Mount Ngauruhoe is the youngest of the three volcanoes in the the taupo volcanic zone. Although thought by many to be a volcano in its own right, it is actually a secondary vent of Mount Tongariro.
it is located near the Waiotapu area of taupo volcanic zone
The Taupo Volcanic zone of North Island New Zealand.
It is in the Taupo Volcanic Zone of North Island New Zealand.
The Taupo Volcanic Zone is its formal name, with extensive active centres.
he Rotorua geothermal region in New Zealand, is part of the much larger Taupo Volcanic Zone.
Mount Tongariro is a compound volcano in the Taupo Volcanic Zone of the North Island of New Zealand. stratovolcano
The various features of the Taupo Volcanic Zone are at the centre of the North Island. These include Lake Taupo, and the mountains of the Tongariro National Park. This was the fourth National Park formed in the World, in 1886.
The general name is the Taupo Volcanic Zone, and includes White Island (Whakaaru) but not the Edgecombe area, nor Mayor Island. In the south it extends beyond Taupo to finish with Ruapehu, Ngaruahoe and Tongariro. This zone is about 350 km long and 100 km wide. This is one of the very active volcanic areas in the world, and has produced about 10 000 cubic km of material.Fortunately, a volcanic eruption is preceded a number of signs, and GNS [Inst of Geological & Nuclear sciences] of New Zealand have developed a scale for the expected hazard from volcanic activity.
Mt Ruapehu is the highest volcanic mountain in the North Island, and is an active volcano, notable for its crater lake. It is relatively active, with an average of 50 years or so between major eruptions, but it has had about 50 minor events since 1945. It first erupted about 250 000 years ago, and is part of the Taupo Volcanic Zone. It has ski fields on its slopes in winter, and volcanic warnings are part of the safety feature of these skifields.
The active volcanoes in New Zealand are Ruapehu, Ngaruhoe and White Island. They are all part of the Taupo Volcanic Zone on the North Island.
New Zealand's Taupo Volcanic Zone is primarily located at a tectonic setting characterized by the subduction of the Pacific Plate beneath the Australian Plate. This complex interaction results in intense volcanic and geothermal activity, as well as the formation of a rift zone. The region is marked by significant tectonic uplift and the presence of numerous active volcanoes, making it one of the most geologically dynamic areas in the world.
The state of volcanic hazard in New Zealand is shown, on a scale of 1 - 5, in the website Geonet.org.nz. The biggest volcanic hazard (averaged over a few thousand years) is Taupo. And more broadly, the Taupo Volcanic Zone in general. Taupo has erupted about 27 times in the last 26 000 years, and the last significant eruption was about AD120. As a matter of record, the H2S gas at the Rotorua geothermal area has killed a few folk in the last decade, and unwary footsteps in the geyser field have taken another few.