Whakaari / White Island - Volcanology

Volcanology

Whakaari's eruptions have produced both lava flows and explosive eruptions of ash. It is New Zealand's only active marine volcano and perhaps the most accessible on earth, attracting scientists and volcanologists worldwide as well as many tourists. It is part of the Taupo Volcanic Zone.

Volcanologists from the GeoNet Project continually monitor the volcano’s activity via surveillance cameras. Survey pegs, magnetometers and seismograph equipment for early earthquake warnings via radio have also been installed on the crater walls. The island is usually on an alert level rating of 1 or 2 on a scale of 1–5. At most times the volcanic activity is limited to steaming fumaroles and boiling mud. In March 2000, three small vents appeared in the main crater and began belching ash which covered the island in fine grey powder. An eruption on 27 July 2000 blanketed the island with mud and scoria and a new crater appeared. Major eruptions in 1981–83 altered much of the island’s landscape and decimated the extensive pōhutukawa forest. The large crater created at that time now contains a lake, whose level varies substantially. Between July and August 2012 White Island showed signs of increased activity with lake and gas levels rising from inside the crater. On 5 August 2012 a minor eruption occurred, sending ash into the air. More eruptions have followed since.

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