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Te Kiekie
Mount Somers / Te Kiekie is a mountain in the South Island of New Zealand, located in the foothills of the Southern Alps. At , it is prominently visible from the Canterbury Plains. The area around the mountain offers opportunities for day walks and overnight tramping. Etymology The mountain's Māori language, Māori name, ''Te Kiekie'', refers to a chief who arrived on the ''Āraiteuru'' canoe. The European name was given by the surveyor of the Canterbury Association, Captain Joseph Thomas (surveyor), Joseph Thomas, and recorded on his 1849 map of Canterbury. Like most names assigned by Thomas, it commemorates a member of the Canterbury Association, in this case the banker and MP Thomas Somers-Cocks (1815–1899). The mountain's European name was later used for a settlement, Mount Somers, and then a branch line railway, the Mount Somers Branch. The settlement is south of the mountain's summit. History Māori people, Māori traversed the area both to access the timber and wild ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Winterslow
Mount is often used as part of the name of specific mountains, e.g. Mount Everest. Mount or Mounts may also refer to: Places * Mount, Cornwall, a village in Warleggan parish, England * Mount, Perranzabuloe, a hamlet in Perranzabuloe parish, Cornwall, England People * Mount (surname) * William L. Mounts (1862–1929), American lawyer and politician Computing and software * Mount (computing), the process of making a file system accessible * Mount (Unix), the utility in Unix-like operating systems which mounts file systems Books * ''Mount!'', a 2016 novel by Jilly Cooper Displays and equipment * Mount, a fixed point for attaching equipment, such as a hardpoint on an airframe * Mounting board, in picture framing * Mount, a hanging scroll for mounting paintings * Mount, to display an item on a heavy backing such as foamcore, e.g.: ** To pin a biological specimen, on a heavy backing in a stretched stable position for ease of dissection or display ** To prepare dead animals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Acland (runholder)
John Barton Arundel Acland (25 November 1823 – 18 May 1904), often referred to as J. B. A. Acland, was born in Devon, England, as the youngest child of Sir Thomas Dyke Acland, 10th Baronet. He followed his father's path of education and became a barrister in London. With his colleague and friend Charles George Tripp, he formed the plan to emigrate to Canterbury, New Zealand, Canterbury, New Zealand, to take up sheep farming. They were the first to take up land in the Canterbury high country for this purpose. When they divided their land into separate holdings, Acland kept the that made up the Mount Peel station. Acland was a committed Anglicanism, Anglican and married Emily Weddell Harper, who was one of the daughters of Henry Harper (bishop), Bishop Harper. He gave the land for a church, which they called the Church of the Holy Innocents with reference to four children buried there, including two of the Aclands. They had a homestead built for themselves, which was probably ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Radio New Zealand
Radio New Zealand (), commonly known as RNZ or Radio NZ, is a New Zealand public service broadcaster and Crown entity. Established under the Radio New Zealand Act 1995, it operates news and current affairs station, RNZ National, and a classical music and jazz station, RNZ Concert, with full government funding from NZ On Air. Since 2014, the organisation's focus has been to transform from a radio broadcaster to a multimedia outlet, increasing its production of digital content in audio, video, and written forms, utilising rnz.co.nz and the RNZ app. The organisation plays a central role in New Zealand public broadcasting. The New Zealand Parliament fully funds its AM network, used in part for the broadcast of parliamentary proceedings. RNZ has a statutory role under the Civil Defence Emergency Management Act 2002 to act as a "lifeline utility" in emergencies. It is also responsible for an international service, RNZ Pacific, which broadcasts to the South Pacific in both ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mayor Of Ashburton
The mayor of Ashburton is the elected head of local government in the Ashburton District of New Zealand's South Island; one of 67 Mayors in New Zealand, mayors in the country. The mayor is based in the principle town (and namesake) of the district, Ashburton, New Zealand, Ashburton. The mayor presides over the Ashburton District Council and is directly elected using the First-past-the-post voting, first-past-the-post method. From 1878 until the 1989 local government reforms, the area was administered by a borough council. Neil Brown is the current mayor of Ashburton; he was first elected in the 2019 New Zealand local elections, 2019 local elections. History The Ashburton Borough Council was inaugurated in 1878. The first mayor was Thomas Bullock, who was elected on 2 September 1878. Nine borough councillors were elected on 5 September and the first council meeting was held on 9 September. Hugo Friedlander was the second mayor when he resigned in July 1892 as he had urgent busines ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Staveley, New Zealand
Staveley is a small township in the Ashburton District, Canterbury, New Zealand, Canterbury, New Zealand. Geography Staveley is named for Robert Staveley, who was a wiktionary:runholder, runholder in the area and who had his farm in this location. Staveley is located on the Inland Scenic Route, which is the former New Zealand State Highway 72, State Highway 72. Staveley is located on the Canterbury Plains, in the foothills of the Southern Alps. Adjacent localities are Bushside to the north-east, Springburn, New Zealand, Springburn to the south-east, and Buccleuch, New Zealand, Buccleuch to the south, all between away. Springburn was the terminus of the Mount Somers Branch from 1889 to 1957. Town facilities In the centre of the township, there is a shop and cafe, an old school that now functions as a museum, a small church, a hall, and a small number of houses. The museum holds photos and artefacts of settlements in the vicinity of Mount Somers / Te Kiekie, a peak of that is th ... [...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] |
Columnar Jointing
Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as Joint (geology), joints, result in the formation of a regular array of polygonal Prism (geometry), prisms, or columns. Columnar jointing occurs in many types of igneous rocks (e.g. basalt, andesite, rhyolite), and forms as the rock cools and contracts. Columnar jointing can occur in cooling lava flows and ashflow tuffs (ignimbrites), as well as in some shallow intrusions. Columnar jointing also occurs rarely in sedimentary rocks, due to a combination of Solution_(chemistry), dissolution and Precipitation_(chemistry), reprecipitation of interstitial minerals (often quartz or cryptocrystalline silica) by hot, hydrothermal fluids and the expansion and contraction of the rock unit, both resulting from the presence of a nearby Igneous intrusion, magmatic intrusion. The columns can vary from 3 meters to a few centimeters in diameter, and can be as much as 30 meters tall. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula
Banks Peninsula () is a rocky peninsula on the east coast of the South Island of New Zealand that was formed by two now-extinct volcanoes. It has an area of approximately . It includes two large deep-water harbours — Lyttelton Harbour and Akaroa Harbour — and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula which, is administered by Christchurch City Council. The main settlements are Lyttelton and Akaroa. The peninsula's economy is based on fisheries, farming and tourism. Māori were the first people to visit, and settle, the peninsula. The sparse population was reduced further following massacres by raiding parties of North Island Māori in 1830 and 1832. In 1770, explorer James Cook became the first European to sight the peninsula, which he mistook for an island, naming it after his ship's botanist Joseph Banks. From the 1830s, European whalers set up shore-based stations in some of the bays and harbo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ignimbrite
Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869–1950) coined the term ''ignimbrite'' from the Latin ''igni-'' [fire] and ''imbri-'' [rain]. Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when Lithification, lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhyolite
Rhyolite ( ) is the most silica-rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture (geology), texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained matrix (geology), groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase. It is the extrusive equivalent of granite. Its high silica content makes rhyolitic magma extremely viscosity, viscous. This favors explosive eruptions over effusive eruptions, so this type of magma is more often erupted as pyroclastic rock than as lava flows. Rhyolitic ash-flow tuffs are among the most voluminous of continental igneous rock formations. Rhyolitic tuff has been used extensively for construction. Obsidian, which is rhyolitic volcanic glass, has been used for tools from prehistoric times to the present day because it can be shaped to an extremely sharp edge. Rhyolitic pumice finds use as an abrasive, in concrete, and as a soil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Geology of Mars, Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) to porphyritic (coarse-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
