|
Agassiz Glacier (New Zealand)
The Agassiz Glacier is located near the west coast of New Zealand's South Island. The Agassiz Glacier is a tributary of the larger Franz Josef Glacier, and is itself fed by the Chamberlin Snowfield and the Davis Snowfield. It is named after Louis Agassiz Jean Louis Rodolphe Agassiz ( ; ) FRS (For) FRSE (May 28, 1807 – December 14, 1873) was a Swiss-born American biologist and geologist who is recognized as a scholar of Earth's natural history. Spending his early life in Switzerland, he rec ..., a Swiss-American glaciologist, and was discovered and named by the German geologist, Sir Johann "Julius" von Haast. In 2015, the glacier was informally 'unnamed' as part of a worldwide campaign to disassociate Agassiz's name from various geographic features and, in this instance, to replace it with a relevant Māori name. References External links Agassiz Glacier on NZ Topo MapAgassiz Glacier on Mapcarta.com Glaciers of New Zealand Westland Tai Poutini National Park [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westland District
Westland District is a Districts of New Zealand, territorial authority district on the West Coast, New Zealand, West Coast of New Zealand's South Island. It is administered by the Westland District Council. The district's population is History Westland was originally a part of Canterbury Province, administered from Christchurch in the East coast. The booming population as a result of the gold rush, together with the difficulty of travel and communication across the Southern Alps, led first to the creation of a special Westland County, then the formal separation of Westland from Canterbury to form the short-lived Westland Province (1873–1876). Westland Province also included what is now the southern portion of Grey District with the provincial boundary at the Grey River (New Zealand), Grey and Arnold River (New Zealand), Arnold rivers. Greymouth proper was in Westland Province, Cobden, New Zealand, Cobden, on the north bank of the Grey River, was in Nelson Province . After the ... [...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] |
New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franz Josef Glacier / Kā Roimata O Hine Hukatere
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 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 the Sky Father took pity on her and froze them to form the glacier. The firs ... [...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 services. ... [...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] |
Louis Agassiz
Jean Louis Rodolphe Agassiz ( ; ) FRS (For) FRSE (May 28, 1807 – December 14, 1873) was a Swiss-born American biologist and geologist who is recognized as a scholar of Earth's natural history. Spending his early life in Switzerland, he received a PhD at Erlangen and a medical degree in Munich. After studying with Georges Cuvier and Alexander von Humboldt in Paris, Agassiz was appointed professor of natural history at the University of Neuchâtel. He emigrated to the United States in 1847 after visiting Harvard University. He went on to become professor of zoology and geology at Harvard, to head its Lawrence Scientific School, and to found its Museum of Comparative Zoology. Agassiz is known for observational data gathering and analysis. He made institutional and scientific contributions to zoology, geology, and related areas, including multivolume research books running to thousands of pages. He is particularly known for his contributions to ichthyological classification, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julius Von Haast
Sir Johann Franz Julius von Haast (1 May 1822 – 16 August 1887) was a German-born New Zealand explorer, geologist, and founder of the Canterbury Museum in Christchurch. Early life Johann Franz Julius Haast was born on 1 May 1822 in Bonn, a town in the Kingdom of Prussia, to a merchant and his wife. As a child, he attended a local school but was also educated at a grammar school in Cologne. After completing his formal schooling, he then entered the University of Bonn, where he studied geology and mineralogy. However, he did not graduate. As a young man, he travelled throughout Europe before basing himself in Frankfurt, working in the trading of books and mineral samples collected on his journeys. On 26 October 1846, Haast married Antonia Schmitt at Frankfurt, Germany. The marriage, although unhappy, produced a son named Robert two years later. Haast was fluent in English and, in 1858, was contracted by a British shipping firm, A. Willis, Gann & Company, to report on the ... [...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] |
.svg "Click for more on -> South Island")
