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Wai-O-Tapu

geothermal area, Rotorua, New Zealand

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Wai-O-Tapu is a geothermal area located near Rotorua, New Zealand. It is part of a region known for its remarkable array of hot springs, boiling mud pools, and geysers. A notable feature is the Lady Knox Geyser, which erupts daily. This geothermal activity, along with mineral-water pools, has made Rotorua a popular tourist destination. The geothermal belt in this area is a result of volcanic activity, with features like Waimangu being formed by the eruption of Mount Tarawera in 1886. Geothermal energy is abundant in such volcanic regions, where underground reservoirs of steam and hot water can be harnessed.12

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