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Ōtūtereinga
Ōtūtereinga is a cliff at the northern end of Wainui, on the western side of Akaroa Harbour. Its name is also spelt Otutereinga and O Tu Te Reinga. "Ō" means "place of", "tu" translates to "stand", "te" signifies "the", and "reinga" refers to the "flitting place from which spirits transition to the underworld", similar to Cape Reinga. Since the mid-nineteenth century, the only things that have fallen off this cliff are household waste, as the local council established the Wainui Dump in the area. The landfill has since been closed. At this location, powerful waves crash against the rocky shore, a phenomenon that was traditionally viewed by the Māori as a warning sign of an impending storm. Tāngatahara Tangatahara ( – 13 December 1847) was a Ngāti Irakehu (Banks Peninsula) and Ngāi Tūāhuriri warrior who led the unsuccessful defence of the Ōnawe Peninsula, Ōnawe Pā invasion in 1832, but later restored his prestige by joining war parti ..., the chief defender of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tāngatahara
Tangatahara ( – 13 December 1847) was a Ngāti Irakehu (Banks Peninsula) and Ngāi Tūāhuriri warrior who led the unsuccessful defence of the Ōnawe Peninsula, Ōnawe Pā invasion in 1832, but later restored his prestige by joining war parties to drive Te Rauparaha and his forces from South Island, Te Wai Pounamu. Early life Tangatahara (pronounced Takata Hara in Southern Māori dialect, also spelt Tangata Hara) lived at Kaiapoi Pā and on the western side of Akaroa Harbour, on Banks Peninsula. 'Tangata' means 'man' and 'hara' can mean 'offence' or 'foul'; in other words, his name denotes a criminal or ugly man. Ngāi Tahu, originally a lower North Island tribe, had moved History of Canterbury Region#Classical Māori period, steadily south into Ngāti Mamoe territory, settling where people were already settled, conquering and intermingling, until the Ngāti Mamoe lost their identity as a separate people. In the early 19th century, the Kaiapoi and Banks Peninsula hapū were ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff or rock face is an area of Rock (geology), rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and Dolomite (rock), dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may ... [...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 centres 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 centres with no obvious tectonic ... [...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. Ōnuku, Akaroa, Takapūneke, Takamatua, Robinsons Bay, Duvauchelle, Barrys Bay, French Farm, Tikao Bay and Wainui lie on the shoreline of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Reinga
Cape Reinga / Te Rerenga Wairua (; sometimes spelled Rēinga, ) is the northwestern most tip of the Aupōuri Peninsula, at the northern end of the North Island of New Zealand. Cape Reinga is more than 100 km north of the nearest small town of Kaitaia. In Māori, means the ''leaping-off place of spirits''. is the Māori word for ''underworld''. Both refer to the Māori belief that the cape is the point where the spirits of the dead enter the underworld. Cape Reinga is a popular tourist site, with annual visitor numbers estimated at over 500,000 people. Visitor numbers are growing by about five percent a year, and the increase is likely to become even more now that the road to the cape is fully sealed. Geography Cape Reinga is generally considered the separation marker between the Tasman Sea to the west and the Pacific Ocean to the east. From the lighthouse it is possible to watch the tidal race, as the two seas clash to create unsettled waters just off the coast. Māor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christchurch City Libraries
Christchurch City Libraries is a network of 21 libraries and a mobile book bus. operated by the Christchurch City Council and Following the 2011 Christchurch earthquake the previous Christchurch Central Library building was demolished, and was replaced by a new central library building in Cathedral Square, '' Tūranga'', which opened in 2018. A number of community libraries were also rebuilt post earthquake. Early history The library began as the Mechanics' Institute in 1859, when 100 subscribers leased temporary premises in the then Town Hall. The collection consisted of a few hundred books. By 1863, with the help of a grant from the Provincial Government, the Mechanics' Institute opened a building on a half-acre of freehold land on the corner of Cambridge Terrace and Hereford Street, purchased the year before at a cost of £262.10.0. This site was to remain the home of the library until 1982. Debt, dwindling subscribers and other problems forced the institute to hand o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Star (Christchurch)
''The Star'' is a newspaper published in Christchurch, New Zealand. It was published daily from 1868 to 1991. It became the ''Christchurch Star-Sun'' in June 1935 after merging with a rival newspaper, ''The Sun'', and at the time it ceased daily publication in 1991 it was known as ''The Christchurch Star''. It later became a free newspaper, published twice a week (on Wednesdays and Fridays) until 2016, then once a week (on Thursdays) since 2016. History The ''Star'' was first published on 14 May 1868 as the evening edition of the '' Lyttelton Times''. By 1914, the newspaper faced competition from two other Christchurch-based evening newspapers, ''The Sun'' and ''Evening Times''. The rival ''Evening Times'' subsequently folded in 1917. During the Great Depression, rationalisation and competition led ''The Star'' to lower its price from 2 d to 1d in November 1934, prompting other Christchurch dailies to follow suit. This price proved financially unsustainable and ''The Star'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori People
Māori () are the Indigenous peoples of Oceania, indigenous Polynesians, Polynesian people of mainland New Zealand. Māori originated with settlers from East Polynesia, who arrived in New Zealand in several waves of Māori migration canoes, canoe voyages between roughly 1320 and 1350. Over several centuries in isolation, these settlers developed Māori culture, a distinct 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. Early 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, Treaty of Waitangi/Te Tiriti o Waitangi in 1840, the two cultures coexisted for a generation. Rising ten ... [...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 fortified Māori village). It is part of the Banks Peninsula Volcano. The New Zealand Ministry for Culture and Heritage The Ministry for Culture and Heritage (MCH; ) is the department of the New Zealand Government responsible for supporting the Creative New Zealand, arts, Culture of New Zealand, culture, New Zealand Historic Places Trust, built heritage, Sport Ne ... 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 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. The peninsula is only accessible at low tide; at high tide, the penin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Canterbury Region
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
