The West Coast Range is a mountain range located in the West Coast region of Tasmania, Australia.

The range lies to the west and north of the main parts of the Franklin-Gordon Wild Rivers National Park.

West Coast Range

The range has had a significant number of mines utilising the geologically rich zone of Mount Read Volcanics. A number of adjacent ranges lie to the east: the Engineer Range, the Raglan Range, the Eldon Range, and the Sticht Range but in most cases these are on a west–east alignment, while the West Coast Range runs in a north–south direction, following the Mount Read volcanic arc.

West Coast Range

The range has encompassed multiple land uses including the catchment area for Hydro Tasmania dams, mines, transport routes and historical sites. Of the communities that have existed actually in the range itself, Gormanston, is probably the last to remain.

West Coast Range

Geographical features

These are determined by a number of factors - the southerly direction of glaciation in the King River Valley and around the Tyndalls; as well as the general north -south orientation of the West Coast Range itself.

Mountains

The following mountains are contained within the West Coast Range, including sub-ranges without a specifically named peak and also including subsidiary peaks.

Smaller hills and features

Darwin Crater - a probable meteorite impact crater associated with Darwin glass

Gooseneck Hill

Henty Glacial Moraine

Marble Bluff - adjacent to the confluence of the Eldon and South Eldon rivers and the northern edge of Lake Burbury Teepookana Plateau Thureau Hills - adjacent to the eastern slopes of Mount Owen and Mount Huxley Walford Peak - adjacent to Lake Dora

Rivers

Anthony River on the northern part of the range

Bird River at the southern end of the range

Eldon River on the eastern side of the range

Governor River on the eastern side of the range

Henty River on the western side of the range

King River starting in the Eldon Range and passing between Mount Huxley and Mount Jukes, dammed by The Hydro Mackintosh River Murchison River Pieman River Queen River runs through Queenstown, then to join with the King River to the west of Mount Huxley Sophia River South Eldon River Tofft River runs between the Thureau hills and Mount Owen and Mount Huxley Yolande River between Lake Margaret and the Henty River

Lakes

Basin Lake - on the western side of the range

Lake Adam - a tributary lake for Lake Margaret

Lake Barnabas

Lake Beatrice - on the eastern edge of Mount Sedgwick

Lake Burbury - created by the damming of the King River by The Hydro

Lake Dora

Lake Dorothy

Lake Huntley - on the eastern side of Mount Tyndall

Lake Julia - in the area of the range known as 'The Tyndalls'

Lake Mackintosh - created by damming the Mackintosh River

Lake Magdala - a tributary lake for Lake Margaret

Lake Martha - tributary lake for Lake Margaret

Lake Mary, Tasmania - a tributary lake for Lake Margaret

Lake Margaret on the northern side of Mount Sedgwick

Lake Monica - tributary lake for Lake Margaret

Lake Murchison - created by the damming of the Murchison River

Lake Myra - tributary lake for Lake Margaret

Lake Paul - tributary lake for Lake Margaret

Lake Peter - tributary lake for Lake Margaret

Lake Philip - a tributary lake for Lake Margaret

Lake Plimsoll

Lake Polycarp - a tributary lake for Lake Margaret

Lake Rolleston - between the Tyndall Range and the Sticht Range

Lake Selina - just west of Lake Plimsoll

Lake Spicer - just west of Eldon Peak

Lake Tyndall - south of Mount Tyndall

Lake Westwood - next to Mount Julia

Reserves

Mount Farrell Regional Reserve

Mount Murchison Regional Reserve

Tyndall Regional Reserve

Lake Beatrice Conservation Area

Princess River Conservation Area

Crotty Conservation Area

West Coast Range Regional Reserve (Clark River Valley)

Vegetation

The slopes of Mount Owen, Mount Lyell and Mount Sedgwick are covered in stumps of forest trees killed by fires and smelter fumes from the earlier part of the twentieth century. The devastation of forests close to the mining operations at Queenstown was substantial as early as the 1890s and continued late into the twentieth century.

Some Huon Pine on the slopes of Mount Read have been found that show considerable age.