Whakaari/White Island is currently passively emitting a weak-to-moderate steam and gas plume that contains minor volcanic ash. The Volcanic Alert Level remains at Level 2 and the Aviation Colour Code ...

Cracks in a road in Greymouth, after the 1929 Murchison earthquake, 1929. [Ref #: 1/2-091674-F Part of: West Coast Historical and Mechanical Society: Photographs (PAColl-5376)] The earthquake ...

This earthquake toppled chimneys and furniture in the Arthur's Pass area.

This earthquake caused damage to houses and roads around the Farewell Spit area.

The massive rumbling of the 1929 Buller earthquake was heard as far away as New Plymouth.

The 1931 Hawke’s Bay earthquake caused the largest loss of life and most extensive damage of any quake in New Zealand’s recorded history.

The Aotearoa New Zealand Tsunami Gauge network, also known as the Coastal Sea Level gauge network, supports detection and analysis of potential tsunami threats arriving at New Zealand's coasts. It is ...

The timestamp shown at the top right of the seismograph drum shown above is the time when this image was last refreshed. The previous four hours (240 minutes) of seismic signals (also known as traces) ...

Location history for this earthquake. The automatic earthquake location system makes many locations for each quake. Not all quakes have a location history.

New Zealand’s tectonic setting in the Pacific puts us at risk from many different tsunami sources, some may be generated and arrive at our nearest coasts in less than an hour. To improve tsunami ...

What is an earthquake swarm? Unlike the familiar mainshock-aftershock earthquake sequences, where numerous smaller earthquakes tend to follow a larger earthquake, earthquake swarm sequences do not ...