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Volta Glacier
The Volta Glacier is located in Mount Aspiring National Park in the Southern Alps of the South Island of New Zealand. It is split into upper and lower glaciers which are connected by an icefall. The Upper Volta Glacier is between in altitude and is surrounded by the 3 peaks of Glacier Dome, Pickelhaube and Fastness Peak, while the Lower Volta Glacier sits directly under the North side of Mount Aspiring / Tititea Mount Aspiring / Tititea is New Zealand's 23rd-highest mountain. It is the country's highest outside the Aoraki / Mount Cook region. Description Set within Otago's Mount Aspiring National Park, it has a height of . Māori named it ''Tititea'' ... and lies between . The Lower Volta Glacier feeds an unnamed lake at the Glacier Toe, which in turn feeds the Waiatoto River which eventually runs out to the West Coast. References Glaciers of New Zealand Landforms of the West Coast, New Zealand Mount Aspiring National Park {{WestCoastNZ-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Alps
The Southern Alps (; officially Southern Alps / Kā Tiritiri o te Moana) is a mountain range extending along much of the length of New Zealand's South Island, reaching its greatest elevations near the range's western side. The name "Southern Alps" generally refers to the entire range, although separate names are given to many of the smaller ranges that form part of it. The range includes the South Island's Main Divide, which separates the water catchments of the more heavily populated eastern side of the island from those on the west coast. Politically, the Main Divide forms the boundary between the Marlborough, Canterbury and Otago regions to the southeast and the Tasman and West Coast regions to the northwest. Names The Māori name of the range is , meaning "the Mirage of the Ocean". The English explorer James Cook bestowed the name ''Southern Alps'' on 23 March 1770, admiring their "prodigious height". p. 384. They had previously been noted by Abel Tasman in 1642, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 servi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pickelhaube
The ( pl. ; from german: Pickel, lit=point' or 'pickaxe, and , , a general word for "headgear"), also , is a spiked helmet that was worn in the 19th and 20th centuries by Prussian and German military officers, firefighters and police. Although it is typically associated with the Prussian Army, which adopted it in 1842–43, the helmet was widely imitated by other armies during that period. It is still worn today as part of ceremonial wear in the militaries of certain countries, such as Sweden, Chile, and Colombia. History Origins The Pickelhaube was originally designed in 1842 by King Frederick William IV of Prussia, perhaps as a copy of similar helmets that were adopted at the same time by the Russian military. It is not clear whether this was a case of imitation, parallel invention, or if both were based on the earlier Napoleonic cuirassier. The early Russian type (known as "The Helmet of Yaroslav Mudry") was also used by cavalry, which had used the spike as a holder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Aspiring / Tititea
Mount Aspiring / Tititea is New Zealand's 23rd-highest mountain. It is the country's highest outside the Aoraki / Mount Cook region. Description Set within Otago's Mount Aspiring National Park, it has a height of . Māori named it ''Tititea'', after a chief of the Waitaha tribe, who were the first people to settle the South Island. It was named ''Aspiring'' in December 1857 by the Chief Surveyor for the Otago Province, John Turnbull Thomson.Wises New Zealand Index, 7th Edition, 1979. p. 15. It is also often called 'the Matterhorn of the South,' for its pyramidal peak when seen from the Matukituki River. The first ascent was on 23 November 1909 by Major Bernard Head and guides Jack Clarke and Alec Graham. Head's party climbed to the summit ridge by the west face from the Bonar Glacier, a route not repeated until 1965. Mount Aspiring / Tititea sits slightly to the west of the main divide, 30 kilometres west of Lake Wānaka. It lies at the junction of three major glacial syst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waiatoto River
The Waiatoto River is a river of the West Coast of New Zealand's South Island. Formed from several small rivers which are fed by glaciers surrounding Mount Aspiring, it flows north along a valley flanked in the west by the Haast Range before turning northwest to reach the Tasman Sea southwest of Haast. Much of the river's length is within Mount Aspiring National Park. The New Zealand Ministry for Culture and Heritage gives a translation of "water of blood" for . Gallery File:TWC Waitoto River• Stewart Nimmo • MRD 9644.jpg File:TWC Waitoto River• Stewart Nimmo • MRD 1018.jpg File:TWC Waitoto River• Stewart Nimmo • MRD 0922.jpg 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 * Ākitio R ... References Rivers of the West Coast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of New Zealand
New Zealand contains many glaciers, mostly located near the Main Divide of the Southern Alps in the South Island. They are classed as mid-latitude mountain glaciers. There are eight small glaciers in the North Island on Mount Ruapehu. An inventory of South Island glaciers compiled in the 1980s indicated there were about 3,155 glaciers with an area of at least one hectare (2.5 acres). Approximately one sixth of these glaciers covered more than 10 hectares. These include: *Fox Glacier *Franz Josef Glacier * Hooker Glacier *Mueller Glacier * Murchison Glacier *Tasman Glacier * Volta Glacier New Zealand's territorial claim in Antarctica, the Ross Dependency, also contains many glaciers. Retreat of glaciers New Zealand glaciers have been retreating since 1890, with an acceleration of this retreat since 1920. Most of the glaciers have thinned measurably and have reduced in size, and the snow accumulation zones have risen in elevation during the 20th century. In the period 1971 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The West Coast, New Zealand
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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