- Lechatelierite
Lechatelierite is
silica glass,amorphous SiO2. One common way in which lechatelierite forms naturally is by very high temperature melting ofquartz sand during alightning strike. The result is an irregular, branching, often foamy hollow tube of silica glass called afulgurite .Lechatelierite also forms as the result of high pressure shock
metamorphism duringmeteorite impact cratering and is a common component of a type of glassyejecta calledtektite s. Most tektites are blobs of impure glassy material, but tektites from the Sahara Desert inLibya andEgypt , known as "Libyan desert glass ", are composed of almost pure silica, that is almost pure lechatelierite. High pressure experiments have shown that shock pressures of 85 GPa are needed to produce lechatelierite in quartz grains embedded ingranite . [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1671.pdf]Lechatelierite was formed during the impact of a
meteorite into a layer ofCoconino Sandstone atMeteor Crater inArizona . It was puffed up to more than twice its size by steam and can now float on water. [ [http://www.amnh.org/exhibitions/permanent/meteorites/impacts/crater.php METEOR CRATER: PROOF OF IMPACT - amnh.org] ]Lechatelierite may also form artificially, a unique example being the "
trinitite " produced by melting of quartz sand at the first nuclear bomb explosion at Trinity Flats,White Sands, New Mexico .Lechatelierite is a
mineraloid as it does not have acrystal structure . Although not a true mineral, it is often classified in the quartz mineral group.References
* [http://mineral.galleries.com/minerals/mineralo/lechatel/lechatel.htm Mineral Galleries] retrieved June 4, 2005.
* [http://webmineral.com/data/Lechatelierite.shtml Webmineral] retrieved June 4, 2005.
* [http://www.lpi.usra.edu/meetings/LPSC98/pdf/1671.pdf C. Schrand and A. Deutsch, 1998, "FORMATION OF LECHATELIERITE AND IMPACT MELT GLASSES IN EXPERIMETALLY SHOCKED ROCKS"] , Lunar and Planetary Science XXIX 1671.pdf retrieved June 4, 2005.
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