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| Mount Read | |
|---|---|
| Name | Mount Read |
| Elevation m | 1123 |
| Range | West Coast Range |
| Location | Tasmania, Australia |
| Coordinates | 42°05′S 145°24′E |
Mount Read Mount Read is a mountain on the West Coast of Tasmania, Australia, notable for its complex geology, historic mining operations, and alpine ecology. The mountain forms part of the West Coast Range near the communities of Zeehan and Queenstown and has influenced regional development through mining of copper, gold, and rare minerals. Its rugged terrain, distinctive peaks, and historical infrastructure attract interest from geologists, historians, and bushwalkers.
Mount Read is located within the West Coast Range of western Tasmania, positioned between the towns of Queenstown, Tasmania and Zeehan, Tasmania. The summit rises to approximately 1,123 metres above sea level and features steep ridgelines, glaciated cirques, and prominent spurs that drain into the Franklin River catchment and tributaries leading to the King River. Nearby geographic features include Mt Lyell, Mount Owen, and the Franklin-Gordon Wild Rivers National Park. The surrounding landscape includes highland plateaus, talus slopes, and historic mining infrastructure such as tramways and adits that trace the mountain’s flanks.
The mountain is renowned for its volcanogenic massive sulfide (VMS) and related hydrothermal deposits formed during the Cambrian and Ordovician orogenies associated with the Tasman Orogeny. Host lithologies include altered volcanics, felsic pyroclastics, and sedimentary interbeds correlated with the Lower Cambrian Mount Read Volcanics. Mineralization produced significant concentrations of chalcopyrite, bornite, pyrite, and associated arsenopyrite, along with economically important occurrences of gold and lead-zinc mineral assemblages. Famous mineral species documented in nearby mines include crocoite, stichtite, and strontianite, attracting collectors and mineralogists linked to institutions such as the Tasmanian Museum and Art Gallery and university geology departments at the University of Tasmania. Structural controls involve faulting and folding related to the Lachlan Fold Belt and regional tectonics that localized hydrothermal fluid flow and ore deposition.
The mountain experiences a cool, wet maritime climate influenced by the Roaring Forties and proximity to the Southern Ocean, producing high precipitation, snow in winter months, and frequent cloud cover. Alpine and subalpine vegetation zones host endemic and relict species characteristic of Tasmanian highlands, with communities of Eucalyptus delegatensis (alpine ash) at lower elevations transitioning to montane shrubland and cushion plants such as species found in the Tasmanian Wilderness World Heritage Area. Fauna includes populations of Tasmanian devil, Bennetts wallaby, and various endemic bird species like the Green rosella and Forty-spotted pardalote in broader regional habitats. Peatlands and wet heaths on the flanks support bryophyte assemblages studied by researchers associated with the Australian National University and conservation agencies such as the Tasmanian Parks and Wildlife Service.
European exploration and exploitative activities accelerated in the late 19th century with prospectors from Victoria and prospecting syndicates forming companies such as the Mount Lyell Mining and Railway Company and smaller concession holders operating near the mountain. Mining of copper, gold, and silver led to the development of shafts, adits, and tramways connected to coastal ports including Strahan, Tasmania. The discovery of unusual minerals like crocoite attracted scientific attention from figures connected to the Royal Society of Tasmania and collectors whose specimens entered collections at institutions including the British Museum (Natural History). Industrial heritage includes remnants of hydroelectric schemes, rail infrastructure linked to the Emu Bay Railway, and settlements that shaped the social history of Queenstown, Tasmania and Zeehan, Tasmania. Environmental and Indigenous histories intersect with operations that affected traditional lands of Tasmanian Aboriginal communities and prompted later remediation and heritage protection efforts led by agencies including the Australian Heritage Council.
Access to the mountain is typically via gravel roads and historical tracks from Queenstown, Tasmania and Zeehan, Tasmania, with bushwalkers and mountaineers using routes that traverse historic mine workings and alpine terrain. Recreational activities include day hiking, birdwatching tied to organizations such as the Field Naturalists Club of Victoria, and specialist mineral-collecting excursions coordinated with museum curators from institutions like the Tasmanian Museum and Art Gallery. Conservation frameworks involve management by the Tasmanian Parks and Wildlife Service and inclusion of surrounding landscapes within the Tasmanian Wilderness World Heritage Area buffer zones and regional planning by the Department of State Growth (Tasmania). Ongoing challenges balance heritage tourism, biodiversity protection, and remediation of legacy mining contamination, addressed through programs involving the Commonwealth Scientific and Industrial Research Organisation and state environmental agencies.