Lechatelierite
From Wikipedia, the free encyclopedia
Lechatelierite is silica glass, amorphous SiO2. One common way in which lechatelierite forms naturally is by very high temperature melting of quartz sand during a lightning strike. The result is an irregular, branching, often hollow tube of silica glass called a fulgurite.
Lechatelierite also forms as the result of high pressure shock metamorphism during meteorite impact cratering and is a common component of a type of glassy ejecta called tektites. Most tektites are blobs of impure glassy material, but tektites from the Sahara Desert in Libya and Egypt, 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 in granite. [1]
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 a crystal structure. Although not a true mineral, it is often classified in the quartz mineral group.
[edit] References
- Mineral Galleries retrieved June 4, 2005.
- Webmineral retrieved June 4, 2005.
- 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.
|
||||||||||||||||||||||||||||
 |
This article about a specific mineral or mineraloid is a stub. You can help Wikipedia by expanding it. |
