Cannington Mine
The Cannington Silver and Lead Mine is an Australian underground mine located in north-west Queensland, in the Shire of McKinlay, about southeast of Mount Isa. The deposit was discovered by BHP in 1990. The mine was the supplier of silver for the Sydney 2000 Summer Olympics and the Beijing 2008 Summer Olympics. Cannington takes its name from the pastoral property near the deposit.
Geography
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 of annual rainfall falling mostly between November and March. The mine itself lies near the confluence of the Hamilton River and Trepell Creek.Climate
Due to its very high evapotranspiration, Cannington Mine has a subtropical desert climate with very hot, erratically wetter summers and very mild, dry winters. The wettest recorded day was 27 March 2019 with of rainfall. Extreme temperatures ranged from on 14 January 2013 to on 20 July 2004.Climate data was taken from the nearest weather station at Trepell Airport.
Geology
The deposit is in Paleoproterozoic to Mesoproterozoic metamorphosed sedimentary rocks, known as the "Soldier's Cap Group", and is overlain by approximately 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, Mount Isa, Hilton, and George Fisher, is explored in a 2005 paper by Large, et al.
The major ore minerals are galena and sphalerite. The silver occurs mainly as freibergite but is also present in solid solution within the galena.