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Heretaunga Plains
:''There are two places in New Zealand called Heretaunga. For the suburb of Upper Hutt, see Heretaunga, Wellington.'' The Heretaunga Plains is a alluvial plain at the southern end of Hawke Bay on the east coast of the North Island of New Zealand. The towns of Napier, Hastings and Havelock North are on the plain. The plain was formed over the last 250,000 years from sediment deposited by the Tutaekuri, Ngaruroro and Tukituki Rivers and from coastal marine deposits. It consists of layers of gravel, sand and silt. Permeable gravel beds form aquifers and the artesian groundwater provides 85% of the requirements for public water supply, irrigation and industrial use on the Heretaunga Plains and adjacent areas. The fertile soil, the warm, dry climate of the area, and the water for irrigation make the plain an excellent site for horticulture and agriculture. Half of the total New Zealand production of fruit, vegetables and grapes is on the Heretaunga Plains. It is one of New Zeal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heretaunga, Wellington
Heretaunga is a suburb of the city of Upper Hutt, located in the lower (southern) North Island of New Zealand. The settlement, one of the older suburbs in the Hutt Valley, dates from the 1840s when European settlers sought country sections. A prime example of a "leafy" suburb, Heretaunga includes quiet tree-lined streets. It is characterised by large houses, often Edwardian or from the mid-20th century. The suburb has numerous green spaces, most evident around the site of the Royal Wellington Wellington Golf Club and at Trentham Memorial Park. The Royal Wellington Golf Club has been based in Heretaunga since 20 November 1906 after acquiring 48.5 hectares of land from the Barton family (descendants of Richard Barton). Heretaunga takes its name from one of the Māori names for the nearby Hutt River, originating from a Hawke's Bay district. Heretaunga adjoins the suburb of Silverstream to its south-west, and the two are commonly thought of associated with each other. To t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngaruroro River
The Ngaruroro River is located in the eastern North Island of New Zealand. It runs for a total of 164 kilometres southeast from the Kaweka Range, Kaimanawa Range and Ruahine Range and then east before emptying into Hawke Bay roughly halfway between the cities of Napier and Hastings, near the town of Clive (drainage area above Tutaekuri River confluence). The river is mostly a single-thread channel down to Whanawhana ( from the coast), flowing through a greywacke rock gorge. Below Whanawhana, the river opens to wide braided channel and is joined by the Maraekakaho River. The Ngaruroro shares a river mouth with the Tutaekuri, Clive River and Muddy Creek. The meeting of these rivers forms the Waitangi Estuary. The Ngaruroro is one of several rivers that helped form the alluvial Heretaunga Plains at the south end of the coast of Hawke Bay. The course of the Ngaruroro has changed several times, originally flowing down what is now the Clive River. It changed to much of its prese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hutt River (New Zealand)
Te Awa Kairangi / Hutt River (Māori:''Te Awa Kairangi'', ''Te Wai o Orutu'' or ''Heretaunga'') flows through the southern North Island of New Zealand. It flows south-west from the southern Tararua Range for , forming a number of fertile floodplains, including Kaitoke, central Upper Hutt and Lower Hutt. The Hutt River Trail, a regional park administered by Wellington Regional Council, runs alongside the eastern side of the river. Toponymy The official name since 2011 is Te Awa Kairangi / Hutt River. Early Māori residents, such as Ngāi Tara, called it Te Awa Kairangi. Later Māori settlers named it Te Wai o Orutu after Orutu, a Ngāti Mamoe ancestor. By the time European settlers arrived, Māori called it Heretaunga, a name adopted by an Upper Hutt suburb and secondary school. The river was named ''Hutt'' after Sir William Hutt, chairman of the New Zealand Company. This name was given by Captain Edward Main Chaffers and Colonel William Wakefield while charting Port Nic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wharenui
A wharenui (; literally "large house") is a communal house of the Māori people of New Zealand, generally situated as the focal point of a ''marae''. Wharenui are usually called meeting houses in New Zealand English, or simply called ''whare'' (a more generic term simply referring to a house or building). Also called a ''whare rūnanga'' ("meeting house") or ''whare whakairo'' (literally "carved house"), the present style of wharenui originated in the early to middle nineteenth century. The houses are often carved inside and out with stylized images of the iwi's (or tribe's) ancestors, with the style used for the carvings varying from tribe to tribe. Modern meeting houses are built to regular building standards. Photographs of recent ancestors may be used as well as carvings. The houses always have names, sometimes the name of a famous ancestor or sometimes a figure from Māori mythology. Some meeting houses are built at places that are not the location of a tribe, but where many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wine
Wine is an alcoholic drink typically made from fermented grapes. Yeast consumes the sugar in the grapes and converts it to ethanol and carbon dioxide, releasing heat in the process. Different varieties of grapes and strains of yeasts are major factors in different styles of wine. These differences result from the complex interactions between the biochemical development of the grape, the reactions involved in fermentation, the grape's growing environment (terroir), and the wine production process. Many countries enact legal appellations intended to define styles and qualities of wine. These typically restrict the geographical origin and permitted varieties of grapes, as well as other aspects of wine production. Wines not made from grapes involve fermentation of other crops including rice wine and other fruit wines such as plum, cherry, pomegranate, currant and elderberry. Wine has been produced for thousands of years. The earliest evidence of wine is from the Caucasus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Groundwater
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, perma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artesian Aquifer
An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer has trapped water, surrounded by layers of impermeable rock or clay, which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached. A well drilled into such an aquifer is called an ''artesian well''. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a ''flowing artesian well''. Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks, similar to how many newly tapped oil wells are pressurized. From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmospher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquifer
An aquifer is an underground layer of water-bearing, permeable rock, rock fractures, or unconsolidated materials (gravel, sand, or silt). Groundwater from aquifers can be extracted using a water well. Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or ''aquifuge''), which is a solid, impermeable area underlying or overlying an aquifer, the pressure of which could create a confined aquifer. The classification of aquifers is as follows: Saturated versus unsaturated; aquifers versus aquitards; confined versus unconfined; isotropic versus anisotropic; porous, karst, or fractured; transboundary aquifer. Challenges for using groundwater include: overdrafting (extracting groundwater beyond the Dynamic equilibrium, equilibrium yield of the aquifer), groundwater-related subsidence of land, gro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tukituki River
The Tukituki River is found in the eastern North Island of New Zealand. It flows from the Ruahine Ranges to the Pacific Ocean at the southern end of Hawke's Bay. The river flows for , east and then northeast, passing through the town of Waipukurau before flowing into Hawke's Bay, close to the city of Hastings. There, the Tukituki Valley is separated from Havelock North/Hastings by the craggy range of hills that includes Te Mata Peak. Etymology The Maori name Tukituki roughly translates "to demolish", presumably referring to the power of the river in flood. Maori legend has it that there are two taniwha living in lake at the southern end of the river that fought over a young boy after he fell into the lake. The struggle of the two taniwha was thought to split the river into the Waipawa Waipawa is the second-largest town in Central Hawke's Bay in the east of the North Island of New Zealand. It has a population of At the 2013 census, it had a population of 1,965, a change of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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