With an elevation of 1,123 metres (3,684 ft) above sea level, Mount Read has had as colourful a history, similar to that of Mount Lyell, with mines, settlements and other activities on its slopes for over a hundred years.
The main copper and gold ore bearing deposits in the West Coast Range are known to occur in the Mount Read Volcanics relating to the complex geology of the area.[4][5][6]
Mineralisation and deposits were being identified well beyond the life of the original mines utilised on Mount Read.[7]
The Hercules Mine on Mount Read was connected by a 1,642-foot (500 m) haulage incline to Williamsford and then to the North East Dundas Tramway. The haulage was self-acting and 1-mile (1.6 km) long and 1,642 feet (500 m) high with a maximum gradient of 1 in 5.[9][10]
The mine was in production in the late nineteenth century.[11] It had a major strike in 1906.[12][13] The mine produced well into the mid twentieth century.[14] The mine site had ceased operation and was subject to cleanup processes in the early 2000s.[15][16]
The Hercules Gold and Silver Mining Company was an operating company that ceased in 1916.[17] The Mount Read and Rosebery Mines Limited started as an ex-Mount Lyell offshoot, absorbed by EZ by 1925.[18][19]
The community, mainly known in early sources as the Mount Read township surrounding the Hercules minesite had various struggles for services and facilities.[20][21] The hotel is mentioned as early as 1898[22]
Situated at 1000 metres Mount Read (township) was the most elevated town which has existed in Tasmania[23]
Despite extensive historic mining and human activity on its slopes, Mount Read has unique and significant stands of Huon pine forests on its slopes.[24] The southern slopes of Mount Read have been identified as a special habitat[25][26] enclosed in the Lake Johnston Nature Reserve.[27]
Mount Read has an alpine subpolar oceanic climate (Köppen climate classification: Cfc), bordering on a tundra climate (Köppen climate classification: ET). It currently has a Bureau of Meteorologyautomatic weather station in place, and it scores well in extreme weather conditions. Its extreme rainfall records for Autumn 2006 put it on a par with the Lake Margaret rainfall – which was still apparently recorded till 30 June 2006 by Hydro employees, but not appearing on the BOM website. It has one of the highest annual rain day amount in the world at 282 days, topping Cherrapunji in India, but falling behind Mount Waialeale in Hawaii and López de Micay in Colombia, which have 335 and 315 rainy days respectively. Its monthly temperature averages are comparable to those of Reykjavík in Iceland. Snowfalls are highly frequent and often very heavy, occurring at all times of the year. The mean afternoon relative humidity is the greatest anywhere in Australia, particularly in the cooler months.
Climate data for Mount Read (1996–2022); 1,120 m AMSL; 41.84° S, 145.54° E
^Collins, P. L. F.; Large, Ross R.; University of Tasmania (1986), "The Mount Read volcanics and associated ore deposits : a symposium, Burnie, November 1986", Department of Mines, Tasmania, Geological Society of Australia, Tasmanian Division, ISBN978-0-7246-1955-9
^"MEETING". The Mercury. Hobart, Tas. 25 March 1899. p. 1 Supplement: The Mercury Supplement. Retrieved 10 June 2015 – via National Library of Australia.
^Electrolytic Zinc Co. of Australasia. West Coast Department (1957), Operations of Rosebery and Hercules Mines, Tasmania, [Launceston, Tas.] [Electrolytic Zinc Company of Australasia Limited, West Coast Department], retrieved 10 June 2015
^"Mount Read". The Mercury. Vol. LXXII, no. 8904. Tasmania, Australia. 14 September 1898. p. 4. Retrieved 24 October 2024 – via National Library of Australia.
^page 148, photo caption for image number 73, titled Mount Read township, circa 1897. noting photos of the township also at images 68, Mount Read township in 1898, and 67 A snowy day at Mount Read, 1896 the last from the Zeehan and Dundas Herald, 25th December 1896
^Anker, Sharon A.; Colhoun, Eric A.; Barton, Charles E.; Peterson, Mike; Barbetti, Mike (2001). "Holocene Vegetation and Paleoclimatic and Paleomagnetic History from Lake Johnston, Tasmania". Quaternary Research. 56 (2): 264–274. Bibcode:2001QuRes..56..264A. doi:10.1006/qres.2001.2233. S2CID129934181.
Pink, Kerry. The west coast story : a history of Western Tasmania and its mining fields Rev. ed. Zeehan, Tasmania : West Coast Pioneers' Memorial Museum, 1984. ISBN0-9598295-2-0
Rae, Lou (2001). The Abt Railway and Railways of the Lyell region. Sandy Bay: Lou Rae. ISBN0-9592098-7-5.
Whitham, Charles (2003). Western Tasmania – A land of riches and beauty (Reprint 2003 ed.). Queenstown: Municipality of Queenstown.