Mt Ruapehu Eruptions

Videos - Mt Ruapehu eruptions

Mt Ruapehu erupts 1945

1945 Mt Ruapehu Erupts. Video courtesy of AP Archive.

Mt Ruapehu erupts 1953

1953 Eruption – Tangiwai Disaster

1995 Mt Ruapehu eruptions

2007 Volcanic Lahar at Mt Ruapehu

What type of volcano is Mt Ruapehu?

Mt Ruapehu is a stratovolcano, a composite cone volcano formed by successive layers of andesite lava and ash deposits. It resulted from the subduction of the Pacific Plate beneath the Australian Plate. Mt Ruapehu is situated at the southern end of the Taupo Volcanic Zone within Tongariro National Park.

Mt Ruapehu is a Stratovolcano

Image Sources

1945 Eruption: Eruption of Mt Ruapehu. Davis, Bruce Valentine, 1913-2003 :Photographs and negatives. Ref: 35mm-00702-b-F. Alexander Turnbull Library, Wellington, New Zealand. /records/23140068

1953 Eruption: Wreckage at the scene of the railway disaster at Tangiwai. Evening post (Newspaper. 1865-2002) :Photographic negatives and prints of the Evening Post newspaper. Ref: EP/1953/2617-F. Alexander Turnbull Library, Wellington, New Zealand. /records/23253369

1969 Eruption: The summit of Mt Ruapehu after the 1969 eruption, note the lahar path. GEO Net , New Zealand https://www.geonet.org.nz/news

1975 Eruption: Ruapehu crater during 1945, visitors were able to obtain a spectacular view of the eruption from the crater rim. https://teara.govt.nz/en/video/6862/ruapehu-crater-1945

1995 Eruption: Mt Ruapehu started to erupt in September 1995. This photograph shows one of the first eruptions, on 23 September 1995. https://teara.govt.nz/en/photograph/8691/explosive-eruption-mt-ruapehu

Notes

* A phreatic eruption happens when magma heats up water in the ground or on the surface. The heat turns the water into steam almost instantly, leading to an explosive mix of steam, water, ash, rocks, and volcanic bombs. For example, Mount St. Helens in Washington experienced many steam explosions before its major eruption in 1980. Sometimes, if the geothermal activity is less intense, it can create a mud volcano instead.
* Tephra refers to all the solid material ejected during a volcanic eruption, regardless of its size, composition, or how it’s thrown out. This material includes everything from fine ash to larger rocks known as blocks. When tephra is airborne, it’s specifically called pyroclasts.
* A lahar is a rapid and powerful mudflow or debris flow that originates on a volcano. It consists of a mixture of water, volcanic ash, rock debris, and pyroclastic material, typically flowing along river valleys. Lahars are highly destructive, capable of flowing at high speeds, reaching depths up to 140 meters (460 feet).

* A Surtseyan (or hydrovolcanic) eruption is a volcanic eruption in which shallow water interacts with lava. Surtseyan eruptions are the “wet” equivalent of ground-based Strombolian eruptions, but because they take place in water, they are much more explosive.