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Barratta meteorite, Barratta, Townsend Co., New South Wales, Australiai
Regional Level Types
Barratta meteoriteMeteorite Fall Location
Barratta- not defined -
Townsend Co.County
New South WalesState
AustraliaCountry

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Latitude & Longitude (WGS84):
35° 16' 43'' South , 144° 32' 58'' East
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Old Morago148 (2016)14.4km
Deniliquin8,024 (2016)46.2km
Mindat Locality ID:
255187
Long-form identifier:
mindat:1:2:255187:9
GUID (UUID V4):
1ca49367-4549-41c7-88c7-f280dea9aea8


Ordinary chondrite, black (L4; S4)
Found, 1845; 200 kg, 5 stones.

According to the Australian Museum in Sydney the first fragments of meteorite were first found in 1845. By the early 20th Century, five stones, ranging in mass from 65.8β€”14.1 kg, had been recovered. Barratta is an aggregate of chondrules and chondrule fragments which have been darkened by shock. Chondrule types include barred olivine (BO), porphyritic olivine (PO), and radiating pyroxene (PR) varieties. Olivine is quite variable (Fa22-32). Two petrographically distinct populations of chondrules are also present β€” prominent spherical chondrules within a glassy dark mesostasis with other poorly defined, irregular chondrules which have been partially integrated with the matrix. Fe-Ni metal and troilite are present only in minor amounts β€” usually interstitial to chondrules, but sometimes near chondrule rims. A cosmic ray exposure age of ~ 8.9 Ma has been reported.

Barratta is the most massive L4 chondrite listed at The Meteoritical Bulletin DataBase (as of February 2016). The L group of ordinary chondrites (ordinary chondrites relatively low in total iron) account for roughly 40% of all meteorite falls.

While three stones accounting for most of the mass are at the Australian Museum, 2 stones of slightly smaller total mass are held at the Field Museum of Natural History in Chicago.

The co-ordinates provided are for the general location of Barratta. The exact co-ordinates for the meteorite fragments are unknown.

Classification Problematics. The official classification of Barratta has been changed from the Catalogue of Meteorites (2000) L3.8 classification. The Meteoritical Society has, perhaps, relied on further information which suggests that the primary glass reported here is from non-representative portions of the meteorite?

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


11 valid minerals.

Meteorite/Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ Chromite
Formula: Fe2+Cr3+2O4
β“˜ 'Clinopyroxene Subgroup'
Description: Clinopyroxene β€” The dominant pyroxene is Ca-poor and frequently twinned clinopyroxene (Fs~20) [labelled 'clinohypersthene' by Mason & Wiik].
β“˜ Copper
Formula: Cu
β“˜ 'Fayalite-Forsterite Series'
β“˜ 'Glass'
β“˜ 'Hypersthene'
Formula: (Mg,Fe)SiO3
References:
β“˜ Ilmenite
Formula: Fe2+TiO3
β“˜ Iron
Formula: Fe
References:
β“˜ Iron var. Kamacite
Formula: (Fe,Ni)
β“˜ Iron var. Martensite
Formula: Fe
β“˜ Isocubanite
Formula: CuFe2S3
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
β“˜ Merrillite
Formula: Ca9NaMg(PO4)7
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
β“˜ Schreibersite
Formula: (Fe,Ni)3P
β“˜ Spinel
Formula: MgAl2O4
β“˜ Taenite
Formula: (Fe,Ni)
β“˜ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
β“˜Iron
var. Martensite
1.AE.05Fe
β“˜1.AE.05Fe
β“˜var. Kamacite1.AE.05(Fe,Ni)
β“˜Taenite1.AE.10(Fe,Ni)
β“˜Schreibersite1.BD.05(Fe,Ni)3P
Group 2 - Sulphides and Sulfosalts
β“˜Isocubanite2.CB.55bCuFe2S3
β“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Spinel4.BB.05MgAl2O4
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Merrillite8.AC.45Ca9NaMg(PO4)7
Unclassified
β“˜'Clinopyroxene Subgroup'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Hypersthene'-(Mg,Fe)SiO3
β“˜'Glass'-

List of minerals for each chemical element

OOxygen
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ Hypersthene(Mg,Fe)SiO3
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ SpinelMgAl2O4
Oβ“˜ MerrilliteCa9NaMg(PO4)7
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naβ“˜ MerrilliteCa9NaMg(PO4)7
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ Hypersthene(Mg,Fe)SiO3
Mgβ“˜ SpinelMgAl2O4
Mgβ“˜ MerrilliteCa9NaMg(PO4)7
AlAluminium
Alβ“˜ SpinelMgAl2O4
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ Hypersthene(Mg,Fe)SiO3
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pβ“˜ Schreibersite(Fe,Ni)3P
Pβ“˜ MerrilliteCa9NaMg(PO4)7
SSulfur
Sβ“˜ IsocubaniteCuFe2S3
Sβ“˜ TroiliteFeS
CaCalcium
Caβ“˜ MerrilliteCa9NaMg(PO4)7
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ Hypersthene(Mg,Fe)SiO3
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ IronFe
Feβ“˜ IsocubaniteCuFe2S3
Feβ“˜ Iron var. Kamacite(Fe,Ni)
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ Schreibersite(Fe,Ni)3P
Feβ“˜ Taenite(Fe,Ni)
Feβ“˜ TroiliteFeS
Feβ“˜ Iron var. MartensiteFe
NiNickel
Niβ“˜ Iron var. Kamacite(Fe,Ni)
Niβ“˜ Schreibersite(Fe,Ni)3P
Niβ“˜ Taenite(Fe,Ni)
CuCopper
Cuβ“˜ CopperCu
Cuβ“˜ IsocubaniteCuFe2S3

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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