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Lake Alabaster
Lake Alabaster / Wāwāhi Waka, also known by the Māori name of ''Waiwahuika'', lies at the northern end of Fiordland, in the southwest of New Zealand's South Island. The lake runs from northeast to southwest, is , and covers . Lake Alabaster drains, and is drained by, the Pyke River, a small tributary of the Hollyford River / Whakatipu Kā Tuka. It is one of two lakes (along with Lake McKerrow / Whakatipu Waitai) found in the lower reaches of the Hollyford River system. A branch of the Hollyford Track, one of New Zealand's most well-known and popular tramping Tramping may refer to: Travel *Hiking *Trekking *Tramping in New Zealand, a style of backpacking or hiking * Czech tramping, a Czech outdoors pastime Places * Rural Municipality of Tramping Lake No. 380, Saskatchewan, Canada ** Tramping Lake, Sas ... tracks, extends along the eastern shore of the lake. The lake was formed at the southern end of a glacial valley and, had the sea level been slightly higher, would have ...
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Hollyford Track
The Hollyford Track is a tramping track in New Zealand. Located at the northern edge of Fiordland, in the southwestern South Island, it is unusual among Fiordland's major tracks in that it is largely flat and accessible year-round. It follows the Hollyford River which in turn follows the course of the Hollyford Valley. History The Māori people were the first to settle the area around Martins Bay, though by the time of the arrival of Europeans in the mid-19th century, only a handful remained in the area. One of these was Tūtoko, for whom Mount Tūtoko, which rises 2700m above the Hollyford valley, was subsequently named. he first Europeans to reach the bay via an inland route was Patrick Caples from Hollyford County Tipperary Ireland in 1863, although early runholders David McKellar and George Gunn had mapped some of the valley two years previously. Also in 1863, a small ship captained by a Captain Alabaster crossed the sandbar at Martins Bay to reach Lake McKerrow. In the ...
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South Island
The South Island, also officially named , is the larger of the two major islands of New Zealand in surface area, the other being the smaller but more populous North Island. It is bordered to the north by Cook Strait, to the west by the Tasman Sea, and to the south and east by the Pacific Ocean. The South Island covers , making it the world's 12th-largest island. At low altitude, it has an oceanic climate. The South Island is shaped by the Southern Alps which run along it from north to south. They include New Zealand's highest peak, Aoraki / Mount Cook at . The high Kaikōura Ranges lie to the northeast. The east side of the island is home to the Canterbury Plains while the West Coast is famous for its rough coastlines such as Fiordland, a very high proportion of native bush and national parks, and the Fox and Franz Josef Glaciers. The main centres are Christchurch and Dunedin. The economy relies on agriculture and fishing, tourism, and general manufacturing and services. ...
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Pyke River
The Pyke River is a river in the south west of New Zealand's South Island. It flows generally south into Lake Wilmot then Lake Alabaster, before becoming a tributary of the Hollyford River. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Fiordland {{Fiordland-river-stub ...
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Māori Language
Māori (), or ('the Māori language'), also known as ('the language'), is an Eastern Polynesian language spoken by the Māori people, the indigenous population of mainland New Zealand. Closely related to Cook Islands Māori, Tuamotuan, and Tahitian, it gained recognition as one of New Zealand's official languages in 1987. The number of speakers of the language has declined sharply since 1945, but a Māori-language revitalisation effort has slowed the decline. The 2018 New Zealand census reported that about 186,000 people, or 4.0% of the New Zealand population, could hold a conversation in Māori about everyday things. , 55% of Māori adults reported some knowledge of the language; of these, 64% use Māori at home and around 50,000 people can speak the language "very well" or "well". The Māori language did not have an indigenous writing system. Missionaries arriving from about 1814, such as Thomas Kendall, learned to speak Māori, and introduced the Latin alphabet. In 1 ...
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Fiordland
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. Due to the often steep terrain and high amount of rainfall supporting dense vegetation, the interior of the Fiordland region is largely inaccessible. As a result, Fiordland was never subjected to notable logging operations, and even attempts at whaling, seal hunting, and mining were on a small scale and short-lived, partly also because of the challenging weather. Today, Fiordland contains by far the greatest extent of u ...
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Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ...
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Hollyford River / Whakatipu Kā Tuka
The Hollyford River / Whakatipu Kā Tuka is in the southwest of the South Island of New Zealand. It runs for through Fiordland, its sources being close to the Homer Tunnel and in Gertrude Valley in the southern Darran Mountains. At first, the river flows southeast and east, coming as close as 1km to the east-west divide of the South Island, before continuing north through the glacier-formed Hollyford Valley. Near the end, the river passes through Lake McKerrow before reaching Martins Bay on the coast of the Tasman Sea north of Milford Sound. The Hollyford Track follows the river's course. Part of the river's course is traditionally regarded as the boundary between the Southland and Otago Otago (, ; mi, Ōtākou ) is a region of New Zealand located in the southern half of the South Island administered by the Otago Regional Council. It has an area of approximately , making it the country's second largest local government reg ... regions, however, current maps show ...
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Lake McKerrow / Whakatipu Waitai
Lake McKerrow / Whakatipu Waitai lies at the northern end of Fiordland, in the southwest of New Zealand's South Island. The lake runs from southeast to northwest, is in length, and covers . Lake McKerrow drains, and is drained by, the Hollyford River. It is one of two lakes (along with Lake Alabaster) found in the lower reaches of the Hollyford River system, and the Hollyford Track, one of New Zealand's most well-known and popular tramping tracks, follows its eastern shore for its full length. The lake is technically a fiord which has been cut off from the Tasman Sea by sediment. The sea is now three kilometres from the lake's northern end. The Alpine Fault goes through the lake. Researchers from GNS Science and University of Nevada, Reno have studied sediments from the 24 last Alpine Fault earthquakes near the lake and have found the most regular rupture behaviour yet observed. Following the passage of the Ngai Tahu Claims Settlement Act 1998 Ngai (also called Múrungu or E ...
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Tramping In New Zealand
Tramping, known elsewhere as backpacking, rambling, hill walking or bushwalking, is a popular activity in New Zealand. Tramping is defined as a recreational activity involving walking over rough country. Trampers often carry a backpack and wet-weather gear, and may also carry equipment for cooking and sleeping. History Alpine climbing has been a recreational activity from the early days of European settlement, and possibly earlier. From the 1950s tracks, huts and bridges were built in the forested areas of New Zealand to support hunters culling introduced deer species which had become a threat to the biodiversity of New Zealand. As tramping became popular these facilities were increasingly used by trampers. In later years tramping has become popular for both local and foreign tourists. Tramping clubs were formed in many towns, cities and universities with regular trips being organised. The clubs sometimes own a bus to transport club members to the tracks. Tramping tracks A n ...
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