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Fox Glacier
Fox Glacier (; officially Fox Glacier / Te Moeka o Tuawe) is a temperate maritime glacier located in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. Like nearby Franz Josef Glacier, Fox Glacier is one of the most accessible glaciers in the world, with a terminal face as low as 300 m above sea level, close to the village of Fox Glacier. It is a major tourist attraction and about 1000 people daily visit it during high tourist season. Naming The glacier is known by local Māori as ''Te Moeka o Tuawe'' ('The bed of Tuawe'). 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 glacie ...
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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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NZPA
The New Zealand Press Association (NZPA) was a news agency that existed from 1879 to 2011 and provided national and international news to the media of New Zealand. The largest news agency in the country, it was founded as the United Press Association in 1879, and became the New Zealand Press Association in 1942. Following Fairfax New Zealand's withdrawal from NZPA in April 2011, NZPA told staff that it would be wound up over the next four to six months, and ceased operation on 31 August 2011. NZPA was superseded by three new services, all Australian-owned: APNZ (on-going), Fairfax New Zealand News (on-going as Stuff), and NZ Newswire (folded in April 2018). History Daily and Sunday newspapers owned by APN News & Media, Fairfax New Zealand, Allied Press, Ashburton Guardian, The Gisborne Herald, The Wairoa Star Ltd, Whakatane Beacon and the Westport News were members of NZPA. Until January 2006, member newspapers were obliged by contract to supply their home town news copy to NZPA ...
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Fox Glacier Hotel
Fox Glacier Hotel is a hotel in Fox Glacier, on the West Coast of New Zealand's South Island. Completed in 1928 for the Sullivan brothers, the building was granted historic place category 2 status by Heritage New Zealand in 1989. Context In the 1920s, a concerted effort was made to promote the West Coast, and the glacier region in particular, as a tourist destination. At Fox Glacier village, then known as Weheka, the Sullivan family had used their farm homestead as tourist accommodation, but increased demand saw the Sullivan brothers, Mick and John, decide to construct a purpose-built hotel, and they established a sawmill to mill local rimu for the project. Architecture The hotel was built in 1928, at a cost of approximately £20,000, and was officially opened on 20 December 1928. Although a two-storey building, the hotel was described as have a bungalow style, owing to the generous upper-floor verandahs. The hotel was built with 40 bedrooms, designed to accommodate up to 100 gu ...
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Tourists Climbing Fox Glacier 1966 (25898945172)
Tourism is travel for pleasure or business; also the theory and practice of touring (other), touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tour (other), tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be Domestic tourism, domestic (within the traveller's own country) or International tourism, international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of t ...
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Ebenezer Teichelmann
Ebenezer Teichelmann (23 March 1859 – 20 December 1938), known as 'the little Doctor' to his friends, was an Australian-born surgeon, mountaineer, explorer, conservationist and photographer in New Zealand. He was a survivor of the sinking of the SS ''Marquette'' in 1915. He achieved 26 first ascents of mountains and seven first ascents, or crossings, of passes, cols, or saddles, and is credited with reviving climbing in New Zealand when the sport was almost dead. A keen photographer, he used a full-plate glass camera, which was hauled up many mountains. His photographs were used in books and advertisements, and helped to achieve conservation status for West Coast reserves. Early life and education Teichelmann was born on 23 March 1859 near Callington, South Australia, the ninth child of fifteen born to German Lutheran missionary Christian Teichelmann and his Scottish wife Margaret, Nicholson. The Teichelmanns could only afford secondary education for one child, Ebenezer. ...
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Franz Josef / Waiau
Franz Josef / Waiau is a small town in the West Coast region of the South Island of New Zealand. Whataroa is to the north-east, and the township of Fox Glacier is to the south-west. The Waiho River runs from the Franz Josef Glacier to the south, through the town, and into the Tasman Sea to the north-west. Name Local Māori called the area , which means swirling waters. In the 1860s Sir Julius von Haast named the Franz Josef Glacier in honour of the Emperor of Austria Franz Josef I of Austria. The town Franz Josef was then named after the glacier. Following the passage of the Ngāi Tahu Claims Settlement Act 1998, the name of the town was officially altered to Franz Josef / Waiau. Geography Flood protection The bed of the Waiho (Waiau) River has significantly risen over the years, and increased rainfall and snow melt from the retreating glacier has caused the river's water flow to vary greatly. The riverbed is currently predicted to rise 2 m every 10 years, and in 30 y ...
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Cook River / Weheka
The Cook River / Weheka is in the South Island of New Zealand. The headwaters are from the La Perouse Glacier on the western flanks of the Southern Alps, and it flows west, then northeast, then northwest and into the Tasman Sea. Its tributaries include the Balfour River, fed by Balfour Glacier, and the Fox River, fed by Fox Glacier. Much of the river lies within the Westland Tai Poutini National Park. The river was renamed from Cook River to Cook River / Weheka as a result of the Ngai Tahu Claims Settlement Act 1998. Brown trout can be fished for in the river. Access along the river by foot is difficult beyond the junction with the Balfour River. There are no approved helicopter landing sites in the river valley, but there are chamois, tahr and small numbers of red deer The red deer (''Cervus elaphus'') is one of the largest deer species. A male red deer is called a stag or hart, and a female is called a hind. The red deer inhabits most of Europe, the Caucasus Mountains ...
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Party Inspecting A Crevasse On The Fox Glacier (3307743585)
A party is a gathering of people who have been invited by a host for the purposes of socializing, conversation, recreation, or as part of a festival or other commemoration or celebration of a special occasion. A party will often feature food and beverages, and often conversation, music, dancing, or other forms of entertainment. Some parties are held in honor of a specific person, day, or event, such as a birthday party, a Super Bowl party, or a St. Patrick’s Day party. Parties of this kind are often called celebrations. A party is not necessarily a private occasion. Public parties are sometimes held in restaurants, pubs, beer gardens, nightclubs, or bars, and people attending such parties may be charged an admission fee by the host. Large parties in public streets may celebrate events such as Mardi Gras or the signing of a peace treaty ending a long war. Types Balls Banquets Birthday party A birthday party is a celebration of the anniversary of the birth of t ...
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Department Of Conservation (New Zealand)
The Department of Conservation (DOC; Māori: ''Te Papa Atawhai'') is the public service department of New Zealand charged with the conservation of New Zealand's natural and historical heritage. An advisory body, the New Zealand Conservation Authority (NZCA) is provided to advise DOC and its ministers. In addition there are 15 conservation boards for different areas around the country that provide for interaction between DOC and the public. Function Overview The department was formed on 1 April 1987, as one of several reforms of the public service, when the '' Conservation Act 1987'' was passed to integrate some functions of the Department of Lands and Survey, the Forest Service and the Wildlife Service. This act also set out the majority of the department's responsibilities and roles. As a consequence of Conservation Act all Crown land in New Zealand designated for conservation and protection became managed by the Department of Conservation. This is about 30% of New ...
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Kettle (landform)
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluvio ...
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Lake Matheson
Lake Matheson ( mi, Te Ara Kairaumati) is a small glacial lake in South Westland, New Zealand, near the township of Fox Glacier. It was a traditional food-gathering place for local Māori. An easy walking track circles the lake, which is famous for its reflected views of Aoraki / Mount Cook and Mount Tasman. Geography Lake Matheson formed between two moraine terraces left by the rapid retreat of Fox Glacier / Te Moeka o Tuawe 14,000 years ago, at the end of the last glacial period. The retreating glacier left behind a valley and a huge slab of ice insulated by a deep layer of moraine gravel, which gradually melted and collapsed to form the lake bed. The lake is now about from the current terminus of the glacier in the Southern Alps. Moraines, outwash gravels, and river gravels dammed the valley, and the lake grew, fed by small streams and seepage – there is no major river inflow or outflow. Lake Matheson is 30 ha in area, with an approximately 1.5 km shoreline and an ...
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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 P ...
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