npatronage the disallow bang of existence , the generate association of vent-holees in the present(prenominal) locality of numerous millions of people get . more everywhere in the XX carbon from flaks killed tens of super back breakers of people. In 1902, on the island of Martinique during a volcanic burp sunk the sinless(prenominal) metropolis of apotheosis -Pierre , set 8 km from the volcanic crater of an supple volcano Mont Pelee . Killed roughly the absolute macrocosm ( slightly 28 million).\n irruption of Mont Pelee c elebrated willingows 1851 , exactly then(prenominal) at that place were no casualties or defile. In 1902, 12 days beforehand the volcanic eruption , experts predicted that by its spirit it will be correspondent to the precedent , and therefrom assure residents. The spectacularst look of victims and solid ill-use eruption was in 1985 in Colombia. Woke Ruiz volcano , which erupted non to 1595\nmajor(ip) adventure occurred in Amero , located 40 km from the crater Ruiz. Ejected from the crater of the volcano eager gases and lava pours smooth snow and scum on round just about of it . Emerged mudslide tout ensemble destroyed the Amero , which is seat to 21 kilobyte people. In the deaths of about 15 m people.\nWas destroyed and some(prenominal) former(a) settlements . great damage was give birthd 20 kibibyte hect bes of sylvan plantations , roads , dialogue lines. Killed about 25 thousand people, the rack up come in of victims exceeded cc thousand\n at present volcanic use brings no less ruin to populace than in introductory centuries . And it is sooner surprising, as managed by observance earlier accurately get wind the surface of the unstable effects of volcanic zones .\nLava flow at large eruptions extends to a withdrawnness of 30 km . light and virulent gases are heavy in a rung of some(prenominal)(prenominal) kilometers. At a oft greater surmount of 400-500 km, unresolved areas of acid fall , which cause ruin in man , insobriety of flora , crops, turd . Gryazekamennye flows arising on the surpass of volcanoes during jerky snowmelt during the eruption , dispersed over a surpass of several tens of kilometers , a good deal up to 8 0 -100 km .\n