Frequently asked questions about volcanoes.
Please read the advice from the National Emergency Management Agency.
Numerous types of hazards may result from a volcanic eruption they include ash falls, ballistic rock falls, cone-sector collapse, pyroclastic flows and surges, debris flows, lava flows and domes, lahars, volcanic gases, volcanic earthquakes, tsunami and seiches, hydrothermal blasts, and atmospheric effects. Many of these phenomena will only affect an area on the volcano or a few kilometres from the volcano. However, volcanic ash fall can be deposited hundreds to thousands of kilometres from its source, making it the product most likely to affect the largest area and greatest number of people. Volcanic ash can seriously affect aircraft that may fly unintentionally through the ash cloud, often many kilometres from the volcano.
The seismometers that we use are very sensitive instruments and can record signals from a variety of sources. The recorded signals or 'trace' on a volcano drum may represent both volcanic and tectonic earthquakes, as well as human-induced or meteorological noise. The pattern of seismicity on a volcano drum can be complex and often difficult to interpret by the layperson.
This uniquely identifies the seismic site that recorded the trace you are viewing:
"Dino" the dinosaur has been living on Whakaari/White Island since 2004. "Dino" is the unofficial mascot of the Whakaari/White Island volcano camera, and is a testament to whoever made "Dino" and the durability of the plastic he is made from.
Most of our volcano webcams have infrared lenses allowing them to "see" at night. The stars and moon are often photographed as lights in the night sky in the correct conditions. Sometimes, reflections from lights on the camera can also cause the appearance of lights on the picture. Strange interferences are usually caused by glare from the sun or moon reflecting on the perspex camera cover, or occasionally from condensation inside the camera housing. Others can be car lights.
We don't publish the exact locations of our cameras for security reasons, although if official groups need their locations for research or response, they can contact us directly.
A seismograph is coloured red if it is clipped, i.e. the largest parts of the signal are not shown. If this was not done, then a large earthquake would obscure much of the seismograph from view. In other words, if the signal is red, the real size is larger than is shown on the seismograph.
The temperature of Ruapehu Volcano Crater Lake fluctuates slowly (over weeks to months) in response to pulses of heat rising from deep within the volcano. Recent peak recorded temperatures during a warming cycle have reached almost 40 °C while dropping to less than 15 °C during a cooling period.
Auckland City sits on a volcanic field comprised of approximately 50 volcanic cones and craters that erupted at irregular intervals over the past 250,000 years. These volcanoes have formed as a result of intraplate volcanism - this means that there is an active hot spot of magma located approximately 100 kilometres beneath the city. Each time magma rose from the active hot spot it erupted in a new location at the surface. We think that faults might have influenced where magma rose through the crust but there is no successive pattern of where volcanoes have formed, so we cannot predict where a new eruption is most likely to occur. Rangitoto volcano erupted about 600 years ago and is the only volcano in the Auckland Volcanic Field thought to have erupted twice (two eruptions about 50 years apart). However, because it is the only known example of two eruptions occurring from one volcano throughout the entire history of the Auckland Volcanic Field, we think it is unlikely Rangitoto will erupt again.
Yes, there are many volcanoes and volcanic fields, but none have erupted for several million years. Well-known examples are the Otago (Dunedin) and Banks Peninsula volcanoes which are the eroded remnants of large shield volcanoes that were active around 8 to 20 million years ago, during the Miocene period. There are also Miocene-Pliocene age provinces of intraplate basaltic volcanoes, similar to those in the Auckland Volcanic Field. For example, there are remains of cones and lava flows inland of Dunedin and Oamaru, and in the Timaru-Geraldine area. Much older volcanic lavas and dikes also occur in the South Island.