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Manawatū Plains
The Manawatu Plains is an area of low-lying land in New Zealand, located on the floodplains of the Manawatu and Rangitikei Rivers. It is some of the most fertile lands in the southwestern North Island. Stretching from the northern Horowhenua around Levin in the south to Marton in the north, the triangular area of land extends inland from the South Taranaki Bight to almost as far as Ashhurst at the mouth of the Manawatu Gorge. It covers an area of around . In the south, around Lake Horowhenua, the plains were once an extensive wetland, which has been largely drained and turned into profitable dairy farming land. There are conservation moves in progress to restore some of these wetlands to their former state. Further north, the plains provide the basis for the economy which drives the city of Palmerston North and the towns of Foxton, Feilding, and Bulls, all of which rely on the agricultural dollar to an extent. As floodplains, the land is not always entirely dry. Althou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dairy Farming
Dairy farming is a class of agriculture for long-term production of milk, which is processed (either on the farm or at a dairy plant, either of which may be called a dairy A dairy is a business enterprise established for the harvesting or processing (or both) of animal milk – mostly from cows or buffaloes, but also from goats, sheep, horses, or camels – for human consumption. A dairy is typically located on ...) for eventual sale of a dairy product. Dairy farming has a history that goes back to the early Neolithic era, around the seventh millennium BC, in many regions of Europe and Africa. Before the 20th century, milking was done by hand on small farms. Beginning in the early 20th century, milking was done in large scale dairy farms with innovations including Rotary milking parlor, rotary parlors, the milking pipeline, and Automatic milking, automatic milking systems that were commercially developed in the early 1990s. Milk preservation methods have improved starti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plains Of New Zealand
In geography, a plain is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or uplands. In a valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs. Where a geological region contains more than one plain, they may be connected by a pass (sometimes termed a gap). Coastal plains mostly rise from sea level until they run into elevated features such as mountains or plateaus. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. Plains can be formed from flowing lava; from deposition of sediment by water, ice, or wind; or formed by erosion by the agents from hills and mountains. Biomes on plains include grassland (temperate or subtropical), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Manawatū-Whanganui
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tangimoana
Tangimoana is a community in the Manawatū-Whanganui Region of the North Island of New Zealand. It had a population of 303 permanent residents in 2018. It is located 15 kilometres southwest of Bulls, and 30 kilometres west of Palmerston North. The New Zealand Ministry for Culture and Heritage gives a translation of "weeping sea" for . The settlement lies on the southern bank of the Rangitīkei River near the mouth. It was developed in 1920 as a holiday place for people from Palmerston North and other inland towns and sections sold from 1921. The Boating Club has a licensed facility for members and their guests. A small corner store is open daily, it sells basic supplies as well as takeaway food. Tangimoana is well known for its laid back attitude and is popular with those seeking an alternative lifestyle. Many residents are artists and once a year they hold an Art Festival to showcase their works. Tangimoana has limited facilities and very few employment opportunities. Most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Whereve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bulls, New Zealand
Bulls is a small town north west of Palmerston North on the west coast of the North Island of New Zealand. It is in a fertile farming area in the Rangitikei District at the junction of State Highways 1 and 3 about 135 kilometres (84 mi) north of Wellington. According to a Statistics New Zealand estimate, Bulls has a population of inhabitants. Recent marketing makes puns with the name, for example, "New Zealand gets its milk from Bulls" or the sign for the local police station "Const-a-bull". Etymology There are two recorded Māori toponyms for the area – Te Ara Taumaihi and Ō-hine-puhiawe. The origins of Te Ara Taumaihi have yet to be explicitly explored. Ō-hine-puhiawe, a land block where Parewahawaha marae is situated, acts as a synecdoche to refer to the current town area. The modern town name is named after James Bull who owned the first general store there. The town was originally called Bull Town, but this was changed to Clifton and then renamed back to Bulls a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Feilding
Feilding ( mi, Aorangi) is a town in the Manawatū District of the North Island of New Zealand. It is located on State Highway 54, 20 kilometres north of Palmerston North. The town is the seat of the Manawatū District Council. Feilding has won the annual New Zealand's Most Beautiful Town award 15 times. It is an Edwardian-themed town, with the district plan encouraging buildings in the CBD to be built in that style. The town is currently extending its CBD beautification featuring paving and planter boxes on the footpaths on the main streets in the CBD, including the realignment and beautification of Fergusson Street to the South Street entrance of Manfeild Park. The town is a service town for the surrounding farming district. The Feilding Saleyards has been a vital part of the wider Manawatū community for over 125 years. As transport systems improved and farming practices changed, the need for small, local saleyards all but disappeared, leaving few major selling complexes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foxton, New Zealand
Foxton ( mi, Te Awahou) is a town in the Manawatū-Whanganui region of New Zealand - on the lower west coast of the North Island, in the Horowhenua district, southwest of Palmerston North and just north of Levin. The town is located close to the banks of the Manawatu River. It is situated on State Highway 1, roughly in the middle between Tongariro National Park and Wellington. The slightly smaller coastal settlement of Foxton Beach is considered part of Foxton, and is located to the west, on the Tasman Sea coastline. The population was as of Foxton has preserved its heritage - both Maori and Pakeha - through its parks, heritage buildings and four museums. The Manawatu River Loop and estuary creates an environment that features walkways and Ramsar wetlands with 93 species of birds. Changing identity The 50 or so flax mills that once operated in Foxton's vicinity slowly disappeared before WWII, while the Feltex carpet factory closed in 2008, causing unemployment. What ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palmerston North
Palmerston North (; mi, Te Papa-i-Oea, known colloquially as Palmy) is a city in the North Island of New Zealand and the seat of the Manawatū-Whanganui region. Located in the eastern Manawatu Plains, the city is near the north bank of the Manawatu River, from the river's mouth, and from the end of the Manawatu Gorge, about north of the capital, Wellington. Palmerston North is the country's eighth-largest urban area, with an urban population of The official limits of the city take in rural areas to the south, north-east, north-west and west of the main urban area, extending to the Tararua Ranges; including the town of Ashhurst at the mouth of the Manawatu Gorge, the villages of Bunnythorpe and Longburn in the north and west respectively. The city covers a land area of . The city's location was once little more than a clearing in a forest and occupied by small communities of Māori, who called it ''Papa-i-Oea'', believed to mean "How beautiful it is". In the mid-1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Horowhenua
Lake Horowhenua is in the Horowhenua District, an area of the southern Manawatū-Whanganui region in New Zealand's North Island. It covers an area of . The lake, also known as ''Punahau'', is an aeolian lake that lies on a sandy plain west of Levin and from the coast of the Tasman Sea. It is a shallow lake, only some deep, fed by various small streams, and is drained by the Hokio Stream. History The lake was once surrounded by podocarp forest as the centre of a rich wetland ecosystem. Today the trees are gone and the wetland has been substantially drained. The lake is owned by the Māori Muaūpoko iwi, who, with the help of the Horowhenua Lake Trust, are actively attempting to restore the wetland system (which also contains the smaller Lake Papaitonga) to its former state, as a conservation area. In the 1820s the Muaūpoko were attacked by Te Rauparaha and the Ngati Toa. Two island pā on the lake were destroyed. Water quality Between 1952 and 1987 treated sewage from Le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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