Moderate volcanic unrest continues at Whakaari/White Island, with substantial gas, steam and mud bursts observed at the vent located at the back of the crater lake. Other monitoring parameters remain elevated and the Volcanic Alert Level stays at Level 2.
In the second of our behind-the-scenes series looking at the National Geohazards Monitoring Centre (NGMC) in the lead up to its one-year anniversary in December, we have a look at some interesting non-earthquake events the Geohazard Analysts have picked up
Moderate volcanic unrest continues at Whakaari/White Island, but no new changes are observed in the monitored parameters. The Volcanic Alert Level remains at Level 2.
Volcanic unrest continues at Whakaari/White Island and some monitored parameters show further increases in activity. Hazards on the island are now greater than during the past few weeks, and the Volcanic Alert Level is raised to Level 2.
Volcanic unrest continues at Whakaari/White Island and some monitored parameters show an increase in activity, with a level of uncertainty about what this means. Hazards on the island remain unchanged and the Volcanic Alert Level remains at Level 1.
In the first of our behind-the-scenes series looking at the National Geohazards Monitoring Centre in the lead up to its one-year anniversary in December, we get to know three of the Centre’s Geohazard Analysts.
Small, muddy, geyser-like explosions are occurring in the active crater at Whakaari/White Island due to a rising crater lake drowning the active vents. This geysering poses no risk to visitors. The Volcanic Alert Level remains at Level 1.
GeoNet keeps a close eye on all active volcanoes in New Zealand (and the Kermadecs). To help us do this we have the New Zealand Volcanic Alert Level System, which defines the current level of activity at each volcano.
Submarine eruptions rarely happen close to New Zealand, so when the eruption happened off Tonga in August, GeoNet got a chance to test our satellite data analysis tools.
Earthquakes in the Taupo region are often associated with existing faults caused by the spreading of the Taupo Volcanic Zone due to large scale tectonic processes.