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Hunters Hills
Hunters Hills (also known as The Hunters Hills, ) is a range of mountains in South Canterbury, New Zealand. Naming The Hunters Hills are named as they were a significant hunting area for the local Māori at the time of European settlement. They are known in the Māori language as Te Tari a Te Kaumira meaning "the long range of Te Kaumira" who perished there in a snowstorm. Surveyor Charles Torlesse camped in the Hunters Hills with the chief (rangatira) Te Huruhuru in 1849, who has one of the peaks named after him. Mount Studholme is named after the Studholme family who were early and successful farming pioneers. Geography The hills extend inland from Waimate in a north-west trending line that gets higher and accumulates in Mount Nessing with a height of . To their south is the valley of the Hakataramea River. Geology The Hunter Hills are based on uplifted sediments including coal deposits with a greywacke basement. Hunters Hills fault The uplift is related to the predo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geographic Board
The New Zealand Geographic Board Ngā Pou Taunaha o Aotearoa (NZGB) is the authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local Māori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The board was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (Ngā Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The NZGB secretariat is part of Toitū Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geogra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other Chemical element, elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is a type of fossil fuel, formed when dead plant matter decays into peat which is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous (Pennsylvanian (geology), Pennsylvanian) and Permian times. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its Electricity generation, electricity. Some iron and steel-maki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Department Of Conservation (New Zealand)
The Department of Conservation (DOC; Māori language, 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, 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. Functions and history 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 New Zealand Forest Service, Forest Service and the New Zealand Wildlife Service, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foehn Wind
A Foehn, or Föhn (, , , ), is a type of dry, relatively warm downslope wind in the lee of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Foehn winds can raise temperatures by as much as in just a matter of hours. Switzerland, southern Germany, and Austria have a warmer climate due to the Foehn, as moist winds off the Mediterranean Sea blow over the Alps. Etymology The name ''Foehn'' (, ) arose in the Alpine region. Originating from Latin , a mild west wind of which Favonius was the Roman personification and probably transmitted by or just , the term was adopted as . In the Southern Alps, the phenomenon is known as but also and in Serbo-Croatian and Slovene. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Nimrod
Mount Nimrod (officially Mount Nimrod/Kaumira since 2010) is a hill in the Hunters Hills area of Canterbury, New Zealand. Naming The English name first appears on a map in 1863 but the reason for it being used is unknown. Nimrod was a biblical hunter which has led to speculation. The Hunters Hills are named as they were a significant hunting area for the local Māori at the time of European settlement. Known in the Māori language as Te Tari a Te Kaumira meaning "the long range of Te Kaumira" who perished there in a snowstorm, hence the Māori name for Mount Nimrod. Geology The uplifted Hunter Hills are built on greywacke basement with overlaying sediments including coal deposits. The uplift is related to the predominantly reverse Hunter Hills fault. The fault zone is not particularly active and has been mapped for , with a slip rate of less than /year, an average displacement at events between that occur more than 10,000 years apart. Recreation Hunting The western slopes of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a Fracture (geology), planar fracture or discontinuity in a volume of Rock (geology), rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust (geology), crust result from the action of Plate tectonics, plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction, subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the Plane (geometry), plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geological maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greywacke
Greywacke or graywacke ( ) is a variety of sandstone generally characterized by its hardness (6–7 on Mohs scale), dark color, and Sorting (sediment), poorly sorted angular grains of quartz, feldspar, and small rock fragments or sand-size Lithic fragment (geology), lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic Stratum, strata. The larger Particle size (grain size), grains can be sand- to gravel-sized, and Matrix (geology), matrix materials generally constitute more than 15% of the rock by volume. Formation The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mixed-sediment slurries, in which the resulting deposits may ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hakataramea River
The Hakataramea River flows generally south through the Hakataramea Valley, which is separated from the more inland Mackenzie Basin by the Kirkliston Range in Canterbury, New Zealand. A major tributary of the Waitaki River The Waitaki River is a large braided river in the South Island of New Zealand. It drains the Mackenzie Basin and runs south-east to enter the Pacific Ocean between Timaru and Oamaru on the east coast. It starts at the confluence of the Ōhau Ri ..., it flows for before joining the river from the northeast just below the town of Kurow in the village of Hakataramea. References Rivers of the Canterbury Region Rivers of New Zealand {{CanterburyNZ-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canterbury
Canterbury (, ) is a City status in the United Kingdom, city and UNESCO World Heritage Site, in the county of Kent, England; it was a county borough until 1974. It lies on the River Stour, Kent, River Stour. The city has a mild oceanic climate. Canterbury is a popular tourist destination, with the city's economy heavily reliant upon tourism, alongside higher education and retail. As of 2011, the city's population was over 55,000, including a substantial number of students and one of the highest student-to-permanent-resident ratios in Britain. The site of the city has been occupied since Paleolithic times and served as the capital of the Celtic Cantiaci and Jutes, Jute Kingdom of Kent. Many historical structures fill the area, including a city wall founded in Roman Britain, Roman times and rebuilt in the 14th century, the Westgate Towers museum, the ruins of St Augustine's Abbey, the Norman Canterbury Castle, and the List of the oldest schools in the world, oldest extant schoo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waimate
Waimate is a town in Canterbury, New Zealand, and the seat of Waimate District. It is situated just inland from the eastern coast of the South Island. The town is reached via a short detour west when travelling on State Highway One, the main North/South road. Waimate is 45.7 km south of Timaru, Canterbury's second city, 20 km north of the Waitaki River, which forms the border between Canterbury and the Otago province to the south and 47.5 km north of Oamaru, the main town of the Waitaki District. Waimate is well known for its population of Bennett's wallabies. These marsupials were introduced from Australia and now live wild in the countryside surrounding the town. It is also recognised for the White Horse Monument which is a silhouette of a white horse that can be seen on the hills behind the town. It commemorates the Clydesdale horses that helped breaking in the land in earlier days. Visitors to the monument's lookout are rewarded with panoramic views of the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Studholme
John Studholme (1829–1903) was a 19th-century British pioneer of New Zealand, farmer and politician in the Canterbury region of New Zealand.Mosley, vol.3 p. 2803 Early life John Studholme was born in 1829 the son of John Studholme, a landowner in Cumberland, now part of Cumbria, England. He was educated at Sedbergh School and The Queen's College, Oxford, where he was a university scholar and earned a blue rowing in the university eight. At the age of 22, Studholme sailed to New Zealand with his two younger brothers Michael and Paul. Together they bought farmland in Selwyn and Rakaia. The following year, after having set up farms, they travelled to Australia to pursue the Victorian gold rush. Establishing settlement and farming In 1852, the Studholme brothers returned to New Zealand. Famously, they took a ship which only went as far as Nelson. Together they walked the 350 miles back to Christchurch. From this time on John and Michael began establishing large stations in bot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
