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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 1971–75 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franz Josef Glacier
The Franz Josef Glacier (; officially Franz Josef Glacier / ) is a temperate maritime glacier in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. Together with the Fox Glacier to the south, and a third glacier, it descends from the Southern Alps to less than above sea level. The area surrounding the two glaciers is part of Te Wahipounamu, a World Heritage Site park. The Waiho River emerges from the glacier terminal of Franz Josef. Naming The Māori people, Māori name for the glacier is , literally: 'The tears of Hine Hukatere'. According to oral tradition, Hine Hukatere loved climbing in the mountains and persuaded her lover Tuawe to climb with her. Tuawe was a less experienced climber than Hine Hukatere but loved to accompany her, until an avalanche swept him from the peaks to his death. Hine Hukatere was broken-hearted and her many, many tears flowed down the mountain. Rangi and Papa, Rangi the Sky Father took pity on her and froze them to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
List Of Glaciers In The Antarctic
There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. The lists include outlet glaciers, valley glaciers, cirque glaciers, tidewater glaciers and ice streams. Ice streams are a type of glacier and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves. For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System). List by letters * List of glaciers in the Antarctic: A–H * List of glaciers in the Antarctic: I–Z See also * List of Antarctic and subantarctic islands * List of Antarctic ice rises * List of Antarctic ice shelves * List of Antarctic ice streams * List of glaciers * List of subantar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climate Change In New Zealand
Climate change in New Zealand involves historical, current and future changes in the climate of New Zealand; and New Zealand's contribution and response to global climate change. Summers are becoming longer and hotter, and some glaciers have melted completely and others have shrunk. In 2021, the Ministry for the Environment estimated that New Zealand's gross emissions were 0.17% of the world's total gross greenhouse gas emissions. However, on a per capita basis, New Zealand is a significant emitter, the sixth highest within the Annex I countries, whereas on absolute gross emissions New Zealand is ranked as the 24th highest emitter. Almost half New Zealand's greenhouse gas emissions are from agriculture, mainly methane from sheep and cow belches. Between 1990 and 2019, New Zealand's gross emissions (excluding removals from land use and forestry) increased by 26%. When the uptake of carbon dioxide by forests (sequestration) is taken into account, net emissions (including carbon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers In New Zealand
New Zealand contains approximately 2900 glaciers over in size, almost all of them along the Southern Alps, the main divide of the South Island. This is down from around 3100 glaciers recorded in the late 1970s, due to ongoing changes to the earth's climate. Roughly one-sixth of New Zealand's glaciers are over in size, with the largest Tasman Glacier with an area of . Eight of New Zealand's glaciers are found on Mount Ruapehu, and represent the only glaciers within mainland New Zealand outside of the South Island. The below is a list of named glaciers in mainland New Zealand as recorded by the New Zealand Geographic Board, who are responsible for the naming of geographic places and features in New Zealand. It does not include the several glaciers located within the Ross Dependency, a region of Antarctica claimed by New Zealand. North Island South Island See also * List of glaciers * Glaciers of New Zealand New Zealand contains many glaciers, mostly located near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Department Of The Interior
The United States Department of the Interior (DOI) is one of the executive departments of the U.S. federal government headquartered at the Main Interior Building, located at 1849 C Street NW in Washington, D.C. It is responsible for the management and conservation of most federal lands and natural resources, and the administration of programs relating to Native Americans, Alaska Natives, Native Hawaiians, territorial affairs, and insular areas of the United States, as well as programs related to historic preservation. About 75% of federal public land is managed by the department, with most of the remainder managed by the Department of Agriculture's Forest Service. The department was created on March 3, 1849. The department is headed by the secretary of the interior, who reports directly to the president of the United States and is a member of the president's Cabinet. The current secretary is Deb Haaland. Despite its name, the Department of the Interior has a different ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Coast Region
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jim Salinger
Michael James Salinger (born 25 April 1947) is a New Zealand climate change researcher and teacher who has worked for a range of universities in his home country and around the world. He was a senior climate scientist for a Crown Research Institute, the National Institute of Water and Atmospheric Research (NIWA), and President of the Commission for Agricultural Meteorology of the World Meteorological Organization (WMO). He has received several awards and other honours for his work with climate change and is involved in researching and monitoring past and current climate trends. Within his area of specialist scientific knowledge, Salinger has co-authored and edited a range of reports, articles and books. He was involved in an employment dispute and elements of his theory and practice were at the centre of a case against NIWA. Career Salinger was a scientist at the University of Otago Medical School from 1972–1975. He then lectured in geography at Victoria University of Wellin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ross Dependency
The Ross Dependency is a region of Antarctica defined by a sector originating at the South Pole, passing along longitudes 160° east to 150° west, and terminating at latitude 60° south. It is claimed by New Zealand, a claim accepted only by the other six countries with territorial claims in Antarctica. Under the 1961 Antarctic Treaty, of which all territorial claimants are signatories, including New Zealand, all claims are held in abeyance. Article IV states: "No acts or activities taking place while the present Treaty is in force shall constitute a basis for asserting, supporting or denying a claim to territorial sovereignty in Antarctica or create any rights of sovereignty in Antarctica". The Dependency takes its name from Sir James Clark Ross, who discovered the Ross Sea, and includes part of Victoria Land, and most of the Ross Ice Shelf. Ross, Balleny, Scott and Roosevelt Islands also form part of the Dependency. History of claim Following his discovery of Victo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasman Glacier
Haupapa / Tasman Glacier is the largest glacier in New Zealand, and one of several large glaciers which flow south and east towards the Mackenzie Basin from the Southern Alps in New Zealand's South Island. Geography At in length, Tasman Glacier is still New Zealand's longest glacier, despite shrinking considerably from the 1990s onwards. It is as much as wide and thick, and lies entirely within the borders of Aoraki / Mount Cook National Park. The glacier covers an area of and starts at a height of above sea level. Snowfall during the winter and spring seasons may accumulate up to . After the summer melt, may remain in the high altitude glacier head. The Tasman flows south west from Hochstetter Dome and Mount Elie De Beaumont alongside the southern slopes of The Minarets and south along the eastern flank of New Zealand's two highest mountains, Mount Tasman and its higher southern neighbour Aoraki / Mount Cook. Although its upper reaches are snow-covered, rocks carried by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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