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A 19th-century carving of a tattooed Maori from kauri gum. The carving is owned and displayed by the Dargaville Museum, New Zealand.
Kauri gum is resin from kauri trees (Agathis australis), which historically had several important industrial uses. It can also be used to make crafts such as jewellery. Kauri forests once covered much of the North Island of New Zealand, before early settlers caused the forests to retreat, causing several areas to revert to weeds, scrubs, and swamps. Even afterwards, ancient kauri fields and the remaining forests continued to provide a source for the gum. Between 1820 and 1900, over 90% of Kauri forests were logged or burnt by Europeans.
Kauri gum forms when resin from kauri trees leaks out through fractures or cracks in the bark, hardening upon exposure to air. Lumps commonly fall to the ground and can be covered with soil and forest litter, eventually fossilising. Other lumps form as branches forked or trees are damaged, releasing the resin. (Full article...)
Image 3Strong winds in the Cook Strait produce high waves which erode the shore, as shown in this image (from Geography of New Zealand)
Image 4The Mission House at Kerikeri is New Zealand's oldest surviving building, having been completed in 1822 (from History of New Zealand)
Image 5Māori 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 6New Zealand is antipodal to points of the North Atlantic, the Iberian Peninsula and Morocco.
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 28A 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 29The 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 35Percentages 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 40The 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 48European 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 51Men 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...)
Rapanui Rock during sunset, Sumner, Christchurch, New Zealand
Shag Rock (also known as Rapanui) is a sea stack that marks the entrance of the Avon Heathcote Estuary near Christchurch, New Zealand. It is a prominent landmark for navigators at sea as well as travelers on the road to Sumner. The rock stands close to the southern shore just above the low tide level. In the February 2011 Christchurch earthquake it shattered and the remains, which are still easily seen from the road, have, with dark humour by some locals, been called "Shag Pile" (a pun referencing the style of carpet). (Full article...)
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