Microplate · oceanic and continental crust

Kermadec Plate

The Kermadec Plate is a narrow microplate that runs from south of Tonga to the eastern North Island of New Zealand. The Pacific Plate sinks beneath it along the Kermadec Trench and Hikurangi Trough, feeding a long chain of volcanoes.

Area
505,360 km²
Share of Earth
0.1%
Size rank
28 of 52
Avg boundary speed
5.2 cm/yr
Map showing the location of the Kermadec Plate and its neighbors Kermadec Open on interactive map

Boundaries of the Kermadec Plate

4,858 km of boundary in total: 54% convergent, 38% divergent, 8% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
Pacific Plate Convergent Subduction zone 2,388 km 3.1-13.0 cm/yr
Australian Plate Divergent Mid-ocean spreading ridge, Continental rift 2,219 km 0.3-5.9 cm/yr
Tonga Plate Transform Continental transform fault, Oceanic transform fault 251 km 3.8-4.2 cm/yr

Where it is and what it carries

The Kermadec Plate covers about 505,000 km² and stretches from just south of Tonga to New Zealand’s North Island. Most of it is seafloor along the Kermadec Ridge and the volcanic Kermadec Arc, which reaches the surface at the Kermadec Islands. In the south it includes about 19% of New Zealand: the eastern part of the North Island, including the East Cape and Gisborne.

Many maps include this region in the Australian Plate. PB2002 separates it because the Havre Trough, a back-arc basin west of the Kermadec Ridge, is opening and lets the arc move on its own.

What happens at its edges

The 2,388 km boundary with the Pacific Plate is all subduction. In the north it follows the Kermadec Trench, one of the deepest trenches on Earth, and in the south the shallower Hikurangi Trough off the North Island. Relative speeds average about 7.8 cm/yr, falling from about 13 cm/yr in the north to about 3.1 cm/yr in the south. The Hikurangi margin is slower partly because the Pacific crust there includes a thick oceanic plateau.

The 2,219 km boundary with the Australian Plate opens behind the arc. Offshore it is the Havre Trough, with spreading and rifting. On land it continues as the Taupo Volcanic Zone, where the crust of the North Island is stretching. Relative speeds average about 2.6 cm/yr, from under 1 cm/yr in parts of New Zealand to about 5.9 cm/yr in the north.

At its northern end, the plate meets the Tonga Plate along a short transform boundary at about 3.9 cm/yr.

Earthquakes

The dataset lists 143 earthquakes of magnitude 6.5 or larger since 1900, two of them magnitude 8 or more. The 2021 Kermadec Islands earthquake (M8.1) is the largest, followed by the 1976 Kermadec Islands earthquake (M8.0). Others include M7.7 in 1986 and M7.6 in 2011 near the Kermadec Islands, and a deep M7.8 quake at 153 km south of Fiji in 2007.

Off Gisborne, two quakes in 1947, M7.7 in March and M7.6 in May, produced tsunamis much larger than expected for their size. Geologists call events like these tsunami earthquakes.

Volcanoes

The plate holds 18 volcanoes in the dataset, many of them underwater. Raoul Island in the Kermadec group erupted in 2006, and Monowai, a submarine volcano, in 2014. In 2012, the Havre Seamount erupted deep underwater and released a vast raft of floating pumice. In New Zealand, the Okataina volcanic center produced the 1886 Tarawera eruption, and Whakaari/White Island, often called New Zealand’s most active volcano, has erupted as recently as 2026.

Countries on the Kermadec Plate

Share of each country's land area that lies on this plate.

Largest earthquakes on the Kermadec Plate

143 earthquakes of magnitude 6.5 or more since 1900 had their epicenter on this plate, 2 of them magnitude 8 or larger. Data: USGS.

Volcanoes on the Kermadec Plate

The Smithsonian Global Volcanism Program lists 18 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

What is the Hikurangi Subduction Zone?

It is the southern end of the boundary where the Pacific Plate sinks beneath the Kermadec Plate, running offshore along the east coast of New Zealand's North Island. Here the sinking Pacific seafloor is thick and moves more slowly than farther north. Scientists study it closely because parts of it slip in slow slip events lasting days to weeks, and because it could produce a large earthquake and tsunami.

Why is Whakaari/White Island so active?

Whakaari sits at the southern end of the Kermadec Arc, above magma generated as the Pacific Plate sinks beneath the region. A shallow hydrothermal system of hot, acidic water lies inside its crater, so steam-driven explosions can happen with little warning. The eruption of December 2019 killed 22 people who were visiting the island.

What was the 2021 Kermadec Islands earthquake?

On 4 March 2021 an M8.1 earthquake struck near the Kermadec Islands, on the boundary where the Pacific Plate sinks beneath the Kermadec Plate. It came the same day as an M7.4 foreshock and triggered tsunami warnings around the Pacific, including evacuations in parts of New Zealand. It is the largest quake on the plate in the dataset.

Do all plate models include a Kermadec Plate?

No. Many maps and textbooks treat the Kermadec arc and the eastern North Island as part of the Australian Plate. The PB2002 model separates them because the Havre Trough and Taupo Volcanic Zone are actively opening, which means the arc moves independently of Australia.

How big is the Kermadec Plate?

The Kermadec Plate covers about 505,360 km² (195,121 sq mi), roughly 0.1% of Earth's surface. That makes it the 28th largest of the 52 plates in the PB2002 model.

How fast does the Kermadec Plate move?

Measured against its neighbors, the Kermadec Plate moves at an average of 5.2 cm/yr (2.1 in/yr) along its boundaries. The fastest motion is against the Pacific Plate, where relative speeds reach 13.0 cm/yr on a convergent boundary.

What countries are on the Kermadec Plate?

Countries partly on it: New Zealand. Shares are measured by land area using Natural Earth outlines.

What plates border the Kermadec Plate?

The Kermadec Plate shares boundaries with 3 plates: the Pacific Plate (convergent), the Australian Plate (divergent), the Tonga Plate (transform).

All 52 tectonic plates