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Marokopa
Marokopa is a rural community in Waitomo District and Waikato region of New Zealand. It is located close to the coast between Awakino and Kawhia Harbour. The meshblock includes the coastal township of Marokopa, at the mouth of the Marokopa River, and the south side of the small village of Awamarino, about upstream. The area was settled by forestry workers in the 19th century. It has been predominantly a farming locale since the early 20th century. In 1911 a large dairy factory was built, which mainly made butter which was shipped to Auckland. The Awamarino factory was enlarged in 1932, but closed in 1937. A telephone link to Te Kuiti was completed in 1914 and a service car ran on Tuesdays and Fridays from 1920. The town also had a post office, a flaxmill and a school (1908-1982). The nearest school is now Piripiri, upstream. There is a campground. Demographics In 2018, Marokopa was in meshblocks 4002699-700. Previously, it was in meshblock 1019000. These meshblocks had ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marokopa
Marokopa is a rural community in Waitomo District and Waikato region of New Zealand. It is located close to the coast between Awakino and Kawhia Harbour. The meshblock includes the coastal township of Marokopa, at the mouth of the Marokopa River, and the south side of the small village of Awamarino, about upstream. The area was settled by forestry workers in the 19th century. It has been predominantly a farming locale since the early 20th century. In 1911 a large dairy factory was built, which mainly made butter which was shipped to Auckland. The Awamarino factory was enlarged in 1932, but closed in 1937. A telephone link to Te Kuiti was completed in 1914 and a service car ran on Tuesdays and Fridays from 1920. The town also had a post office, a flaxmill and a school (1908-1982). The nearest school is now Piripiri, upstream. There is a campground. Demographics In 2018, Marokopa was in meshblocks 4002699-700. Previously, it was in meshblock 1019000. These meshblocks had ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marokopa River
The Marokopa River is a river of the Waikato Region of New Zealand. It flows west to join the Tasman Sea at Marokopa. The main part of the river is long, with about of tributaries. The catchment is some . Near Te Anga, the river flows over the picturesque Marokopa Falls. The settlements of Awamarino and Marokopa are located on the river's banks. Trout were introduced about 1910. The lower river is polluted. See also *List of rivers of New Zealand This is a list of all waterways named as rivers in New Zealand. A * Aan River * Acheron River (Canterbury) * Acheron River (Marlborough) * Ada River * Adams River * Ahaura River * Ahuriri River * Ahuroa River * Akatarawa River * Ākiti ... References Rivers of Waikato Waitomo District Rivers of New Zealand {{Waikato-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Kinohaku
Kinohaku was a Maori woman of Ngāti Maniapoto in the Tainui tribal confederation from the Waikato region, New Zealand. She is the eponymous ancestor of the Ngāti Kinohaku hapu (sub-tribe) of Ngāti Maniapoto and probably lived in the seventeenth century. Life Kinohaku was a daughter of Rereahu, through whom she was a direct male-line descendant of Hoturoa, the captain of the Tainui canoe, and his second wife Hine-au-pounamu, also a descendant of Hoturoa. She had one older half-brother, Te Ihinga-a-rangi, six full brothers, Maniapoto, Matakore, Tū-whakahekeao, Tūrongo-tapu-ārau, Te Io-wānanga / Te Āio-wānanga, and Kahu-ariari, and one full sister Te Rongorito. Kinohaku and her full siblings were raised in region around Kāwhia. Subsequently, they settled along the Waipā River and the Manga-o-kewa Stream, with a central hub at Te Kūiti. Marriage to Tū-irirangi Kinohaku married Tū-irirangi, who was her cousin on both sides, since his father, Huiao son of Whāita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitomo District
Waitomo District is a territorial authority, located in the Waikato region, at the north of the King Country area in the North Island of New Zealand. A small part of the district, the locality of Tiroa, however, lies in the Manawatū-Whanganui region. The District covers the west coast from Te Maika, on Kawhia Harbour, to the north of Taharoa, to Mokau in the south and extends inland to Maniaiti / Benneydale and Mount Pureora. Demographics Waitomo District covers and had an estimated population of as of with a population density of people per km2. Waitomo District had a population of 9,303 at the 2018 New Zealand census, an increase of 396 people (4.4%) since the 2013 census, and a decrease of 135 people (−1.4%) since the 2006 census. There were 3,384 households, comprising 4,695 males and 4,605 females, giving a sex ratio of 1.02 males per female. The median age was 38.2 years (compared with 37.4 years nationally), with 2,082 people (22.4%) aged under 15 years, 1, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geologic Time Scale
While also using the international geologic time scale, many nations–especially those with isolated and therefore non-standard prehistories–use their own systems of dividing geologic time into epochs and faunal stages. In New Zealand, these epochs and stages use local place names (mainly Māori in origin) back to the Permian. Prior to this time, names mostly align to those in the Australian geologic time scale, and are not divided into epochs. In practice, these earlier terms are rarely used, as most New Zealand geology is of a more recent origin. In all cases, New Zealand uses the same periods as those used internationally; the renaming only applies to subdivisions of these periods. Very few epochs and stages cross international period boundaries, and the exceptions are almost all within the Cenozoic Era. New Zealand updates will always be behind any significant international updates in the International Geological Time Scale. Although the New Zealand geologic time scale h ... [...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] |
List Of Sovereign Nations
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 UN member states, 2 UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a special political status (2 states, both in free association with New Zealand). Compiling a list such as this can be a complicated and controversial process, as there is no definition that is binding on all the members of the community of nations concernin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Triassic
The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series (stratigraphy), series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Geologic time scale, Ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich August von Namoh, Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hakarimata Range
Hakarimata Range is a range of hills on the western edge of Ngāruawāhia township, Retrieved 2016 in the Waikato region of New Zealand, overlooking the confluence of the Waikato and Waipā Rivers. The Hakarimata Range is separated from the Taupiri Range by the Taupiri Gorge, through which the Waikato River flows. After the invasion of the Waikato, parts of the Hakarimatas were confiscated in 1864. of native forest on the range are protected as a scenic reserve. A council supported community group, the Hakarimata Restoration Trust, created in 2001, is helping care for the range. Location Although now usually applied to the hills immediately west of Ngāruawāhia, maps such as Hochstetter's of 1859, the 1925 geology map and 1944 one inch map show 'Hakarimata Range' as extending south to what is now SH23. Similarly, old accounts describe the Whatawhata- Raglan road as passing over the Hakarimatas. Name Hakarimata's name derives from a 17th-century feast, when Ngāti Maniapot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syncline
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimposed smaller folds. Synclines are typically a downward fold (synform), termed a synformal syncline (i.e. a trough), but synclines that point upwards can be found when strata have been overturned and folded (an antiformal syncline). Characteristics On a geologic map, synclines are recognized as a sequence of rock layers, with the youngest at the fold's center or ''hinge'' and with a reverse sequence of the same rock layers on the opposite side of the hinge. If the fold pattern is circular or elongate, the structure is a basin. Folds typically form during crustal deformation as the result of compression that accompanies orogenic mountain building. Notable examples * Powder River Basin, Wyoming, US * Sideling Hill roadcut along Interstate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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