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Karamea Bluff Scenic Reserve
Karamea is a town on the West Coast of the South Island of New Zealand. It is the northernmost settlement of any real size on the West Coast, and is located northeast by road from Westport. Apart from a narrow coastal strip, the town of Karamea and its local area are completely surrounded to the south, east and north by Kahurangi National Park. The town is located on the coastal plain adjacent to the Karamea River and the Ōtūmahana Estuary. There are two small settlements, Market Cross and Karamea, located about apart. Karamea is a gateway to the Kahurangi National Park, and a base for visitors coming to see popular local attractions such as the Ōpārara Basin, Ōpārara Arches, the Fenian Track and caves, the Big Rimu Walk and the coastal scenery north of Kōhaihai on the Heaphy Track. Toponymy The name ''Karamea'' is Māori – despite local jokes suggesting it was named by an Italian for his love – and is thought to either mean "red ochre" or be a corrupti ... [...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] |
Radiocarbon Dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon. The method was developed in the late 1940s at the University of Chicago by Willard Libby. It is based on the fact that radiocarbon () is constantly being created in the Earth's atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and thereafter the amount of it contains begins to decrease as the undergoes radioactive decay. Measuring the amount of in a sample from a dead plant or animal, such as a piece of wood or a fragment of bone, provides information that can be used to calc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diphtheria
Diphtheria is an infection caused by the bacterium '' Corynebacterium diphtheriae''. Most infections are asymptomatic or have a mild clinical course, but in some outbreaks more than 10% of those diagnosed with the disease may die. Signs and symptoms may vary from mild to severe and usually start two to five days after exposure. Symptoms often come on fairly gradually, beginning with a sore throat and fever. In severe cases, a grey or white patch develops in the throat. This can block the airway and create a barking cough as in croup. The neck may swell in part due to enlarged lymph nodes. A form of diphtheria which involves the skin, eyes or genitals also exists. Complications may include myocarditis, inflammation of nerves, kidney problems, and bleeding problems due to low levels of platelets. Myocarditis may result in an abnormal heart rate and inflammation of the nerves may result in paralysis. Diphtheria is usually spread between people by direct contact or through th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1929 Murchison Earthquake
The 1929 Murchison earthquake occurred at 10:17 am on 17 June. It struck the Murchison region of the South Island, with an estimated magnitude of 7.3, and was felt throughout New Zealand. There were 17 deaths, mostly as a result of landslides triggered by the earthquake. The rumbling sound of the earthquake was loud enough to be heard at New Plymouth, more than 250 km (155 mi) away. Tectonic setting New Zealand sits astride the boundary between the Indo-Australian Plate and the Pacific Plate. In the South Island most of the displacement is taken up on the Alpine Fault passing to the north onto a set of strike-slip faults, the Marlborough Fault System. The sense of displacement across the plate boundary is oblique and most of the faults have a reverse component of slip. Some of the resulting deformation is accommodated within the plates themselves away from the boundary. The 1929 Murchison earthquake occurred on the White Creek Fault, located in the Buller Gorge. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pakihi
Pakihi or pākihi is a vegetation association unique to the West Coast of the South Island of New Zealand, characterised by flat boggy land with infertile, waterlogged soil on which only rushes, ferns, moss, and mānuka grow. Name The Māori word can mean "open country" or "barren land", or alternatively "a clearing in forest" or "place where fern root was dug up". Both these ideas are encompassed by the use of pakihi in New Zealand English to refer to open country, mainly on the West Coast of the South Island, from which forest was once cleared but which no longer allows tree growth. Extent Pakihi habitat ranges over 540 km of the west of the South Island, from Golden Bay in the north to Awarua Bay in the south, being particularly common in the central West Coast between Westport and Hokitika, usually near the coast but sometimes extending some 50 km inland. Pakihi can be both natural or induced. Some pakihi has existed for thousands of years, even back to g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand House Of Representatives
The House of Representatives is the sole chamber of the New Zealand Parliament. The House passes Law of New Zealand, laws, provides Ministers of the New Zealand Government, ministers to form Cabinet of New Zealand, Cabinet, and supervises the work of government. It is also responsible for adopting the state's New Zealand Budget, budgets and approving the state's accounts. The House of Representatives is a Representative democracy, democratic body consisting of representatives known as members of parliament (MPs). There are normally 120 MPs, though this number can be higher if there is an Overhang seat, overhang. Elections in New Zealand, Elections take place usually every three years using a mixed-member proportional representation system which combines First-past-the-post voting, first-past-the-post elected legislative seat, seats with closed party lists. 72 MPs are elected directly in single-member New Zealand electorates, electoral districts and further seats are filled by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eugene O'Conor
Eugene Joseph O'Conor (23 February 1835 – 5 July 1912) was a New Zealand Member of Parliament for the Buller electorate, in the South Island. Private life Born in Ireland in 1835, O'Conor went to Victoria, Australia in 1854, and came to New Zealand in the early 1860s. He was a cattle dealer and storekeeper. O'Conor had 'several useful inventions patented' and lectured on his opinion that Francis Bacon (Baconian theory) was the author of Shakespeare's plays. He was a significant land owner on the West Coast. Member of Parliament O'Conor was a member of the Nelson Provincial Council. From November 1869 to October 1873, he represented the Buller electorate. From May 1874 until the abolition of the Nelson Province in October 1876, he represented the Westport electorate. From June 1874, he was on the Nelson Executive Council for a time (the source does not record an end date). Eugene O'Conor represented the Buller electorate in the New Zealand House of Representatives fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colony Of New Zealand
The Colony of New Zealand was a Crown colony of the United Kingdom of Great Britain and Ireland that encompassed the islands of New Zealand from 1841 to 1907. The power of the British government was vested in the Governor of New Zealand, as the representative of their monarch. The colony had three capitals: Old Russell in 1841; Auckland from 1841 to 1865; and Wellington, which was the capital until the colony's reorganisation into a Dominion, and continues to be the capital of New Zealand till the present day. In 1852, the colony was granted self-government with the passage of the New Zealand Constitution Act 1852. Subsequently, the first parliament was elected in 1853, and responsible government was established in 1856. In 1907, the colony became the Dominion of New Zealand, which heralded a more explicit recognition of self-government within the British Empire. History Establishment Following a proclamation of sovereignty over New Zealand from Sydney in January ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nelson Province
Nelson Province was constituted in 1853 under the New Zealand Constitution Act 1852, and originally covered the entire upper South Island, including all of present-day Buller, Kaikoura, Marlborough, and Tasman districts, along with Nelson City, Grey District north of the Grey River, and the Hurunui District north of the Hurunui River. It was reduced in size by the creation of Marlborough Province in November 1859, then abolished in 1876, along with all the provinces of New Zealand. Area Nelson Province initially covered the entire upper South Island. The Marlborough Province split away from the Nelson Province on 1 November 1859 because the majority of the income of the Provincial Council came from land sales in the Marlborough region, but the funds were mostly used in the Nelson region. Land sales in Nelson and Marlborough netted the Nelson Provincial Council £33,000 and £160,000, respectively. Of that, £200 were expended benefiting the Marlborough region. There was c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāi Tahu
Ngāi Tahu, or Kāi Tahu, is the principal Māori (tribe) of the South Island. Its (tribal area) is the largest in New Zealand, and extends from the White Bluffs / Te Parinui o Whiti (southeast of Blenheim), Mount Mahanga and Kahurangi Point in the north to Stewart Island / Rakiura in the south. The comprises 18 (governance areas) corresponding to traditional settlements. Ngāi Tahu originated in the Gisborne District of the North Island, along with Ngāti Porou and Ngāti Kahungunu, who all intermarried amongst the local Ngāti Ira. Over time, all but Ngāti Porou would migrate away from the district. Several were already occupying the South Island prior to Ngāi Tahu's arrival, with Kāti Māmoe only having arrived about a century earlier from the Hastings District, and already having conquered Waitaha, who themselves were a collection of ancient groups. Other that Ngāi Tahu encountered while migrating through the South Island were Ngāi Tara, Rangitāne, Ngāti T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chert
Chert () is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO2). Chert is characteristically of biological origin, but may also occur inorganically as a precipitation (chemistry), chemical precipitate or a diagenesis, diagenetic replacement, as in petrified wood. Chert is typically composed of the petrified remains of siliceous ooze, the biogenic sediment that covers large areas of the deep ocean floor, and which contains the silicon skeletal remains of diatoms, Dictyochales, silicoflagellates, and radiolarians. Precambrian cherts are notable for the presence of fossil cyanobacteria. In addition to Micropaleontology, microfossils, chert occasionally contains macrofossils. However, some chert is devoid of any fossils. Chert varies greatly in color (from white to black), but most often manifests as gray, brown, grayish brown and light green to rusty redW.L. Roberts, T.J. Campbell, G.R. Rapp Jr. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Obsidian
Obsidian () is a naturally occurring volcanic glass formed when lava extrusive rock, extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock. Obsidian is produced from felsic lava, rich in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. It is commonly found within the margins of rhyolite, rhyolitic lava flows known as obsidian flows. These flows have a high content of silicon dioxide, silica, granting them a high viscosity. The high viscosity inhibits atomic diffusion, diffusion of atoms through the lava, which inhibits the first step (nucleation) in the formation of mineral crystals. Together with rapid cooling, this results in a natural glass forming from the lava. Obsidian is hard, Brittleness, brittle, and amorphous; it therefore Fracture (mineralogy)#Conchoidal fracture, fractures with sharp edges. In the past, it was used to manufacture cutting and piercing tools, and it has been used experimentally as surgic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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