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Whanganui River
The Whanganui River is a major river in the North Island of New Zealand. It is the country's third-longest river, and has special status owing to its importance to the region's Māori people. In March 2017 it became the world's second natural resource (after Te Urewera) to be given its own legal identity, with the rights, duties and liabilities of a legal person. The Whanganui Treaty settlement brought the longest-running litigation in New Zealand history to an end. Geography With a length of , the Whanganui is the country's third-longest river. Much of the land to either side of the river's upper reaches is part of the Whanganui National Park, though the river itself is not part of the park. The river rises on the northern slopes of Mount Tongariro, one of the three active volcanoes of the central plateau, close to Lake Rotoaira. It flows to the north-west before turning south-west at Taumarunui. From here it runs through the rough, bush-clad hill country of the Kin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wanganui River
The Wanganui River is in the West Coast of the South Island of New Zealand. It flows northwest for from its headwaters in the Southern Alps, entering the Tasman Sea near Lake Ianthe, southwest of Hokitika Hokitika is a town in the West Coast region of New Zealand's South Island, south of Greymouth, and close to the mouth of the Hokitika River. It is the seat and largest town in the Westland District. The town's estimated population is as of .... After heavy rain in January 2013 the flooded river partially washed away the single-lane road bridge that carries , closing the only through road on the West Coast. Gravel buildup has gradually raised the riverbed, and in 2021 the West Coast Regional Council planned to elevate stopbanks by 1 m at a cost of $5.7 million to protect neighbouring farmland from flooding. Farmers protested the rates rise that would be needed to pay back this 30-year loan, and suggested the Department of Conservation should contribute. Ref ... [...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 whic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Ruapehu
Mount Ruapehu (; ) is an active stratovolcano at the southern end of the Taupō Volcanic Zone and North Island volcanic plateau in New Zealand. It is northeast of Ohakune and southwest of the southern shore of Lake Taupō, within the Tongariro National Park. The North Island's major ski resorts and only glaciers are on its slopes. Ruapehu, the largest active volcano in New Zealand, has the highest point in the North Island and has three major peaks: Tahurangi (2,797 m), Te Heuheu (2,755 m) and Paretetaitonga (2,751 m). The deep, active crater is between the peaks and fills with water between major eruptions, being known as Crater Lake ( mi, Te Wai ā-moe). The name ''Ruapehu'' means "pit of noise" or "exploding pit" in Māori. Geography Ruapehu is located in the center of the North Island of New Zealand, northeast of Ohakune, New Zealand and southwest of the southern shore of Lake Taupō, within Tongariro National Park. Ruapehu is the largest and southernm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Timeline Of New Zealand History
This is a timeline of the history of New Zealand that includes only events deemed to be of principal importance – for less important events click the year heading or refer to List of years in New Zealand. Prehistory (to 1000 CE) * 85 mya: Around this time New Zealand splits from the supercontinent Gondwana. * 5 mya: New Zealand's climate cools as Australia drifts north. Animals that have adapted to warm temperate and subtropical conditions become extinct. * 26,500 BP: The Taupō volcano erupts extremely violently, covering much of the country with volcanic ash and causing the Waikato River The Waikato River is the longest river in New Zealand, running for 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 th ... to avulse from the Hauraki Plains to its current path through the Waikato to the Tasman Sea. * 18,000 BP: New Zealand's North and Sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1843 Wanganui Earthquake
The 1843 Whanganui earthquake occurred on 8 July at 16:45 local time with an estimated magnitude of 7.5 on the scale. The maximum perceived intensity was IX (''Violent'') on the Mercalli intensity scale, and possibly reaching X (''Extreme''). The epicentre is estimated to have been within a zone extending 50 km northeast from Whanganui towards Taihape. GNS Science has this earthquake catalogued and places the epicentre 35 km east of Taihape, near the border of Hawke's Bay. This was the first earthquake in New Zealand over magnitude 7 for which written records exist, and the first for which deaths were recorded. Tectonic setting New Zealand lies along the boundary between the Australian and Pacific Plates. In South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In North Island the displacement is mainly taken up along the Kermadec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jasons Travel Media
Jasons is a publisher of travel guides and an online directory of activities and lodging in New Zealand, Australia, and the South Pacific. Jasons produces 62 free travel guides annually. History The company was started as a family business in 1967 by John Sanford. In 1996, the company launched a website. Jason Publishing Co Ltd was renamed to Jasons Travel Media in 2000. In 2005, it became a public company via an initial public offering on the New Zealand Stock Exchange. In August 2006, Steven Joyce, later Minister of Economic Development, Minister of Science and Innovation, Minister for Tertiary Education, Skills and Employment and Associate Minister of Finance in New Zealand, became chief executive officer of the company after he acquired an 8.8% stake. In 2008, the company acquired Strait Solutions; the Today-Tonight visitor guide print publications in Christchurch and Queenstown; and the brochure distribution services and two visitor guides of Whytewaters in Queenstown. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jerusalem, New Zealand
Jerusalem, named for the Biblical Jerusalem (in Māori, ''Hiruhārama''), is a settlement up the Whanganui River from Whanganui, New Zealand. Originally called Patiarero, it was one of the largest settlements on the Whanganui River in the 1840s, with several hundred Ngāti Hau inhabitants of the iwi Te Āti Haunui-a-Pāpārangi. Unlike other Whanganui River settlements given transliterated place names by Reverend Richard Taylor in the 1850s, Jerusalem is usually referred to using the English version of its name. It grew into several small settlements, including Roma (named for Rome) and Peterehama (named for Bethlehem), founded by the remains of Taylor's congregation after the majority converted to Catholicism when a Roman Catholic mission was built in 1854. Jerusalem was the isolated site where, in 1892, Suzanne Aubert (better known as Mother Mary Joseph) established the congregation of the Sisters of Compassion. They became a highly respected charitable nursing/religious or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pipiriki
Pipiriki is a settlement in New Zealand, on the east bank of the Whanganui River, due west of the town of Raetihi and upriver from Whanganui; it was originally on the opposite bank. It is the home of Ngāti Kura, a hapū of the Ngāti Ruanui iwi. It is also the location of the Paraweka Marae of the hapū Ngāti Kurawhatia of the iwi Te Āti Haunui-a-Pāpārangi. In the 1840s Pipiriki was a large stockaded settlement, the second largest on the Whanganui River, consisting of eight pā with a total population of 250–300. Wheat was a major crop from 1848 onward, and the water-powered Kaukore flour mill was built in 1854. In 1865 three redoubts across the river were besieged for several weeks by Pai Mārire warriors. Pipiriki was an important part of the riverboat trade in the 1890s–1920s, marking a major stop for paddle steamers making the 11-hour journey from Whanganui. There are four marae in the Pipiriki area affiliated with local iwi and hapū: * Kirikiriroa Marae and K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King Country
The King Country (Māori: ''Te Rohe Pōtae'' or ''Rohe Pōtae o Maniapoto'') is a region of the western North Island of New Zealand. It extends approximately from the Kawhia Harbour and the town of Otorohanga in the north to the upper reaches of the Whanganui River in the south, and from the Hauhungaroa and Rangitoto Ranges in the east to near the Tasman Sea in the west. It comprises hill country, large parts of which are forested. The region, albeit loosely defined, is very significant in New Zealand's history. The term "King Country" dates from the New Zealand Wars of the 1860s, when colonial forces invaded the Waikato and forces of the Māori King Movement withdrew south of what was called the ''aukati'', or boundary, a line of '' pa'' alongside the Puniu River near Kihikihi. Land behind the ''aukati'' remained native territory, with Europeans warned they crossed it under threat of death. Known for its rugged, rural roads and diverse landscape, the King Country has a warm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Rotoaira
Lake Rotoaira (sometimes written ''Lake Roto-aira'') is a small lake to the south of Lake Taupō on the North Island Volcanic Plateau in New Zealand. It covers an area of 13 km². Lake Rotoaira is one of the few privately owned lakes in New Zealand being administered by the Lake Rotoaira Trust on behalf of its owners. An access permit must be held by those using the lake for fishing and similar activities. The lake is located in a graben between the broad volcanic dome of Mount Tongariro to the south and the smaller volcanic peak of Pihanga to the northwest. It is naturally drained by the Poutu Stream into the Tongariro River. However the Tongariro Power Scheme utilised Rotoaira as a storage lake for the Tokaanu Hydropower Station. Extensive engineering works were carried out including the diversion of a number of other streams (including Whanganui River) into Rotoaira via the Otamangakau Hydro Lake and construction of a tunnel through Pihanga to the Tokaanu Power Station ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Island Volcanic Plateau
The North Island Volcanic Plateau (often called the Central Plateau and occasionally the Waimarino Plateau) is a volcanic plateau covering much of central North Island of New Zealand with volcanoes, lava plateaus, and crater lakes. It contains the Taupō caldera complex, Okataina caldera complex and Tongariro Volcanic Centre being currently the most frequently active and productive area of silicic volcanism on Earth. New Zealand is part of the Pacific Ring of Fire. Location and description The plateau is approximately east–west and the north–south distance is about . Extensive ignimbrite sheets spread east and west from the Central Taupō Volcanic Zone, centred on the huge active supervolcanic caldera of Lake Taupō, now the largest lake in New Zealand. This last erupted less than 2000 years ago. The volcanic area includes the three active peaks of Mount Tongariro, Mount Ngāuruhoe, and Mount Ruapehu in the south, and extends beyond Rotorua in the north reach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whanganui National Park
The Whanganui National Park is a national park located in the North Island of New Zealand. Established in 1986, it covers an area of 742 km2 bordering the Whanganui River. It incorporates areas of Crown land, former state forest and a number of former reserves. The river itself is not part of the park.Department of Conservation"Whanganui National Park. Flora & fauna" retrieved 21 April 2013 Flora and fauna The park protects the habitat of several thousand North Island brown kiwi, and the also-endangered blue duck. Other birds in the park include the grey warbler, New Zealand pigeon, silvereye, tomtit, tui and whitehead. See also * Bridge to Nowhere, New Zealand *National parks of New Zealand *Protected areas of New Zealand *Conservation in New Zealand Conservation in New Zealand has a history associated with both Māori and Europeans. Both groups of people caused a loss of species and both altered their behaviour to a degree after realising their effect on indigenous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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