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Hūnga Volcanic Activity

The Manawatū-Whanganui Region encompasses portions of Tongariro National Park and the North Island Volcanic Plateau, home to three active cone volcanoes - Ruapehu, Tongariro and Ngāuruhoe.

These maunga (mountains) are recognised for their geological dynamism and their cultural significance; they are regarded as tūpuna (ancestral entities) possessing mana (power) and mauri (life force). Planning for the risks posed by volcanic activity recognises this duality and seeks to integrate Western science and mātauranga Māori. A key part of this planning is the Central Plateau Volcanic Advisory Group (CPVAG), which you can learn more about on the About Us page.

You can head to the Department of Conservation website to find out about the current volcanic risk in Tongariro National Park.

Volcanic activity may manifest through a range of hazardous processes and physical phenomena, including but not limited to:

  • Atmospheric particulate deposition (ash fall), with varied effects in nearby and distant locations.
  • Pyroclastic density currents and ballistic ejecta - predominantly in nearby locations.
  • Lahar (volcanic debris-flow) events - effects both nearby and along river channels.
  • Localised volcanic seismic activity (e.g. earthquake swarms associated with magma movement, or larger earthquakes linked to eruption initiation) - mostly nearby effects.

Ruapehu is identified as the most prominent source of volcanic activity, particularly in relation to population centres such as Ohakune and Waimarino (National Park). A substantial eruption could result in significant impacts to critical infrastructure and economic sectors, notably tourism and agriculture. Furthermore, any eruption will likely have long-term impacts on the cultural and natural environments, including wāhi tapu (sacred sites) and wai māori (freshwater).

The Manawatū-Whanganui Region's boundary intersects these maunga, resulting in shared jurisdictional considerations with the Waikato Region. While Taranaki Maunga is not in the Manawatū-Whanganui Region, an eruption there could impact our region through ash dispersal and associated downstream impacts.

What you need to know

Lahar mapping in our region

Ruapehu is a composite andesitic stratovolcano. Throughout its historic and prehistoric records there have been frequent lahars (volcanic mudflows and debris flows) generated on its flanks, particularly where Te Wai ā-moe (the Crater Lake) overflows into the Whangaehu River and drains eastwards to the Desert Road Fault, where it then diverts southwards past Tangiwai.

This natural hazard map viewer uses lahar deposits from Ruapehu to create zones of lahar risk around Ruapehu.