Gaylussite
| Gaylussite | |
|---|---|
efflorescent | |
| References | [2][3][4] |
Gaylussite is a
monoclinic prismatic crystals. It is an unstable mineral which dehydrates in dry air and decomposes in water.[2]
Discovery and occurrence
It is formed as an evaporite from alkali lacustrine waters. It also occurs rarely as veinlets in alkalic igneous rocks.[2] It was first described in 1826 for an occurrence in Lagunillas, Mérida, Venezuela. It was named for French chemist Joseph Louis Gay-Lussac (1778–1850).[3]
The mineral has been recently (2014) reported from drill core in
meteor impact during the Pleistocene Epoch[5] and it is one of only four known hyper-velocity impact craters in basaltic rock anywhere on Earth.[6][7]
References
- S2CID 235729616.
- ^ a b c Handbook of Mineralogy
- ^ a b Mindat
- ^ Webmineral
- ^ "Geology". Government of Maharashtra. Gazetteers Department. Retrieved 2008-09-08.
- ^ Deshpande, Rashmi (3 December 2014). "The Meteor Mystery Behind Lonar Lake". National Geographic Traveller Idia. National Geographic Group. Archived from the original on 6 January 2015. Retrieved 27 July 2015.
- ^ Anoop et al., Palaeoenvironmental implications of evaporative gaylussite crystals from Lonar Lake, central India, Journal of Quaternary Science, V., Issue 4, pp. 349–359, May 2013
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