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Love in Motion is the fourth studio album by New Zealand singer-songwriter Anika Moa. The album's underlying theme is love. Moa's civil partner, Azaria Universe, was her biggest influence when writing the album. With Love in Motion, Moa moved from the folk and country pop influences of In Swings the Tide to a pop rock sound. The album was released by EMI Records internationally on 12 March 2010, with releases in Moa's home country and Australia following on 5 April and 10 September, respectively. Moa toured Westfield malls the week of the album's release, and a concert tour followed in May and June 2010.
Critical reviews for the album have been mostly positive, with Moa's lyrical writing received well. It debuted and peaked on the New Zealand Albums Chart at number four. "Running Through the Fire (Storm)" served as the album's lead single, which peaked at number thirty-eight on the New Zealand Singles Chart. "Blame It on the Rain", the second single, did not appear on any record chart. Love in Motion Covers was released in October 2011; it comprises covers of the songs from Love in Motion by other musicians. (Full article...)
The following are images from various New Zealand-related articles on Wikipedia.
Image 1The Forty-Fours viewed from the north; the leftmost islet is the easternmost point of New Zealand. (from Geography of New Zealand)
Image 2A 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 10Men of the Māori Battalion, New Zealand Expeditionary Force, after disembarking at Gourock in Scotland in June 1940 (from History of New Zealand)
Image 17European 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 24The 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 27Māori 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 32Percentages 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 41Hinepare 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 55The 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.
...that Frank Rennie joined the New Zealand Army at age 16, to prove to himself 20 months in hospital hadn't crippled him, and went on to become Colonel?
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...)
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