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Völkner Rocks
Te Paepae o Aotea, also known the Volkner Rocks (named after Carl Sylvius Völkner), are a group of andesitic rock stacks and pinnacles located northwest of Whakaari/White Island in New Zealand's Bay of Plenty. They reach 113 metres above sea level from 400 metres below the sea floor, while the saddle separating them from Whakaari/White Island is over 200 metres deep. Te Paepae o Aotea Marine Reserve was established around them in 2006. The area is popular with divers due to good visibility (35–40 m), spectacular scenery and colourful marine life. The rocks and marine reserve are acccesible by boat. There are several boat ramps, boating facilities and charter boat services in Eastern Bay of Plenty. History According to oral history, Te Paepae o Aotea was used as a landmark to show land was close. The rocks became culturally significant to Ngāti Awa and other iwi descending from the Mātaatua waka, as the departure place for the spirits of all their people. Sp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whakaari/White Island
Whakaari / White Island (, mi, Te Puia Whakaari, lit. "the dramatic volcano"), also known as White Island or Whakaari, is an active andesite stratovolcano situated from the east coast of the North Island of New Zealand, in the Bay of Plenty. The island covers an area of approximately , which is just the peak of a much larger submarine volcano. The island is New Zealand's most active cone volcano, and has been built up by continuous volcanic activity over the past 150,000 years. The nearest mainland towns are Whakatane and Tauranga. The island has been in a nearly continuous stage of releasing volcanic gas at least since it was sighted by James Cook in 1769. Whakaari erupted continually from December 1975 until September 2000, and also erupted in 2012, 2016, and 2019. Sulphur was mined on the island until the 1930s. Ten miners were killed in 1914 when part of the crater wall collapsed. The main activities on the island now include guided tours and scientific research. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Awa
Ngāti Awa is a Māori iwi (tribe) centred in the eastern Bay of Plenty Region of New Zealand. It is made of 22 hapū (subtribes), with 15,258 people claiming affiliation to the iwi in 2006. The Ngāti Awa people are primarily located in towns on the Rangitaiki Plain, including Whakatāne, Kawerau, Edgecumbe, Te Teko and Matatā. Two urban hapū also exist in Auckland (''Ngāti Awa-ki-Tamaki'') and Wellington (''Ngāti Awa-ki-Poneke''). History Early history Ngāti Awa traces its origins to the arrival of Māori settlers on the ''Mātaatua'' waka (canoe). The ''Mātaatua'' settlers established settlements in the Bay of Plenty and Northland. Initially, the tribe controlled a large area in Northland, but conflicts with other northern iwi resulted in a southward migration. One group eventually settled in the eastern Bay of Plenty, whose descendants would eventually found the iwi. Awanuiarangi II is recognised as the eponymous ancestor of Ngāti Awa. Awanuiarangi II was a chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taupō Volcanic Zone
The Taupō Volcanic Zone (TVZ) is a volcanic area in the North Island of New Zealand that has been active for the past two million years and is still highly active. Mount Ruapehu marks its south-western end and the zone runs north-eastward through the Taupō and Rotorua areas and offshore into the Bay of Plenty. It is part of the larger Central Volcanic Region that extends further westward through the western Bay of Plenty to the eastern side of the Coromandel Peninsula and has been active for four million years. At Taupō the rift volcanic zone is widening east–west at the rate of about 8 mm per year while at Mount Ruapehu it is only 2–4 mm per year but this increases at the north eastern end at the Bay of Plenty coast to 10–15 mm per year. It is named after Lake Taupō, the flooded caldera of the largest volcano in the zone, the Taupō Volcano and contains a large central volcanic plateau as well as other landforms associated with its containing tectonic i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Islands Of The Bay Of Plenty Region
An island (or isle) is an isolated piece of habitat that is surrounded by a dramatically different habitat, such as water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental and oceanic. There are also artificial islands, which are man-made. Etymology The word ''island'' derives from Middle English ''iland'', from Old English ''igland'' (from ''ig'' or ''ieg'', similarly meaning 'island' when used independently, and -land carrying its contemporary meaning; cf. Dutch ''eiland'' ("island"), German ''Eiland'' ("small island")). However, the spelling of the word ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of The Bay Of Plenty Region
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Desert Island
A desert island, deserted island, or uninhabited island, is an island, islet or atoll that is not permanently populated by humans. Uninhabited islands are often depicted in films or stories about shipwrecked people, and are also used as stereotypes for the idea of "paradise". Some uninhabited islands are protected as nature reserves, and some are privately owned. Devon Island in Canada's far north is the largest uninhabited island in the world. Small coral atolls or islands usually have no source of fresh water, but occasionally a freshwater lens can be reached with a well. Terminology Uninhabited islands are sometimes also called "deserted islands" or "desert islands". In the latter, the adjective '' desert'' connotes not desert climate conditions, but rather "desolate and sparsely occupied or unoccupied". The word ''desert'' has been "formerly applied more widely to any wild, uninhabited region, including forest-land", and it is this archaic meaning that appears in the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Islands Of New Zealand
New Zealand consists of more than six hundred islands, mainly remnants of a larger land mass now beneath the sea. New Zealand is the seventh-largest island nation on earth, and the third-largest located entirely in the Southern Hemisphere. The following is a list of islands of New Zealand. The two largest islands – where most of the human population lives – have names in both English and in the Māori language. They are the North Island or ''Te Ika-a-Māui'' and the South Island or ''Te Waipounamu''. Various Māori iwi sometimes use other names, with some preferring to call the South Island ''Te Waka o Aoraki''. The two islands are separated by Cook Strait. In general practice, the term ''mainland'' refers to the North Island and South Island. However, the South Island alone is sometimes called "the mainland" – especially by its residents, as a nickname – because it is the larger of the two main islands. To the south of the South Island, Stewart Island / Rakiura is t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marine Reserves Of New Zealand
New Zealand has 44 marine reserves (as of August 2020) spread around the North, the South Island, and neighbouring islands, and on outlying island groups. They are governed by the Marine Reserves Act 1971 and administered by the Department of Conservation with assistance from the Ministry of Fisheries, New Zealand Customs and the New Zealand Defence Forces. History The Marine Reserves Act was passed by the Parliament of New Zealand in 1971. In 2000 the Department of Conservation started a review of the Act resulting in a draft Marine Reserves Bill that was introduced into Parliament in June 2002, but has not yet been voted on. The first marine reserve to be created was the Cape Rodney-Okakari Point Marine Reserve. The Poor Knights Islands Marine Reserve was established next, although with only a partial ban on fishing; a full ban was implemented in 1998. The first two marine reserves in Fiordland were established at the request of New Zealand Federation of Commercial Fishe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mātaatua
''Mātaatua'' was one of the great voyaging canoes by which Polynesians migrated to New Zealand, according to Māori tradition. Māori traditions say that the ''Mātaatua'' was initially sent from Hawaiki to bring supplies of kūmara to Māori settlements in New Zealand. The ''Mātaatua'' was captained by Toroa, accompanied by his brother, Puhi; his sister, Muriwai; his son, Ruaihona; and daughter, Wairaka. Mātaatua Māori include the tribes of Ngāi Tūhoe, Ngāti Awa, Te Whakatōhea, Te Whānau-ā-Apanui, Ngāpuhi, Ngāi Te Rangi, Ngāti Pūkenga. History The ''Mātaatua'' waka likely arrived in Aotearoa more than a century after the ''Tainui'' and '' Arawa'' waka. Bay of Plenty settlement In local Māori tradition, the ''Mātaatua'' waka was the first to land at Whakatāne, approximately 700 years ago. According to various accounts, at some point, a dispute arose between the commander, Toroa, and Puhi, eponymous ancestor of Ngāpuhi, over kūmara planting rituals. As a r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ministry For Culture And Heritage
The Ministry for Culture and Heritage (MCH; ) is the department of the New Zealand Government responsible for supporting the arts, culture, built heritage, sport and recreation, and broadcasting sectors in New Zealand and advising government on such. History The Ministry of Cultural Affairs had been created in 1991; prior to this, the Department of Internal Affairs (DIA) had provided oversight and support for arts and culture functions. MCH was founded in 1999 with the merger of the former Ministry of Cultural Affairs and the history and heritage functions of the DIA, as well as some functions from the Department of Conservation and Ministry of Commerce. The purpose of the merger of functions and departments was to create a coherent, non-fragmented overview of the cultural and heritage sector, rather than spreading services and functions across several departments. Minister for Cultural Affairs Marie Hasler oversaw the transition of functions into the new agency. Opposition La ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Ara - The Encyclopedia Of New Zealand
''Te Ara: The Encyclopedia of New Zealand'' is an online encyclopedia established in 2001 by the New Zealand Government's Ministry for Culture and Heritage. The web-based content was developed in stages over the next several years; the first sections were published in 2005, and the last in 2014 marking its completion. ''Te Ara'' means "the pathway" in the Māori language, and contains over three million words in articles from over 450 authors. Over 30,000 images and video clips are included from thousands of contributors. History New Zealand's first recognisable encyclopedia was ''The Cyclopedia of New Zealand'', a commercial venture compiled and published between 1897 and 1908 in which businesses or people usually paid to be covered. In 1966 the New Zealand Government published ''An Encyclopaedia of New Zealand'', its first official encyclopedia, in three volumes. Although now superseded by ''Te Ara'', its historical importance led to its inclusion as a separate digital reso ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
