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Piako River
The Piako River is a lowland river system that drains into the Firth of Thames on the North Island of New Zealand. Together with the Waihou River, it is one of the two main rivers systems which drains the Hauraki Plains. It is the dominant river system in the Matamata-Piako District, and on its journey it passes through the towns of Morrinsville and Ngatea. The Piako River has an annual mean flow of (at Paeroa-Tahuna Road), with a total catchment area of approximately . The river system is approximately long, aligned in a north-south direction and occupies much of the central and western Hauraki Plains (or more broadly, the Thames Valley), extending from Hinuera in the south before discharging into the Firth of Thames in the north, five kilometres west of Thames. The Piako River has two major stems: the first, and main, stem drains the northern Te Miro-Tahuroa hills, and the Pakaroa Range. The dominant tributaries on the eastern slopes of these hills are the Piakonui and Piako ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Miro
Te Miro is an area in the Waipa District of the Waikato Region of the North Island of New Zealand. Te Miro is situated 31 kilometres east southeast of Hamilton, New Zealand, Hamilton, and 24 kilometres northeast of Cambridge, New Zealand, Cambridge. Te Miro has a population of approximately 500. History The name Te Miro for the area first became used in 1916, when it was surveyed and developed for European settlement. Prior to that, the area was known as Maungakawa. The first Maori Pā settlement in the Te Miro area was by the Ngati Haua people at Te Kawehitiki (37 49 20; 175 34 50), located on the lower reaches of the Maungakawa volcanic cone, which is on the present day Hopehill farm,Hewitt, Joslyn (1995). ''Te Miro a history book to commemorate the 75th school and district reunion 1975''. Te Miro. at 789 Te Miro Road. There is a history of large Maori gatherings beginning at the site in the 1880s, with a notable large gathering in 1893. Maungakawa became a focal point for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitakaruru Stream
The Waitakaruru Stream is a major tributary of the Piako River, within the Waikato region of New Zealand's North Island. It should not be confused with the similarly named Waitakaruru River, which is also in the Waikato Region. The Waitakaruru Stream has its origin in the Te Miro-Tahuroa Hills south of Morrinsville, within the Waikato District. Initially the stream flows south and south-west through Scotsman's Valley before turning northwards at Tauwhare flowing roughly parallel to the Pakaroa Range as it passes the boundary of Eureka before entering the Matamata-Piako District. The stream passes through the settlement of Motumaoho, progressively turning a more easterly direction towards Morrinsville, where it has a walkway beside it and converges with the larger Piako River The Piako River is a lowland river system that drains into the Firth of Thames on the North Island of New Zealand. Together with the Waihou River, it is one of the two main rivers systems which drains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Waikato
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tauranga
Tauranga () is a coastal city in the Bay of Plenty region and the fifth most populous city of New Zealand, with an urban population of , or roughly 3% of the national population. It was settled by Māori late in the 13th century, colonised by Europeans in the early 19th century, and was constituted as a city in 1963. The city lies in the north-western corner of the Bay of Plenty, on the south-eastern edge of Tauranga Harbour. The city extends over an area of , and encompasses the communities of Bethlehem, New Zealand, Bethlehem, on the south-western outskirts of the city; Greerton, on the southern outskirts of the city; Matua, west of the central city overlooking Tauranga Harbour; Maungatapu; Mount Maunganui, located north of the central city across the harbour facing the Bay of Plenty; Otūmoetai; Papamoa, Tauranga's largest suburb, located on the Bay of Plenty; Tauranga City; Tauranga South; and Welcome Bay. Tauranga is one of New Zealand's main centres for business, interna ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaihere
Kaihere is a dispersed Waikato rural settlement on SH27, overlooking the Hauraki Plains. It has a school, hall, domain a rest area and is the starting point for the Hapuakohe Walkway. Demographics Kaihere's meshblock (1069500 includes the school and most houses) had these census results - Geology The village lies on the edge of greywacke, of the Jurassic Manaia Hill Group, and the peat of the Hauraki graben. Much of the village is built on the Pliocene Puketoka formation between those. That formation has boulders of andesite, quartz vein-stone, cryptocrystalline silica, and banded rhyolite, with cobbles of greywacke, in a poorly cemented bed of pumice silt. The Hauraki rift probably started about 3 million years ago. Subsidence now is about a year. History The early inhabitants largely used the wetlands for fishing. Ngāti Hako and Ngāti Pāoa lived in the area when early settlers arrived. The Musket Wars caused much disruption in the 1820s. Government gradually ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intensive Farming
Intensive agriculture, also known as intensive farming (as opposed to extensive farming), conventional, or industrial agriculture, is a type of agriculture, both of crop plants and of animals, with higher levels of input and output per unit of agricultural land area. It is characterized by a low fallow ratio, higher use of inputs such as capital and labour, and higher crop yields per unit land area. Most commercial agriculture is intensive in one or more ways. Forms that rely heavily on industrial methods are often called industrial agriculture, which is characterised by innovations designed to increase yield. Techniques include planting multiple crops per year, reducing the frequency of fallow years, and improving cultivars. It also involves increased use of fertilizers, plant growth regulators, pesticides, antibiotics for livestock and mechanised agriculture, controlled by increased and more detailed analysis of growing conditions, including weather, soil, water, weeds, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hapuakohe Range
Hapuakohe Range of hills is aligned north-south, between the Waikato River and the Hauraki Plains in the Waikato region of New Zealand. It is separated from the Taupiri Range by an air-gap at Mangawara, where the Waikato flowed about 20,000 years ago. The range is drained by the Waitakaruru and Whangamarino Rivers and their tributaries at the north end. Further south, tributaries of the Piako River drain the east side of the range and streams flow to the Waikato on the west. The 1865 confiscation boundary ran along the range. The boundary between Waikato and Ohinemuri (from 1920 Hauraki Plains) counties followed a similar line, as does the current boundary between Waikato, Hauraki and Matamata Piako Districts. Named summits and road From north to south, the features named on the LINZ map are: * Pukekamaka * Okaeria * Karamuroa * Otane * Ikeike - west of main ridge – a low priority walkway plan may link them. * Matahuru Rd - in 2007 the lower part of the road ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tahuna, Waikato
Tahuna is a small rural settlement located 18 km north of Morrinsville. In the Māori language Tahuna means sandbank, likely to refer to the sandbanks along the nearby Piako River, where a Māori settlement started. Tahuna is seen as the upper limit for navigatable travel on the Piako River. The settlement has a rugby club, a lawn bowls club, a golf course and various shops. Although Tahuna is in the Matamata-Piako District for local government, its representation in national government is within the Coromandel electorate due to the abolition of the Piako electorate for the . A town water supply was proposed in the 1980s and installed in the 2000s. There are two marae in the Tahuna area. The Waiti-Raungaunu marae and Paoa meeting house are also associated with the Waikato Tainui hapū of Ngāti Makirangi, and with the iwi of Ngāti Paoa. Hoe o Tainui marae and surrounding settlement is affiliated with Ngāti Makirangi. Demographics Tahuna is in an SA1 statistical area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kopuatai Peat Dome
The Kopuatai Peat Dome is a large peatland complex on the Hauraki Plains in the North Island of New Zealand. It consists of two raised domes, one in the north and the other in the south, that are up to three metres higher at the center than at the edge. The wetland contains the largest intact raised bog in New Zealand and was listed under the Ramsar Convention in 1989 as a Wetland of International Importance. Most of the wetland is ombrotrophic, meaning it receives water and nutrient inputs solely from rain and is hydrologically isolated from the surrounding canals and rivers. Locally, a popular misconception persists that water flows from the nearby Piako River into the bog and that the wetland acts as a significant store for floodwater. History of the wetland Kopuatai has survived extensive draining of the wetlands on the Hauraki Plains and was given protection in 1987 when it came under the administration of the newly formed Department of Conservation. Scientific and co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitoa River
Waitoa is a settlement in the Matamata-Piako District of New Zealand. State Highway 26 runs through the town, and connects to Te Aroha 10 km to the north-east. A Fonterra dairy factory is a prominent blue building in the middle of the town. The Waitoa River runs through the village and is prone to flooding. A railway line runs to the dairy factory, and used to go to Te Aroha, however this section was closed and the line only runs to service the dairy factory. Two freezing works and a rendering plant also operate in the Waitoa area. Workers commute from nearby towns of Te Aroha, Morrinsville and Matamata. Demographics Statistics New Zealand describes Waitoa as a rural settlement, which covers . Waitoa is part of the larger Waitoa-Ngarua statistical area. Waitoa had a population of 291 at the 2018 New Zealand census, an increase of 6 people (2.1%) since the 2013 census, and unchanged since the 2006 census. There were 114 households, comprising 144 males and 150 females, gi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thames, New Zealand
Thames () ( mi, Pārāwai) is a town at the southwestern end of the Coromandel Peninsula in New Zealand's North Island. It is located on the Firth of Thames close to the mouth of the Waihou River. The town is the seat of the Thames-Coromandel (district), New Zealand, Thames-Coromandel District Council. The Māori people, Māori iwi are Ngāti Maru (Hauraki), Ngāti Maru, who are descendants of Marutuahu's son Te Ngako. Ngāti Maru is part of the Ngati Marutuahu confederation of tribes or better known as Hauraki Iwi. Thames had an estimated population of 15,000 in 1870, but this declined to 4,500 in 1881, and it has increased modestly since. It is still the biggest town on the Coromandel. Until 2016, a historical Oak, oak tree that was planted by Governor George Grey stood on the corner of Grey and Rolleston streets. Demographics Thames covers and had an estimated population of as of with a population density of people per km2. Thames had a population of 7,293 at the 2018 Ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Thames
The Firth of Thames ( mi, Tikapa Moana-o-Hauraki) is a large bay located in the north of the North Island of New Zealand. It is the firth of the rivers Waihou and Piako, the former of which was formerly named the Thames River, and the town of Thames lies on its southeastern coast. Its Maori name is ''Tikapa''. In traditional legend, the firth and the greater Hauraki Gulf are protected by a taniwha named Ureia, who takes the form of a whale. The firth lies at the southern end of the Hauraki Gulf, southeast of the city of Auckland. It occupies a rift valley or graben between the Coromandel Peninsula and Hunua Ranges, which continues into the Hauraki Plains to the south. Conservation The Firth of Thames is an important site for waders or shorebirds, and is listed as a wetland of international importance under the Ramsar Convention. The Miranda Shorebird Centre, operated by the Miranda Naturalists' Trust, is located on the Seabird Coast, on the western shore of the bay at M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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