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Hutt River Trail
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 Nich ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tararua Ranges
The Tararua Range, often referred to as the Tararua Ranges or Tararua, is one of several mountain ranges in the North Island of New Zealand. The Tararua Range runs northeast–southwest for from near Palmerston North to the upper reaches of the Hutt Valley, where the northern tip of the Remutaka Range begins. It is separated in the north from the southern end of the Ruahine Range by the Manawatu Gorge. Most of the Range is wilderness, protected as the Tararua Forest Park. The highest peak in the Tararua Range is Pukeamoamo / Mitre (not to be confused with Mitre Peak) at . Other prominent peaks include Mount Bannister at and Mount Hector at , which is named after the scientist Sir James Hector. Its Māori name is Pukemoumou, or 'hill of desolation'. Geography The Tararua Range is divided into two distinct northern and southern regions. Each of these is dominated by a central mountain peak: Arete in the north and Hector in the south. A total of ten rivers rise on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Company
The New Zealand Company, chartered in the United Kingdom, was a company that existed in the first half of the 19th century on a business model focused on the systematic colonisation of New Zealand. The company was formed to carry out the principles devised by Edward Gibbon Wakefield, who envisaged the creation of a new-model English society in the southern hemisphere. Under Wakefield's model, the colony would attract capitalists who would then have a ready supply of labour—migrant labourers who could not initially afford to be property owners, but who would have the expectation of one-day buying land with their savings. The New Zealand Company established settlements at Wellington, Nelson, Wanganui and Dunedin and also became involved in the settling of New Plymouth and Christchurch. The original New Zealand Company started in 1825, with little success, then rose as a new company when it merged with Wakefield's New Zealand Association in 1837, received its royal charter in 1840, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mangaroa River
The Mangaroa River is a river of the Wellington Region of New Zealand's North Island. It flows north from the western foothills of the Remutaka Range to the west of Lower Hutt, meeting with the Hutt River on the northern outskirts of Upper Hutt. 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 the Wellington Region Rivers of New Zealand {{Wellington-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Mārua
Te Mārua (previously also known as Te Marua) is the easternmost urban suburb of Upper Hutt. For reasons of location and distance from the city, the area is often classified as rural. Te Mārua is well known for its Plateau Reserve where remnants of the old Rimutaka Railway path can be found, which now form part of a historic walk. Mt Climie, the highest peak of the Remutaka Range, can also be reached from the reserve. The suburb is also the location of the Wellington Speedway, a nationally important venue for stock car racing, and of the Wellington Naturist Club's club grounds, venue of the historic 2016 World Congress of the International Naturist Federation. Te Mārua is situated on State Highway 2, and is the last significant township (and shop) on the road before it reaches the head of the Hutt Valley and crosses the Remutaka Range into the Wairarapa. Te Mārua is situated in the original floodplain of the Hutt River and parts, particularly the Golf course, have been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rafting
Rafting and whitewater rafting are recreational outdoor activities which use an inflatable raft to navigate a river or other body of water. This is often done on whitewater or different degrees of rough water. Dealing with risk is often a part of the experience. This activity as an adventure sport has become popular since the 1950s, if not earlier, evolving from individuals paddling to rafts with double-bladed paddles or oars to multi-person rafts propelled by single-bladed paddles and steered by a person at the stern, or by the use of oars. Rafting on certain sections of rivers is considered an extreme sport and can be fatal, while other sections are not so extreme or difficult. Rafting is also a competitive sport practiced around the world which culminates in a world rafting championship event between the participating nations. The International Rafting Federation, often referred to as the IRF, is the worldwide body which oversees all aspects of the sport. Equipme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drinking Water
Drinking water is water that is used in drink or food preparation; potable water is water that is safe to be used as drinking water. The amount of drinking water required to maintain good health varies, and depends on physical activity level, age, health-related issues, and environmental conditions. This 2004 article focuses on the USA context and uses data collected from the US military. Recent work showed that the most important driver of water turnover which is closely linked to water requirements is energy expenditure. For those who work in a hot climate, up to a day may be required. Typically in developed countries, tap water meets drinking water quality standards, even though only a small proportion is actually consumed or used in food preparation. Other typical uses for tap water include washing, toilets, and irrigation. Greywater may also be used for toilets or irrigation. Its use for irrigation however may be associated with risks. Water may also be unacceptable due to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaitoke Regional Park
Kaitoke Regional Park is regional park located at Kaitoke, northeast of Upper Hutt, in the Wellington Region of New Zealand's southern North Island. It is administered by Wellington Regional Council, alongside the adjacent regional park of Hutt Water Collection Area. Geography The park covers in the Tararua Ranges foothills. The steep hills and Hutt River gorge are covered in native trees. The conifer-broadleaf rainforest at the fork of Pakuratahi River and Te Awa Kairangi / Hutt River typifies the original vegetation of the area. There is centuries-old rātā, rimu, hinau and kamahi on the upper slopes, red beech on the lower slopes, and black beech on higher spurs and ridge tops with poorer soils. The forests form an ecological corridor between the Remutaka Ranges and Tararua Ranges, and Pakuratahi and Hutt River catchments. The connected bush provides a habitat for a range of birds and native fish, including tūī, kererū, piwakawaka (fantails), korimako (bellbirds) o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headwaters
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Willow Trees
Willows, also called sallows and osiers, from the genus ''Salix'', comprise around 400 speciesMabberley, D.J. 1997. The Plant Book, Cambridge University Press #2: Cambridge. of typically deciduous trees and shrubs, found primarily on moist soils in cold and temperate regions. Most species are known as willow, but some narrow-leaved shrub species are called osier, and some broader-leaved species are referred to as sallow (from Old English ''sealh'', related to the Latin word ''salix'', willow). Some willows (particularly arctic and alpine species) are low-growing or creeping shrubs; for example, the dwarf willow (''Salix herbacea'') rarely exceeds in height, though it spreads widely across the ground. Description Willows all have abundant watery bark sap, which is heavily charged with salicylic acid, soft, usually pliant, tough wood, slender branches, and large, fibrous, often stoloniferous roots. The roots are remarkable for their toughness, size, and tenacity to live, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Levee
A levee (), dike (American English), dyke (English in the Commonwealth of Nations, Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually soil, earthen and that often runs parallel (geometry), parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill dirt, fill or wall that regulates water levels. Ancient civilizations in the Indus Valley civilisation, Indus Valley, ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters. Etymology Speakers of American English (notably in the Midwestern United States, Midwest and Deep South) u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Braided River
A braided river, or braided channel, consists of a network of river channels separated by small, often temporary, islands called braid bars or, in English usage, ''aits'' or ''eyots''. Braided streams tend to occur in rivers with high sediment loads or coarse grain sizes, and in rivers with steeper slopes than typical rivers with straight or meandering channel patterns. They are also associated with rivers with rapid and frequent variation in the amount of water they carry, i.e., with "flashy" rivers, and with rivers with weak banks. Braided channels are found in a variety of environments all over the world, including gravelly mountain streams, sand bed rivers, on alluvial fans, on river deltas, and across depositional plains. Description A braided river consists of a network of multiple shallow channels that diverge and rejoin around ephemeral ''braid bars''. This gives the river a fancied resemblance to the interweaved strands of a braid. The braid bars, also known as channel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
