The Cannington Silver and Lead Mine is an Australian underground mine located in north-west Queensland, in the Shire of McKinlay, about 200 kilometres (124 mi) southeast of Mount Isa. The deposit was discovered by Broken Hill Proprietary Company (BHP) in 1990.[1] Although sitework and underground mining began in 1997, full production was not achieved until early 1999, with 1.5 million tons of ore processed in 1999.[2] Production since has reached 3 million tons of ore per year.[2] As of 2010 it was the largest and lowest cost silver and lead mine in the world.[3][4] The expected life of the Cannington mine is 25 years.[4] On August 19, 2014, the mine's owner BHP Billiton announced it was splitting the company in two. A newly formed entity called South32 is to house BHP Billiton's non-core businesses including the Cannington Mine. South32 is listed on the Australian Securities Exchange (under the code S32), with a secondary listing in Johannesburg.[5]

Cannington mine
Opened1997 (1997)


Cannington lies on a broad plain with a few low mesas. The plain is crossed by meandering rivers which are dry for a large part of the year, but which flood periodically. The area is semi-arid with 250 millimetres (9.84 in) of annual rainfall falling mostly between November and March. The mine itself lies near the confluence of the Hamilton River and Trepell Creek.[4]


The deposit is in Paleoproterozoic to Mesoproterozoic (2500–1000 mya) metamorphosed sedimentary rocks, known as the "Soldier's Cap Group", and is overlain by approximately 60 metres (197 ft) of Cretaceous and more recent overburden. The deposit was discovered as result of an aeromagnetic survey of the Soldiers Cap Group in the eastern Mount Isa inlier. The area was selected for survey based upon extrapolations from known prospects and associated lithostratigraphy. In other words, the rocks were the same as other known prospects, only slightly more deeply buried. The aeromagnetic survey pinpointed Cannington as a potential site and subsequent drilling proved it out.

The theory of formation of the Cannington deposit, and the related deposits at McArthur River, Century, Mt Isa, Hilton, and George Fisher, is explored in a 2005 paper by Large, et al.[6]

The major ore minerals are galena and sphalerite. The silver occurs mainly as freibergite but is also present in solid solution within the galena.


  1. ^ Walters, Stephen; Skrzeczynski, Bob; Whiting, Tom; Bunting, Frank; Arnold, Gary (2002). "Discovery and Geology of the Cannington Ag-Pb-Zn Deposit, Mount Isa Eastern Succession, Australia: Development and Application of an Exploration Model for Broken Hill-Type Deposits". In Goldfar, Richard J.; Nielsen, Richard L. (eds.). Integrated methods for discovery: Global exploration in the 21st Century. Littleton, Colorado: Society of Economic Geologists. pp. 93–116. ISBN 978-1-887483-91-9. Abstract Archived 2011-02-25 at the Wayback Machine
  2. ^ a b Staff (2011). "Cannington Silver and Lead Mine, Queensland, Australia". of Net Resources International. Archived from the original on 26 February 2013. Cite uses deprecated parameter |deadurl= (help)
  3. ^ Obel, Mike (15 December 2011). "10 Biggest Silver Mines in the World". International Business Times. Archived from the original on 26 May 2013. Cite uses deprecated parameter |deadurl= (help)
  4. ^ a b c "Cannington". Mine Sites: Major Mining Operations Around the World. 2010. Archived from the original on 24 September 2010. Cite uses deprecated parameter |deadurl= (help)
  5. ^
  6. ^ Large, Ross R.; Bull, Stuart W.; McGoldrick, Peter J.; Walters, Stephen (2005). "Stratiform and strata-bound Zn-Pb-Ag deposits in Proterozoic sedimentary basins, northern Australia". In Hedenquist, Jeffrey W. (ed.). Economic Geology 100th Anniversary Volume: 1905-2005. Littleton, Colorado: Society of Economic Geologists. pp. 931–963. ISBN 978-1-887483-01-8.

Coordinates: 21°51′23″S 140°54′25″E / 21.8564°S 140.9070°E / -21.8564; 140.9070