Redcliffs
Redcliffs is an outer coastal suburb of Christchurch, Canterbury, New Zealand. History The area of Redcliffs was first populated by humans about 700 years ago. In the 14th century, large groups of Māori, initially the Waitaha people and then the Ngāti Māmoe tribe, settled in the area. The Ngāi Tahu eventually displaced Ngāti Māmoe and were still living in the area when the first Europeans arrived. During 19th excavations of Moa Bone Point Cave in Redcliffs numerous artefacts were found. These included moa bones and egg shells, bones of seals, birds and fish, shellfish and many Māori taonga. This suggests that Moa Bone Point Cave was used as shelter by the first Māori people but also used as a place to store valuable items. Location The suburb is most directly accessed from the city centre by a causeway that crosses the Avon Heathcote Estuary and is the suburb immediately before Sumner. Alternatively, Redcliffs can be accessed through McCormack's Bay Road, whic ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Redcliffs Landslide1
Redcliffs is an outer coastal suburb of Christchurch, Canterbury, New Zealand, Canterbury, New Zealand. History The area of Redcliffs was first populated by humans about 700 years ago. In the 14th century, large groups of Māori people, Māori, initially the Waitaha (South Island iwi), Waitaha people and then the Kāti Māmoe, Ngāti Māmoe tribe, settled in the area. The Ngāi Tahu eventually displaced Ngāti Māmoe and were still living in the area when the first Europeans arrived. During 19th excavations of Moa Bone Point Cave in Redcliffs numerous artefacts were found. These included moa bones and egg shells, bones of seals, birds and fish, shellfish and many Māori taonga. This suggests that Moa Bone Point Cave was used as shelter by the first Māori people but also used as a place to store valuable items. Location The suburb is most directly accessed from the city centre by a causeway that crosses the Avon Heathcote Estuary and is the suburb immediately before Sumner ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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2011 Christchurch Earthquake
A major earthquake occurred in Christchurch on Tuesday 22 February 2011 at 12:51 p.m. local time (23:51 UTC, 21 February). The () earthquake struck the entire of the Canterbury region in the South Island, centred south-east of the central business district. It caused widespread damage across Christchurch, killing 185 people, in New Zealand's fifth-deadliest disaster. Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the magnitude 7.1 Canterbury earthquake of 4 September 2010 and its aftershocks. Significant liquefaction affected the eastern suburbs, producing around 400,000 tonnes of silt. The earthquake was felt across the South Island and parts of the lower and central North Island. While the initial quake only lasted for approximately 10 seconds, the damage was severe because of the location and shallowness of the earthquake's focus in relation to Christchurch as well as ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sumner, New Zealand
Sumner is a coastal seaside suburb of Christchurch, New Zealand and was surveyed and named in 1849 in honour of John Bird Sumner, the then newly appointed Archbishop of Canterbury and president of the Canterbury Association. Originally a separate borough, it was amalgamated with the city of Christchurch as communications improved and the economies of scale made small town boroughs uneconomic to operate. Toponymy Captain Thomas named the settlement for Bishop John Bird Sumner, one of the leading members of the Canterbury Association. The Ngāi Tahu name for the beach between Cave Rock (''Tuawera'') and Scarborough is ''Matuku Tako Tako''. This name has been used by both the state primary school and the city libraries. A. W. Reed gives the Māori name for is ''Ohikaparuparu'' ("o" means place of; "hika" means rubbing, kindling, or planting; "paruparu" means dirt, deeply laden, or a preparation of fermented cockles). However, J. F Menzies indicates this name is associated with a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Christchurch
Christchurch ( ; mi, Ōtautahi) is the largest city in the South Island of New Zealand and the seat of the Canterbury Region. Christchurch lies on the South Island's east coast, just north of Banks Peninsula on Pegasus Bay. The Avon River / Ōtākaro flows through the centre of the city, with an urban park along its banks. The city's territorial authority population is people, and includes a number of smaller urban areas as well as rural areas. The population of the urban area is people. Christchurch is the second-largest city by urban area population in New Zealand, after Auckland. It is the major urban area of an emerging sub-region known informally as Greater Christchurch. Notable smaller urban areas within this sub-region include Rangiora and Kaiapoi in Waimakariri District, north of the Waimakariri River, and Rolleston and Lincoln in Selwyn District to the south. The first inhabitants migrated to the area sometime between 1000 and 1250 AD. They hunted moa, which ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Moncks Bay
Moncks Bay is a south-eastern suburb of Christchurch, New Zealand. The first European owner of in Moncks Bay was George Heath, who arrived in Lyttelton in March 1851 on the ''Isabella Hercus''. He also had of land on the hills behind. Heath sold the land to William McCormack in 1860; McCormacks Bay in the adjacent suburb Mount Pleasant is named for his brother. Moncks Bay changed owner again in 1868, and was purchased in 1869 by John Stanley Monck, after whom the area was named. Monck increased his land holdings up the hill by purchasing adjacent property from Dr Alfred Charles Barker () and in 1882, he acquired land from the estate of Alfred Watson that brought his holdings in Redcliffs to a total of about . Demographics Moncks Bay is part of the Clifton Hill SA2 statistical area. Moncks Bay, comprising the SA1 statistical areas of 7026568–570, covers . It had a population of 486 at the 2018 New Zealand census Eighteen or 18 may refer to: * 18 (number), the natural ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mount Pleasant, New Zealand
Mount Pleasant (Tauhinukorokio) is a coastal suburb of Christchurch, New Zealand. The suburb is located on the northern flank of the mountain Tauhinukorokio/Mount Pleasant in the Port Hills. It takes its name from the English version of the mountain's name. The area was originally administered by the borough of Sumner. A petition in September 1920, by 57 of the suburb's 66 ratepayers, asked for it to be included as a riding of the Heathcote County. At the time of the petition, the area was mostly farmland, with 21 dwelling houses and an estimated population of 80. Whilst the mayor of Sumner, John Barr, submitted against the petition, it was granted and took effect on 1 April 1921. As a result of the 1989 local government reforms, Heathcote County was amalgamated with and became part of Christchurch City Council. The suburb and its houses were extensively damaged in the 2011 Christchurch earthquake. Demographics Mount Pleasant covers . It had an estimated population of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Port Hills
The Port Hills are a range of hills in Canterbury Region, so named because they lie between the city of Christchurch and its port at Lyttelton. They are an eroded remnant of the Lyttelton volcano, which erupted millions of years ago. The hills start at Godley Head, run approximately east–west along the northern side of Lyttelton Harbour, and continue running to the south, dividing the city from the harbour. The range terminates near Gebbies Pass above the head of the harbour. The range includes a number of summits between 300 and 500 metres above sea level. The range is of significant geological, environmental and scenic importance. History The volcano is one of two from which Banks Peninsula was originally formed 12 million years ago. The area was first populated by Māori during the 14th century. During early European settlement some 500 years later the Port Hills presented a challenging barrier between the harbour and the planned settlement of Christchurch, their stee ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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2010 Canterbury Earthquake
The 2010 Canterbury earthquake (also known as the Darfield earthquake) struck the South Island of New Zealand with a moment magnitude of 7.1 at on , and had a maximum perceived intensity of X (''Extreme'') on the Mercalli intensity scale. Some damaging aftershocks followed the main event, the strongest of which was a magnitude 6.3 shock known as the Christchurch earthquake that occurred nearly six months later on 22 February 2011. Because this aftershock was centred very close to Christchurch, it was much more destructive and resulted in the deaths of 185 people. The earthquake on 4 September caused widespread damage and several power outages, particularly in the city of Christchurch, New Zealand's second largest city at that time. Two residents were seriously injured, one by a collapsing chimney and a second by flying glass. One person died of a heart attack suffered during the quake. Another person died after a fall during the quake. Mass fatalities were avoided partly due ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Avon Heathcote Estuary
The Estuary of the Heathcote and Avon Rivers / Ihutai is the largest semi-enclosed shallow estuary in Canterbury and remains one of New Zealand’s most important coastal wetlands. It is well known as an internationally important habitat for migratory birds, and it is an important recreational playground and educational resource. It was once highly valued for ''mahinga kai'' ( Māori for food gathering). Location The Avon River / Ōtākaro enters the estuary from the northwest, and the Ōpāwaho / Heathcote River from the south-west. The estuary has a triangular shape, a short inlet connection with Pegasus Bay, and is primarily enclosed by the long Brighton Spit, on which the suburbs New Brighton, South New Brighton and Southshore are located. The most prominent features of the inlet are the single deep channel between Rapanui Rock ("Shag Rock") and Brighton Spit. Description It is shallow with the mean at high water of ordinary spring tides (HWOST) of —and is pred ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Earthquake Damage To Stately Home In Redclifts - Panoramio
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes c ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Baby Boomer
Baby boomers, often shortened to boomers, are the Western demographic cohort following the Silent Generation and preceding Generation X. The generation is often defined as people born from 1946 to 1964, during the mid-20th century baby boom. The dates, the demographic context, and the cultural identifiers may vary by country. The baby boom has been described variously as a "shockwave" and as "the pig in the python". Most baby boomers are children of either the Greatest Generation or the Silent Generation, and are often parents of late Gen Xers and Millennials. Late baby boomers can also be the parents of older members of Generation Z. In the West, boomers' childhoods in the 1950s and 1960s had significant reforms in education, both as part of the ideological confrontation that was the Cold War, and as a continuation of the interwar period. In the 1960s and 1970s, as this relatively large number of young people entered their teens and young adulthood—the oldest turned 1 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |