|
Waimangaroa River
The Waimangaroa River is located on the West Coast of New Zealand. The river passes through tussock, scrub and forested areas before draining into the Karamea Bight in the Tasman Sea. It passes through the town of Waimangaroa and is crossed by the Ngakawau Branch railway, with the rail bridge brought into service in 1877. That year, the Conns Creek Branch opened, a sub-branch line A branch line is a phrase used in railway terminology to denote a secondary railway line which branches off a more important through route, usually a main line. A very short branch line may be called a spur line. Industrial spur An industr ... that closely followed the southern bank of the river east from Waimangaroa to the foot of the Denniston Incline. It closed in 1967. Buller District Rivers of the West Coast, New Zealand Rivers of New Zealand {{WestCoastNZ-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waimangaroa Township
Waimangaroa is a small town located on the West Coast of New Zealand. The township lies on the south-west bank of the Waimangaroa River, at the western foot of the Denniston Plateau. It is to the north east of Westport and 13 km south-east of Granity. The abandoned coaltown of Denniston is about to the south-east. The Bridle Track, a scenic bush track, leads south-east along the Denniston Incline into the foothills of the Mt William Range, to Denniston. The Stockton mine, a large open cast coal mine, is operated in the vicinity by Solid Energy. The Ngakawau Branch, a branch line railway, runs through the town. It opened to Waimangaroa on 5 August 1876; it formerly ran to Seddonville but now terminates in Ngakawau. From 1877 until 1967, Waimangaroa was also the junction for the Conns Creek Branch, which ran east alongside the Waimangaroa River to the foot of the Denniston Incline. Passenger services ceased on the Conns Creek Branch in 1931 and Ngakawau Branch on ... [...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] |
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] |
Tussock Grass
Tussock grasses or bunch grasses are a group of grass species in the family Poaceae. They usually grow as singular plants in clumps, tufts, hummocks, or bunches, rather than forming a sod or lawn, in meadows, grasslands, and prairies. As perennial plants, most species live more than one season. Tussock grasses are often found as forage in pastures and ornamental grasses in gardens. Many species have long roots that may reach or more into the soil, which can aid slope stabilization, erosion control, and soil porosity for precipitation absorption. Also, their roots can reach moisture more deeply than other grasses and annual plants during seasonal or climatic droughts. The plants provide habitat and food for insects (including Lepidoptera), birds, small animals and larger herbivores, and support beneficial soil mycorrhiza. The leaves supply material, such as for basket weaving, for indigenous peoples and contemporary artists. Tussock and bunch grasses occur in almost any habitat w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasman Sea
The Tasman Sea (Māori: ''Te Tai-o-Rēhua'', ) is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about across and about from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known person to cross it. British explorer Lieutenant James Cook later extensively navigated the Tasman Sea in the 1770s during his three voyages of exploration. The Tasman Sea is informally referred to in both Australian and New Zealand English as the Ditch; for example, "crossing the Ditch" means travelling to Australia from New Zealand, or vice versa. The diminutive term "the Ditch" used for the Tasman Sea is comparable to referring to the North Atlantic Ocean as "the Pond". Climate The south of the sea is passed over by depressions going from west to east. The northern limit of these westerly winds is near to 40°S. During the southern winter, from April to October, the northern branch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waimangaroa
Waimangaroa is a small town located on the West Coast of New Zealand. The township lies on the south-west bank of the Waimangaroa River, at the western foot of the Denniston Plateau. It is to the north east of Westport and 13 km south-east of Granity. The abandoned coaltown of Denniston is about to the south-east. The Bridle Track, a scenic bush track, leads south-east along the Denniston Incline into the foothills of the Mt William Range, to Denniston. The Stockton mine, a large open cast coal mine, is operated in the vicinity by Solid Energy. The Ngakawau Branch, a branch line railway, runs through the town. It opened to Waimangaroa on 5 August 1876; it formerly ran to Seddonville but now terminates in Ngakawau. From 1877 until 1967, Waimangaroa was also the junction for the Conns Creek Branch, which ran east alongside the Waimangaroa River to the foot of the Denniston Incline. Passenger services ceased on the Conns Creek Branch in 1931 and Ngakawau Branch on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seddonville Branch
The Seddonville Branch, later truncated as the Ngākawau Branch, is a branch line railway in the West Coast region of New Zealand's South Island. Construction began in 1874 and it reached its terminus at the Mokihinui Mine just beyond Seddonville in 1895. In 1981 it was closed past Ngākawau and effectively became an extension of the Stillwater–Westport Line, since formalised as the Stillwater–Ngākawau Line. Construction The branch was built for transporting coal from mines to the harbour at Westport. Unlike most other railways of the era, there was no expectation that it would open up country for settlement and farming, as the terrain was mountainous and not suited to settlements of significant size. Coalfield surveys had identified significant deposits of bituminous coal on the Mount Rochfort and Stockton plateaus high above the coastal plain and outcrops of sub-bituminous coal had been located at low level close to the rivers at Waimangaroa and Ngākawau. However ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Railway
Rail transport (also known as train transport) is a means of transport that transfers passengers and goods on wheeled vehicles running on rails, which are incorporated in tracks. In contrast to road transport, where the vehicles run on a prepared flat surface, rail vehicles (rolling stock) are directionally guided by the tracks on which they run. Tracks usually consist of steel rails, installed on sleepers (ties) set in ballast, on which the rolling stock, usually fitted with metal wheels, moves. Other variations are also possible, such as "slab track", in which the rails are fastened to a concrete foundation resting on a prepared subsurface. Rolling stock in a rail transport system generally encounters lower frictional resistance than rubber-tyred road vehicles, so passenger and freight cars (carriages and wagons) can be coupled into longer trains. The operation is carried out by a railway company, providing transport between train stations or freight customer facilit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conns Creek Branch
The Conns Creek Branch was a 2.7 kilometre (1.7 mile) branch line railway in the West Coast region of New Zealand's South Island. It diverged from the Seddonville Branch at Waimangaroa and followed the southern bank of the Waimangaroa River to the line's terminus at Conns Creek at the foot of the Denniston Incline. The line operated from 1877 until 1967 and existed for the sole purpose of conveying coal from mines to the port of Westport. Construction Construction of the Seddonville Branch railway from Westport to Seddonville had begun in 1874. In September 1875 the Wellington Coal Mining Company called for tenders for a private line from a junction with the Seddonville branch at Waimangaroa to a site 1.6 kilometres (1 mile) up the Waimangaroa River adjacent to the company's mine. The Seddonville Branch was completed as far as Waimangaroa on 5 August 1876 and the first portion of the Conns Creek Branch - as far as the Wellington Mine - opened in 1877. A bridge across the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Branch Line
A branch line is a phrase used in railway terminology to denote a secondary railway line which branches off a more important through route, usually a main line. A very short branch line may be called a spur line. Industrial spur An industrial spur is a type of secondary track used by railroads to allow customers at a location to load and unload railcars without interfering with other railroad operations. Industrial spurs can vary greatly in length and railcar capacity depending on the requirements of the customer the spur is serving. In heavily industrialized areas, it is not uncommon for one industrial spur to have multiple sidings to several different customers. Typically, spurs are serviced by local trains responsible for collecting small numbers of railcars and delivering them to a larger yard, where these railcars are sorted and dispatched in larger trains with other cars destined to similar locations. Because industrial spurs generally have less capacity and traffic t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Denniston Incline
Denniston is a small settlement, 15 kilometres (9 miles) east of Westport, on the West Coast of the South Island of New Zealand. It is situated on the Denniston Plateau, above sea level in the Papahaua Ranges. It is named for R. B. Denniston, manager of the first major mine to open on the West Coast in the 1870s. During the first few decades of the 20th century, up to 1400 people lived in the townships on the Denniston Plateau to service the large coal mines there. Coal was transported in railway wagons from the plateau via the Denniston Incline to Conns Creek, where steam locomotives of New Zealand Railways took coal trains to the port of Westport. The Denniston Incline closed in 1967. The plateau now has a population of fewer than 10 people, and virtually all the buildings and structures are gone, although many historical relics remain – scattered throughout the plateau and incline area amongst the scrub vegetation. The open-cast Escarpment Mine Project was establish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buller District
Buller District is one of 53 districts of New Zealand, and is within the West Coast Region. It covers Westport, Karamea, Reefton and Inangahua Junction. Buller District's overall land area is . The district is administered by the Buller District Council with the seat in Westport, in which 45% of the district's population live. History It is understood by the carbon dating of Umu (ovens) that the Maori people settled in this region some 700 years ago. The district takes its name from the Buller River, itself named for Charles Buller, a Member of Parliament in the United Kingdom of Great Britain and Ireland (UK) and director of the New Zealand Company, a UK-based company established in the early 19th century with a royal charter supporting colonisation efforts of New Zealand. During the period 1853 to 1876, the current area of Buller District was administered as part of Nelson Province. With the Abolition of Provinces Act 1876, much of the current area of Buller District w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
