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Kurnalpi Goldfield, Kalgoorlie-Boulder Shire, Western Australia, Australiai
Regional Level Types
Kurnalpi GoldfieldOre Field
Kalgoorlie-Boulder ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
30° 32' 20'' South , 122° 14' 44'' East
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
146979
Long-form identifier:
mindat:1:2:146979:3
GUID (UUID V4):
0


Gold was discovered here by Alex Slater and party in 1894, 95 kilometres north-east of Kalgoorlie. The goldfield produced incredibly rich alluvial gold in its initial years and was known as the 'home of slugs' referring to the large slug shaped gold nuggets lying around all over the ground.

Kurnalpi is mainly known as a rich alluvial gold area, rather than a reefing location. Large slugs were found scattered across the flats and gullies by early prospectors. The largest area historically was Social Flat, near the former Kurnalpi town site, as a large flat area, with several tributing gullies. Two miles north of the town site is a discontinuous belt of alluvial gold. A site called Cemetery, south-east of the town also saw large nuggets obtained. The source also mentions a location called Six Mile.

These locations consist of red soil lying on a largely barren cement (hardpan). Some ironstone nodules, angular quartz, and cement nodules are found just above the cement in deeper areas. Generally the cement was 4-6 inches to 4 feet below the surface.

Normally the gold mineralisation would be expected to increase with depth, but this did not occur at Kurnalpi. By 1900 it was noted that the alluvial gold had pettered out and people began drifting away. A 1902 correspondent stated:'with the exception of a few unimportant shows, worked by small parties of men, the place has little to recommend itself to public notice. Once the initial goldrush was over, the place fell silent.

The area has a large number of shallow historic workings of various names which include but not restricted to: Richies, Kug, Success, Brilliant, Scottish Lass, Dazzle, Sparkle, Discovery Hill. Modern mining companies have named Halfway Hill, Colour Dam Pit, and Kurnalpi South as locations, apparently not discouraged by the lack of historic underground gold.

The area was explored in the 1970's by Amax Exploration (Australia) Inc, Aquitaine Australia Minerals Pty Ltd, Esso Exploration and Production Australia Inc. Further exploration has been conducted in the early 2000's by Carrick Gold and Fairstar Resources.

Regionally the geology is a lower basaltitic unit, overlain by Komatiite, followed by an upper basalt unit, then a sequence of felsic volcanic and volcaniclastic rocks, overlain by clastic sedimentary rocks. The volcanic and volcaniclastic rocks have been altered to quartz-sericite-carbonate-pyrite in association with quartz-sulphide vein arrays developed within the shear zones. Minor copper, lead and zinc has been found.

What is rarer than gold in a desert? Newspapers reported snow falling at Kurnalpi early in October 1900.

The area is mostly scattered bulldozed shallow scrapes from modern prospectors and exploration companies. Mainly north of the Kanowna-Kurnalpi road, with a few exceptions. About nine of these were counted, (some relatively extensive) anywhere from one to ten kilometres from the road. Only two sections were identified as retaining significant historic workings, being in the edge of a large area of scrapings at the far northern end, and another line of old shafts a short distance south of the road.

The town of Kurnalpi no longer exists.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

12 valid minerals.

Rock Types Recorded

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

Rock list contains entries from the region specified including sub-localities

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

Anthophyllite
Formula: ◻{Mg2}{Mg5}(Si8O22)(OH)2
'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Chalcopyrite
Formula: CuFeS2
'Fayalite-Forsterite Series'
Hematite
Formula: Fe2O3
'Limonite'
Magnesite
Formula: MgCO3
Magnetite
Formula: Fe2+Fe3+2O4
Millerite
Formula: NiS
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Native Gold
Formula: Au
Localities: Reported from at least 11 localities in this region.
Pyrite
Formula: FeS2
Pyrrhotite
Formula: Fe1-xS
Quartz
Formula: SiO2
Localities: Reported from at least 6 localities in this region.
'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
Siegenite
Formula: CoNi2S4
'Tourmaline'
Formula: AD3G6 (T6O18)(BO3)3X3Z

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
Millerite2.CC.20NiS
Siegenite2.DA.05CoNi2S4
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Magnesite5.AB.05MgCO3
Group 9 - Silicates
Anthophyllite9.DD.05◻{Mg2}{Mg5}(Si8O22)(OH)2
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
'Limonite'-
'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z
'Fayalite-Forsterite Series'-
'Serpentine Subgroup'-D3[Si2O5](OH)4

List of minerals for each chemical element

HHydrogen
H Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
H MuscoviteKAl2(AlSi3O10)(OH)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
H Serpentine SubgroupD3[Si2O5](OH)4
BBoron
B TourmalineAD3G6 (T6O18)(BO3)3X3Z
CCarbon
C MagnesiteMgCO3
OOxygen
O Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
O HematiteFe2O3
O MagnesiteMgCO3
O MagnetiteFe2+Fe23+O4
O MuscoviteKAl2(AlSi3O10)(OH)2
O QuartzSiO2
O TourmalineAD3G6 (T6O18)(BO3)3X3Z
O Fayalite-Forsterite Series
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
O Serpentine SubgroupD3[Si2O5](OH)4
FFluorine
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
MgMagnesium
Mg Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mg MagnesiteMgCO3
Mg Fayalite-Forsterite Series
AlAluminium
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si QuartzSiO2
Si Fayalite-Forsterite Series
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Si Serpentine SubgroupD3[Si2O5](OH)4
SSulfur
S ChalcopyriteCuFeS2
S MilleriteNiS
S PyriteFeS2
S PyrrhotiteFe1-xS
S SiegeniteCoNi2S4
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
K MuscoviteKAl2(AlSi3O10)(OH)2
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
TiTitanium
Ti BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeIron
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fe ChalcopyriteCuFeS2
Fe HematiteFe2O3
Fe MagnetiteFe2+Fe23+O4
Fe PyriteFeS2
Fe PyrrhotiteFe1-xS
Fe Fayalite-Forsterite Series
CoCobalt
Co SiegeniteCoNi2S4
NiNickel
Ni MilleriteNiS
Ni SiegeniteCoNi2S4
CuCopper
Cu ChalcopyriteCuFeS2
AuGold
Au Native GoldAu

Localities in this Region

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

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