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Hoba meteorite: Difference between revisions

Coordinates: 19°35′32″S 17°56′01″E / 19.59222°S 17.93361°E / -19.59222; 17.93361
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==Discovery==
==Discovery==
{{meteoroid_size_comparison.svg}}

The Hoba meteorite left no preserved [[Impact crater|crater]] and its discovery was a chance event. In 1920,<ref name=database/> the owner of the land, Jacobus Hermanus Brits, encountered the object while ploughing one of his fields with an [[ox]]. During this work, he heard a loud metallic scratching sound and the plough came to an abrupt halt. The obstruction was excavated, identified as a meteorite and described by Mr. Brits, whose report was published in 1920 and can be viewed at the [[Grootfontein]] Museum in Namibia.
The Hoba meteorite left no preserved [[Impact crater|crater]] and its discovery was a chance event. In 1920,<ref name=database/> the owner of the land, Jacobus Hermanus Brits, encountered the object while ploughing one of his fields with an [[ox]]. During this work, he heard a loud metallic scratching sound and the plough came to an abrupt halt. The obstruction was excavated, identified as a meteorite and described by Mr. Brits, whose report was published in 1920 and can be viewed at the [[Grootfontein]] Museum in Namibia.


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==Description and composition==
==Description and composition==

{{meteoroid_size_comparison.svg}}
Hoba is a tabular body of metal, measuring {{convert|2.7|*|2.7|*|0.9|m|ftin|abbr=on}}. In 1920, its mass was estimated at 66 tonnes. Erosion, scientific sampling and vandalism reduced its bulk over the years. The remaining mass is estimated at just over 64 tonnes. The meteorite is composed of about 84% iron and 16% [[nickel]], with traces of [[cobalt]]. It is classified as an [[ataxite]] [[iron meteorite]] belonging to the nickel-rich chemical class [[IVB meteorites|IVB]]. A crust of [[iron hydroxide]]s is locally present on the surface due to [[weathering]] [[oxidation]].
Hoba is a tabular body of metal, measuring {{convert|2.7|*|2.7|*|0.9|m|ftin|abbr=on}}. In 1920, its mass was estimated at 66 tonnes. Erosion, scientific sampling and vandalism reduced its bulk over the years. The remaining mass is estimated at just over 64 tonnes. The meteorite is composed of about 84% iron and 16% [[nickel]], with traces of [[cobalt]]. It is classified as an [[ataxite]] [[iron meteorite]] belonging to the nickel-rich chemical class [[IVB meteorites|IVB]]. A crust of [[iron hydroxide]]s is locally present on the surface due to [[weathering]] [[oxidation]].


==Modern history==
==Modern history==
In an attempt to control vandalism, with permission from the farm owner, on March 15, 1955, the government of [[South West Africa]] (now Namibia) declared the Hoba meteorite to be a national monument.<ref>{{cite journal |journal=Geochimica et Cosmochimica Acta |volume=31 |issue=9 |date=September 1967 |page=1470 |first=M.F. |last=Comerford |title=Comparative erosion rates of stone and iron meteorites under small-particle bombardment |doi=10.1016/0016-7037(67)90021-X |publisher=Elsevier Science, New York |issn=0016-7037|bibcode=1967GeCoA..31.1457C}}</ref> Since 1979 the proclamation has been extended to land of 425&nbsp;m².<ref name=Voigt>{{Cite book | title=National Monuments in Namibia: An Inventory of Proclaimed National Monuments in the Republic of Namibia | last=Voigt | first=Andreas | publisher=Gamsberg Macmillan | year=2004 | pages=4–5 | isbn= 9991605932 | url=https://books.google.com/books?id=h0h0AAAAMAAJ}}</ref>
In an attempt to control vandalism, with permission from the farm owner, Mrs O Scheel <ref name=Comerford>{{cite journal |journal=Geochimica et Cosmochimica Acta |volume=31 |issue=9 |date=September 1967 |page=1470 |first=M.F. |last=Comerford |title=Comparative erosion rates of stone and iron meteorites under small-particle bombardment |doi=10.1016/0016-7037(67)90021-X |publisher=Elsevier Science, New York |issn=0016-7037|bibcode=1967GeCoA..31.1457C}}</ref>, on March 15, 1955, the government of [[South West Africa]] (now Namibia) declared the Hoba meteorite to be a national monument. Since 1979 the proclamation has been extended to land of 425&nbsp;m².<ref name=Voigt>{{Cite book | title=National Monuments in Namibia: An Inventory of Proclaimed National Monuments in the Republic of Namibia | last=Voigt | first=Andreas | publisher=Gamsberg Macmillan | year=2004 | pages=4–5 | isbn= 9991605932 | url=https://books.google.com/books?id=h0h0AAAAMAAJ}}</ref>


From about the 1970s, development of the meteorite site for tourism was hampered by its location in the Otavi triangle of Otavi, Tsumeb and Grootfontein, <ref> https://www.nytimes.com/1982/08/01/magazine/inside-namibia.html</ref> a key arena of the Namibian war of independence or [[South_African_Border_War]]. The war and liberation struggle ended with the [[Tripartite_Accord_(1988)]]. General elections under universal franchise, in 1989, led to formation of the the independent [[Republic of Namibia]] in 1990.


In 1987, the farm owner donated the meteorite and the site where it lies to the state for educational purposes. Later that year, the government opened a tourist centre at the site.<ref name=Voigt/> As a result of these developments, vandalism of the Hoba meteorite has ceased and it is now visited by thousands of tourists every year.
In 1987, the farm owner donated the meteorite and the site where it lies to the state for educational purposes. Later that year, the government opened a tourist centre at the site.<ref name=Voigt/> As a result of these developments, vandalism of the Hoba meteorite has ceased and it is now visited by thousands of tourists every year.

Nevertheless, specimens sourced from earlier theft and vandalism continue to be traded. On the 7th of December 2021, an unusually large 2.8 Kg specimen illegally harvested in 1968, was sold for $59062 <ref name=BonhamMeteoSale> https://www.bonhams.com/auctions/26880/lot/2366/</ref> in Los Angeles, by international auction house [[Bonhams]]. The Bonhams sale notice states " the present specimen was obtained in 1968 by the father of the present owner when he visited the main mass of Hoba together with some friends. Using a hand saw, they cut a large block of the meteorite from the main mass "as a souvenir", an activity which took them between three and four hours", <ref name=BonhamMeteoSale/>.



<gallery mode="packed" height="150px">
<gallery mode="packed" height="150px">
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File:Tatton Park 2016 205 (4x3).jpg|{{convert|365|lb|kg|order=flip|abbr=on}} of the meteorite at the [[National Trust for Places of Historic Interest or Natural Beauty|National Trust]]'s [[Tatton Park]] near [[Manchester]], [[England]].
File:Tatton Park 2016 205 (4x3).jpg|{{convert|365|lb|kg|order=flip|abbr=on}} of the meteorite at the [[National Trust for Places of Historic Interest or Natural Beauty|National Trust]]'s [[Tatton Park]] near [[Manchester]], [[England]].
</gallery>
</gallery>



==See also==
==See also==

Revision as of 18:21, 9 October 2022

Hoba
The meteorite in 2014 after becoming a tourist attraction
TypeIron
Class12
CountryNamibia
Coordinates19°35′32″S 17°56′01″E / 19.59222°S 17.93361°E / -19.59222; 17.93361
Fall dateLess than 80,000 years ago
Found date1920
Related media on Wikimedia Commons

The Hoba[1] (/ˈhbə/ HOH-bə) meteorite, short for Hoba West, is a meteorite that lies on the farm of the same name, not far from Grootfontein, in the Otjozondjupa Region of Namibia. It has been uncovered, but because of its large mass, has never been moved from where it fell. The main mass is estimated at more than 60 tonnes.[1] It is the largest known intact meteorite (as a single piece)[2] and about twice as massive as the largest fragment of either the Cape York meteorite's 31-tonne Ahnighito kept in Manhattan or the Campo del Cielo's 31-tonne Gancedo in Argentina. It is also the most massive naturally occurring piece of iron (actually ferronickel) known on Earth's surface. The name "Hoba" comes from a Khoekhoegowab word meaning "gift".[3] Following donation to the government in 1987, a visitor centre was constructed with a circular stone access and seating area.

Impact

The Hoba meteorite impact is thought to have occurred less than 80,000 years ago. It is inferred[4] that the Earth's atmosphere slowed the object in such a way that it impacted the surface at terminal velocity, thereby remaining intact and causing little excavation (expulsion of earth). Assuming a drag coefficient of about 1.3, the meteor appears to have slowed to about 320 m/s (720 mph) from an entry speed to the atmosphere typically in excess of 10 km/s (22,370 mph). The meteorite is unusual in that it is flat on both major surfaces.

Discovery

Comparison of approximate sizes of notable impactors with the Hoba meteorite, a Boeing 747 and a New Routemaster bus

The Hoba meteorite left no preserved crater and its discovery was a chance event. In 1920,[1] the owner of the land, Jacobus Hermanus Brits, encountered the object while ploughing one of his fields with an ox. During this work, he heard a loud metallic scratching sound and the plough came to an abrupt halt. The obstruction was excavated, identified as a meteorite and described by Mr. Brits, whose report was published in 1920 and can be viewed at the Grootfontein Museum in Namibia.

Friedrich Wilhelm Kegel took the first published photograph of the Hoba meteorite.[5]

Description and composition

Hoba is a tabular body of metal, measuring 2.7×2.7×0.9 m (8 ft 10 in×8 ft 10 in×2 ft 11 in). In 1920, its mass was estimated at 66 tonnes. Erosion, scientific sampling and vandalism reduced its bulk over the years. The remaining mass is estimated at just over 64 tonnes. The meteorite is composed of about 84% iron and 16% nickel, with traces of cobalt. It is classified as an ataxite iron meteorite belonging to the nickel-rich chemical class IVB. A crust of iron hydroxides is locally present on the surface due to weathering oxidation.

Modern history

In an attempt to control vandalism, with permission from the farm owner, Mrs O Scheel [6], on March 15, 1955, the government of South West Africa (now Namibia) declared the Hoba meteorite to be a national monument. Since 1979 the proclamation has been extended to land of 425 m².[7]


From about the 1970s, development of the meteorite site for tourism was hampered by its location in the Otavi triangle of Otavi, Tsumeb and Grootfontein, [8] a key arena of the Namibian war of independence or South_African_Border_War. The war and liberation struggle ended with the Tripartite_Accord_(1988). General elections under universal franchise, in 1989, led to formation of the the independent Republic of Namibia in 1990.

In 1987, the farm owner donated the meteorite and the site where it lies to the state for educational purposes. Later that year, the government opened a tourist centre at the site.[7] As a result of these developments, vandalism of the Hoba meteorite has ceased and it is now visited by thousands of tourists every year.

Nevertheless, specimens sourced from earlier theft and vandalism continue to be traded. On the 7th of December 2021, an unusually large 2.8 Kg specimen illegally harvested in 1968, was sold for $59062 [9] in Los Angeles, by international auction house Bonhams. The Bonhams sale notice states " the present specimen was obtained in 1968 by the father of the present owner when he visited the main mass of Hoba together with some friends. Using a hand saw, they cut a large block of the meteorite from the main mass "as a souvenir", an activity which took them between three and four hours", [9].



See also

Notes and references

  1. ^ a b c Meteoritical Bulletin Database: Hoba
  2. ^ McSween, Harry (1999). Meteorites and their parent planets (2nd ed.). Cambridge: Cambridge University Press. ISBN 0521583039. OCLC 39210190.
  3. ^ Cassidy, Joseph (2009). Place Names of Namibia A Historical Dictionary. Windhoek: Macmillan Education Namibia Publishers (Pty) Ltd. p. 37. ISBN 978-99916-0-654-5.
  4. ^ Field Guide to Meteors and Meteorites O. Richard Norton and Lawrence Chitwood. Springer Science + Business Media 2008, ISBN 978-1-84800-156-5
  5. ^ Spencer, L. J.; Hey, M. H. (March 1932). "Hoba (South-West Africa), the largest known meteorite" (PDF). Mineralogical Magazine and Journal of the Mineralogical Society. XXIII (136): 4. Bibcode:1932MinM...23....1S. doi:10.1180/minmag.1932.023.136.03. Archived (PDF) from the original on 2016-12-15.
  6. ^ Comerford, M.F. (September 1967). "Comparative erosion rates of stone and iron meteorites under small-particle bombardment". Geochimica et Cosmochimica Acta. 31 (9). Elsevier Science, New York: 1470. Bibcode:1967GeCoA..31.1457C. doi:10.1016/0016-7037(67)90021-X. ISSN 0016-7037.
  7. ^ a b Voigt, Andreas (2004). National Monuments in Namibia: An Inventory of Proclaimed National Monuments in the Republic of Namibia. Gamsberg Macmillan. pp. 4–5. ISBN 9991605932.
  8. ^ https://www.nytimes.com/1982/08/01/magazine/inside-namibia.html
  9. ^ a b https://www.bonhams.com/auctions/26880/lot/2366/

Further reading