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{{Short description|Chondrite meteorite}}
{{Infobox meteorite
|Name = Pultusk
Line 7 ⟶ 8:
|Group = [[H chondrite|H5]]
|Structural_classification =
|Composition = Olivine and bronzite, kamacite, troilite and chromite also present.
|Composition = SiO2 36.44 wt%, TiO2 0.18 wt%, Al2O3 1.88 wt%, Cr2O3 0.37 wt%, FeO 9.48 wt%, MnO 0.25 wt%, MgO 23.75 wt%, CaO 1.82 wt%, Na2O 0.83 wt%, K2O 0.09 wt%, P2O5 0.22 wt%, Fe 16.02 wt%, Ni 1.61 wt%, FeS 5.97 wt%, Fe (metallic) 17.62 wt%, Ni (metallic) 9.13 wt%, Fe as iron sulphide 3.80 wt%, S as iron sulphide 2.17 wt%, total content of iron 27.19 wt%.<ref>Diakonov and Kharitonova (1961)</ref>▼
|Shock =
|Weathering =
|Country = [[Poland]]
|Region = [[Ostrołęka]]
|Lat_Long = {{coord|52|46|N|21|16|E|display=inline,title}}
|Observed_fall = Yes
|Fall_date = January 30, 1868
|Found_date =
|TKW = about
|Strewn_field = Yes
|Image2 = Pultusk meteorite strewnfield.png
|Image2_caption = Distribution ellipse of Pultusk fall.
}}
'''Pultusk''' is an [[H chondrite|H5 ordinary chondrite]] [[meteorite]]
==History==
The fall occurred on January 30, 1868, at 7:00 pm near the town of [[Pułtusk]], about {{convert|60
The fragments ranged in weight from half a gram to {{convert|9.095
==Composition and classification==
Pultusk is brecciated and contains two varieties of [[xenolith]]s embedded in a dark brecciated matrix. It is a veined and brecciated [[chondrite]] with abundant
===Chemical composition===
[[File:Pultusk Meteorite Composition Plot.svg|thumb|right|The chemical elements and the respective quantity found in the Pultusk meteorite.]]
▲
==See also==
* [[Glossary of meteoritics]]
* [[Sikhote-Alin (meteorite)]]
==Gallery==
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</gallery>
==Additional information==
<references/>▼
==
▲<references group=n/>
===References===
{{Reflist}}
==External links==
* [https://web.archive.org/web/20080724221747/http://www.geo.uw.edu.pl/MUZEUM/METEORITE/pultusk_a.htm Museum of the Faculty of Geology of the Warsaw University: '''Pultusk''']
* [https://books.google.com/books?id=k3Tu0BcNEaoC&dq=Pultusk+meteorite+largest+fall&pg=PA100 Meteorites: An Introduction], on [[Google Books]]
* {{metbull|18901|Pultusk}}
{{Meteorites}}
{{Meteorites by name}}
{{Authority control}}
[[Category:Meteorites found in Poland]]
[[Category:1868 in
[[Category:1860s in science]]
[[Category:1868 in the Russian Empire]]
[[Category:January 1868 events]]
|
Pultusk | |
---|---|
Type | Chondrite |
Class | Ordinary chondrite |
Group | H5 |
Composition | Olivine and bronzite, kamacite, troilite and chromite also present. |
Country | Poland |
Region | Ostrołęka |
Coordinates | 52°46′N 21°16′E / 52.767°N 21.267°E / 52.767; 21.267 |
Observed fall | Yes |
Fall date | January 30, 1868 |
TKW | about 8860 kg (about 9.8 tons) |
Strewn field | Yes |
Distribution ellipse of Pultusk fall. | |
Related media on Wikimedia Commons |
Pultusk is an H5 ordinary chondrite meteorite which fell on 30 January 1868 in Poland. The event has been known as the stony meteorite shower with the largest number of pieces yet recorded in history.[1] Made up of rocky debris, it consists of pyroxeneorolivine chondrules deployed in mass plagioclase, there being also kamacite.
The fall occurred on January 30, 1868, at 7:00 pm near the town of Pułtusk, about 60 kilometres (37 mi) northeast of Warsaw. Thousands of people witnessed a large fireball followed by detonations and a very large shower of small fragments falling on ice, land and houses within an area of about 127 sq km (appx. 78 sq. miles). The estimated number of fragments was 68780.[2][n 1]
The fragments ranged in weight from half a gram to 9.095 kilograms (20.05 lb) (the largest specimen). The overall estimated mass of the meteorites was 8,863 kilograms (19,540 lb). The vast majority of the fragments were small (few grams), known as Pultusk Peas. The Pultusk meteorite is the largest stony meteorite shower ever recorded.[3]
Pultusk is brecciated and contains two varieties of xenoliths embedded in a dark brecciated matrix. It is a veined and brecciated chondrite with abundant xenoliths with various degrees of recrystallisation. Petrologic type 5 xenoliths prevail,[4] so it has been classified as H5: an ordinary chondrite significantly thermally metamorphosed and with the contours of the chondrules frequently difficult to distinguish. The main minerals are olivine and bronzite. Kamacite, troilite and chromite are also present.
The chemical elements and the respective quantity found in the Pultusk meteorite have been described as SiO2 36.44 wt%, TiO2 0.18 wt%, Al2O3 1.88 wt%, Cr2O3 0.37 wt%, FeO 9.48 wt%, MnO 0.25 wt%, MgO 23.75 wt%, CaO 1.82 wt%, Na2O 0.83 wt%, K2O 0.09 wt%, P2O5 0.22 wt%, Fe 16.02 wt%, Ni 1.61 wt%, FeS 5.97 wt%, Fe (metallic) 17.62 wt%, Ni (metallic) 9.13 wt%, Fe as iron sulfide 3.80 wt%, S as iron sulfide 2.17 wt%, total content of iron 27.19 wt%.[5]
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