SMALL BODIES
be associated with the asteroid
have ever been found. Even if a sin-
gle crater unequivocally attributa-
ble to the ground impact of an
asteroid is never identified, studies
from a decade ago propose Lake
Cheko, located 8 km north of the
epicenter, as a probable site of fall
of a secondary fragment. This lake,
half a kilometer long and about
300 meters wide, does not seem to
have existed before 1908.
The very approximate knowledge
of the physical parameters of the
asteroid has never allowed for an
accurate description of the dynam-
ics of the Tunguska event; conse-
quently, all the forecasts made in
the past on the possible repetition
of such an occurrence were suspect
S
atellite views
of the vast
area affected by
the transit and
final explosion of
the Tunguska as-
teroid. Vanavara,
North-Northwest
of Lake Baikal,
was in 1908 the
nearest town to
the epicenter.
[Google Maps]
has undergone some significant updates.
The object that exploded in flight had to
be a small rocky asteroid (although the
cometary nucleus hypothesis has not been
entirely ruled out), with an initial diameter
between 30 and 60 meters, which traveled
at least 15 km/s and which produced an en-
ergy of 5 - 20 megatons, exploding at a
height between 5 and 10 km above the
ground. The explosion devastated a sur-
face are of over 2000 km^2 , destroying up-
to 80 million trees. No fragments that could
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