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Molten rock accumulates in a magma chamber outside the North Island’s main volcanoes
http://www.scientificamerican.com/article/zombie-volcano-slowly-grows-beneath-new-zealand/
Something for folks near Taupo to keep an eye on.
Where's Taupo? https://en.wikipedia.org/wiki/Taupo
http://www.newzealand.com/int/lake-taupo/ Nice place.
http://www.newzealand.com/int/feature/huka-falls/
http://www.scientificamerican.com/article/zombie-volcano-slowly-grows-beneath-new-zealand/
Something for folks near Taupo to keep an eye on.
Where's Taupo? https://en.wikipedia.org/wiki/Taupo
http://www.newzealand.com/int/lake-taupo/ Nice place.
http://www.newzealand.com/int/feature/huka-falls/
A 2015 study found that much of the main Taupo Volcanic Zone was subsiding, or sinking, as is expected after magma erupts and drains from an underground chamber. But one area, to the north and west along the Bay of Plenty coast, seemed to be rising. “I just discounted it at the time, because we were so focused on looking at the more volcanic part,” says Hamling.
Later, the team took a closer look, taking in data from global-positioning stations as well as geodetic surveys dating back to the 1950s. They found that the ground had risen by 5 millimetres per year in the 1950s, but that rate had more than doubled to about 12 millimetres a year starting in the mid-2000s. It has since dropped back to the lower rate.