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Waitematā Harbour
The Waitematā Harbour is the main access by sea to Auckland, New Zealand. The harbour forms the northern and eastern coasts of the Auckland isthmus and is crossed by the Auckland Harbour Bridge. It is matched on the southern side of the city by the shallower waters of the Manukau Harbour. With an area of , it connects Ports of Auckland, the city's main port and the Auckland waterfront to the Hauraki Gulf and the Pacific Ocean. It is sheltered from Pacific storms by Auckland's North Shore, New Zealand, North Shore, Rangitoto Island, and Waiheke Island. Etymology The oldest Māori language, Māori name of the harbour was Te Whanga-nui o Toi (The Big Bay of Toi), named after Toi-te-huatahi, Toi, an early Māori explorer. The name ''Waitematā'' means "Te Mata Waters", which according to some traditions refers to a mauri stone (a stone of Religion of Māori people, Māori religious significance) called Te Mata, which was placed on Boat Rock (in the harbour south-west of Chatsw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Harbour Bridge
The Auckland Harbour Bridge is an eight-lane motorway bridge over Waitematā Harbour in Auckland, New Zealand. It joins Saint Marys Bay, New Zealand, St Marys Bay on the Auckland city side with Northcote, Auckland, Northcote on the North Shore, New Zealand, North Shore side. It is part of State Highway 1 (New Zealand), State Highway 1 and the Auckland Northern Motorway. The bridge is operated by the NZ Transport Agency Waka Kotahi (NZTA). It is the second-longest road bridge in New Zealand, and the longest in the North Island. The original inner four lanes, opened in 1959, are of truss, box truss construction. Two lanes were added to each side in 1968–1969 and are of orthotropic deck, orthotropic box structure construction extend as cantilevers from the original pier (architecture), piers. The bridge is 1,020 m (3,348 ft) long, with a main span of 243.8 metres (800 feet) rising 43.27 metres (142 feet) above high water, allowing ships access to the deepwater wharf at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whau River
The Whau River () is an estuarial arm of the southwestern Waitemata Harbour (rather than a river) within the Auckland metropolitan area in New Zealand. It flows north for from its origin at the confluence of the Avondale Stream and Whau Stream to its mouth between the Te Atatū Peninsula and the long, thin Rosebank Peninsula in Avondale. It is at its widest and wide at its mouth. The estuary extends past the suburbs of Glendene and Kelston. It has one small estuarial tributary arm, the Wairau Creek in the southwest. The tide flows up the Wairau Creek as far as Sabulite Road in Kelston, and up the Rewarewa Creek to Clark Street and Wolverton Road in New Lynn. The area at the mouth of the estuary is legally protected as the Motu Manawa (Pollen Island) Marine Reserve. The Whau River is named after a native tree, the whau (''Entelea arborescens''). Geography The geology of the area is mainly composed of marine and riverine sediment. The stream's intertidal banks are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chatswood, New Zealand
Chatswood is a suburb in the city of Auckland, New Zealand, in the middle-eastern side of the North Shore. It contains a primary school and many parks. To the south of Chatswood is Kendall's Bay, a small bay of the Waitematā Harbour. The suburb is under the governance of Auckland Council. The Royal New Zealand Navy's Kauri Point Armament Depot is located in Chatswood. Chelsea Sugar Refinery is located in Chatswood. Etymology The name Chatswood was decided by property developers in 1973. In the latter 19th century, the sparsely populated area near Kauri Point was often referred to as Balmain. Geography The Chatswood area is primarily uplifted Waitemata Group sandstone, that was deposited on the sea floor during the Early Miocene, between 22 and 16 million years ago. Prior to human settlement, the inland North Shore was a mixed podocarp-broadleaf forest dominated by kauri and other conifer trees. Pōhutukawa trees dominated the coastal margins of Birkenhead. Some kauri r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Religion Of Māori People
The Māori people, Māori people have a Polynesian mythology, Polynesian religion that, prior to the introduction of Christianity in New Zealand, Christianity to New Zealand was the main religious belief for Māori. By 1845, more than half of the Māori population attended church and Christianity remains the largest religion for Māori. Very few Māori still follow traditional Māori religion, although many elements of it are still observed. Several Māori religious movements have been born out of Christianity, such as the Ratana movement. Traditional Māori religion Traditional Māori religion, that is, the pre-European belief-system of the Māori people , Māori, differed little from that of their perceived homeland, Hawaiki, Hawaiki Nui, aka Raʻiātea or Raiatea, conceiving of everything – including natural elements and all living things – as connected by common descent through whakapapa or genealogy. Accordingly, Māori regarded all things as possessing a life force ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toi-te-huatahi
Toi-te-huatahi, also known as Toi and Toi-kai-rākau, is a legendary Māori people, Māori ''tupuna'' (ancestor) of many Māori people, Māori iwi (tribes) from the Bay of Plenty area, including Ngāti Awa, Ngāi Te Rangi and Ngāi Tūhoe. The Bay of Plenty's name in te reo Māori, Te Moana-a-Toi, references Toi-te-huatahi. Names His name Toi-te-huatahi is a reference to Toi being an only child. Toi-kai-rākau ("Toi the Wood Eater"), was a name given to him by later settlers in the region who introduced agriculture, and is a reference to how Toi would eat the foods of the forest. Traditions Toi-te-huatahi's legendary ancestor in Māori mythology was the tīwakawaka (New Zealand fantail). Based on the traditional genealogies of Ngāti Awa, Ngāi Te Rangi and Ngāi Tūhoe, Toi-te-huatahi is estimated to have lived between the 13th and 14th centuries. According to different traditions, Toi was either born in Hawaiki and came to Aotearoa by Māori migration canoes, a migratory ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Language
Māori (; endonym: 'the Māori language', commonly shortened to ) is an Eastern Polynesian languages, Eastern Polynesian language and the language of the Māori people, the indigenous population of mainland New Zealand. The southernmost member of the Austronesian language family, it is related to Cook Islands Māori, Tuamotuan language, Tuamotuan, and Tahitian language, Tahitian. The Māori Language Act 1987 gave the language recognition as one of New Zealand's official languages. There are regional dialects of the Māori language. Prior to contact with Europeans, Māori lacked a written language or script. Written Māori now uses the Latin script, which was adopted and the spelling standardised by Northern Māori in collaboration with English Protestant clergy in the 19th century. In the second half of the 19th century, European children in rural areas spoke Māori with Māori children. It was common for prominent parents of these children, such as government officials, to us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Skyline From Harbour
Auckland ( ; ) is a large metropolitan city in the North Island of New Zealand. It has an urban population of about It is located in the greater Auckland Region, the area governed by Auckland Council, which includes outlying rural areas and the islands of the Hauraki Gulf, and which has a total population of as of It is the List of cities in New Zealand, most populous city of New Zealand and the fifth-largest city in Oceania. The city lies between the Hauraki Gulf to the east, the Hunua Ranges to the south-east, the Manukau Harbour to the south-west, and the Waitākere Ranges and smaller ranges to the west and north-west. The surrounding hills are covered in rainforest and the landscape is dotted with 53 volcanic centres that make up the Auckland Volcanic Field. The central part of the urban area occupies a narrow isthmus between the Manukau Harbour on the Tasman Sea and the Waitematā Harbour on the Pacific Ocean. Auckland is one of the few cities in the world to have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waiheke Island
Waiheke Island is the second-largest island (after Great Barrier Island) in the Hauraki Gulf of New Zealand. Its ferry terminal in Matiatia Bay at the western end is from the central-city terminal in Auckland. It is the most populated island in the gulf, with permanent residents, and the List of islands of New Zealand, third most populous island in New Zealand (behind the two main islands). An additional estimated 3,400 people have second homes or holiday homes on the island. It is more densely populated than the North Island, North and South Islands. It is the most accessible island in the gulf, with regular passenger and Roll-on/roll-off, car-ferry services, a helicopter operator based on the island, and other air links. In November 2015, Lonely Planet rated Waiheke Island the fifth-best region in the world to visit in 2016. Geography Overview The island is off the coast of the North Island. It is in length from west to east, varies in width from , and has a surface are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rangitoto Island
Rangitoto Island is a volcanic island in the Hauraki Gulf near Auckland, New Zealand. The wide island is a symmetrical shield volcano cone capped by central scoria cones, reaching a height of . Rangitoto is the youngest and largest of the approximately 50 volcanoes of the Auckland volcanic field, having erupted in two phases about 1450 CE and 1500 CE and covering an area of . It is separated from the mainland of Auckland's North Shore, New Zealand, North Shore by the Rangitoto Channel. Since World War II, it has been linked by a causeway to the much older, non-volcanic Motutapu Island. is Māori language, Māori for 'Bloody Sky',What happened to local Maori? (from the Rangitoto page on the GNS Science website) with the name coming from the full phrase ("The days of the bleeding of Tama-te-kapua"). Tama ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Shore, New Zealand
The North Shore ( or ) is one of the major geographical regions of Auckland, the largest city in New Zealand. The area is defined as the northern shores of the Waitematā Harbour as far north as the Ōkura River. The North Shore is primarily uplifted Waitemata Group sandstone from the Miocene, and includes the northernmost features of the Auckland volcanic field, such as Lake Pupuke, the oldest known feature of the field. Settled by Tāmaki Māori in the 13th or 14th centuries, the Waitematā Harbour headlands became important places for harvesting seasonal resources and for controlling transportation across the region. European settlers arrived in the North Shore in the 1840s, and by the turn of the 20th century, the inland area has become a hub for fruit growing, while the eastern coast had developed into a tourism destination for Aucklanders. The North Shore rapidly suburbanised after the construction of the Auckland Harbour Bridge in 1959, and by 1989 the five local ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Coromandel Peninsula, and |
Auckland Waterfront
The Auckland waterfront (rarely the Auckland harbourfront) is a city-side stretch of the southern Waitematā Harbour coastline in Auckland, New Zealand. Previously mostly dominated by Ports of Auckland uses, from the 2000s on it is becoming increasingly open to recreational public use, with a number of former wharves being converted to office, entertainment, and later also some residential uses. Extents The waterfront stretches roughly from the suburb of Saint Marys Bay, New Zealand, Saint Marys Bay / the Auckland Harbour Bridge in the west to the Ports of Auckland areas in the east. However, in most usage, 'Auckland waterfront' only refers to those parts freely accessible to the public (such as around the Viaduct Basin and the Auckland CBD), and thus at the moment excludes much of the Western Reclamation and almost the whole of the Ports of Auckland area to the east. While Auckland City technically has a second waterfront on the Manukau Harbour, this is never called 'Aucklan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
