Microplate · oceanic crust

North Bismarck Plate

The North Bismarck Plate is an oceanic microplate under the northern Bismarck Sea, north of New Guinea. It moves almost in step with the Pacific Plate, while the South Bismarck Plate slides rapidly past its southern edge.

Area
388,136 km²
Share of Earth
<0.1%
Size rank
32 of 52
Avg boundary speed
5.7 cm/yr
Map showing the location of the North Bismarck Plate and its neighbors North Bismarck South Bismarck Manus Woodlark Solomon Sea Open on interactive map

Boundaries of the North Bismarck Plate

3,836 km of boundary in total: 63% convergent, 10% divergent, 27% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
South Bismarck Plate Transform Oceanic transform fault, Continental transform fault 1,217 km 11.3-14.6 cm/yr
Pacific Plate Convergent Oceanic convergent boundary, Oceanic transform fault 1,143 km 0.7-1.0 cm/yr
Caroline Plate Convergent Oceanic convergent boundary, Continental collision zone 900 km 0.9-1.7 cm/yr
Manus Plate Convergent Mid-ocean spreading ridge, Continental collision zone 223 km 0.3-9.5 cm/yr
Woodlark Plate Convergent Subduction zone 194 km 7.7-7.9 cm/yr
Solomon Sea Plate Convergent Subduction zone 159 km 8.1-8.2 cm/yr

Where it is and why it is separate

The North Bismarck Plate covers about 388,000 km² of the northern Bismarck Sea, north of New Guinea and New Britain. Only about 2.3% of Papua New Guinea sits on it, mainly small islands in the Admiralty group around Manus.

Geologists separate it because a sharp band of earthquakes, the Bismarck Sea Seismic Lineation, cuts straight across the Bismarck Sea. North of that line the seafloor moves almost with the Pacific Plate; south of it, the South Bismarck Plate moves very differently. Because the North Bismarck Plate moves so slowly relative to the Pacific, many simplified maps do not show it at all.

What happens at its edges

The southern boundary with the South Bismarck Plate is the longest, at 1,217 km. It is mostly a transform fault, with short spreading and collision segments, and relative motion averages about 13 cm/yr, very fast for a transform boundary.

To the north and east, the boundary with the Pacific Plate is slow convergence of about 0.9 cm/yr. To the northwest, it meets the Caroline Plate along the Manus Trench at about 1.3 cm/yr. In the middle of the Bismarck Sea, the tiny Manus Plate sits between the two Bismarck plates, opening the Manus Basin.

At its southeastern corner, two short subduction boundaries carry the Solomon Sea Plate and the Woodlark Plate beneath it, at about 8.2 and 7.8 cm/yr. This corner, where the New Britain Trench bends toward Bougainville, is where almost all of the plate’s great earthquakes happen.

Earthquakes and volcanoes

The dataset lists 79 earthquakes of magnitude 6.5 or larger since 1900, three of them magnitude 8 or more. The 1919 Papua New Guinea earthquake (M8.15) is the largest. In July 1971, the New Britain earthquake (M8.0) and the Bougainville earthquake (M8.1) struck 12 days apart. More recently, an M7.9 quake in December 2016, about 140 km east of Kokopo, struck 95 km deep. Several of these quakes broke inside the sinking Solomon Sea slab rather than on the shallow plate boundary.

Volcanoes are scarce. The dataset lists two, including the St. Andrew Strait volcanic complex near Manus Island, which last erupted in 1957.

Countries on the North Bismarck Plate

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

Largest earthquakes on the North Bismarck Plate

79 earthquakes of magnitude 6.5 or more since 1900 had their epicenter on this plate, 3 of them magnitude 8 or larger. Data: USGS.

Volcanoes on the North Bismarck Plate

The Smithsonian Global Volcanism Program lists 2 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

What caused the 1971 earthquakes near New Britain and Bougainville?

In July 1971, an M8.0 earthquake on 14 July and an M8.1 earthquake on 26 July struck where the New Britain Trench bends southeast toward Bougainville. Here the Solomon Sea Plate sinks steeply beneath the surrounding plates, and the sharp bend in the trench concentrates stress. The same corner produced the M8.15 quake of 1919 and an M7.9 quake in 2016.

Is the Manus Trench still active?

Only barely. The Manus Trench along the northern edge of the plate marks an old subduction zone where the Caroline Plate once sank southward. Today PB2002 shows slow convergence of about 1.3 cm/yr there, and the trench produces far fewer earthquakes than the New Britain Trench to the south.

How is the North Bismarck Plate different from the South Bismarck Plate?

The North Bismarck Plate is mostly quiet ocean floor that drifts with the Pacific Plate. The South Bismarck Plate carries New Britain and the Huon Peninsula, rotates clockwise and rides over the Solomon Sea Plate, so it has many more volcanoes and large earthquakes. The two meet along the Bismarck Sea Seismic Lineation.

How big is the North Bismarck Plate?

The North Bismarck Plate covers about 388,136 km² (149,860 sq mi), roughly <0.1% of Earth's surface. That makes it the 32nd largest of the 52 plates in the PB2002 model.

How fast does the North Bismarck Plate move?

Measured against its neighbors, the North Bismarck Plate moves at an average of 5.7 cm/yr (2.2 in/yr) along its boundaries. The fastest motion is against the South Bismarck Plate, where relative speeds reach 14.6 cm/yr on a transform boundary.

What countries are on the North Bismarck Plate?

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

What plates border the North Bismarck Plate?

The North Bismarck Plate shares boundaries with 6 plates: the South Bismarck Plate (transform), the Pacific Plate (convergent), the Caroline Plate (convergent), the Manus Plate (convergent), the Woodlark Plate (convergent), the Solomon Sea Plate (convergent).

All 52 tectonic plates