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JOURNALS // Fizika Goreniya i Vzryva // Archive

Fizika Goreniya i Vzryva, 1998 Volume 34, Issue 1, Pages 120–122 (Mi fgv2433)

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Hypothesis on the nature of the Tunguska meterorite

Yu. A. Nikolaev

Lavrentyev Institute of Hydrodynamics of Siberian Branch of the Russian Academy of Sciences, 630090, Novosibirsk

Abstract: It is shown that all the specific features of the Tunguska catastrophe in 1908 can be explained by an explosion of a methane-air cloud which was initiated by a stony or iron meteorite whose mass was of the order of several tens of tons. The meteorite gently flied at an altitude of several kilometers with a velocity of 1–2 km/sec. A single ejection of 200 ktons of methane into the atmosphere is sufficient to form such a cloud. The meteorite fell several tens of kilometers from the epicenter of the explosion.

UDC: 523.07+523.261

Received: 14.11.1997


 English version:
Combustion, Explosion and Shock Waves, 1998, 34:1, 109–111

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