Lake Gault
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| Lake Gault | |
|---|---|
Lake Gault | |
| Location | Fox Glacier, West Coast, South Island |
| Coordinates | 43°25′49″S 169°59′05″E / 43.43028°S 169.98472°E |
| Surface area | 31.8 ha (79 acres) |
| Average depth | 14.5 m (48 ft) |
| Surface elevation | 333 m (1,093 ft) |
| Location | |
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Lake Gault is a small glacial lake in South Westland, New Zealand, near the township of Fox Glacier. A walking track from Lake Matheson leads to the lake, which is surrounded by mature native forest. A small hydro-electric power plant was constructed piping water from the lake to power a gold mining dredge at Gillespies Beach. Endangered Ōkārito kiwi (rowi) have been released into the wild around Lake Gault.
Lake Gault is located at an altitude of 333 m (1,093 ft) in the Omoeroa Range. It has an area of 31.8 ha (79 acres) and an average depth of 14.5 m (48 ft). Its only access is via a 4-kilometre (2.5 mi) walking track that climbs 200 metres (660 ft) from the eastern shore of Lake Matheson.[1] The lake was created by glacial advance and retreat about 16,000 years ago, when moraines were deposited by what is now Fox Glacier in the Okarito Formation.[2]

Lake Gault drains into pakihi wetland to the north, part of Skiffington Swamp, which is itself drained to the west by the Waihapi Creek and to the east by the Hauraki Creek, both of which reach the coast of the Tasman Sea between Gillespies Point and the mouth of the Waikūkūpa River.[3]
Like nearby Lake Matheson, Lake Gault is dystrophic: its water is stained brown in colour with tannins leached from surrounding forest, low in nutrients, acidic, and has a sparse and specialised phytoplankton.[4][5] And as in Lake Matheson the dark water creates spectacular reflected views of the Southern Alps, especially Aoraki / Mount Cook and Mount Tasman.[6][7]
History
A pipeline takes water from Lake Gault over the ridgeline to a small hydroelectric power station on the Cook River flats. Built in the 1930s, the station powered a gold-mining dredge that worked the sands of Gillespies Beach 15 km to the west through to the 1940s.[6] In 1958 an earth dam was constructed between Lake Gault and Skiffington Swamp to the north to raise the lake level: by this time the hydroelectric plant was powering the village of Fox Glacier.[2]

