Everything about The Popigai Crater totally explained
The
Popigai crater in
Siberia,
Russia is tied with
Manicouagan Reservoir as the 4th largest
impact crater on
Earth. A large
bolide impact created the 100-kilometer diameter crater about 35
million years ago during the late
Eocene epoch.
The Popigai impact crater was possibly simultaneous with the
Chesapeake Bay and
Toms Canyon impacts, but evidence varies. For decades the Popigai crater has fascinated paleontologists and
geologists, but the entire area has been off limits because of the diamonds and the mines constructed by
gulag prisoners under
Stalin.
The impactor in this event has been identified as either an eight-kilometer diameter
chondrite asteroid, or a five-kilometer diameter stony asteroid.
The shock pressures from the impact instantaneously transformed
graphite in the ground into
diamonds within a 13.6 kilometer radius of ground zero. No exact count nor measure of
caratage has been made available, but it's estimated that this one impact formed more diamonds than have been formed by the Earth's own processes.
Popigai is the best example yet of the formation of a crater of this type. Three other craters are larger, but they're either buried (
Chicxulub), strongly deformed (
Sudbury), or deformed and severely eroded (
Vredefort).
The crater is just north of the Siberian city
Norilsk, or 1 1/2 hours (by helicopter) from the outpost of
Khatanga.
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