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Te Mata, Waikato District
Te Mata is a small settlement from Hamilton and from Raglan. Demographics Te Mata is in an SA1 statistical area which extends from Te Mata to Pakoka Landing and covers . The SA1 area is part of the larger Te Uku statistical area. The SA1 area had a population of 186 at the 2018 New Zealand census, an increase of 51 people (37.8%) since the 2013 census, and an increase of 87 people (87.9%) since the 2006 census. There were 57 households, comprising 87 males and 99 females, giving a sex ratio of 0.88 males per female. The median age was 33.8 years (compared with 37.4 years nationally), with 60 people (32.3%) aged under 15 years, 21 (11.3%) aged 15 to 29, 87 (46.8%) aged 30 to 64, and 15 (8.1%) aged 65 or older. Ethnicities were 91.9% European/Pākehā, 17.7% Māori, 3.2% Pacific peoples, 1.6% Asian, and 1.6% other ethnicities. People may identify with more than one ethnicity. Although some people chose not to answer the census's question about religious affiliation, 67.7 ... [...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] |
Opotoru River
The Opotoru River is a river of the Waikato Region of New Zealand's North Island. It flows north, reaching the Raglan Harbour southwest of the town of Raglan. There is no regular monitoring of pollution, but (31.2%) of the river has been fenced to protect it from farm stock. Name ThOct 1947 Lands and Survey one inch mapshows the name 'Opotoru R' applied to the tidal creek of the harbour and 'Opotoru S' to the stretch through Te Mata. The 1971 2nd edition and current 1:50,000 maps (see http://www.topomap.co.nz/NZTopoMap/37544) show 'Opotoru River' for the lower part of the waterway, but 'Te Mata Stream' for the part up from the Te Hutewai Stream confluence. 'Te Mata Stream' appears to have been named 'Takapaunui Stream' in the 1910 postcards (see link below) and in the 1915 Bradbury's Illustrated Guide to The Raglan & Kawhia District. On 7 February 1974 the name Opotoru River was gazetted as the official name for the short length of waterway from Opotoru Creek to Te Mata St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitetuna River
The Waitetuna River is a river of the Waikato Region of New Zealand's North Island. It flows generally northwest from its sources southwest of Whatawhata to reach the southeastern coast of the Raglan Harbour. Geology Mainly Upper Pliocene–Lower Pleistocene Okete volcanics erupted from many vents,Geology of the Raglan-Kawhia Area: Institute of Geological & Nuclear Sciences (N.Z.), Barry Clayton Waterhouse, P. J. White 1994 mainly forming greywacke, with small areas of tephra. History A study for the Regional Council said, "Harbour-wide sediment accumulation rates (SAR) have averaged 0.3-0.5 mm yr−1 over the last 8000-6500 years. The effects of large-scale catchment deforestation (1890-1920s), conversion to pasture and plantation forestry (1985-) on sedimentation have occurred very differently in the Waingaro and Waitetuna arms of the harbour. In the Waitetuna arm, 14C dating of shell and exotic-pollen profiles preserved in core 12B indicate that pre-human SAR of 0.35 mm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Awakino
Awakino is a settlement in the south of Waitomo District, in the North Island of New Zealand. It is located on State Highway 3 at the mouth of the Awakino River, five kilometres north of Mokau. It is 79 km southwest of Te Kuiti, and 98 km northeast of New Plymouth. North of Awakino, State Highway 3 turns inland, and the coast is largely unpopulated. Beyond Awakino there are no settlements of any size on the coast south of the Kawhia Harbour. The New Zealand Ministry for Culture and Heritage gives a translation of "bad creek" for ''Awakino''. The local Maniaroa Marae and meeting house are affiliated with the Ngāti Maniapoto hapū of Ngāti Rākei, Rungaterangi and Waiora. Awakino is in meshblocks 1016500 and 1016900, which had a population of 51 people in the 2018 census. References Further reading General historical works :* :* :* Business history :*Records for the Awakino Co-operative Dairy Company Ltd. ''(active 1911–1925; liquidated 1935)'' are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manukau Heads
The Manukau Heads is the name given to the two promontories that form the entrance to the Manukau Harbour – one of the two harbours of Auckland in New Zealand. The southern head, at the northern tip of Āwhitu Peninsula, is simply termed "The South Head", whereas the northern head is named "Burnett Head" (the term North Head is used to indicate a promontory in the nearby Waitematā Harbour). Both heads are hilly areas of land that rise steeply from the water to over 240m within less than 400m of the shoreline. History In Pre-European times, the west coast of the Āwhitu Peninsula was the site of Paorae, a flat sand dune land which was a major kūmara (sweet potato) cultivation site for Tāmaki Māori iwi. The land eroded during the 18th century, however the sand from the dune feature continued to move northwards, creating vast sand banks in the Manukau Heads and at Whatipu. The foot of the South Head cliffs is the location of the Matatuahu archaeological site, one of the ... [...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] |
The Bush
"The bush" is a term mostly used in the English vernacular of Australia and New Zealand where it is largely synonymous with '' backwoods'' or ''hinterland'', referring to a natural undeveloped area. The fauna and flora contained within this area must be indigenous to the region, although exotic species will often also be present. The Australian and New Zealand usage of the word "bush" for "forest" or scrubland, probably comes from the Dutch word "bos/bosch" ("forest"), used by early Dutch settlers in South Africa, where it came to signify uncultivated country among Afrikaners. Many English-speaking early European settlers to South Africa later migrated to Australia or New Zealand and brought the term with them. Today, in South Africa Fynbos tends to refer to the heath vegetation of the Western Cape and Eastern Cape. It is also widely used in Canada to refer to the large, forested portion of the country. The same usage applies in the US state of Alaska. History Indigenous A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kahikatea
''Dacrycarpus dacrydioides'', commonly known as kahikatea (from Māori) and white pine, is a coniferous tree endemic to New Zealand. A podocarp, it is New Zealand's tallest tree, gaining heights of 60 m and a life span of 600 years. It was first described botanically by the French botanist Achille Richard in 1832 as ''Podocarpus'' ''dacrydioides'', and was given its current binomial name ''Dacrycarpus dacrydioides'' in 1969 by the American botanist David de Laubenfels. Analysis of DNA has confirmed its evolutionary relationship with other species in the genera ''Dacrycarpus'' and ''Dacrydium''. In traditional Māori culture, it is an important source of timber for the building of waka and making of tools, of food in the form of its berries, and of dye. When Europeans discovered it in the 18th century they found large remnant stands in both the North and South Islands, despite burning of forest by early Māori. Its use for timber and its damp fertile habitat, ideal for dairy far ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wiremu Neera Te Awaitaia
Wiremu Neera Te Awaitaia (c.1796 – 27 April 1866) was a Māori chief in New Zealand during first contact with European traders, the 1820s Musket Wars up to the 1860s New Zealand Wars. Born in or around 1796 into the Waikato Tribe of Ngāti Māhanga, he has been described as a "friend of Pākehā and a Chief of great influence" in the region of Raglan, New Zealand. He witnessed the coming of Christianity to Māoridom (specifically the Wesleyan missionaries to Raglan, James and Mary Wallis) in the mid-1830s, the sale of native land to the first European settlers, and the signing of the Treaty of Waitangi in the 1840s. Te Awaitaia also witnessed the Māori King Movement in the 1850s, and the New Zealand Wars in the 1860s. He died on 27 April 1866. The name "Wiremu Neera" is the Maori phonetic rendering of the English name "William Naylor", which Te Awaitaia (his original name) took for himself to mark his conversion to Christianity in 1836. The monument that stands in Raglan, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rohe
The Māori people of New Zealand use the word ''rohe'' to describe the territory or boundaries of ''iwi'' (tribes), although some divide their rohe into several ''takiwā''. The areas shown on the map (right) are indicative only, and some iwi areas may overlap. The term ''rohe'' also combines with other words to form more modern terms. These include ''rohe pōti'', meaning an electoral district or constituency, ''rohe wā'', meaning time zone, and ''whatunga rohe paetata'', meaning a local area network. The term ''rohe'' on its own has also been adopted to mean an internet domain. The term is also used for the mission districts (''rohe mihana'') of Te Pīhopatanga o Aotearoa, the Māori Anglican Church in Aotearoa/New Zealand. See also * List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū (sub-tribes) of larger iwi. Moriori are included on this list. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron Oxide
Iron oxides are chemical compounds composed of iron and oxygen. Several iron oxides are recognized. All are black magnetic solids. Often they are non-stoichiometric. Oxyhydroxides are a related class of compounds, perhaps the best known of which is rust. Iron oxides and oxyhydroxides are widespread in nature and play an important role in many geological and biological processes. They are used as iron ores, pigments, catalysts, and in thermite, and occur in hemoglobin. Iron oxides are inexpensive and durable pigments in paints, coatings and colored concretes. Colors commonly available are in the "earthy" end of the yellow/orange/red/brown/black range. When used as a food coloring, it has E number E172. Stoichiometries Iron oxides feature as ferrous ( Fe(II)) or ferric ( Fe(III)) or both. They adopt octahedral or tetrahedral coordination geometry. Only a few oxides are significant at the earth's surface, particularly wüstite, magnetite, and hematite. * Oxides of FeII ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoria
Scoria is a pyroclastic, highly vesicular, dark-colored volcanic rock that was ejected from a volcano as a molten blob and cooled in the air to form discrete grains or clasts.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. It is typically dark in color (generally dark brown, black or purplish-red), and basaltic or andesitic in composition. Scoria is relatively low in density as a result of its numerous macroscopic ellipsoidal vesicles, but in contrast to pumice, all scoria has a specific gravity greater than 1, and sinks in water. The holes or vesicles form when gases that were dissolved in the magma come out of solution as it erupts, creating bubbles in the molten rock, some of which are frozen in place as the rock cools and solidifies. Scoria may form as part of a lava flow, typically near its surface, or as fragmental ejecta (lapilli, blocks and bombs), for inst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
