Motukorea
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Motukorea
Motukorea or Browns Island is a small New Zealand island, in the Hauraki Gulf north of Musick Point, one of the best preserved volcanoes in the Auckland volcanic field. The age of eruption is about 25,000 years ago, when the Tāmaki Estuary and the Waitemata Harbour were forested river valleys. Due to centuries of cultivation, little native bush remains except on the north-eastern cliffs, leaving the volcanic landforms easily visible. It exhibits the landforms from three styles of eruption. The island consists of one main scoria cone with a deep crater, a small remnant arc of the tuff ring forming the cliffs in the northeast, and the upper portions of lava flows. The area was dry land when the eruptions occurred, but much of the lava is now submerged beneath the sea. Geology Motukorea erupted approximately 24,500 years ago. It began life with a series of wet explosive eruptions that cleared it of any debris and created a 1-kilometre shallow crater, as seen today. The eject ...
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Hauraki Gulf / Tīkapa Moana
The Hauraki Gulf / Tīkapa Moana is a coastal feature of the North Island of New Zealand. It has an area of 4000 km2,
Zeldisl, J. R. et al. (1995) Salp grazing: effects on phytoplankton abundance, vertical distribution and taxonomic composition in a coastal habitat. Marine Ecology Progress Series, Vol. 126, p 267-283
and lies between, in anticlockwise order, the , the , the , and

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Hauraki Gulf
The Hauraki Gulf / Tīkapa Moana is a coastal feature of the North Island of New Zealand. It has an area of 4000 km2,
Zeldisl, J. R. et al. (1995) Salp grazing: effects on phytoplankton abundance, vertical distribution and taxonomic composition in a coastal habitat. Marine Ecology Progress Series, Vol. 126, p 267-283
and lies between, in anticlockwise order, the , the Hauraki Plains, the , and
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Auckland Volcanic Field
The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island. The approximately 53 volcanoes in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With the exception of Rangitoto, no volcano has erupted more than once, but the other eruptions lasted for various periods ranging from a few weeks to several years. Rangitoto erupted several times and recently twice; in an eruption that occurred about 600 years ago, followed by a second eruption approximately 50 years later. The field is fuelled entirely by basaltic magma, unlike the explosive subduction-driven volcanism in the central North Island, such as at Mount Ruapehu and Lake Taupō.Ian E.M. Smith and Sharon R. Allen. Auckland volcanic field geology'. Volcanic Hazards Working Group, Civil Defence Scientific Advisory Committee. Retrieved 30 March 2013. Also ...
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Bucklands Beach
Bucklands Beach is a suburb east of Auckland's CBD in New Zealand. The suburb is in the Howick ward, one of the thirteen administrative divisions of Auckland Council. Demographics Bucklands Beach covers and had an estimated population of as of with a population density of people per km2. Bucklands Beach had a population of 9,042 at the 2018 New Zealand census, an increase of 225 people (2.6%) since the 2013 census, and an increase of 444 people (5.2%) since the 2006 census. There were 2,919 households, comprising 4,446 males and 4,593 females, giving a sex ratio of 0.97 males per female, with 1,662 people (18.4%) aged under 15 years, 1,812 (20.0%) aged 15 to 29, 4,317 (47.7%) aged 30 to 64, and 1,257 (13.9%) aged 65 or older. Ethnicities were 51.1% European/Pākehā, 3.3% Māori, 2.2% Pacific peoples, 45.3% Asian, and 3.3% other ethnicities. People may identify with more than one ethnicity. The percentage of people born overseas was 55.2, compared with 27.1% natio ...
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Musick Point
Musick Point Te Naupata (; officially Musick Point / Te Naupata) is the headland of the peninsula that forms the eastern shore of the Tāmaki River in Bucklands Beach, a suburb of Auckland, New Zealand. In 1942, Musick Point was named after Ed Musick, an aviator who visited New Zealand in 1937,Musick Point - Early History
(from the New Zealand Association of Radio Transmitters (NZART) website. Retrieved 2007-10-02.)
although the headland is also known as ''Te Waiarohia'', after an ancient Māori stronghold. Today, it is occupied by a golf club and the Musick Memorial Radio Station. The peninsula itself terminates between the Motukorea Channel and the
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Ngāti Whātua
Ngāti Whātua is a Māori iwi (tribe) of the lower Northland Peninsula of New Zealand's North Island. It comprises a confederation of four hapū (subtribes) interconnected both by ancestry and by association over time: Te Uri-o-Hau, Te Roroa, Te Taoū, and Ngāti Whātua-o-Ōrākei. The four hapū can act together or separately as independent tribes. Ngāti Whātua's territory or ''rohe'' is traditionally expressed as, "''Tāmaki ki Maunganui i te Tai Hauauru''" and "''Tāmaki ki Manaia i te Rawhiti''". The northern boundary is expressed as, "''Manaia titiro ki Whatitiri, Whatitiri titiro ki Tutamoe, Tutamoe titiro ki Maunganui''". The southern boundary is expressed as, "''Te awa o Tāmaki''". The area runs from Tāmaki River in the south to Maunganui Bluff (at the northern end of Aranga Beach on the west coast) in the north, and to Whangarei Harbour on the east coast. By the time of European settlement in New Zealand, Ngāti Whātua's territory was around the Kaipara Harbour an ...
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Tainui
Tainui is a tribal waka confederation of New Zealand Māori iwi. The Tainui confederation comprises four principal related Māori iwi of the central North Island of New Zealand: Hauraki, Ngāti Maniapoto, Ngāti Raukawa and Waikato. There are other Tainui iwi whose tribal areas lay outside the traditional Tainui boundaries – Ngāi Tai in the Auckland area, Ngāti Raukawa ki Te Tonga and Ngāti Toa in the Horowhenua, Kapiti region, and Ngāti Rārua and Ngāti Koata in the northern South Island. History Early history The Tainui iwi share a common ancestry from Polynesian migrants who arrived in New Zealand on the ''Tainui'' waka, which voyaged across the Pacific Ocean from Hawaiki to Aotearoa (North Island) approximately 800 years ago. According to Pei Te Hurinui Jones, the Tainui historian, Tainui first entered the Waikato about 1400 bringing with them kumara plants. By about 1450 they had conquered the last of the indigenous people in a battle at Atiamuri. Contact with ...
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Firth Of Thames
The Firth of Thames ( mi, Tikapa Moana-o-Hauraki) is a large bay located in the north of the North Island of New Zealand. It is the firth of the rivers Waihou and Piako, the former of which was formerly named the Thames River, and the town of Thames lies on its southeastern coast. Its Maori name is ''Tikapa''. In traditional legend, the firth and the greater Hauraki Gulf are protected by a taniwha named Ureia, who takes the form of a whale. The firth lies at the southern end of the Hauraki Gulf, southeast of the city of Auckland. It occupies a rift valley or graben between the Coromandel Peninsula and Hunua Ranges, which continues into the Hauraki Plains to the south. Conservation The Firth of Thames is an important site for waders or shorebirds, and is listed as a wetland of international importance under the Ramsar Convention. The Miranda Shorebird Centre, operated by the Miranda Naturalists' Trust, is located on the Seabird Coast, on the western shore of the bay at M ...
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Arawa (canoe)
''Arawa'' was one of the great ocean-going, voyaging canoes in Māori traditions that was used in the migrations that settled New Zealand. The Te Arawa confederation of Māori iwi and hapū based in the Rotorua and Bay of Plenty areas trace their ancestry from the people of this canoe. Background Te Arawa's ancestors on board the ''Arawa'' were of the Ngāti Ohomairangi of Ra'iātea Island. Following a battle that broke out between them and Uenuku, in which their own Whakatūria fell in battle, Tama-te-kapua promised to captain the voyage to the islands of New Zealand, which had been discovered by Ngāhue of the '' Tāwhirirangi'' canoe. Construction of the canoe A large tree was cut down by four men called Rata, Wahieroa, Ngāhue and Parata, to make the waka which came to be known as ''Arawa''. "Hauhau-te-rangi" and "Tuutauru" (made from New Zealand greenstone brought back by Ngāhue) were the adzes used for the time-consuming and intensive work. Upon completion, the w ...
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Ngāti Paoa
Iwi () are the largest social units in New Zealand Māori society. In Māori roughly means "people" or "nation", and is often translated as "tribe", or "a confederation of tribes". The word is both singular and plural in the Māori language, and is typically pluralised as such in English. groups trace their ancestry to the original Polynesian migrants who, according to tradition, arrived from Hawaiki. Some cluster into larger groupings that are based on (genealogical tradition) and known as (literally "canoes", with reference to the original migration voyages). These super-groupings generally serve symbolic rather than practical functions. In pre-European times, most Māori were allied to relatively small groups in the form of ("sub-tribes") and ("family"). Each contains a number of ; among the of the Ngāti Whātua iwi, for example, are Te Uri-o-Hau, Te Roroa, Te Taoū, and Ngāti Whātua-o-Ōrākei. Māori use the word ''rohe'' to describe the territory or boundaries ...
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Māori Language
Māori (), or ('the Māori language'), also known as ('the language'), is an Eastern Polynesian language spoken by the Māori people, the indigenous population of mainland New Zealand. Closely related to Cook Islands Māori, Tuamotuan, and Tahitian, it gained recognition as one of New Zealand's official languages in 1987. The number of speakers of the language has declined sharply since 1945, but a Māori-language revitalisation effort has slowed the decline. The 2018 New Zealand census reported that about 186,000 people, or 4.0% of the New Zealand population, could hold a conversation in Māori about everyday things. , 55% of Māori adults reported some knowledge of the language; of these, 64% use Māori at home and around 50,000 people can speak the language "very well" or "well". The Māori language did not have an indigenous writing system. Missionaries arriving from about 1814, such as Thomas Kendall, learned to speak Māori, and introduced the Latin alphabet. In 1 ...
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Mana
According to Melanesian and Polynesian mythology, ''mana'' is a supernatural force that permeates the universe. Anyone or anything can have ''mana''. They believed it to be a cultivation or possession of energy and power, rather than being a source of power. It is an intentional force. In the 19th century, scholars compared ''mana'' to similar concepts such as the ''orenda'' of the Iroquois Indians and theorized that ''mana'' was a universal phenomenon that explained the origin of religions. ''Mana'' is not universal to all of Melanesia. Etymology The reconstructed Proto-Oceanic word "mana" is thought to have referred to "powerful forces of nature such as thunder and storm winds" rather than supernatural power. That meaning became detached as the Oceanic-speaking peoples spread eastward and the word started to refer to unseen supernatural powers. Polynesian culture ''Mana'' is a foundation of Polynesian theology, a spiritual quality with a supernatural origin and a sacr ...
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