|Latitude & Longitude (WGS84):||30° 1' 47'' South , 120° 39' 48'' East|
|Latitude & Longitude (decimal):||-30.02991,120.66334|
|Köppen climate type:||BSh : Hot semi-arid (steppe) climate|
The mine is 2 kilometres east north-east of the Davyhurst townsite. The Great Ophir pit borders it to the west. Despite the Light of Israel being presently a large abandoned open pit and underground decline, the mine had a rather inauspicious start.
It was discovered around 1906 by John Stout and Charles Wainwright. Local folklore at the time states the mine name was somehow poking fun at Herman Mandelstamm, the rotund Jewish owner of the neighbouring Great Ophir mine. The Mandelstamm family were active in a number of gold mines in the Eastern Goldfields. It is doubtful the reasoning for the name would be allowed in Australia today.
Stout and Wainwright sank a 40 foot shaft, then extracted 100 tonnes of ore, creating a cavern at the bottom of the shaft. In 1907, they attempted to float a company, promoted by Kalgoorlie mining engineer, William Manners. There was some criticism, the mine had yet to prove its worth. This was vehemently denied by Manners, suggesting a few bottles of whiskey given out to its critics would solve the problem. The float was unsuccessful. Stout and Wainwright continued mining to a small degree but soon abandoned the lease. GML 858U. 18 acres.
George Cassidy took over in 1909, with the intention of re-opening the mine. Some small crushings were taken out, but the focus was mainly on public crushing at the new Huntingdon mill Cassidy had erected. By 1913, he declared he was ceasing mining at the location, excessive water charges by the Mines Department were to blame Cassidy claimed.
In 1912, 250 pounds of slimes was stolen from the zinc boxes at the mill. Charles Mitchell was arrested at Goongarrie shortly after with the boxes in his possession.
By 1911, the mine had only produced 731 ounces of gold from 3062 tonnes of ore.
The mine was active to a limited degree in the early 1930's, subsidised by the government, probably as a response to the Great Depression.
GML 1102U. Ronald James O'Brien controlled the lease in the late 1940's, with exemptions, late rent payments and little in the way of crushings.
Modern exploration began with drilling in 1987, then an open pit destroyed the old workings from 1988 to 1989 and a second period 1993 to 1994. 1.65 Mt was produced at 2.79 g/t, and from an underground decline 1.6 Mt at 4.5 g/t which was active until 2004. A company called Aberfoyle was involved with the 1990's mining period, before the grounds were acquired by 1996 by Consolidated Gold. Activity after this was combined with entities owning most or all of the goldfield, as noted under the Davyhurst Goldfield sub-heading.
Historically, in 1907, the deposit was described as two lodes. An east-west lode consisting of a series of stratified and laminated quartose schists, partly kaolinised and intermixed with clay and hornblende schist, and small veins of limonite and hematite ironstone. The whole was very decomposed. There was also a north-south lode of finely laminated quartz embedded in a lode of decomposed hornblende schist. This description is for the upper levels, from limited development work.
The following is from a CSIRO report in 2003. The mineralised zone is schist to 20 metres thick, dipping 10 to 40 degrees west, and strikes north north-east for about 1 kilometre. The trend thins to the north, outcrops poorly, variably weathered to a depth of 40 to 50 metres. The wall rocks are tholeiitic metabasalt, now metamorphosed to amphibolite, with minor interflow sediments and dolerite. These have been intruded by felsic dykes, and small quartz-schorl veinlets.
The weathered profile is truncated by saprolite, and blocks of saprock surrounded by brownish saprolite can be seen in the pit wall. The soil is structureless carbonate rich brown loam, small iron nodules, a few fibrous halite crystals, and at the base of the soil a 5 to 20 mm layer of coarse decussate gypsum crystals. The soil also contains quartz, kaolinite, smectite, hematite, goethite, minor maghemite, sericite, calcite, and trace anatase and K feldspar. Gold in the saprolite is patchy. There is a zone of enrichment 30 metres below the surface, but no corresponding zone of depletion.
Feldspar porphyry bodies occur in the schist, along the Hanging Wall, and beneath the Footwall. The porphyry is biotite altered, tightly folded.
Fresh angular schorl is abundant near the gold, which is found in intensely foliated and laminated biotite-plagioclase-actinolite-calcite-quartz schist. The base of the zone contains intense quartz-feldspar alteration, with up to 10% pyrite and pyrrhotite, trace chalcopyrite and sphalerite, with zones of schorl. Generally the deposit is sulphide poor, with coarse gold found in quartz veins.
At Lights of Israel an ore shoot within the shear has been tracked with drilling for approximately 1.5 km down plunge and mined approximately 900 m down plunge. A similar shoot development could occur in the adjacent Maiki and Great Ophir deposits
Commodity ListThis is a list of exploitable or exploited mineral commodities recorded at this locality.
17 valid minerals.
Rock Types Recorded
Select Rock List TypeAlphabetical List Tree Diagram
Entries shown in red are rocks recorded for this region.
- Igneous rock
- Sedimentary rock and sediment
- Metamorphic rock
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
0 - 2.588 Ma
Age: Pleistocene (0 - 2.588 Ma)
Comments: regolith; synthesis of multiple published descriptions
Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia). 
|Neoarchean - Mesoarchean|
2500 - 3200 Ma
|Archean intrusive rocks|
Age: Archean (2500 - 3200 Ma)
Comments: Yilgarn Craton
Lithology: Intrusive igneous rocks
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529.