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Ōpōtiki District
Ōpōtiki District is a Districts of New Zealand, territorial authority district in the eastern Bay of Plenty Region on the North Island of New Zealand. It stretches from Kutarere and the eastern shore of Ōhiwa Harbour in the west to Cape Runaway in the north-east, and south from Ōpōtiki town up the Waioeka River into the Raukumara Range. Ōpōtiki District Council is headquartered in Ōpōtiki, the largest town. The district has an area of 3101 square kilometres, of which 3090 square kilometres are land. The population was as of Council history The Whakatane County Council established in 1876 included Ōpōtiki. Opotiki became a Town District in 1882. Opotiki County separated from Whakatane County in 1899 or 1900, and Opotiki town became a borough in 1908 or 1911. The borough and county merged in 1973. In the 1989 local government reforms, some parts of the Opotiki district became part of Whakatane District again. Geography Ōpōtiki District is bounded on one long side b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Districts Of New Zealand
Territorial authorities ( Māori: ''mana ā-rohe'') are a tier of local government in New Zealand, alongside regional councils. There are 67 territorial authorities: 13 city councils, 53 district councils and the Chatham Islands Council. District councils serve a combination of rural and urban communities, while city councils administer the larger urban areas.City councils serve a population of more than 50,000 in a predominantly urban area. Auckland, Gisborne, Nelson, Tasman and Marlborough each have a unitary authority, which performs the functions of both a territorial authority and a regional council. The Chatham Islands Council is a '' sui generis'' territorial authority that is similar to a unitary authority. Territorial authority districts are not subdivisions of regions, and some of them fall within more than one region. Regional council areas are based on water catchment areas, whereas territorial authorities are based on community of interest and road access ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1989 Local Government Reforms
The 1989 New Zealand local government reform was the most significant reform of local government in New Zealand in over a century. Some 850 local bodies were amalgamated into 86 local authorities, on Regions of New Zealand, regional and Territorial authorities of New Zealand, territorial levels. The new authorities were established on 1 November, following the election of members on 14 October 1989. Background The previous major local government reform was the replacement of Provinces of New Zealand, provincial government with elected borough and county councils at the end of 1876. The Counties Act 1876 created Counties of New Zealand, 63 counties out of the rural parts of the provinces. Over subsequent decades, many new bodies were set up, some of them multi-purpose, and others single-purpose, such as harbour boards. The Local Government Act 1974 (New Zealand), Local Government Act 1974 consolidated the law relating to territorial local authorities, removing the distinction b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotorua
Rotorua () is a city in the Bay of Plenty region of New Zealand's North Island. It is sited on the southern shores of Lake Rotorua, from which it takes its name. It is the seat of the Rotorua Lakes District, a territorial authorities of New Zealand, territorial authority encompassing Rotorua and several other nearby towns. It has an estimated resident population of , making it the country's list of New Zealand urban areas by population, 13th largest urban area, and the Bay of Plenty's second-largest urban area behind Tauranga. Māori people, Māori first settled in Rotorua in the 14th century, and a thriving pā was established at Ohinemutu by the people who would become Ngāti Whakaue. The city became closely associated with conflict during the Musket Wars of the 1820s. Ohinemutu was invaded by a Ngāpuhi-led coalition in 1823, commanded by Hongi Hika and Pōmare I (Ngāpuhi), Pōmare I. In the 19th century early European settlers had an interest in developing Rotorua, due to i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
A loess (, ; from ) is a clastic rock, clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposition (geology), deposits. A loess is a periglacial or aeolian processes, aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay with a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. Usually, they are homogeneity and heterogeneity, homogeneous and highly Porosity#Porosity in earth sciences and construction, porous and have vertical capillaries that permit the sediment to fracture and form vertical cliff, bluffs. Properties Loesses are wikt:homogeneous, homogeneous, Porosity#Porosity in earth sciences and construction, porous, friable, pale yellow or buff (color), buff, slightly wikt:coherent, coherent, typically non-stratum, stratified, and often calc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...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 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon 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 (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...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] |
Ōtara River
The Ōtara River is found in the north of New Zealand's North Island. It flows north for , reaching the sea at Ōpōtiki in the eastern Bay of Plenty. It shares its estuary with the Waioeka River The Waioeka River is in the eastern Bay of Plenty Region of New Zealand's North Island. Its name was officially changed to Waioweka River in 2024. The river flows northwards for from Te Urewera National Park to reach the sea at Ōpōtiki. It .... References Rivers of the Bay of Plenty Region Ōpōtiki District {{BayofPlenty-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mōtū River
The Mōtū River is a major waterway in the eastern part of the North Island of New Zealand. It rises south-west of Mātāwai in the Gisborne District, on the south-western side of the Raukūmara Range, and heads roughly northwards to the Pacific Ocean. It flows in a gorge the whole way through the range, where its important tributaries merge with it. It empties into the eastern Bay of Plenty at Houpoto, between Hāwai and Ōmāio, north-east of Ōpōtiki. Description The river passes through mostly uninhabited hill country, very steep and still thickly covered in rainforest. History The first modern traverse of the river, from the Mōtū Falls to its mouth, was in 1920 by the Fisher brothers and S. Thorburn, and this was re-enacted in 2013 by Kevin Biggar and Jamie Fitzgerald in series 2 of the "First Crossings" TV series. A mid-20th century proposal to dam the river for hydroelectricity was rejected.G. W. Gray, 1954. "An Account of the Motu River Hydro Investigations". '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ōhiwa
Ōhiwa is a rural settlement in the Ōpōtiki District and Bay of Plenty Region of New Zealand's North Island. It is on a headland on the eastern side of Ōhiwa Harbour, and on the western side of the Waiotahe River mouth. The New Zealand Geographic Board officially included the macron in the name from 16 July 2020. The Ferry Hotel was opened at Ōhiwa in 1873, together with a ferry service to Ōhope. A post office opened in the growing town in 1877. Unstable sand and erosion from 1915 destroyed the town. A second attempt to create sections for baches in the 1960s was also lost to erosion in 1978. Onekawa Te Mawhai Regional Park was created on the headland in 2010. It incorporates areas of archaeological importance from long Māori use of the area, including Onekawa pā. A local campground provides accommodation. Demographics Ōhiwa is described by Statistics New Zealand as a rural settlement, which covers and had an estimated population of as of with a population de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Hikurangi (Gisborne District)
Mount Hikurangi (or ''Te Ara ki Hikurangi'' in Māori) is a peak in the eastern corner of New Zealand's North Island, about north of Gisborne, and southwest of the East Cape Lighthouse. On a spur of the Raukumara Range in the Waiapu Valley, it is the North Island's highest non-volcanic peak. Mount Hikurangi is within the rohe of Ngāti Porou and Ngati Uēpohatu and is the iwi's most significant icon. In Māori mythology, it was the first part of the North Island to emerge when Māui pulled it as a giant fish from the ocean. According to these beliefs, his waka, '' Nukutaimemeha'', became stranded on the mountain, and lies petrified between the mountain's peaks in Lake Hinetakawhiti. Nearby summits include Whanokao (), Aorangi (), Wharekia () and Taitai (). Together, these mountains provide what '' Te Ara: The Encyclopedia of New Zealand'' calls an "awe-inspiring vista". The early arrivals to Aotearoa commonly gave Polynesian ancestral names and symbolism to New Zea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
