Microplate · oceanic and continental crust

South Bismarck Plate

The South Bismarck Plate is a fast-rotating microplate under the southern Bismarck Sea, New Britain and the Huon Peninsula of Papua New Guinea. It overrides the Solomon Sea Plate at the New Britain Trench, one of the most active subduction zones in the Pacific.

Area
309,087 km²
Share of Earth
<0.1%
Size rank
36 of 52
Avg boundary speed
9.8 cm/yr
Map showing the location of the South Bismarck Plate and its neighbors South Bismarck North Bismarck Woodlark Solomon Sea Manus Open on interactive map

Boundaries of the South Bismarck Plate

2,784 km of boundary in total: 44% convergent, 22% divergent, 34% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
North Bismarck Plate Transform Oceanic transform fault, Continental transform fault 1,217 km 11.3-14.6 cm/yr
Woodlark Plate Convergent Continental collision zone, Continental rift 721 km 0.9-7.1 cm/yr
Solomon Sea Plate Convergent Subduction zone 655 km 7.1-15.8 cm/yr
Manus Plate Divergent Mid-ocean spreading ridge, Oceanic transform fault 191 km 3.9-15.6 cm/yr

Where it is and what it carries

The South Bismarck Plate covers about 309,000 km² in northern Papua New Guinea. It holds about 16% of the country’s land: the island of New Britain, the Huon Peninsula and the Finisterre Range on the mainland, and a chain of volcanic islands along the north coast. The rest is the floor of the southern Bismarck Sea.

The plate’s western end is caught in a collision between the Finisterre volcanic arc and mainland New Guinea that is still under way. Coral reef terraces on the Huon Peninsula have been lifted far above sea level as the arc pushes into the mainland.

What happens at its edges

The longest boundary, 1,217 km, separates it from the North Bismarck Plate along the Bismarck Sea Seismic Lineation. This is mostly a transform boundary, and the plates slide past each other fast, at about 13 cm/yr on average.

To the south, the Solomon Sea Plate dives beneath New Britain at the New Britain Trench. Relative speeds average about 11.3 cm/yr and reach about 15.8 cm/yr, among the highest in the PB2002 model. Subduction here feeds the volcanoes along New Britain.

In the northeast, the plate spreads away from the tiny Manus Plate along the Manus Basin at about 8.5 cm/yr on average. In the west it meets the Woodlark Plate along the Ramu and Markham valleys, where collision, rifting and strike-slip faulting combine at about 3.5 cm/yr.

Earthquakes and volcanoes

The dataset lists 141 earthquakes of magnitude 6.5 or larger since 1900, two of them magnitude 8. The 1906 Papua New Guinea earthquake (M8.0) struck near the Huon Gulf. In November 2000 the New Ireland earthquake (M8.0) was followed within a day by two M7.8 quakes southeast and south-southwest of Kokopo. An M8.0 quake also struck southeast of Kokopo on 1 January 1916. In 2022 an M7.6 quake hit 116 km beneath the mainland near Kainantu.

With 24 volcanoes in the dataset, this small plate is one of the most volcanic places in the southwest Pacific. Manam, Langila and Ulawun have erupted recently. Rabaul, a caldera at the northeast tip of New Britain, last erupted in 2014. In 1888 part of Ritter Island collapsed into the sea and set off a destructive tsunami. Long Island, Karkar and Kadovar are also active.

Countries on the South Bismarck Plate

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

Largest earthquakes on the South Bismarck Plate

141 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 South Bismarck Plate

The Smithsonian Global Volcanism Program lists 24 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

What happened at Rabaul in 1994?

In September 1994, two volcanoes on the rim of the Rabaul caldera, Tavurvur and Vulcan, erupted at the same time. Ash buried much of Rabaul town, and the provincial capital was later moved to nearby Kokopo. Tavurvur kept erupting on and off for years afterward.

Why does the South Bismarck Plate rotate?

Its two ends are held in very different ways. In the west, the Huon Peninsula and Finisterre Range are jammed against mainland New Guinea, while in the east the plate rides over the Solomon Sea Plate, which sinks quickly at the New Britain Trench. Pinned at one end and free to move at the other, the plate swings clockwise.

What is the Bismarck Sea Seismic Lineation?

It is a narrow, straight band of earthquakes running east-west across the Bismarck Sea. It marks the transform boundary where the South Bismarck Plate slides past the North Bismarck Plate, with short spreading segments in the Manus Basin. Relative motion along it averages about 13 cm/yr.

How big is the South Bismarck Plate?

The South Bismarck Plate covers about 309,087 km² (119,339 sq mi), roughly <0.1% of Earth's surface. That makes it the 36th largest of the 52 plates in the PB2002 model.

How fast does the South Bismarck Plate move?

Measured against its neighbors, the South Bismarck Plate moves at an average of 9.8 cm/yr (3.9 in/yr) along its boundaries. The fastest motion is against the Solomon Sea Plate, where relative speeds reach 15.8 cm/yr on a convergent boundary.

What countries are on the South Bismarck Plate?

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

What plates border the South Bismarck Plate?

The South Bismarck Plate shares boundaries with 4 plates: the North Bismarck Plate (transform), the Woodlark Plate (convergent), the Solomon Sea Plate (convergent), the Manus Plate (divergent).

All 52 tectonic plates