Lake Wānaka
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Lake Wānaka
Lake Wānaka is New Zealand's fourth-largest lake and the seat of the town of Wānaka in the Otago region. The lake is 278 meters above sea level, covers , and is more than deep. "Wānaka" is the South Island dialect pronunciation of , which means "the lore of the tohunga or priest" or a place of learning. Geography Geography Lake Wānaka lies at the heart of the Otago Lakes in the lower South Island of New Zealand. The township of Wānaka, which sits in a glacier-carved basin on the shores of the lake, is the gateway to Mt Aspiring National Park. Lake Hāwea is a 15-minute drive away, en route to the frontier town of Makarora, the last stop before the West Coast Glacier region. To the south is the historic Cardrona Valley, a popular scenic alpine route to neighbouring Queenstown. Geology Lake Wānaka lies in a u-shaped valley formed by glacial erosion during the last ice age more than 10,000 years ago. It is fed by the Mātukituki and Makarora Rivers, and is the so ...
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Disruptive Editing
Disruption, disruptive, or disrupted may refer to: Business * Creative disruption, disruption concept in a creative context, introduced in 1992 by TBWA's chairman Jean-Marie Dru *Disruptive innovation, Clayton Christensen's theory of industry disruption by new technology or products Psychology and sociology * Disruptive behavior disorders, a class of mental health disorders * Disruptive physician, a physician whose obnoxious behaviour upsets patients or other staff * Social disruption, a radical alteration, transformation, dysfunction or breakdown of social life Other uses * Cell disruption is a method or process in cell biology for releasing biological molecules from inside a cell *'' Disrupted: My Misadventure in the Start Up Bubble'', a 2016 book by Daniel Lyons * Disruption (adoption) is also the term for the cancellation of an adoption of a child before it is legally completed * Disruption (of schema), in the field of computer genetic algorithms * Disruption of 1843, the div ...
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Mount Aspiring National Park
Mount Aspiring National Park is in the Southern Alps of the South Island of New Zealand, north of Fiordland National Park, situated in Otago and Westland regions. The park forms part of the Te Wahipounamu World Heritage site. Geography Established in 1964 as New Zealand's tenth national park, Mount Aspiring National Park covers at the southern end of the Southern Alps, directly to the west of Lake Wānaka, and is popular for tramping, walking and mountaineering. Mount Aspiring / Tititea, elevation above sea level, gives the park its name. Other prominent peaks within the park include Mount Pollux, elevation , and Mount Brewster, elevation . The Haast Pass, one of the three principal road routes over the Southern Alps, crosses the north-eastern corner of the park. History Landsborough Station added In April 2005 the Nature Heritage Fund purchased private land in the Landsborough River valley as an addition to the park. Milford Sound tunnel proposal In 2006, the Mil ...
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West Coast, New Zealand
The West Coast ( mi, Te Tai Poutini, lit=The Coast of Poutini, the Taniwha) is a region of New Zealand on the west coast of the South Island that is administered by the West Coast Regional Council, and is known co-officially as Te Tai Poutini. It comprises the territorial authorities of Buller District, Grey District and Westland District. The principal towns are Westport, Greymouth and Hokitika. The region, one of the more remote areas of the country, is also the most sparsely populated. With a population of just 32,000 people, Te Tai Poutini is the least populous region in New Zealand, and it is the only region where the population is declining. The region has a rich and important history. The land itself is ancient, stretching back to the Carboniferous period; this is evident by the amount of carboniferous materials naturally found there, especially coal. First settled by Kāi Tahu in approximately 1200 CE, the area was famous across New Zealand for its richness in pounamu ...
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Haast Pass
Haast Pass / Tioripatea is a mountain pass in the Southern Alps of the South Island of New Zealand. Māori used the pass in pre-European times. The pass takes its name from Julius von Haast, a 19th-century explorer who also served as provincial geologist for the provincial government of Canterbury. Following the passage of the Ngāi Tahu Claims Settlement Act 1998, the name of the pass was officially altered to Haast Pass / Tioripatea. The pass lies within the limits of Mount Aspiring National Park and forms part of the boundary between the Otago and West Coast regions. The Haast Pass is one of the three passes where a road crosses over the Southern Alps – alongside the Lewis Pass and Arthur's Pass, although the Homer Tunnel passes under the Main Divide. The Haast Pass rises to a height of above sea level at the saddle between the valleys of the Haast and Makarora Rivers. As such, it is the lowest of the passes traversing the Southern Alps. The route through Haast Pas ...
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Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to ...
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Albert Town, New Zealand
Albert Town is located to the east of Wānaka in Otago, New Zealand. Until recently only a farming settlement, the population boom in this area has led to much new development. The confluence of the Clutha and Hāwea Rivers is located here. The town was named after Prince Albert of Saxe-Coburg and Gotha. Albert Town was formerly called Newcastle. Demographics Albert Town covers and had an estimated population of as of with a population density of people per km2. Albert Town had a population of 2,031 at the 2018 New Zealand census Eighteen or 18 may refer to: * 18 (number), the natural number following 17 and preceding 19 * one of the years 18 BC, AD 18, 1918, 2018 Film, television and entertainment * ''18'' (film), a 1993 Taiwanese experimental film based on the sh ..., an increase of 744 people (57.8%) since the 2013 census, and an increase of 1,326 people (188.1%) since the 2006 census. There were 687 households. There were 1,020 males and 1,014 females, giv ...
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Hemideina Maori
''Hemideina maori'', also known as the mountain stone wētā, is a wētā of the family Anostostomatidae. They are a large, flightless, nocturnal orthopteran endemic to New Zealand. Mountain stone wētā are long lived and are found on many central mountain ranges in New Zealand's South Island. __TOC__ Taxonomy ''Hemideina maori'' was first described in 1891 by Swiss Entomologists Alphonse Pictet and Henri de Saussure. Habitat and distribution Unlike other ''Hemideina'' species ''H. maori'' occupy an alpine habitat. They are found at high elevation (above the tree line) of the South Island of New Zealand. They have been found above 1500 metres above sea level (m.a.s.l) with a lower limit of 1100m.a.s.l, from the Kaikoura Ranges south to the Rock and Pillar range in Otago. They use cavities under rock slabs ('tors') broken from schist outcrops as retreats during the day. Tors are separated by alpine meadows with no rocks and therefore are assumed to have no wētā, causin ...
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Television New Zealand
Television New Zealand ( mi, Te Reo Tātaki o Aotearoa), more commonly referred to as TVNZ, is a television network that is broadcast throughout New Zealand and parts of the Pacific region. All of its currently-operating channels are free-to-air and commercially funded. TVNZ was established in February 1980 following the merger of the two government-owned television networks, Television One (now TVNZ 1) and South Pacific Television (now TVNZ 2), under a single administration. It was the sole television broadcaster in New Zealand until November 1989 when private channel TV3 (now Three (TV channel), Three) was launched. TVNZ operates playout services from its Auckland studio via Kordia's fibre and microwave network for TVNZ 1, TVNZ 2 and TVNZ Duke, with new media video services via the American-owned Brightcove which is streamed on the Akamai Technologies, Akamai Real Time Messaging Protocol, RTMP/HTTP Live Streaming, HLS DNS based caching network. Its former channels include TVNZ Ki ...
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Weka
The weka, also known as the Māori hen or woodhen (''Gallirallus australis'') is a flightless bird species of the rail family. It is endemic to New Zealand. It is the only extant member of the genus '' Gallirallus''. Four subspecies are recognized but only two (northern/southern) are supported by genetic evidence. The weka are sturdy brown birds, about the size of a chicken. As omnivores, they feed mainly on invertebrates and fruit. Weka usually lay eggs between August and January; both sexes help to incubate. Description Weka are large rails. They are predominantly rich brown mottled with black and grey; the brown shade varies from pale to dark depending on subspecies. The male is the larger sex at in length and in weight. Females measure in length and weigh . The reduced wingspan ranges from . The relatively large, reddish-brown beak is about long, stout and tapered, and used as a weapon. The pointed tail is near-constantly being flicked, a sign of unease characterist ...
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Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called ''interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for t ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ...
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U-shaped Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, ...
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