Born in Gore in 1891, Hargest was a farmer when he volunteered for the New Zealand Expeditionary Force following the outbreak of the First World War in August 1914. Commissioned as an officer, he served in the Gallipoli campaign in 1915 and was seriously wounded. Following his recovery from his wounds, he returned to active duty on the Western Front. He commanded an infantry battalion during the later stages of the war and received several awards for his leadership. After the war, he returned to New Zealand to resume farming. In 1931 Hargest entered the Parliament of New Zealand as the member for Invercargill. Initially an independent, he was one of the strongest supporters of the National Party that was formed in 1936, and held an executive role in the party hierarchy. From 1938, he represented the Awarua electorate and had been considered for the party leadership, but he was no longer available once he volunteered for active service. (Full article...)
Image 2European 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 4Men of the Māori Battalion, New Zealand Expeditionary Force, after disembarking at Gourock in Scotland in June 1940 (from History of New Zealand)
Image 18Percentages 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 19Richard Seddon, Liberal Prime Minister from 1893 to his death in 1906 (from History of New Zealand)
Image 21Māori 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 25A 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 26Strong winds in the Cook Strait produce high waves which erode the shore, as shown in this image (from Geography of New Zealand)
Image 28Hinepare 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 33The 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 38The 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.
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. Scientists classified it as an intraplate earthquake and potentially an aftershock of the 2010 Canterbury earthquake.
Christchurch's central city and eastern suburbs were badly affected, with damage to buildings and infrastructure already weakened by the 2010 Canterbury earthquake 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 when soprano Rosina Buckman returned to New Zealand for a concert tour in 1922, the prime minister and a former prime minister spoke at the reception?
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