File:Trachyte obsidian (Quaternary; Ol Doinyo Nyukie Volcano, Kenya) 2.jpg

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English: Trachyte obsidian (glassy trachyte) from the Quaternary of Kenya. (7.9 centimeters across)

Obsidian is an uncommon igneous rock that varies in chemistry from felsic to intermediate to mafic to alkaline. Chemical analysis can show whether an obsidian is rhyolitic, dacitic, etc. The rock seen here is a trachyte obsidian from a small volcano in the East African Rift Valley called Ol Doinyo Nyukie (several variant spellings exist). Eastern Africa is being ripped apart by the Afar Hotspot and quite a few volcanoes having unusual lava chemistries are present along the rift zone. Ol Doinyo Nyukie is a Quaternary-aged volcano that has principally erupted phonolites and trachytes - both lithologies are intermediate extrusive igneous rocks that are high in alkali content (sodium and potassium). This rock is almost 100% glass, but there are some small, scattered phenocrysts of feldspar.

Locality: Ol Doinyo Nyukie Volcano, southern side of the Mt. Suswa caldera, southern Kenya, eastern Africa (the volcano is at 01º 09’ South latitude, 36º 21’ East longitude)
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Source https://www.flickr.com/photos/47445767@N05/50732153848/
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50732153848. It was reviewed on 18 December 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

18 December 2020

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current15:20, 18 December 2020Thumbnail for version as of 15:20, 18 December 20203,145 × 2,325 (6.47 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50732153848/ with UploadWizard

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