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Goalpara meteorite, Goalpara District, Assam, Indiai
Regional Level Types
Goalpara meteoriteMeteorite Fall Location
Goalpara DistrictDistrict
AssamState
IndiaCountry

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Latitude & Longitude (WGS84):
26° 10' North , 90° 36' East
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Goālpāra50,759 (2014)2.9km
JogΔ«ghopa2,415 (2014)7.2km
Abhayāpuri15,802 (2014)19.3km
Chāpar19,301 (2014)19.4km
Lakhipur14,045 (2014)33.0km
Mindat Locality ID:
211887
Long-form identifier:
1:2:211887:4
GUID (UUID V4):
d17f8a52-e882-4a5a-bba0-aa14c3c2f5db


Goalpara (India) [1868 Find] A single meteoritic 2.7 kg stone
Classification: Ureilite (Ca-poor achondrite)

A single stone of 2.7 kg was sent by the Rajah of Goalpara to the Calcutta Museum. Goalpara is now known as a ureilite. While by 2013 over 300 ureilite stones have been listed in the Meteoritical Society’s Database, most of them are quite small and/or have been recovered in the 21st Century. Goalpara is actually the most massive of the three known ureilites recovered in the 19th Century. Indeed, Goalpara was the most massive ureilites known before the recovery of the Kenna (New Mexico, USA) ureilite in 1972. Consequently, as small portions of Goalpara have been available in different museums, Goalpara has been around long enough to be the subject of several inquiries.
Ureilites are known for their curious amalgam of cumulate silicates (mostly olivine and pyroxene) mixed with elemental carbon. The carbon itself is always an enigmatic graphite-diamond mix . In Goalpara, four polymorphs of carbon are known (chaoite, diamond, graphite and lonsdaleite). The presence of Lonsdaleite, a hexagonal diamond-like polymorph, may indicate a directional pressure associated with impact shock. The ureilites also usually contain a number of minor opaque minerals. Metallic iron (kamacite) and iron sulfide (as troilite) are invariably present. The ureilites are particularly intriguing because their microscopic textures may have been due to both vapor condensation and to shock impact. Both the relative importance and the timing of these nebular and collisional processes does not appear to be a settled matter at this time.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


10 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“˜ Chaoite
Formula: C
Reference: Handbook of Mineralogy
β“˜ Chromite
Formula: Fe2+Cr3+2O4
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.
β“˜ Clinoenstatite
Formula: MgSiO3
Reference: Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Diamond
Formula: C
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ 'Fayalite-Forsterite Series'
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Graphite
Formula: C
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Iron
Formula: Fe
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.
β“˜ Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Lonsdaleite
Formula: C
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Maghemite
Formula: (Fe3+0.670.33)Fe3+2O4
Reference: Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Pigeonite
Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.; Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.
β“˜ Troilite
Formula: FeS
Reference: Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Chaoite1.CB.05bC
β“˜Diamond1.CB.10aC
β“˜Graphite1.CB.05aC
β“˜Iron1.AE.05Fe
β“˜var. Kamacite1.AE.05(Fe,Ni)
β“˜Lonsdaleite1.CB.10bC
Group 2 - Sulphides and Sulfosalts
β“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Maghemite4.BB.15(Fe3+0.67β—»0.33)Fe3+2O4
Group 9 - Silicates
β“˜Clinoenstatite9.DA.10MgSiO3
β“˜Pigeonite9.DA.10(CaxMgyFez)(Mgy1Fez1)Si2O6
Unclassified Minerals, Rocks, etc.
β“˜'Fayalite-Forsterite Series'-

List of minerals for each chemical element

CCarbon
Cβ“˜ ChaoiteC
Cβ“˜ DiamondC
Cβ“˜ GraphiteC
Cβ“˜ LonsdaleiteC
OOxygen
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6
Oβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
Oβ“˜ ClinoenstatiteMgSiO3
MgMagnesium
Mgβ“˜ Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6
Mgβ“˜ ClinoenstatiteMgSiO3
SiSilicon
Siβ“˜ Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6
Siβ“˜ ClinoenstatiteMgSiO3
SSulfur
Sβ“˜ TroiliteFeS
CaCalcium
Caβ“˜ Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ Iron var. Kamacite(Fe,Ni)
Feβ“˜ Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6
Feβ“˜ TroiliteFeS
Feβ“˜ IronFe
Feβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
NiNickel
Niβ“˜ Iron var. Kamacite(Fe,Ni)

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
John L. Berkley, G. Jeffrey Taylor, Klaus Keil, George E. Harlow & Martin Prinz (1980). The nature and origin of ureilites. G&CA 44, #10, 1579-1697.
Monica M. Grady (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.
S. J. Singletary & T. L. Grove (2003) Early petrologic processes on the ureilite parent body. Meteoritics & Planetary Science 38, #1, 95-108. (Jan 2003).
Gennady P. Vdovykin (1970). Ureilites. Space Science Reviews 10, #4, 483-510.
Nakamuta, Y., & Toh, S. (2013). Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM. American Mineralogist, 98(4), 574-581.

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