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Magdala gold deposit (Magdalena mine), Stawell, Northern Grampians Shire, Victoria, Australia

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Gold mineralization in the Magdala deposit at Stawell is hosted within deformed turbidites and the underlying mafic volcanic successions. This setting is atypical when compared to the slate-hosted gold deposits elsewhere in the Lachlan orogen.

Note: the 'Hangingwall reefs' are high-grade auriferous quartz lodes that occur in the upper levels of the Magdalena mine (Henry et al., 2006).
Gold was produced from these reefs in 1856-1880.

Mineral List

23 entries listed. 21 valid minerals.

The above list contains all mineral locality references listed on 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 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.


- Econ Geol (1994) 89:566-583
- J. McL. Miller and C. J. L. Wilson (2002): The Magdala Lode System, Stawell, Southeastern Australia: Structural Style and Relationship to Gold Mineralization across the Western Lachlan Fold Belt. Economic Geology 97, 325-349.
- A. L. Dugdale, C. J. L. Wilson and R. J. Squire (2006): Hydrothermal alteration at the Magdala gold deposit, Stawell, western Victoria. Australian Journal of Earth Sciences 53 (in press)
- Henry, D. A. et al. (2006): Australian Journal of Earth Sciences 53, 759-766.
- Mineralium Deposita 43 (2008), 759-776.
- Mineralium Deposita (2009) 44, 205-219
- Dugdale, A. L. et al. (2010): Gold mineralization under cover in southeast Australia: A review of an exploration initiative for Stawell-type deposits. Ore Geology Reviews, 37, 41-63.


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