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Puketutu
Puketutu Island, also known as Te Motu a Hiaroa, is a volcanic island in the Manukau Harbour, New Zealand, and is part of the Auckland volcanic field. European settlers called it Weekes' Island, but this was eventually abandoned in favour of the historical Māori name. However this can confuse as there are multiple hills called Puketutu in the North Island of New Zealand. The island is joined to the mainland via a causeway known as Te Ara Tāhuna. Te Motu a Hiaroa means "the island of Hiaroa" in reference to an ancestor who arrived on the island after journeying on the Tainui waka. Puketutu refers to one of the several maunga (mountains) and puke (hills) on the island. The New Zealand Ministry for Culture and Heritage gives a translation of " tutu shrub hill" for . History Approximately 18,000 years ago during the Last Glacial Maximum when sea levels were over 100 metres lower than present day levels, the Manukau Harbour was a river valley. Puketutu was a hilly feature which ros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry Joseph Kelliher
Sir Henry Joseph Kelliher (2 March 1896 – 29 September 1991) was a New Zealand businessman, brewer, publisher, managing director, art patron and credit reformer. Early life Henry Joseph Kelliher (né Keliher) was born in Waikerikeri, near Clyde in Central Otago, New Zealand on 2 March 1896; the son of an Irish immigrant Michael Keliher who came to New Zealand during the Goldrush in Central Otago. Information about his early years is not plentiful but moved to the Wairarapa at the age of 17 to work as a Drover in Carterton prior to the outbreak of World War I. World War I When war broke out in Europe in 1914 Kelliher enlisted with the Otago Mounted Rifles as served as a Trooper until he was transferred during service at Gallipoli in 1915. Kelliher survived the Gallipoli campaign and served in France at the Somme in a specialised Trench Warfare mortar team until he was gassed and invalided to Britain in 1917. Business By the time the war ended in 1918, Kelliher and his n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manukau Harbour
The Manukau Harbour is the second largest natural harbour in New Zealand by area. It is located to the southwest of the Auckland isthmus, and opens out into the Tasman Sea. Geography The harbour mouth is between the northern head ("Burnett Head" / "Ohaka Head") located at the southern end of the Waitākere Ranges and South Head at the end of the Āwhitu Peninsula reaching up from close to the mouth of the Waikato River. The mouth is only 1800 metres wide, but after a nine kilometre channel it opens up into a roughly square basin 20 kilometres in width. The harbour has a water surface area of 394 square kilometres. There is a tidal variation of up to 4 metres, a very substantial change, especially since the harbour, being silted up with almost 10 million years of sedimentation, is rather shallow itself.Manukau Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tainui (canoe)
In Māori tradition, ''Tainui'' was one of the great ocean-going canoes in which Polynesians migrated to New Zealand approximately 800 years ago. In Māori tradition, the ''Tainui'' waka was commanded by the chief Hoturoa, who had decided to leave Hawaiki because over-population had led to famine and warfare. The crew of the ''Tainui'' were the ancestors of the iwi that form the Tainui confederation. Crafting The Tainui waka (canoe) was made from a great tree, at a place in Hawaiki known then as Maungaroa, on the spot where a stillborn child had been buried. According to Te Tāhuna Herangi the waka was named after the child who had been called Tainui. The canoe was made by Rakatāura, an expert boat builder in the tradition of Rātā, or according to Wirihana Aoterangi by Rātā himself. It was built with three adzes (''toki''): ''Hahau-te-pō'' ('Chop the night-world') to chop down the tree, ''Paopao-te-rangi'' ('Shatter the heavens') to split the wood, and ''Manu-tawhi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māngere Mountain
Māngere Mountain is a volcanic cone in Māngere, Auckland. Located within Māngere Domain, it is one of the largest volcanic cones in the Auckland volcanic field, with a peak above sea level. It was the site of a major pā (Māori fortified settlement) and many of the pā's earthworks are still visible. It has extensive panoramic views of Auckland from its location in the southeastern portion of the city's urban area. It is also known as Te Pane-o-Mataaho ("the head of Mataaho"), and Te Ara Pueru ("the Path of Dogskin Cloaks"). The volcano features two large craters. It has a wide crater with a lava dome near its centre, a feature shared by no other volcano in Auckland. It first erupted approximately 70,000 years ago. The mountain is one of the largest and best preserved of Auckland's volcanic cones. Many archaeological features remain, including kumara pits, garden terraces, walled garden mounds and stone boundary walls. Near the mountain to the southwest is Māngere Lagoo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whare
A wharenui (; literally "large house") is a communal house of the Māori people of New Zealand, generally situated as the focal point of a ''marae''. Wharenui are usually called meeting houses in New Zealand English, or simply called ''whare'' (a more generic term simply referring to a house or building). Also called a ''whare rūnanga'' ("meeting house") or ''whare whakairo'' (literally "carved house"), the present style of wharenui originated in the early to middle nineteenth century. The houses are often carved inside and out with stylized images of the iwi's (or tribe's) ancestors, with the style used for the carvings varying from tribe to tribe. Modern meeting houses are built to regular building standards. Photographs of recent ancestors may be used as well as carvings. The houses always have names, sometimes the name of a famous ancestor or sometimes a figure from Māori mythology. Some meeting houses are built at places that are not the location of a tribe, but where man ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robinson Crusoe
''Robinson Crusoe'' () is a novel by Daniel Defoe, first published on 25 April 1719. The first edition credited the work's protagonist Robinson Crusoe as its author, leading many readers to believe he was a real person and the book a travelogue of true incidents. Epistolary, confessional, and didactic in form, the book is presented as an autobiography of the title character (whose birth name is Robinson Kreutznaer) – a castaway who spends 28 years on a remote tropical desert island near the coasts of Venezuela and Trinidad, roughly resembling Tobago, encountering cannibals, captives, and mutineers before being rescued. The story has been thought to be based on the life of Alexander Selkirk, a Scottish castaway who lived for four years on a Pacific island called "Más a Tierra" (now part of Chile) which was renamed Robinson Crusoe Island in 1966. Despite its simple narrative style, ''Robinson Crusoe'' was well received in the literary world and is often credited as ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridget Williams Books
Bridget Williams Books is a New Zealand book publisher, established in 1990 by Bridget Williams. Establishment Williams established the company in 1990 when the company she was working for, Allen & Unwin, was sold. She purchased the titles which she had developed as Allen & Unwin's managing director and started her own publishing company. Williams' vision for the company was for it to publish "good books that sell" – books with significant messages. Her personal interests in women's and Māori history, and New Zealand general history, have influenced the books that the company publishes. From 1995 to 1998, the company published under a joint imprint with Auckland University Press, before returning to independent publisher status in 1998. Development In 2006, the company established the Bridget Williams Publishing Trust, which applies for grants from philanthropic organisations to support publication of specific titles. For example, in 2013 the J.R. McKenzie Trust provided ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waiohua
Te Waiohua or Te Wai-o-Hua is a Māori iwi (tribe) confederation that thrived in the early 18th century. The iwi's rohe (tribal area) was primarily the central Tāmaki Makaurau area (the Auckland isthmus) and the Māngere peninsula, until the 1740s when the paramount chief Kiwi Tāmaki was defeated by the Ngāti Whātua hapū Te Taoū. The descendants of the Waiohua confederation today include Ngāti Te Ata Waiohua, Te Ākitai Waiohua, Ngā Oho of Ngāti Whātua Ōrākei and Waikato Tainui. History Waiohua was a confederation of tribes of the Tāmaki Makaurau region, who were united as a single unit by Huakaiwaka (from which the name of the tribe, ''The Waters of Hua'', can be traced). Huakaiwaka lived and died at Maungawhau / Mount Eden. The three main groups who Huakaiwaka merged were known as Ngā Oho, based in Papakura, Ngā Riki, based in South Auckland with a rohe spanning from Papakura to Ōtāhuhu, and Ngā Iwi, who settled from Ōtāhuhu to the North Shore. The confe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tāmaki Māori
Tāmaki Māori are Māori ''iwi'' and ''hapū'' (tribes and sub-tribes) who have a strong connection to Tāmaki Makaurau (the Auckland Region), and whose rohe was traditionally within the region. Among Ngā Mana Whenua o Tāmaki Makaurau (the Māori tribes of Auckland), also known as the Tāmaki Collective, there are thirteen iwi and hapū, organised into three rōpū (collectives), however Tāmaki Māori can also refer to subtribes and historical iwi not included in this list. Ngāti Whātua Rōpū Ngāti Whātua descend from the '' Māhuhu-ki-te-rangi'' waka, which landed north of the Kaipara Harbour. The rōpū includes Ngāti Whātua o Kaipara, Ngāti Whātua Ōrākei and Te Rūnanga o Ngāti Whātua. Te Rūnanga o Ngāti Whātua is a Māori Trust Board formed in the mid 2000s to represent the interests of Ngāti Whātua iwi and hapū collectively, including those outside of Ngāti Whātua o Kaipara and Ngāti Whātua Ōrākei. The rūnanga represents Ngā Oho, Ngāi Tāh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoria
Scoria is a pyroclastic, highly vesicular, dark-colored volcanic rock that was ejected from a volcano as a molten blob and cooled in the air to form discrete grains or clasts.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. It is typically dark in color (generally dark brown, black or purplish-red), and basaltic or andesitic in composition. Scoria is relatively low in density as a result of its numerous macroscopic ellipsoidal vesicles, but in contrast to pumice, all scoria has a specific gravity greater than 1, and sinks in water. The holes or vesicles form when gases that were dissolved in the magma come out of solution as it erupts, creating bubbles in the molten rock, some of which are frozen in place as the rock cools and solidifies. Scoria may form as part of a lava flow, typically near its surface, or as fragmental ejecta (lapilli, blocks and bombs), for inst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flounder
Flounders are a group of flatfish species. They are demersal fish, found at the bottom of oceans around the world; some species will also enter estuaries. Taxonomy The name "flounder" is used for several only distantly related species, though all are in the suborder Pleuronectoidei (families Achiropsettidae, Bothidae, Pleuronectidae, Paralichthyidae, and Samaridae). Some of the better known species that are important in fisheries are: * Western Atlantic ** Gulf flounder – ''Paralichthys albigutta'' ** Southern flounder – ''Paralichthys lethostigma'' ** Summer flounder (also known as ''fluke'') – ''Paralichthys dentatus'' ** Winter flounder – ''Pseudopleuronectes americanus'' * European waters **European flounder – ''Platichthys flesus'' ** Witch flounder – ''Glyptocephalus cynoglossus'' * North Pacific ** Halibut – ''Hippoglossus stenolepis'' ** Olive flounder – ''Paralichthys olivaceus'' Eye migration Larval flounder are born with one eye on each side o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
