Many of the lakes in the Auckland Region are man made reservoirs, constructed in the hilly catchment areas of the Waitakere and Hunua ranges in order to provide a water supply for the Auckland urban area.
The following is a list of named pools on the Tongariro River. Full details of these pools, many of which are little more than widenings of the river or clear areas of the river's delta marshes, can be found at Pools of the Tongariro River.
In 1917 Lake Rahui was described as no more than a few feet deep, with portions free of flax and raupo. It is probably the remnant of a larger ox-bow lake in a former channel of the Buller.[23] It has been part of the Orikaka Ecological Area since 2001, as lowland swamp forests are rare in the area and it has roroa.[24]
Many of the lakes in the Chatham Islands are either lagoons filling sinkholes in the island's limestone structure, or low-lying peat lakes. The island chain is dominated by Te Whanga Lagoon, which occupies the centre of the main island and accounts for one sixth of the surface area of the archipelago.
New Zealand is divided into sixteen regions for local government purposes. Eleven are administered by regional councils, and five are administered by unitary authorities, which are territorial authorities that also perform the functions of regional councils. The Chatham Islands Council is not a region but is similar to a unitary authority, authorised under its own legislation.
Taupō, sometimes written Taupo, is a town located in the central North Island of New Zealand. It is situated on the edge of Lake Taupō, which is the largest freshwater lake in New Zealand. Taupō was constituted as a borough in 1953. It has been the seat of Taupō District Council since the council was formed in 1989.
The Waikato is a region of the upper North Island of New Zealand. It covers the Waikato District, Waipa District, Matamata-Piako District, South Waikato District and Hamilton City, as well as Hauraki, Coromandel Peninsula, the northern King Country, much of the Taupō District, and parts of the Rotorua Lakes District. It is governed by the Waikato Regional Council.
The Waikato River is the longest river in New Zealand, running for 425 kilometres (264 mi) through the North Island. It rises on the eastern slopes of Mount Ruapehu, joining the Tongariro River system and flowing through Lake Taupō, New Zealand's largest lake. It then drains Taupō at the lake's northeastern edge, creates the Huka Falls, and flows northwest through the Waikato Plains. It empties into the Tasman Sea south of Auckland, at Port Waikato. It gives its name to the Waikato region that surrounds the Waikato Plains. The present course of the river was largely formed about 17,000 years ago. Contributing factors were climate warming, forest being reestablished in the river headwaters and the deepening, rather than widening, of the existing river channel. The channel was gradually eroded as far up river as Piarere, leaving the old Hinuera channel through the Hinuera Gap high and dry. The remains of the old course are seen clearly at Hinuera, where the cliffs mark the ancient river edges. The Waikato's main tributary is the Waipā River, which converges with it at Ngāruawāhia.
Franklin District was a New Zealand territorial authority that lay between the Auckland metropolitan area and the Waikato Plains. As a formal territory, it was abolished on 31 October 2010 and divided between Auckland Council in the Auckland Region to the north and Waikato and Hauraki districts in the Waikato region to the south and east. The Auckland portion is now part of the Franklin Ward, which also includes rural parts of the former Manukau City.
Tuakau is a town in the Waikato region at the foot of the Bombay Hills, formerly part of the Franklin District until 2010, when it became part of Waikato District in the North Island of New Zealand. The town serves to support local farming, and is the residence of many employees of New Zealand Steel at Glenbrook.
Hakarimata Range is a range of hills on the western edge of Ngāruawāhia township, in the Waikato region of New Zealand, overlooking the confluence of the Waikato and Waipā Rivers. The Hakarimata Range is separated from the Taupiri Range by the Taupiri Gorge, through which the Waikato River flows.
Aotea Harbour is a settlement and smallest of three large natural inlets in the Tasman Sea coast of the Waikato region of New Zealand's North Island. It is located between Raglan Harbour to the north and Kawhia Harbour to the south, 30 kilometres southwest of Hamilton.
Regional parks of New Zealand are protected areas administered by regional councils, the top tier of local government. Regional parks are found across five regions of New Zealand: the Auckland Region, Waikato Region, Bay of Plenty Region, Wellington Region and Canterbury Region. Regional parks in the Auckland and Waikato regions are administered by the Auckland Council, while parks in other areas are administered by regional councils: the Bay of Plenty Regional Council, Greater Wellington Regional Council, and Canterbury Regional Council.
The Tongariro River is a river in the North Island of New Zealand. The part of the Waikato River from the Waihohonu Stream, down to Lake Taupō, was formally named the Tongariro River in 1945. The river originates in the Central Plateau of the North Island where it is fed by numerous tributaries that flow off the surrounding hill ranges and mountains such as Mount Ruapehu. It then winds its way north, through the township of Tūrangi before entering Lake Taupō via a number of river mouths. The minimum volume of water flowing down the lower Tongariro River ranges from approximately 16 cubic metres per second (570 cu ft/s) to 21 cubic metres per second (740 cu ft/s). This volume can substantially increase due to catchment of rainfall by the surrounding mountains and hill ranges.
Urban bus transport is the main form of public transport in New Zealand. Two of the country's largest cities, Auckland and Wellington, also have suburban rail systems, while some cities also operate local ferry services. There are no rapid transit metros and no remaining tram systems active anywhere in New Zealand, though trams once had a major role in New Zealand's public transport.
The Tongariro Power Scheme is a 360 MW hydroelectricity scheme in the central North Island of New Zealand. The scheme diverts water from tributaries of the Rangitikei, Whangaehu, Whanganui, and Tongariro rivers. These rivers drain a 2,600-square-kilometre (1,000 sq mi) area including Ruapehu, Ngauruhoe, Tongariro and the western Kaimanawa Ranges. The water diverted from these rivers is sent through canals and tunnels to generate electricity at three hydro power stations, Rangipo (120 MW), Tokaanu (240 MW) and Mangaio (2 MW). The water is then discharged into Lake Taupō where it adds to the water storage in the lake and enables additional electricity generation in the succession of power stations down the Waikato River.
Lake Disappear is an intermittent volcanogenic lake situated in the North Island of New Zealand, just over 20 km from Raglan, 4 km beyond Bridal Veil waterfall. It has also been described as a solution lake. The south end can be seen from Kawhia Rd and, when the north end is full, it can be seen from the point which is at the end of Plateau Rd on the Pipiwharauroa Way. It is the largest known polje in the country, though another large one is in Paparoa National Park.
Public transport in Hamilton and the Waikato Region consists mainly of bus services, as well as some limited train and ferry services. Services are mainly infrequent, and investment hasn't been sufficient to compete with cars, so that subsidies, first introduced in 1971, have increased.
The Awaroa River is a short river in the Waikato District of New Zealand's North Island. It flows east from its source in the dunes near Karioitahi Beach and Lake Puketi, then south from Waiuku joining with the Aka Aka Stream before reaching the Waikato River in its tidal reaches close to Motutieke Island.
Lake Whangape is shallow, supertrophic, lateral and the second largest lake in the lower Waikato River basin in New Zealand. One source said the name translated to 'a large sheet of water', another that it was a chief's name.
Lake Opuatia is a small lake in the much larger Opuatia wetland, which drains from the west into the Waikato River. It lies near the foot of a long valley drained by the Opuatia Stream.
Lake Rotongaro is located to the west of Ohinewai in the Waikato Region of New Zealand. It is a large shallow riverine lake, which links to the Waikato River. It is situated between the Waikato River and the larger Lake Whangape.
Āwhitu Regional Park is a regional park situated on the Āwhitu Peninsula, just south of Manukau Heads on the western side of the Manukau Harbour. It is situated in Franklin in Auckland in New Zealand's North Island, and is administered by Auckland Council.
Portages in New Zealand, known in Māori as Tō or Tōanga Waka, are locations where waka (canoes) could easily be transported overland. Portages were extremely important for early Māori, especially along the narrow Tāmaki isthmus of modern-day Auckland, as they served as crucial transportation and trade links between the east and west coasts. Portages can be found across New Zealand, especially in the narrow Northland and Auckland regions, and the rivers of the Waikato Region.
References
↑ Lowe, D.J.; Green, J.D. (1987). Viner, A.B. (ed.). Inland waters of New Zealand. Wellington: DSIR Science Information Publishing Centre. pp.471–474. ISBN0-477-06799-9.
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