Fiordland is a geographical region of New Zealand in the south-western corner of the South Island, comprising the westernmost third of Southland. Most of Fiordland is dominated by the steep sides of the snow-capped Southern Alps, deep lakes, and its steep, glacier-carved and now ocean-flooded western valleys. The name "Fiordland" comes from a variant spelling of the Scandinavian word for this type of steep valley, "fjord". The area of Fiordland is dominated by, and very roughly coterminous with, Fiordland National Park, New Zealand's largest National Park.
Fiordland National Park occupies the southwest corner of the South Island of New Zealand. It is by far the largest of the 13 national parks in New Zealand, with an area of 12,607 square kilometres (4,868 sq mi), and a major part of the Te Wahipounamu World Heritage Site. The park is administered by the Department of Conservation.
Fox Glacier is a 13-kilometre-long (8.1 mi) temperate maritime glacier located in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. Like nearby Franz Josef Glacier, Fox Glacier is one of the most accessible glaciers in the world, with a terminal face as low as 300 m above sea level, close to the village of Fox Glacier. It is a major tourist attraction and about 1000 people daily visit it during high tourist season.
The Routeburn Track is a world-renowned, 32 km tramping (hiking) track found in the South Island of New Zealand. The track can be done in either direction, starting on the Queenstown side of the Southern Alps, at the northern end of Lake Wakatipu or on the Te Anau side, at the Divide, several kilometres from the Homer Tunnel to Milford Sound.
Lake Monowai is a large lake in the southern part of Fiordland National Park, in New Zealand's South Island, 120 kilometres northwest of Invercargill. At an altitude of 180 metres in a long curved valley, the lake appears on maps shaped like a letter "U". The western part of the lake is set in beautiful mountainous country. It is drained in the northeast by the short Monowai River, which enters the Waiau River eight kilometres to the northeast.
Lake Hauroko is the deepest lake in New Zealand. The lake, which is 462 metres deep, is located in a mountain valley in Fiordland National Park.
Lake Waikaremoana is located in Te Urewera in the North Island of New Zealand, 60 kilometres northwest of Wairoa and 80 kilometres west-southwest of Gisborne. It covers an area of 54 km2 (21 sq mi). From the Māori Waikaremoana translates as 'sea of rippling waters'.
The Waiau River is the largest river in the Southland region of New Zealand. 'Waiau' translates to 'River of Swirling Currents'. 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. It also takes water from Lake Monowai.
Rotomairewhenua / Blue Lake is a small lake in Nelson Lakes National Park, in the northern reaches of New Zealand's Southern Alps. Sacred to local Māori, it has the clearest natural fresh water in the world.
HMNZS Monowai (F59) was a former Peninsular and Oriental Steam Navigation Company (P&O) merchant vessel. At the outbreak of World War II she became an armed merchant cruiser of the Royal New Zealand Navy (RNZN). She subsequently became HMS Monowai, a Landing Ship, Infantry and mostly operated as a troopship. In 1946 she returned to her old trade as a passenger ship.
The Monowai Power Station, fed by the Monowai River from Lake Monowai in Southland, New Zealand, was one of the earliest hydroelectric power stations in the country. Originally commissioned in 1925, it was refurbished between 2005 and 2007 and now contains modern turbines and plant, though the original buildings are still in use.
The Wilmot Pass is a 671 m (2,201 ft) high pass on the main divide of New Zealand's South Island. It connects Doubtful Sound, a deep indentation in the coast of Fiordland, to the valley of the West Arm of Lake Manapouri. The pass is named after E. H. Wilmot, a former surveyor-general of New Zealand, who had noted it while surveying the area in 1897. It lies between Mount Wilmot and Mount Mainwaring. On the east side the Spey River drains to Lake Manapouri and on the west side the Lyvia River drains to Deep Cove.
The Hunter Mountains of Lake Manapouri, New Zealand, were named by surveyor James McKerrow after the famous anatomist John Hunter. The Hunter Mountain Range covers an area between The South Arm and Hope Arm of Lake Manapouri South to the Green Lake.
The Grebe River is a river in Fiordland, New Zealand. It arises north-west of Lake Monowai in an area once part of the lake but cut off by an enormous landslide about 13,000 years ago. The river now flows north, between the Townley Mountains to the west, and the Hunter Mountains to the east, and into Lake Manapouri's South Arm. Its major tributaries are Jaquiery Stream, Florence Stream, Emerald Stream, and Percy Stream, all from the west.
The Monowai River is a river in New Zealand, draining Lake Monowai into the Waiau River and feeding the Monowai Power Station.
The Stanley River is a river of the Tasman Region of New Zealand's South Island. It flows southeast from its sources in the Douglas and Anatoki Ranges, reaching the Waingaro River 12 kilometres west of Upper Takaka.
The Guardians of Lake Manapouri, Monowai and Te Anau is a statutory body appointed to make recommendations to the New Zealand Minister of Conservation on any matters arising from the environmental, ecological, and social effects of the operation of the Manapouri Power Station on the townships of Manapouri and Te Anau, Lake Manapouri and Lake Te Anau and their shorelines, and on the rivers flowing in and out of those lakes, having particular regard to the effects of the operation on social values, conservation, recreation, tourism, and related activities and amenities.
Monowai Seamount is a volcanic seamount to the north of New Zealand. It is formed by a large caldera and a volcanic cone just south-southeast from the caldera. The volcanic cone rises to depths of up to 100 metres (330 ft) but its depth varies with ongoing volcanic activity, including sector collapses and the growth of lava domes. The seamount and its volcanism were discovered after 1877, but only in 1980 was it named "Monowai" after a research ship of the same name.
