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Lake Poerua
Lake Poerua ( mi, Pouerua) is a shallow lake located in the West Coast region of New Zealand's South Island roughly 13 km southeast from Lake Brunner. It is located between the Alexander Range and the slopes of Mount Te Kinga, to the north of the lake. The area around Lake Poerua is sparsely populated. A number of small streams flow into the lake, and the Poerua River flows from the lake into the Crooked River, which leads to Lake Brunner. The first description of the lake by Europeans comes from the journeys of Julius von Haast, who explored the West Coast region in the 1860s. The lake is bounded on its eastern side by the main fault scarp of the Alpine Fault, and is believed to be very recent in geological age. Lake Poerua sits on the Australia-Pacific plate boundary, with granite rock from the Australian plate to the west and metasedimentary rocks from the Pacific plate to the east. The lake is popular with trout fishermen and is easily accessible from the adja ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Coast, New Zealand
The West Coast ( mi, Te Tai Poutini, lit=The Coast of Poutini, the Taniwha) is a regions of New Zealand, 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 New Zealand, territorial authorities of Buller District, Grey District and Westland District. The principal towns are Westport, New Zealand, 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 Ngāi Tahu, Kāi T ... [...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] |
Poerua River (Grey District)
Poerua River is a river in the Grey District in the West Coast region of New Zealand's South Island. It flows around the base of Mount Te Kinga from Lake Poerua into the Crooked River, which leads to Lake Brunner Lake Brunner ( mi, Kōtuku Moana or ) is the largest lake in the West Coast Region of New Zealand, located southeast of Greymouth. The main settlement, Moana, New Zealand, Moana, is on its northern shore. It is an important settlement and ways .... Grey District Rivers of the West Coast, New Zealand Rivers of New Zealand {{WestCoastNZ-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Brunner
Lake Brunner ( mi, Kōtuku Moana or ) is the largest lake in the West Coast Region of New Zealand, located southeast of Greymouth. The main settlement, Moana, New Zealand, Moana, is on its northern shore. It is an important settlement and waystation for local Māori people, Māori. The first Europeans in the area were loggers, and sawmills were an important early industry. Being several kilometres inland from the coast road (), it is less frequently visited by tourists than many of the West Coast's scenic highlights, but it is becoming increasingly popular, in part due to its reputation for fishing. Geography Lake Brunner is the largest lake in the West Coast region, across with an area of 4061 ha, just over . The outlet of the lake is the Arnold River (New Zealand), Arnold River, a tributary of the Grey River (New Zealand), Grey River / Māwheranui, next to the largest settlement of Moana, on the north shore of the lake. The largest rivers feeding into Lake Brunner are the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Te Kinga
Mount Te Kinga ( mi, Tekimoka) is a mountain on the West Coast of New Zealand's South Island within the western foothills of the Southern Alps / Kā Tiritiri o te Moana. The mountain is on the south-eastern shore of Lake Brunner and is not a part of a larger mountain range, being separated from the Hohonu Range to the west by the Orangipuku River and from the Alexander Range to the southeast by the Poerua River. Numerous small creeks flow from Te Kinga, all of which end up eventually flowing into the nearby Lake Brunner. Despite being surrounded by former wetlands which have been converted into dairy farms, Te Kinga has been largely untouched. Almost the entire mountain is covered by native forest, with the lower reaches containing large old-growth podocarp trees, including tōtara, rimu, kahikatea and miro. As the altitude increases the vegetation gradually shifts, including larger amounts of species such as kaikawaka, neinei and southern rata. From an altitude of abou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crooked River, New Zealand
Crooked River is a river that flows from headwaters in the Southern Alps to Lake Brunner in the West Coast region of New Zealand's South Island. It is named for the erratic path it takes. Near Lake Brunner, it passes through reasonably flat farmland, but closer to its source, it rushes through gorges and rapids. One tributary is the Poerua River from Lake Poerua. Fishers visit Crooked River to catch trout. The river is also used by canoeists. Recently, there has been a minor silt build-up in the river's middle reaches. There are two backcountry hut A wilderness hut, bothy, backcountry hut, or backcountry shelter is a free, primitive mountain hut for temporary accommodation, usually located in wilderness areas, national parks and along backpacking (wilderness), backpacking and hiking route ...s available for trampers along the Crooked River. References Grey District Rivers of the West Coast, New Zealand Rivers of New Zealand {{WestCoastNZ-river-stub ... [...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] |
Inchbonnie
Inchbonnie is a rural locality in the West Coast region of the South Island of New Zealand. It is located on the north bank of the Taramakau River and is just to the south of Lake Poerua. "Inchbonnie" is a hybrid of Lowland Scots, ''bonnie'' meaning "pretty" and Scottish Gaelic ''innis'' meaning island, often anglicised as "Inch", as in Inchkeith or Inchkenneth in Scotland. Location State Highway 73 and the Midland Line railway both pass through Inchbonnie, though the TranzAlpine passenger train does not stop. Prior to the opening of the road bridge in December 1972, the only crossing of the Taramakau River at Inchbonnie was the railway bridge on the Midland Line. Anecdotal history reports that locals in the Inchbonnie area adapted vehicles to run on the railway bridge so that they could cross to the pub at Jacksons. Inchbonnie has a mean annual rainfall of around and up to has been recorded in a 24 hour period. Locations around Inchbonnie are of particular interest for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand State Highway Network
The New Zealand state highway network is the major national highway network in New Zealand. Nearly 100 roads in the North and South Islands are state highways. All state highways are administered by the NZ Transport Agency. The highways were originally designated using a two-tier system, national (SH 1 to 8) and provincial, with national highways having a higher standard and funding priorities. Now all are state highways, and the network consists of SH 1 running the length of both islands, SH 2 to 5 and 10 to 59 in the North Island, and SH 6 to 8 and 60 to 99 in the South Island, numbered approximately north to south. State highways are marked by red shield-shaped signs with white numbering (shields for the former provincial highways were blue). Road maps usually number state highways in this fashion. Of the total state highway network, New Zealand currently has of motorways and expressways with grade-separated access and they carry ten percent of all New Zealand traffic. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midland Line, New Zealand
The Midland line is a 212 km section of railway between Rolleston and Greymouth in the South Island of New Zealand. The line features five major bridges, five viaducts and 17 tunnels, the longest of which is the Otira tunnel. It is the route of the popular TranzAlpine passenger train. History Railway development in the South Island in the 1870s was concentrated on a main line linking the established centres of Christchurch, Timaru, Dunedin and Invercargill and light, easily constructed branch lines serving the arable plains; (see Vogel Era). These later included a branch to Springfield which was reached by January 1880. In 1882 the East and West Coast Railway League was formed and in 1884 a Royal Commission, although fully aware of the construction difficulties of the Waimakariri Valley-Arthurs Pass route, as compared with the somewhat easier but longer Hurunui Valley-Harpers Pass route, chose the more direct route. The construction of the line was rejected in 1883 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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