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Oruaiti River
The Oruaiti River is a river of the northern Northland Region of New Zealand's North Island. It is fed by Wainui River and flows generally north, draining into Mangonui Harbour at the southern end of Doubtless Bay. It is within the rohe of Ngāti Kahu ki Whangaroa. The river drains the northern edge of Omahuta Forest, runs in a gorge through the Otangaroa massif, then meanders into the Oruaiti estuary, where it is joined by the Kenana River. The catchment is mainly farmland, pine forest and native bush. Pollution in the river is classed as fair to good. In 1862 the lower reaches of the river were described as fern A fern (Polypodiopsida or Polypodiophyta ) is a member of a group of vascular plants (plants with xylem and phloem) that reproduce via spores and have neither seeds nor flowers. The polypodiophytes include all living pteridophytes except t ... country. The native forest was logged after was sold to Auckland Timber Co for £1,250 in 1878. A wharf was au ...
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Doubtless Bay
Doubtless Bay is a bay on the east coast of the Northland Region, north-east of Kaitaia, in New Zealand. It extends from Knuckle Point on Karikari Peninsula in the north to Berghan Point at Hihi in the south. There are rocky headlands, backed by many extensive beaches, such as Tokerau Beach, Taipa, Cable Bay, Coopers Beach, and Mangonui Harbour."Doubtless Bay", An Encyclopedia of New Zealand 1966, ''Te Ara''
(retrieved 12 December 2011)


Māori discovery

, the discoverer of New Zealand, is said to have made his initial lan ...
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New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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Northland Region
The Northland Region ( mi, Te Tai Tokerau) is the northernmost of New Zealand's 16 local government regions. New Zealanders sometimes refer to it as the Winterless North because of its mild climate all throughout the year. The main population centre is the city of Whangārei, and the largest town is Kerikeri. At the 2018 New Zealand census, Northland recorded a population growth spurt of 18.1% since the previous 2013 census, placing it as the fastest growing region in New Zealand, ahead of other strong growth regions such as the Bay of Plenty (2nd with 15%) and Waikato (3rd with 13.5%). Geography The Northland Region occupies the northern 80% (265 km) of the 330 km Northland Peninsula, the southernmost part of which is in the Auckland Region. Stretching from a line at which the peninsula narrows to a width of just 15 km a little north of the town of Wellsford, Northland Region extends north to the tip of the Northland Peninsula, covering an area of 13,940&nb ...
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North Island
The North Island, also officially named Te Ika-a-Māui, is one of the two main islands of New Zealand, separated from the larger but much less populous South Island by the Cook Strait. The island's area is , making it the world's 14th-largest island. The world's 28th-most-populous island, Te Ika-a-Māui has a population of accounting for approximately % of the total residents of New Zealand. Twelve main urban areas (half of them officially cities) are in the North Island. From north to south, they are Whangārei, Auckland, Hamilton, Tauranga, Rotorua, Gisborne, New Plymouth, Napier, Hastings, Whanganui, Palmerston North, and New Zealand's capital city Wellington, which is located at the south-west tip of the island. Naming and usage Although the island has been known as the North Island for many years, in 2009 the New Zealand Geographic Board found that, along with the South Island, the North Island had no official name. After a public consultation, the board officially ...
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Wainui River (Northland)
The Wainui River is a river of the Northland Region of New Zealand's North Island. It flows generally northeast from its sources at the eastern end of the Maungataniwha Range The Maungataniwha Range is a volcanic mountain range located in Northland Region of New Zealand. The Mangamukas, as it is known by the local residents and many Northlanders because of the name of the settlement and river on the southern side, separ ... to reach the Oruaiti River five kilometres southwest of the Whangaroa Harbour. See also * List of rivers of New Zealand References Rivers of the Northland Region Rivers of New Zealand {{Northland-river-stub ...
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Taipa-Mangonui
Taipa-Mangonui or Taipa Bay-Mangonui is a string of small resort settlements – Taipa, Cable Bay, Coopers Beach, and Mangōnui – that lie along the coast of Doubtless Bay and are so close together that they have run together to form one larger settlement. The miniature conurbation lies 150 kilometres by road northwest of Whangārei (and 100 kilometres as the crow flies), 20 kilometres northeast of Kaitaia, and nearly 100 kilometres southeast of the northernmost tip of the North Island. It is the northernmost centre in New Zealand with a population of more than 1000. The New Zealand Ministry for Culture and Heritage gives a translation of "great shark" for ''Mangōnui''. Demographics Taipa-Mangonui, called Taumarumaru for census purposes, covers and had an estimated population of as of with a population density of people per km2. Taumarumaru had a population of 2,193 at the 2018 New Zealand census, an increase of 381 people (21.0%) since the 2013 census, and an increase ...
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Rohe
The Māori people of New Zealand use the word ''rohe'' to describe the territory or boundaries of ''iwi'' (tribes), although some divide their rohe into several ''takiwā''. The areas shown on the map (right) are indicative only, and some iwi areas may overlap. The term ''rohe'' also combines with other words to form more modern terms. These include ''rohe pōti'', meaning an electoral district or constituency, ''rohe wā'', meaning time zone, and ''whatunga rohe paetata'', meaning a local area network. The term ''rohe'' on its own has also been adopted to mean an internet domain. The term is also used for the mission districts (''rohe mihana'') of Te Pīhopatanga o Aotearoa, the Māori Anglican Church in Aotearoa/New Zealand. See also * List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū (sub-tribes) of larger iwi. Moriori are included on this list. ...
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Ngāti Kahu Ki Whangaroa
Ngāti Kahu ki Whangaroa are a Maori ''iwi'' (tribe) based at the Whangaroa Harbour harbour area in New Zealand's Northland Region. The iwi's rohe (tribal area) covers a coastal area from Kaeo and the Whangaroa Harbour in the east, to Oruaiti River, Mangonui and the eastern end of Doubtless Bay in the west. It extends just south of State Highway 10. The rohe of Ngāti Kahu and Ngāpuhi neighbours the rohe of Ngāti Kahu ki Whangaroa. Another similarly named iwi ⁠— Ngāpuhi / Ngāti Kahu ki Whaingaroa ⁠— is also located in Northland. Hapū and marae The iwi consists of the hapū (sub-tribes), who hold gatherings at marae (meeting places) and wharenui (meeting houses): * Hāhi Katorika are affiliated with the Waitāruke Marae and Kahukura Ariki meeting house at Waitāruke. * Hāpeta, Ngāti Kaitangata and Ngāti Rua, based at Taupō Marae and Te Tiriti meeting house at Taupō Bay. *Waimahana, Riwhi and Te Pania are affiliated with Waimahana marae and Te ...
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Massif
In geology, a massif ( or ) is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term also refers to a group of mountains formed by such a structure. In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology. The word is taken from French (in which the word also means "massive"), where it is used to refer a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France. The Face on Mars is an example of an extraterrestrial massif. Massifs may also form underwater, as with the Atlanti ...
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Kenana River
The Kenana River is a river of the North Auckland Peninsula, in New Zealand's North Island. It is located in the north of the peninsula, and flows into Mangonui harbour, an inlet in the south of Doubtless Bay Doubtless Bay is a bay on the east coast of the Northland Region, north-east of Kaitaia, in New Zealand. It extends from Knuckle Point on Karikari Peninsula in the north to Berghan Point at Hihi in the south. There are rocky headlands, backed by .... See also * List of rivers of New Zealand References Far North District Rivers of the Northland Region Rivers of New Zealand {{Northland-river-stub ...
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Tree Fern
The tree ferns are arborescent (tree-like) ferns that grow with a trunk elevating the fronds above ground level, making them trees. Many extant tree ferns are members of the order Cyatheales, to which belong the families Cyatheaceae (scaly tree ferns), Dicksoniaceae, Metaxyaceae, and Cibotiaceae. It is estimated that Cyatheales originated in the early Jurassic, and is the third group of ferns known to have given rise to tree-like forms. The others are the extinct '' Tempskya'' of uncertain position, and Osmundales where the extinct Guaireaceae and some members of Osmundaceae also grew into trees. In addition there were the Psaroniaceae and Tietea in the Marattiales, which is the sister group to most living ferns including Cyatheales. Other ferns which are also tree ferns, are ''Leptopteris'' and ''Todea'' in the family Osmundaceae, which can achieve short trunks under a metre tall. Fern species with short trunks in the genera ''Blechnum'', '' Cystodium'' and ''Sadleria'' from ...
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George Holdship
George Holdship (1839–1923) emigrated to Auckland in 1855 and became a businessman, mainly involved in timber logging and sawmills. His companies (Auckland Timber Company and, from 1888, Kauri Timber Company) removed much of North Island’s native forest, initially kauri and later kahikatea. He moved to Sydney in 1913. Early life George Holdship was born in, or near, Belfast in 1839. When he was 17 (or more likely 16) he emigrated on the Josephine Willis, which left Plymouth on 23 October 1854 and arrived at Auckland on 5 February 1855. A jury list in 1856 showed Henry Holdship of Wakefield St as a grocer. In 1858 it showed Henry Holdship of Chapel St as a draper and George Holdship, also of Chapel St as a carpenter. George trained as a carpenter before forming his own timber firm about 1865, which included a sash and door factory in Newton. During the invasion of the Waikato in 1864, George Holdship gained exemption from service by paying £10, as member of Auckland M ...
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