AKA:
A.D. 1908 Big Bang in Tunguska
Synopsis:
The Tunguska event, or Tunguska blast or Tunguska explosion, was an
enormously powerful explosion that occurred near the Podkamennaya
Tunguska River in what is now Krasnoyarsk Krai, Russia, at about 7:14
a.m. KRAT (0:14 UT) on June 30 [O.S. June 17, 1908.
The
explosion is believed to have been caused by the air burst of a large
meteoroid or comet fragment at an altitude of 5--10 kilometres (3--6 mi)
above the Earth's surface. Different studies have yielded varying
estimates of the object's size, with general agreement that it was a few
tens of metres across.
The number of scholarly publications on the
problem of the Tunguska explosion since 1908 may be estimated at about
1,000 (mainly in Russian). Many scientists have participated in Tunguska
studies, the best-known of them being Leonid Kulik, Yevgeny Krinov,
Kirill Florensky, Nikolai Vladimirovich Vasiliev and Wilhelm Fast.
Although
the meteoroid or comet burst in the air rather than hitting the
surface, this event is still referred to as an impact. Estimates of the
energy of the blast range from 5 to as high as 30 megatons of TNT
(21--130 PJ), with 10--15 megatons of TNT (42--63 PJ) the most
likely—roughly equal to the United States' Castle Bravo thermonuclear
bomb tested on March 1, 1954, about 1,000 times more powerful than the
atomic bomb dropped on Hiroshima, Japan, and about one-third the power
of the Tsar Bomba, the largest nuclear weapon ever detonated. The
explosion knocked over an estimated 80 million trees covering 2,150
square kilometres (830 sq mi). It is estimated that the shock wave from
the blast would have measured 5.0 on the Richter scale. An explosion of
this magnitude is capable of destroying a large metropolitan area. This
possibility has helped to spark discussion of asteroid deflection
strategies.
The Tunguska event is the largest impact event over land
in Earth's recent history. Impacts of similar size over remote ocean
areas would most likely have gone unnoticed before the advent of global
satellite monitoring in the 1960s and 1970s
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