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The slender smooth-hound or gollumshark (Gollum attenuatus) is a species of ground shark in the familyPseudotriakidae. It is endemic to the waters around New Zealand, where it is usually found close to the bottom over the continental slope at depths of 300–600 m (980–1,970 ft). An extremely slim, plain brownish shark reaching 1.1 m (3.6 ft) in length, the slender smooth-hound can be identified by its broad, flattened head with a long, distinctively bell-shaped snout. Its mouth is angular with short furrows at the corners, and contains a very high number of tooth rows in both jaws. Its two dorsal fins are roughly equal in size.
The diet of the slender smooth-hound is diverse, but dominated by small, benthicbony fishes and decapodcrustaceans. It exhibits a specialized form of aplacental viviparity with oophagy: the females produce a single capsule in each uterus that contains 30–80 ova, of which one ovum develops into an embryo that consumes the rest of the ova and stores the yolk material in its external yolk sac. The growing embryo is mainly sustained by this yolk sac during gestation, though it may be additionally supplied with histotroph ("uterine milk") produced by the mother. The typical litter size is two pups, one per uterus. The International Union for Conservation of Nature (IUCN) has assessed the slender smooth-hound as Least Concern; it is taken as fisherybycatch but not in great numbers, and furthermore large portions of its range see minimal fishing activity. (Full article...)
Image 4Richard Seddon, Liberal Prime Minister from 1893 to his death in 1906 (from History of New Zealand)
Image 5European 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 6The 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 22Men of the Māori Battalion, New Zealand Expeditionary Force, after disembarking at Gourock in Scotland in June 1940 (from History of New Zealand)
Image 25The 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 26The Forty-Fours viewed from the north; the leftmost islet is the easternmost point of New Zealand. (from Geography of New Zealand)
Image 29New Zealand is antipodal to points of the North Atlantic, the Iberian Peninsula and Morocco.
Image 30Hinepare 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 42The Mission House at Kerikeri is New Zealand's oldest surviving building, having been completed in 1822 (from History of New Zealand)
Image 43Māori 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 47Percentages 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 48Pavlova, a popular New Zealand dessert, garnished with cream and strawberries. (from Culture of New Zealand)
Image 53A 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)
A major earthquake occurred in Christchurch on Tuesday 22 February 2011 at 12:51 p.m. local time (23:51 UTC, 21 February). The Mw6.2 (ML6.3) earthquake struck the Canterbury region in the South Island, centred 6.7 kilometres (4.2 mi) 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 previous quake damage. Subsequent population loss saw the Christchurch main urban area fall behind the Wellington equivalent, to decrease from second- to third-most populous area in New Zealand. Adjusted for inflation, the 2010–2011 Canterbury earthquakes caused over $44.8 billion in damages, making it New Zealand's costliest natural disaster and the 21st-most-expensive disaster in history. (Full article...)
... that New Zealand opera singer Helen Medlyn's first performing role was as one of the Three Kings?
... that before bungee jumping with White House aides in New Zealand, senior White House correspondent Bill Plante said he was "proving that you're never too old to do something really stupid"?
... that Phomen Singh, an early Indian migrant to New Zealand, sold sweets and chutneys out of a suitcase?
... that in 1981, New Zealand prime minister Robert Muldoon controversially published a list of "subversives", including many members of the Workers' Communist League?
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