Tucson-ring
From Wikipedia (Af) - Reading time: 2 min
| Tucson-ring | ||
| ||
| Die Tucson-ring in die Smithsonian-natuurgeskiedenismuseum. | ||
| Voorwerp | ||
| Tipe | Yster[1] | |
| Datum | 1850 (ontdek)[1] | |
| Waargenome val | Nee | |
| TBG | 975 kg[1] | |
| Gebied | ||
| Land |  Verenigde State
| |
| Streek | Arizona | |
Die Tucson-ring is 'n meteorietfragment van brezinaïet wat in Arizona, VSA, geval en die eerste keer deur Bunch en Fuchs beskryf is.[2] Dit is aangemeld as een van verskeie massas rou yster wat omstreeks 1850 aan die voet van die Sierra de la Madera ontdek is en na die plaza van Tucson, Arizona, gebring is. Hier is dit deur 'n grofsmid as 'n aambeeld gebruik.[3]
Verwysings
[wysig | wysig bron]- ↑ 1,0 1,1 1,2 "Tucson". The Meteoritical Society. Besoek op 21 April 2019.
- ↑ Anthony, John W.; Williams, Sidney A.; Bideaux, Richard A.; Grant, Raymond W. (26 Mei 2016). Mineralogy of Arizona (in Engels). University of Arizona Press. ISBN 9780816534043.
- ↑ Clarke, Roy S., Jr.; Plotkin, Howard; McCoy, Timothy (2006), "Meteorites and the Smithsonian Institution", in McCall, G. J. H.; Bowden, A. J.; Bowden, R. J., The History of Meteoritics and Key Meteorite Collections: Fireballs, Falls and Finds, Londen: The Geological Society, p. 241, ISBN 9781862391949, https://books.google.com/books?id=7SvtVoa1W-cC&dq=nogata+meteorite&pg=PA16
Skakels
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Hierdie artikel is in sy geheel of gedeeltelik uit die Engelse Wikipedia vertaal.
Licensed under CC BY-SA 3.0 | Source: https://af.wikipedia.org/wiki/Tucson-ring1 views | ↧ Download this article as ZWI file
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