75km south west of Bundaberg, Queensland, Australia
Year commenced operations
2001
History
1998: Project acquired by Equigold NL
2001: Gold production commences
2008: Equigold NL Merger with Lihir Gold Limited
2010: Lihir Gold Limited Merger with Newcrest
2011: 1Moz gold produced since commissioning
2011: Evolution acquired 100% of Mt Rawdon via Catalpa Resources and Conquest Mining merging and the concurrent acquisition of Newcrest Mining's Cracow and Mt Rawdon gold mines.
Style of mineralisation
Volcaniclastic hosted
Contained metals
Gold, silver
Measured, Indicated and Inferred Resources (at 31 Dec 2012)
Conventional crush-grind-CIL to produce gold-silver dore
Nominal treatment rate
3.5Mtpa
Forecast mine life
10 years
Geology
The Mt Rawdon gold deposit is a massive, volcaniclastic hosted, low grade gold deposit that exhibits excellent characteristics conducive to low cost mining and treatment. The surface extent of mineralisation greater than 0.7g/t gold formed an ovoid zone 400 metres x 280 metres in diameter on the southern flanks of the original Mt Rawdon. The gold mineralisation is closely associated with fine disseminated pyrite within the host rocks as well as more discrete sulphide veinlets. Gold grade generally increases as pyrite alteration and sulphide veining increases. The principal host volcaniclastic rocks dip moderately to the southwest, as does the orebody.
Mining
Mines production is derived from a single open pit, utilising conventional drill and blast, load and haul methodologies. These functions are undertaken by separate contractors with management by Evolution staff. The operation is scheduled to continue until FY2023 at current estimates with a life-of-mine strip ratio of 2.2:1.
Processing
The processing plant consists of primary and secondary crushing, SAG and ball milling, followed by conventional cyanidation leaching. Mill throughput is maintained at ~3.5Mtpa of ore with a recovery of approximately 90%.