Microplate · oceanic crust

New Hebrides Plate

Also called the Vanuatu Plate

The New Hebrides Plate is a microplate in the southwest Pacific that carries the islands of Vanuatu. The Australian Plate sinks beneath it at the New Hebrides Trench at about 11 cm/yr, making Vanuatu one of the most earthquake-prone places on Earth.

Area
643,471 km²
Share of Earth
0.1%
Size rank
24 of 52
Avg boundary speed
7.5 cm/yr
Map showing the location of the New Hebrides Plate and its neighbors New Hebrides Conway Reef Balmoral Reef Open on interactive map

Boundaries of the New Hebrides Plate

3,513 km of boundary in total: 45% convergent, 48% divergent, 7% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
Australian Plate Convergent Subduction zone, Oceanic transform fault 1,540 km 9.1-12.9 cm/yr
Pacific Plate Divergent Mid-ocean spreading ridge, Continental collision zone 793 km 0.3-2.3 cm/yr
Conway Reef Plate Divergent Mid-ocean spreading ridge, Oceanic transform fault 738 km 5.6-11.8 cm/yr
Balmoral Reef Plate Divergent Mid-ocean spreading ridge, Oceanic transform fault 442 km 2.1-3.9 cm/yr

Where it is and what it carries

The New Hebrides Plate covers about 643,000 km² of the southwest Pacific between New Caledonia and Fiji. It carries all of Vanuatu, a long, Y-shaped chain of volcanic islands. To the west, the Loyalty Islands of New Caledonia sit on the Australian Plate, just across the trench.

The plate is a volcanic arc and the young seafloor behind it. Geologists separate it from its neighbors because the North Fiji Basin, east of Vanuatu, is opening along spreading ridges that cut it off from the plates around Fiji.

The New Hebrides Trench

The Australian Plate sinks east beneath Vanuatu along the New Hebrides Trench. This 1,540 km boundary is the plate’s longest, and relative speeds average about 11.4 cm/yr, ranging from about 9.1 to 12.9 cm/yr. Vanuatu’s earthquakes and volcanoes come from this fast subduction.

Here the sinking plate dips east, the opposite of most western Pacific subduction zones, where Pacific seafloor sinks west. Geologists think subduction once ran the other way, along the Vitiaz Trench to the north, where the Pacific Plate sank southwest. In the late Miocene that system jammed, and a new trench formed on the opposite side of the arc. As the new trench pulled back, the arc swung clockwise and the North Fiji Basin opened behind it.

Midway along the arc, the d’Entrecasteaux Ridge on the Australian Plate jams into the trench next to Espiritu Santo and Malakula, slowing subduction there and lifting the islands.

The back-arc side

East of Vanuatu, the North Fiji Basin keeps opening. Along a spreading ridge, the plate moves away from the Conway Reef Plate at about 8.7 cm/yr on average and up to about 11.8 cm/yr. Farther north it spreads from the Balmoral Reef Plate at about 3 cm/yr. Its northern boundary with the Pacific Plate is slow, about 1.1 cm/yr.

Earthquakes and volcanoes

The dataset lists 233 earthquakes of magnitude 6.5 or larger since 1900, one of them above magnitude 8: the 1920 Vanuatu earthquake (M8.1). An M7.9 quake struck southeast of the Loyalty Islands in 1901, and another M7.9 hit about 99 km southwest of Port-Vila in 1950. In February 2021 an M7.7 quake southeast of the Loyalty Islands generated a small tsunami.

The plate holds 14 volcanoes in the dataset. Yasur on Tanna erupts almost continuously. Ambrym, a broad volcano with a large summit caldera, erupted in 2024, and Ambae’s 2017-2018 eruption forced the evacuation of the whole island. Gaua, East Epi and Lopevi have also erupted since 2000.

Countries on the New Hebrides Plate

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

Largest earthquakes on the New Hebrides Plate

233 earthquakes of magnitude 6.5 or more since 1900 had their epicenter on this plate, 1 of them magnitude 8 or larger. Data: USGS.

Volcanoes on the New Hebrides Plate

The Smithsonian Global Volcanism Program lists 14 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

Why is it called the New Hebrides Plate?

New Hebrides was the name of Vanuatu under joint British and French rule. The country became independent as Vanuatu in 1980, but geologists kept the older name for the plate and the trench. Some sources call it the Vanuatu Plate.

Why does Vanuatu have so many earthquakes?

Vanuatu sits directly above a fast subduction zone. The Australian Plate sinks beneath the islands at about 11 cm/yr on average, and the slab breaks in earthquakes from near the surface down to deep below the islands. The dataset lists 233 earthquakes of magnitude 6.5 or larger on this small plate since 1900.

What is Mount Yasur?

Mount Yasur is a small stratovolcano on Tanna Island in southern Vanuatu. It has erupted almost continuously for centuries, throwing out bursts of lava and ash every few minutes. It is one of the most visited active volcanoes in the world, though access is closed when activity rises.

Why are Espiritu Santo and Malakula rising?

The d'Entrecasteaux Ridge on the Australian Plate is too buoyant to sink easily. Where it meets the New Hebrides Trench next to Espiritu Santo and Malakula, it jams into the arc and pushes the islands up. Old coral reefs on these islands now sit well above sea level.

How big is the New Hebrides Plate?

The New Hebrides Plate covers about 643,471 km² (248,445 sq mi), roughly 0.1% of Earth's surface. That makes it the 24th largest of the 52 plates in the PB2002 model.

How fast does the New Hebrides Plate move?

Measured against its neighbors, the New Hebrides Plate moves at an average of 7.5 cm/yr (2.9 in/yr) along its boundaries. The fastest motion is against the Australian Plate, where relative speeds reach 12.9 cm/yr on a convergent boundary.

What countries are on the New Hebrides Plate?

Countries mostly on the New Hebrides Plate: Vanuatu. Shares are measured by land area using Natural Earth outlines.

What plates border the New Hebrides Plate?

The New Hebrides Plate shares boundaries with 4 plates: the Australian Plate (convergent), the Pacific Plate (divergent), the Conway Reef Plate (divergent), the Balmoral Reef Plate (divergent).

All 52 tectonic plates