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Ōnawe Peninsula
The Ōnawe Peninsula is a volcanic plug inside Akaroa Harbour, on Banks Peninsula in Canterbury, New Zealand. It is the site of a former pā (a Māori village). It is part of the Banks Peninsula Volcano. The New Zealand Ministry for Culture and Heritage explains that the name ''Ōnawe'' is made up of "Ō" meaning "place of" and "nawe" meaning "to set on fire". It was the site of a Ngāi Tahu pā captured by Te Rauparaha, chief of the Ngāti Toa Ngāti Toa, Ngāti Toarangatira or Ngāti Toa Rangatira, is a Māori '' iwi'' (tribe) based in the southern North Island and in the northern South Island of New Zealand. Its '' rohe'' (tribal area) extends from Whanganui in the north, Palmerston ... in 1831. Up to 1,200 people were killed here, and the land is sacred to Ngāi Tahu so "is deemed to be vested in Te Runanga o Ngāi Tahu" as part of the Ngāi Tahu Waitangi claims settlement in 1998. References Peninsulas of New Zealand Volcanic plugs of New Zealand Rock f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ōnawe Peninsula
The Ōnawe Peninsula is a volcanic plug inside Akaroa Harbour, on Banks Peninsula in Canterbury, New Zealand. It is the site of a former pā (a Māori village). It is part of the Banks Peninsula Volcano. The New Zealand Ministry for Culture and Heritage explains that the name ''Ōnawe'' is made up of "Ō" meaning "place of" and "nawe" meaning "to set on fire". It was the site of a Ngāi Tahu pā captured by Te Rauparaha, chief of the Ngāti Toa Ngāti Toa, Ngāti Toarangatira or Ngāti Toa Rangatira, is a Māori '' iwi'' (tribe) based in the southern North Island and in the northern South Island of New Zealand. Its '' rohe'' (tribal area) extends from Whanganui in the north, Palmerston ... in 1831. Up to 1,200 people were killed here, and the land is sacred to Ngāi Tahu so "is deemed to be vested in Te Runanga o Ngāi Tahu" as part of the Ngāi Tahu Waitangi claims settlement in 1998. References Peninsulas of New Zealand Volcanic plugs of New Zealand Rock f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Plug
A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption. In a plinian eruption the plug is destroyed and ash is ejected. Glacial erosion can lead to exposure of the plug on one side, while a long slope of material remains on the opposite side. Such landforms are called crag and tail. If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive upstanding landform. Examples of volcanic plugs Africa Near the village of Rhumsiki in the Far North Province of Cameroon, Kapsiki Peak is an example of a volcanic plug and is one of the most photographed parts of the Mandara Mountains. Spectacular volcanic plugs are present in the center of La Gomer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akaroa Harbour
Akaroa Harbour, is part of Banks Peninsula in the Canterbury region of New Zealand. The harbour enters from the southern coast of the peninsula, heading in a predominantly northerly direction. It is one of two major inlets in Banks Peninsula, on the coast of Canterbury, New Zealand; the other is Lyttelton Harbour on the northern coast. The name Akaroa is an alternative spelling of Whakaroa, Whangaroa or Wangaloa from the Kāi Tahu dialect of Māori. Whakaroa means "Long Harbour". The harbour was used commercially in the mid-19th century for ship-based and shore-based whaling. Cruise ships occasionally enter the harbour, with the passengers visiting Akaroa. Ōnawe Peninsula is at the head of the harbour, the former site of a Māori pā. Settlements Akaroa Harbour's waterfront has been continually inhabited since the 1840s. Akaroa, Duvauchelle, Takapūneke, Takamatua, Barrys Bay, French Farm and Wainui lie on the shoreline of the harbour. They are connected to the rest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canterbury, New Zealand
Canterbury ( mi, Waitaha) is a region of New Zealand, located in the central-eastern South Island. The region covers an area of , making it the largest region in the country by area. It is home to a population of The region in its current form was established in 1989 during nationwide local government reforms. The Kaikoura District joined the region in 1992 following the abolition of the Nelson-Marlborough Regional Council. Christchurch, the South Island's largest city and the country's second-largest urban area, is the seat of the region and home to percent of the region's population. Other major towns and cities include Timaru, Ashburton, Rangiora and Rolleston. History Natural history The land, water, flora, and fauna of Waitaha/Canterbury has a long history stretching from creation of the greywacke basement rocks that make up the Kā Tiritiri o te Moana/Southern Alps to the arrival of the first humans. This history is linked to the creation of the earth, the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori People
The Māori (, ) are the indigenous Polynesian people of mainland New Zealand (). Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed their own distinctive culture, whose language, mythology, crafts, and performing arts evolved independently from those of other eastern Polynesian cultures. Some early Māori moved to the Chatham Islands, where their descendants became New Zealand's other indigenous Polynesian ethnic group, the Moriori. Initial contact between Māori and Europeans, starting in the 18th century, ranged from beneficial trade to lethal violence; Māori actively adopted many technologies from the newcomers. With the signing of the Treaty of Waitangi in 1840, the two cultures coexisted for a generation. Rising tensions over disputed land sales led to conflict in the 1860s, and massive land confiscations, to which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula Volcano
The Banks Peninsula Volcano is an extinct volcanic complex to the east of Christchurch on New Zealand's South Island.Sewell 1986 While the volcano is highly eroded it still forms the majority of Banks Peninsula with a highest point of . It is a composite of two main eruptive centers one originating at Lyttelton Harbour, the other at Akaroa Harbour. The eruptions were predominantly basaltic, with associated andesite and trachytes, with minor rhyolite. The volcanic activity occurred in the Late Miocene and possibly extended into the Early Pliocene. There are four volcanic groups, all of which are within the Māui Supergroup.Mortimer et al. 2014 The Christchurch earthquakes led to rumors of a possible eruption, however, there is no known magma chamber beneath the volcano and there has not been any sign of volcanic activity in the last 5 million years. Origin and relationship to other volcanoes New Zealand's South Island has many extinct volcanic centers with no obvious tectonic ... [...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] |
Ngāi Tahu
Ngāi Tahu, or Kāi Tahu, is the principal Māori (tribe) of the South Island. Its (tribal area) is the largest in New Zealand, and extends from the White Bluffs / Te Parinui o Whiti (southeast of Blenheim), Mount Mahanga and Kahurangi Point in the north to Stewart Island / Rakiura in the south. The comprises 18 (governance areas) corresponding to traditional settlements. Ngāi Tahu originated in the Gisborne District of the North Island, along with Ngāti Porou and Ngāti Kahungunu, who all intermarried amongst the local Ngāti Ira. Over time, all but Ngāti Porou would migrate away from the district. Several were already occupying the South Island prior to Ngāi Tahu's arrival, with Kāti Māmoe only having arrived about a century earlier from the Hastings District, and already having conquered Waitaha, who themselves were a collection of ancient groups. Other that Ngāi Tahu encountered while migrating through the South Island were Ngāi Tara, Rangitāne, Ngāti T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Rauparaha
Te Rauparaha (c.1768 – 27 November 1849) was a Māori rangatira (chief) and war leader of the Ngāti Toa tribe who took a leading part in the Musket Wars, receiving the nickname "the Napoleon of the South". He was influential in the original sale of land to the New Zealand Company and was a participant in the Wairau Affray in Marlborough. Early days From 1807, muskets became the weapon of choice and partly changed the character of tribal warfare. In 1819 Te Rauparaha joined with a large war party of Ngāpuhi led by Tāmati Wāka Nene; they probably reached Cook Strait before turning back. Migration Over the next few years the intertribal fighting intensified, and by 1822 Ngāti Toa and related tribes were being forced out of their land around Kāwhia after years of fighting with various Waikato tribes often led by Te Wherowhero. Led by Te Rauparaha they began a fighting retreat or migration southwards (this migration was called Te-Heke-Tahu-Tahu-ahi), conquering hapu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ngāti Toa
Ngāti Toa, Ngāti Toarangatira or Ngāti Toa Rangatira, is a Māori ''iwi'' (tribe) based in the southern North Island and in the northern South Island of New Zealand. Its ''rohe'' (tribal area) extends from Whanganui in the north, Palmerston North in the east, and Kaikoura and Hokitika in the south. Ngāti Toa remains a small iwi with a population of only about 4500 ( NZ Census 2001). It has four marae: Takapūwāhia and Hongoeka in Porirua City, and Whakatū and Wairau in the north of the South Island. Ngāti Toa's governing body has the name ''Te Rūnanga o Toa Rangatira''. The iwi traces its descent from the eponymous ancestor Toarangatira. Prior to the 1820s, Ngāti Toa lived on the coastal west Waikato region until forced out by conflict with other Tainui iwi headed by Pōtatau Te Wherowhero ( 1785 - 1860), who later became the first Māori King (). Ngāti Toa, Ngāti Rārua and Ngāti Koata, led by Te Rauparaha ( 1765-1849), escaped south and invaded Taranaki and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Treaty Of Waitangi Claims And Settlements
Claims and settlements under the Treaty of Waitangi have been a significant feature of New Zealand politics since the Treaty of Waitangi Act 1975 and the Waitangi Tribunal that was established by that act to hear claims. Successive governments have increasingly provided formal legal and political opportunity for Māori to seek redress for what are seen as breaches by the Crown of guarantees set out in the Treaty of Waitangi. While it has resulted in putting to rest a number of significant longstanding grievances, the process has been subject to criticisms including those who believe that the redress is insufficient to compensate for Māori losses. The settlements are typically seen as part of a broader Māori Renaissance. The Waitangi Tribunal was set up as the primary means of registering and researching claims because the Treaty of Waitangi itself has little legal standing. The primary means of settling those claims is through direct negotiations with the government of the day. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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