Project Overview

Foster nickel mine was mined by WMC between 1981/82 and 1994. The nickel trough systems accessed underground at this mine produced over 60,000 tonnes of nickel metal. Foster’s nickel production represented up to 30% of the feed at WMC’s Kambalda Concentrator during its peak production period.

The mine is host to four distinct nickel mineralised surfaces or shoots that contain current Mineral Resources reported in accordance with JORC 2012 guidelines and approximately 45 sub-surfaces that play host to historical nickel mineralisation when the mine closed in 1994.

A close up of a black surface.

Famous kambalda nickel belt

The Kambalda Nickel Project (KNP) (shown outlined in red on the adjacent image) features approximately 47km2 of tenements in the Kambalda Nickel District. The KNP is located approximately 570km east of Perth and 50-70km south-southeast of Kalgoorlie, in the Eastern Goldfields of Western Australia. KNP comprises two project areas, Foster and Baker* (19 contiguous mining leases) and Silver Lake and Fisher+ (20 contiguous mining leases).

The world-renowned Kambalda Nickel District has produced in excess of 1.6 million tonnes of nickel metal since its discovery in 1966 by WMC Resources Ltd. In addition, over 15Moz of gold in total has been mined, making the Kambalda/St Ives district a globally significant gold camp in its own right.

The KNP is assessed via public roads, well-established mine road infrastructure and the main St Ives causeway over Lake Lefroy. The KNP is broadly surrounded by tenements held by St Ives Gold Mining Co. Pty Ltd (SIGM), a wholly owned subsidiary of Gold Fields Limited (JSE:GFI) and the Company’s major shareholder.

Foster nickel mine itself is the location of the Company’s site office, hosted in the offices and workshop built to service the mine during its operational life. The mine has over 9.5km of previous decline development (currently flooded), a decline portal access and a shaft that reaches over 750m below surface. The mine and all the Company’s current Mineral Resource at Foster, sit on granted mining tenements, meaning that the regulatory requirements to move from being an explorer, to a developer/producer are modest.

Presently, it is forecast that no processing capital will be required as future nickel ore may be sent to the nearby BHP Nickel West concentrator with Nickel West retaining a right of pre-emption in relation to any proposal by Lunnon Metals to enter into any sales contract or other sales arrangement to realise any revenue or other benefit from the treatment or sale of nickel ore.

Foster Main

Excluding areas of the mine where mineralisation has now been estimated in accordance with the JORC 2012 guidelines and reported as Mineral Resources (namely Foster 85H, S16C/N14C, South and Warren Shoots) significant nickel metal was still reported by WMC at the time of closure in 1996. Note this original historical WMC figure is not capable of being reported under JORC 2012 guidelines.

  • Historical estimate figure is presently not capable of being reported under JORC 2012 guidelines;
  • A Competent Person has not done sufficient work to classify the historical estimates as Mineral Resources or Ore Reserves in accordance with the JORC Code; and
  • It is uncertain whether, following evaluation and/or further exploration work, the historical estimates will subsequently be able to be reported as Mineral Resources or Ore Reserves in accordance with the JORC Code.

Though challenging to assess and estimate, owing to the uncertainty in detail of what has been historically mined or left behind as remnant mineralisation, the main Foster Mine itself is a key target for potential growth in the Mineral Resource. The Company will focus on a thorough review of the extensive diamond drill core and pulp rejects library available at Kambalda, with a view to determining if noteworthy quantities of this remnant mineralisation may have the potential to be re-estimated in accordance with the JORC 2012 and potentially safely exploited in any future re-start and production scenario at the mine.


The 85H surface is a major hangingwall ore surface associated with the base of the interpreted second main ultramafic flow at Foster. It is characterised as an extensive, very planar structure of irregular low-high tenor variation within the mineralisation.

Partially developed on the historical 8, 9 and 10 Levels at Foster, but essentially unmined, the Company interprets this hangingwall mineralised surface to have the potential to extend to the south of the current development and up dip, where programs to test for 85H style nickel anomalism can be executed with surface RC drilling.

Foster South (64C)

Originally termed South, then renamed “Deeps – 64C” by WMC, the Foster South trough is believed to be either a fault offset segment of the main Foster trough system rotated to a more vertical plunge, or a potential new trough in its own right. The high grade massive sulphide hosted there is, under the Company’s current interpretation, open up and down plunge and is located just 300 metres beyond the end of the current main decline.

The up dip/plunge portions of the South minerlisation are being tested by both new surface diamond drilling together with the re-entry and DHTEM testing of historical WMC era surface holes seeking to intersect or locate concentrations of nickel sulphides in this trough.


Previously termed Foster NW by WMC, the area was accessed by an independent decline branching off the main Foster decline near to its portal, and limited development and stoping occurred before an uncontrolled water ingress required the area to be blocked off.

It is interpreted that the Warren Shoot ore trough runs sub-parallel to, potentially, the entirety of the Foster Main trough and may be a significant source of future nickel discovery in its own right. Once more, the up dip/plunge portions of the Warren trough will be tested by new RC and surface diamond drilling.


The N75C is a flanking basal contact surface located up-dip from the main incised Foster nickel channel. The nickel mineralisation itself is of moderate nickel grade largely characterised as 5-40% disseminated nickel sulphides increasing in intensity towards the base where there can be a narrower zone of stringer to massive nickel sulphides. The N75C mineralisation is part of an extensive flanking position surface on the basal contact extending up-dip (up-flank) from the main Foster channel and sits stratigraphically below the 85H hanging wall mineralised surface detailed above.

The S16C/N14C mineralisation is part of an extensive suite of mineralised surfaces at Foster that are in a flanking position at the base of the Kambalda Komatiite on the Lunnon Basalt footwall contact, which is interflow sediment covered in the case of S16C and partially sediment covered for N14C.

This flanking position extends up-dip (up flank) from the main Foster channel. The S16C/N14C surface is on the footwall side of a late intermediate dyke which splits this surface from the N75C mineralised surface (reported to the ASX on 22 April 2022).

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