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Awamarino
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] |
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] |
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] |
Hapū
In Māori and New Zealand English, a ' ("subtribe", or "clan") functions as "the basic political unit within Māori society". A Māori person can belong to or have links to many hapū. Historically, each hapū had its own chief and normally operated independently of its iwi (tribe). Etymology The word literally means "pregnant", and its usage in a socio-political context is a metaphor for the genealogical connection that unites hapū members. Similarly, the Māori word for land, whenua, can also mean "placenta", metaphorically indicating the connection between people and land, and the Māori word for tribe, iwi, can also mean "bones", indicating a link to ancestors. Definition As named divisions of (tribes), hapū membership is determined by genealogical descent; a hapū consists of a number of (extended family) groups. The Māori scholar Hirini Moko Mead states the double meanings of the word hapū emphasise the importance of being born into a hapū group. As a metaphor t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Maniapoto
Ngāti Maniapoto is an iwi (tribe) based in the Waikato-Waitomo region of New Zealand's North Island. It is part of the Tainui confederation, the members of which trace their whakapapa (genealogy) back to people who arrived in New Zealand on the waka (canoe) Tainui. The 2006 New Zealand census shows the iwi to have a membership of 33,627, making it the 7th biggest iwi in New Zealand. History Ngāti Maniapoto trace their lineage to their eponymous ancestor Maniapoto, an 11th generation descendant of the people who arrived on the ''Tainui'' waka and settled at the Kawhia Harbour. His father Rereahu led the Tainui expansion to the interior of the Waikato region, and Maniapoto settled in the southern Waikato area. Maniapoto's older brother Te Ihinga-a-rangi settled at Maungatautari, forming the Ngāti Hauā and Ngāti Korokī Kahukura iwi. Hapū and marae There are many marae (area in front of a wharenui) in the Ngāti Maniapoto area, one of the notable ones being Te Tokanga Nui ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Index Fossils
Index fossils (also known as guide fossils or indicator fossils) are fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...s used to define and identify geologic periods (or faunal stages). Index fossils must have a short vertical range, wide geographic distribution and rapid evolutionary trends. Another term, Zone fossil is used when the fossil have all the characters stated above except wide geographical distribution, they are limited to a zone and can't be used for correlations of strata. See also * Biostratigraphy#Index fossils References {{Reflist he:מאובן#מאובן מנחה ... [...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] |
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] |
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] |
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