Popigai impact structure
![](http://upload.wikimedia.org/wikipedia/commons/thumb/5/53/Popigai_crater_russia.jpg/250px-Popigai_crater_russia.jpg)
The Popigai crater in Siberia, Russia is tied with Manicouagan Crater as the seventh largest verified impact crater on Earth.[1][2] A large bolide impact created the 100 kilometres (62 mi)* diameter crater 35.7 ± 0.2 (2σ) million years ago during the late Eocene (Priabonian stage).[3][4] The crater is 1½ hours (by helicopter) from the outpost of Khatanga. It is designated by UNESCO as a Geopark, a site of special geological heritage.[5]
Popigai is the best example yet of the formation of a crater of this type. Six other craters are larger; some are either buried (Chicxulub), strongly deformed (Sudbury), or deformed and severely eroded (Vredefort).
There is a small possibility that Popigai impact crater formed simultaneous with the approximately 35 million year old Chesapeake Bay and Toms Canyon impact craters.[3]
For decades the Popigai crater has fascinated paleontologists and geologists, but the entire area was completely off limits because of the diamonds and the mines constructed by gulag prisoners under Stalin; however, a major investigatory expedition was undertaken in 1997 (IPEX 1997) which greatly advanced understanding of the enigmatic structure.[5] The impactor in this event has been identified as either an 8 km (5.0 mi) diameter chondrite asteroid, or a 5 km (3.1 mi) diameter stony asteroid.
The shock pressures from the impact instantaneously transformed graphite in the ground into diamonds within a 13.6 km (8.5 mi) radius of the impact point. Diamonds are usually 0.5 to 2 mm (0.020 to 0.079 in) in diameter; a few exceptional specimens are 10 mm (0.39 in) in size. The diamonds not only inherit the tabular shape of the original graphite grains but they additionally preserve the original crystal's delicate striations.[5]
Diamond mines
In September 2012, Russia officially stated there are massive diamond reserves under the crater containing "trillions of carats" (hundreds of thousands of tons) and claimed there are enough diamonds in the field to supply global requirements for 3,000 years. This could alter the market for industrial diamonds, presumably by making them more plentiful and lower cost. The diamonds are estimated to be worth around $1,000,000,000,000,000 (or one quadrillion dollars). [6] Many of the diamonds at Popigai contain crystalline lonsdaleite, an allotrope of carbon that has a hexagonal lattice. [7] These stones are 58% harder than ordinary diamonds if pure. [8] The diamonds also "contain unusual abrasive features and large grain size" which could make them extremely useful for industrial and scientific applications.
These types of diamonds are known as "impact diamonds" because they are thought to be produced when a meteorite strikes a graphite deposit at high velocity.[7]
References
- ^ "Popigai". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2008-12-30.
- ^ Masaitis, Victor L. (2003). Popigai Crater: General Geology. Springer. pp. 81–85. ISBN 978-3-540-43517-4.
- ^ a b Deutsch, Alexander (2006). "Establishing the link between the Chesapeake Bay impact structure and the North American tektite strewn field: The Sr-Nd isotopic evidence". Meteoritics & Planetary Science. 41 (5): 689–703. Bibcode:2006M&PS...41..689D. doi:10.1111/j.1945-5100.2006.tb00985.x. Retrieved 2008-06-16.
{{cite journal}}
: Check|url=
value (help); Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Armstrong, Richard (2003). U-Pb Analysis of zircons from the Popigai impact structure, Russia: First Results. Springer. pp. 99–116. ISBN 978-3-540-43517-4.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ a b c Deutsch, Alexander (2000). "Popigai, Siberia—well preserved giant impact structure, national treasury, and world's geological heritage" (PDF). Episodes. 23 (1): 3–12. Retrieved 2008-06-16.
{{cite journal}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help) - ^ Christian Science Monitor article of September 17, 2012
- ^ a b "Russia declassifies deposit of impact diamonds". ITAR-TASS. 17 September 2012. Retrieved 17 September 2012.
- ^ Pan, Zicheng; Sun, Hong; Zhang, Yi; and Chen, Changfeng (2009). "Harder than Diamond: Superior Indentation Strength of Wurtzite BN and Lonsdaleite". Physical Review Letters. 102 (5): 055503. Bibcode:2009PhRvL.102e5503P. doi:10.1103/PhysRevLett.102.055503. PMID 19257519.
{{cite journal}}
: Unknown parameter|laydate=
ignored (help); Unknown parameter|laysource=
ignored (help); Unknown parameter|laysummary=
ignored (help)CS1 maint: multiple names: authors list (link)