There are some great active volcanoes in New Zealand that you can actually visit and explore and we cover 10 of the best here for some great adventuring! How does the magma form at a plate boundary? The Auckland Volcanic Field is now considered dormant, with less than 0.1 per cent chance of an eruption in any given year. The Auckland Volcanic Field is monogenetic meaning each volcano usually only erupts once. Auckland’s volcanic field All of Auckland’s volcanoes come from one magma source. Active magma has flowed for about 200,000 years, forming a scattered trail of vents at the surface in its wake. When one tectonic plate sinks down beneath another one, its temperature increases and the minerals in the rocks start to release water. The city is really located in a hot spot filled with layers of magma from the The Auckland volcanic field is an area of monogenetic volcanoes covered by much of the metropolitan area of Auckland, New Zealand's largest city, located in the North Island.The approximately 53 volcanoes in the field have produced a diverse array of maars (explosion craters), tuff rings, scoria cones, and lava flows. With this situation makes almost the entire area filled with volcanoes. 3. Auckland’s oldest park is also home to one of the region’s earliest volcanoes, as Pukekawa’s last eruption was believed to have occurred more than 100,000 years ago. Underlying Auckland is a diffuse pool of magma that occasionally finds its way to the surface. Auckland is the only city in the world in the active basaltic volcanic field.
New Zealand’s volcanoes are part of a larger zone of active volcanism at plate boundaries that rim the Pacific Ocean – the "Pacific Ring of Fire".
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