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Piopiotahi (Milford Sound) Marine Reserve is a marine reserve covering an area of 690 hectares (1,700 acres) in the Milford Sound / Piopiotahi, in Fiordland on New Zealand's South Island. It was established in 1993 and is administered by the Department of Conservation .
Milford Sound (Māori: Piopiotahi, officially gazetted as Milford Sound / Piopiotahi) is a fiord in the south west of New Zealand's South Island within Fiordland National Park, Piopiotahi (Milford Sound) Marine Reserve, and the Te Wahipounamu World Heritage site.
Milford Sound village covers 8.34 km 2 (3.22 sq mi), [1] and is part of the much larger but almost entirely unpopulated Fiordland statistical area. [ 15 ] The village had a population of 105 at the 2018 New Zealand census , an increase of 9 people (9.4%) since the 2013 census , and unchanged since the 2006 census .
The fiords of New Zealand (Māori: tai matapari "bluff sea" [1] [2]) are all located in the southwest of the South Island, in a mountainous area known as Fiordland. A fiord is a narrow inlet of the sea between cliffs or steep slopes, which results from marine inundation of a glaciated valley .
The main tourist attractions within Te Wahipounamu are Milford Sound / Piopiotahi and the Milford Track, Lake Te Anau and the Kepler Track, the Routeburn Track and Mount Aspiring / Tititea, Aoraki / Mount Cook and the Haupapa / Tasman, Franz Josef, and Fox Glaciers. There are only two main roads in the region, the Haast Highway and Milford Highway.
RealNZ is a New Zealand tourism company based in Queenstown.The company offers a range of travel, cruises and excursions in Queenstown, Milford Sound / Piopiotahi, Te Anau, Fiordland and Stewart Island / Rakiura. [1]
Bowen Falls. The Bowen Falls (Māori: Hineteawa), also known as Lady Bowen Falls, is a popular tourist attraction at Milford Sound, a fiord in New Zealand. [1]The 9-kilometre (5.6 mi) long Bowen River located in Fiordland National Park supplies the waterfall with water; the Bowen River is also used to generate electricity and supply drinking water to the nearby locality also named Milford Sound.
The most prominent differences between the New Zealand English dialect and other English dialects are the shifts in the short front vowels: the short-i sound (as in kit) has centralised towards the schwa sound (the a in comma and about); the short-e sound (as in dress) has moved towards the short-i sound; and the short-a sound (as in trap) has ...