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The Lake Te Anau control gates which control the flow of water from Lake Te Anau into the Waiau river and maintain the water level between 201.5 and 202.7 metres above sea level. [4] Several rivers feed the lake, of which the most important is the Eglinton River, which joins the lake from the east, opposite the entrance to North Fiord.
The Waiau River is the largest river in the Southland region of New Zealand. [1] ' Waiau' translates to 'River of Swirling Currents'. [2] It is the outflow of Lake Te Anau, flowing from it into Lake Manapouri 10 kilometres (6 mi) to the south, and from there flows south for 70 kilometres (43 mi) before reaching the Foveaux Strait 8 kilometres (5 mi) south of Tuatapere.
Stream near Te Ana-au cave mouth. The Te Ana-au caves are a culturally and ecologically important system of limestone caves on the western shore of Lake Te Anau, in the southwest of New Zealand. They were re-discovered in 1948 by Lawson Burrows, who found the upper entry after three years of searching, following clues in old Māori legends.
Te Anau is a town in the Southland region of the South Island of New Zealand. In Māori, Te-Anau means the Place of the Swirling Waters. [3] It is on the eastern shore of Lake Te Anau in Fiordland. Te Anau is 155 kilometres north of Invercargill and 171 kilometres to the southwest of Queenstown (via state highway 6). Manapouri lies 21 ...
Some tourists also arrive from the smaller tourism centre of Te Anau, 121 km (75 mi) away. There are also scenic flights by light aircraft and helicopter tours to and from Milford Sound Airport . The drive to Milford Sound itself passes through unspoiled mountain landscapes before entering the 1.2 km (0.75 mi) Homer Tunnel which emerges into ...
Te Anau glacial erratic Southland, Te Anau: Glacial deposition A Geological Reserve. During a past glacial advance this boulder was carried c. 50 km from the Fiordland mountains. [10: Truman Track [11] West Coast, Punakaiki Wave erosion