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Kurinelli Meteorites, Kurundi Goldfield, Wauchope, Barkly Region, Northern Territory, Australiai
Regional Level Types
Kurinelli MeteoritesMeteorites
Kurundi GoldfieldOre Field
Wauchope- not defined -
Barkly RegionRegion
Northern TerritoryTerritory
AustraliaCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
20° 36' 48'' South , 135° 2' 51'' East
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
294476
Long-form identifier:
mindat:1:2:294476:3
GUID (UUID V4):
ad26232f-9a42-42fe-9c3c-487a8c986798


The Kurinelli area has been the haunt of many a gold prospector over time including recently, with bulldozing, then metal detected, with oral evidence indicating a number of nuggets found. However, the area also contains another item of interest, with many small meteorite fragments located with metal detectors. The bad news (at least for people searching for meteorites) is the law banns the keeping and/or export of meteorites found in the Northern Territory after 1988, and they must be handed into the Northern Territory Museum department.

A number of prospectors were finding 'hot rocks' in the area, which they would smash open hoping for gold inside. Initially there was much frustration, until one prospector, Nick Byrne recognised nickel in 1996. Believing the rocks represented a major bedrock nickel deposit, he approached Peter Simpson (and other companies) from Giants Reef Mining. A pegging rush ensued, however further investigations by geologists determined the material to be meteorites.

Various local prospectors, including Ray Hall, Colin Wessel, John McDonald, and Tony Campbell, donated material to the Northern Territory Museum for study.

All the meteorites have been found in soil rather than the surface to a depth of one metre. No impact structure has been found, and it is thought the meteorites are 'ancient' in age. While most material has been located in the Kurinelli area, Peter Saint, owner of the Kurundi pastoral station has stated, similar meteorites have been found as far away as Annitowa, 200 kilometres further afield. Most of the material is small, with the largest known being half a brick in size.

The meteorite surface is brown to reddish-brown, internally lustrous dark grey to grey-black, veined with brown and reddish-brown.

The meteorites are an almost completely oxidised octahedrite. Species include goethite which may have been derived from troilite, although no relict troilite was found. Well crystalline magnetite. Common maghemite, interbedded with other species, and bluish colour in polished sections. Native iron being unusual for a meteorite, as small grains and grain patches. Very minor quartz having intruded from weathering. Ragged remnants of a Fe-Ni alloy. Microscopically, kaolinite, montmorillonite and titanomagnetite is mentioned.

Mindat map shows the Kurinelli water tank/cattle yards, although material has been found in a wide area surrounding this. See also 'Kurinelli Gold Mines (Kurinelli Alluvial Gold Area)' Mindat locality.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


10 valid minerals.

Detailed Mineral List:

β“˜ Chromite
Formula: Fe2+Cr3+2O4
β“˜ Goethite
Formula: Ξ±-Fe3+O(OH)
β“˜ Hematite
Formula: Fe2O3
β“˜ Hematite var. Martite
Formula: Fe2O3
β“˜ Iron
Formula: Fe
β“˜ Kaolinite
Formula: Al2(Si2O5)(OH)4
β“˜ Lepidocrocite ?
Formula: γ-Fe3+O(OH)
β“˜ 'Limonite'
β“˜ Maghemite
Formula: (Fe3+0.670.33)Fe3+2O4
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
β“˜ Magnetite var. Titanium-bearing Magnetite
Formula: Fe2+(Fe3+,Ti)2O4
β“˜ Montmorillonite
Formula: (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
β“˜ Quartz
Formula: SiO2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Iron1.AE.05Fe
Group 4 - Oxides and Hydroxides
β“˜Goethite4.00.Ξ±-Fe3+O(OH)
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜var. Titanium-bearing Magnetite4.BB.05Fe2+(Fe3+,Ti)2O4
β“˜Maghemite4.BB.15(Fe3+0.67β—»0.33)Fe3+2O4
β“˜Hematite4.CB.05Fe2O3
β“˜var. Martite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
β“˜Lepidocrocite ?4.FE.15Ξ³-Fe3+O(OH)
Group 9 - Silicates
β“˜Montmorillonite9.EC.40(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 Β· nH2O
β“˜Kaolinite9.ED.05Al2(Si2O5)(OH)4
Unclassified
β“˜'Limonite'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ GoethiteΞ±-Fe3+O(OH)
Hβ“˜ KaoliniteAl2(Si2O5)(OH)4
Hβ“˜ Lepidocrociteγ-Fe3+O(OH)
Hβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
OOxygen
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ GoethiteΞ±-Fe3+O(OH)
Oβ“˜ HematiteFe2O3
Oβ“˜ KaoliniteAl2(Si2O5)(OH)4
Oβ“˜ Lepidocrociteγ-Fe3+O(OH)
Oβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ Hematite var. MartiteFe2O3
Oβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Oβ“˜ QuartzSiO2
Oβ“˜ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
NaSodium
Naβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
MgMagnesium
Mgβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
AlAluminium
Alβ“˜ KaoliniteAl2(Si2O5)(OH)4
Alβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
SiSilicon
Siβ“˜ KaoliniteAl2(Si2O5)(OH)4
Siβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Siβ“˜ QuartzSiO2
CaCalcium
Caβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
TiTitanium
Tiβ“˜ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ GoethiteΞ±-Fe3+O(OH)
Feβ“˜ HematiteFe2O3
Feβ“˜ IronFe
Feβ“˜ Lepidocrociteγ-Fe3+O(OH)
Feβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ Hematite var. MartiteFe2O3
Feβ“˜ Magnetite var. Titanium-bearing MagnetiteFe2+(Fe3+,Ti)2O4

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.

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