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Waimangu Volcanic Rift Valley information


Frying Pan Lake and Cathedral Rocks
Thermal activity on the shore of Lake Rotomahana, near the former site of the Pink Terrace

The Waimangu Volcanic Rift Valley is the hydrothermal system created on 10 June 1886 by the volcanic eruption of Mount Tarawera, on the North Island of New Zealand. It encompasses Lake Rotomahana, the site of the Pink and White Terraces, as well as the location of the Waimangu Geyser, which was active from 1900 to 1904.[1][2] The area has been increasingly accessible as a tourist attraction and contains Frying Pan Lake, which is the largest hot spring in the world,[3] and the steaming and usually pale blue Inferno Crater Lake, the largest geyser-like feature in the world although the geyser itself cannot be seen since it plays at the bottom of the lake.[4]

Waimangu is a Māori-language word meaning "black water". This name comes from the water that was thrown up by the Waimangu Geyser, which was black with mud and rocks.

From the 1890s onwards, the valley has gradually been re-populated naturally by plants ranging from hot water-loving algae and bacteria to mosses and many species of native ferns, shrubs and trees. These in turn support native birdlife including kererū, tūī, shining cuckoo, fantail, bellbird, and pūkeko, as well as introduced bird species such as mynah, magpie, finch and sparrow. A population of black swan thrives in the lower parts of the valley and on Lake Rotomahana. According to local guides, these have been introduced to the region from Western Australia by George Edward Grey in the 19th century along with wallaby.

As a rare eco-system completely naturally re-established following a volcanic eruption, Waimangu is protected as a Scenic Reserve, administered by the Department of Conservation NZ. The developing local native forest is the only current New Zealand instance of vegetation re-establishing from complete devastation without any human influence such as planting.[5] Many of Waimangu's geothermal features are ranked as Category A – extremely important, of international significance.[6]

  1. ^ Bunn, Rex; Nolden, Sascha (7 June 2017). "Forensic cartography with Hochstetter's 1859 Pink and White Terraces survey: Te Otukapuarangi and Te Tarata". Journal of the Royal Society of New Zealand. 48: 39–56. doi:10.1080/03036758.2017.1329748. ISSN 0303-6758. S2CID 134907436.
  2. ^ Bunn and Nolden, Rex and Sascha (December 2016). "Te Tarata and Te Otukapuarangi: Reverse engineering Hochstetter's Lake Rotomahana Survey to map the Pink and White Terrace locations". Journal of New Zealand Studies. NS23: 37–53.
  3. ^ "The Eruption & Birth of Waimangu". Waimangu Volcanic Valley. Retrieved 22 December 2014.
  4. ^ "World & National Importance". Waimangu Volcanic Valley. Retrieved 22 December 2014.
  5. ^ Waimangu Wanderer Guide, October 2013
  6. ^ "Classifying geothermal systems". Waikato Regional Council. Retrieved 22 December 2014.

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Waimangu Volcanic Rift Valley

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