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Linwood House in 2003
Linwood House was built as the homestead for Joseph Brittan, who, as surgeon, newspaper editor and provincial councillor, was one of the dominant figures in early Christchurch, New Zealand. The suburb of Linwood was named after Brittan's farm and homestead. Brittan's daughter Mary married William Rolleston, and they lived at Linwood House following Joseph Brittan's death. During that time, Rolleston was the 4th (and last) Superintendent of the Canterbury Province, and Linwood House served for many important political and public functions.
The property went through many changes in ownership. Land was successively subdivided; at its peak, 110 acres (450,000 m2) of land belonged to Linwood House, of which only 2,013 m2 (21,670 sq ft) remain. For some years, Linwood House was used as a private day and boarding school for girls. The house declined during the mid-20th century, was used for flats for several decades, and was in 1985 described by an historian as the "city's worst example of a house which should be preserved being left to decay". The house's fortunes improved when it was purchased in 1988 by people sympathetic to heritage. Gradually being restored, Linwood House suffered significant damage in the 2010 Canterbury earthquake and partially collapsed in the 2011 Christchurch earthquake. Civil Defence ordered the building's demolition, which was carried out in the second half of 2011. (Full article...)
Image 7Hinepare of Ngāti Kahungunu, is wearing a traditional korowai cloak adorned with a black fringe border. The two huia feathers in her hair, indicate a chiefly lineage. She also wears a pounamuhei-tiki and earring, as well as a shark tooth (mako) earring. The moko-kauae (chin-tattoo) is often based on one's role in the iwi. (from Culture of New Zealand)
Image 8The scalloped bays indenting Lake Taupō's northern and western coasts are typical of large volcanic caldera margins. The caldera they surround was formed during the huge Oruanui eruption. (from Geography of New Zealand)
Image 9Strong winds in the Cook Strait produce high waves which erode the shore, as shown in this image (from Geography of New Zealand)
Image 11Māori whānau (extended family) from Rotorua in the 1880s. Many aspects of Western life and culture, including European clothing and architecture, became incorporated into Māori society during the 19th century. (from History of New Zealand)
Image 15The Māori are most likely descended from people who emigrated from Taiwan to Melanesia and then travelled east through to the Society Islands. After a pause of 70 to 265 years, a new wave of exploration led to the discovery and settlement of New Zealand.
Image 33European settlers developed an identity that was influenced by their rustic lifestyle. In this scene from 1909, men at their camp site display a catch of rabbits and fish. (from Culture of New Zealand)
Image 34The Mission House at Kerikeri is New Zealand's oldest surviving building, having been completed in 1822 (from History of New Zealand)
Image 35Pavlova, a popular New Zealand dessert, garnished with cream and strawberries. (from Culture of New Zealand)
Image 37Percentages of people reporting affiliation with Christianity at the 2001, 2006 and 2013 censuses; there has been a steady decrease over twelve years. (from Culture of New Zealand)
Image 42A 1943 poster produced during the war. The poster reads: "When war broke out ... industries were unprepared for munitions production. To-day New Zealand is not only manufacturing many kinds of munitions for her own defence but is making a valuable contribution to the defence of the other areas in the Pacific..." (from History of New Zealand)
Image 47New Zealand is antipodal to points of the North Atlantic, the Iberian Peninsula and Morocco.
Image 48Men of the Māori Battalion, New Zealand Expeditionary Force, after disembarking at Gourock in Scotland in June 1940 (from History of New Zealand)
Similar to Pamukkale in Turkey, hot water containing large amounts of calcium bicarbonate precipitated calcium carbonate, leaving thick white layers of limestone and travertine cascading down the mountain slope, forming pools of water and terraces. The White terraces were the larger and more beautiful formation while the Pink terraces were where people went to bathe.
The terraces located on the edges of Lake Rotomahana near Rotorua were considered to be the eighth wonder of the natural world and were New Zealand's most famous tourist attraction ( they were attracting tourists from Europe in the early 1880s when New Zealand was still relatively inaccessible) until they were destroyed when Mount Tarawera, five kilometres to the north, erupted at 03:00 on June 10, 1886.
The volcano belched out hot mud, red hot boulders and immense clouds of black ash. The eruption caused approximately 153 deaths and buried the village of Te Wairoa. The lake, and several others nearby, were substantially altered in shape and area by the eruption. (Full article...)
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