Microplate · oceanic and continental crust

Shetland Plate

Also called the South Shetland Plate

The Shetland Plate is a tiny microplate off the tip of the Antarctic Peninsula that carries the South Shetland Islands. It lies between the South Shetland Trench to the north and the Bransfield Strait rift to the south.

Area
72,215 km²
Share of Earth
<0.1%
Size rank
49 of 52
Avg boundary speed
1.0 cm/yr
Map showing the location of the Shetland Plate and its neighbors Shetland Open on interactive map

Boundaries of the Shetland Plate

1,235 km of boundary in total: 53% convergent, 43% divergent, 5% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
Antarctic Plate Divergent Continental rift, Subduction zone 1,021 km 1.0 cm/yr
Scotia Plate Convergent Oceanic convergent boundary, Continental collision zone 214 km 0.9-1.0 cm/yr

Where it is and what it carries

The Shetland Plate is one of the smallest plates in the PB2002 model, about 72,000 km². It carries the South Shetland Islands, a chain of volcanic and ice-covered islands north of the Antarctic Peninsula, including King George Island, Livingston Island, Deception Island and Penguin Island. King George Island hosts several national research stations. In the dataset the plate holds almost none of Antarctica’s land area, because the islands are small next to the continent.

The islands are an old volcanic arc built over a subduction zone. The crust mixes arc rocks and older continental basement, with oceanic crust on the seafloor around them.

What happens at its edges

Almost all of the plate’s boundary is with the Antarctic Plate, about 1,020 km in total, and PB2002 gives it a relative speed of about 1.0 cm/yr. This single boundary has two very different parts. To the north lies the South Shetland Trench, where former Phoenix Plate seafloor, now counted as part of the Antarctic Plate, sank beneath the islands. To the south lies the Bransfield Strait, a young rift where the crust is pulling apart and the islands are separating from the peninsula.

In the east, a short boundary of about 210 km meets the Scotia Plate, converging at about 0.9 cm/yr.

Why geologists treat it as separate

The Phoenix Plate once subducted along this margin. When spreading on its ridge stopped, the leftover slab kept sinking and rolling back, which most researchers think opened the Bransfield Strait behind the arc. That motion cuts the islands off from the peninsula as a separate block. The plate’s motion is slow and its exact edges are uncertain, so it is one of the more debated microplates in PB2002.

Earthquakes and volcanoes

The dataset lists 2 earthquakes of magnitude 6.5 or larger since 1900, a M6.6 in 2012 and a M6.5 in 2026, both in the South Shetland Islands. In 2020 and 2021 an intense earthquake swarm near a submarine volcano in the Bransfield Strait drew scientific attention to the active rifting there.

The plate has 4 volcanoes in the dataset. Deception Island is the most active and best known, with eruptions between 1967 and 1970. Penguin Island, a small cone off King George Island, is another young volcano.

Countries on the Shetland Plate

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

Largest earthquakes on the Shetland Plate

2 earthquakes of magnitude 6.5 or more since 1900 had their epicenter on this plate. Data: USGS.

EarthquakeMagnitudeYearDepth
South Shetland Islands · Antarctica M6.6 2012 8 km
South Shetland Islands · Antarctica M6.5 2026 21 km

Volcanoes on the Shetland Plate

The Smithsonian Global Volcanism Program lists 4 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

Is Deception Island an active volcano?

Yes. Deception Island is the top of a volcano whose center has collapsed into a flooded caldera, and ships can sail inside through a narrow gap called Neptune's Bellows. Eruptions between 1967 and 1970 damaged the research stations on the island. It is still monitored closely because tourist ships visit it often.

Is subduction still happening at the South Shetland Trench?

This is debated. Spreading stopped on the old Phoenix Ridge offshore a few million years ago, so new seafloor no longer pushes toward the trench. Some researchers think the remaining slab is still sinking slowly and pulling the trench back, while others think subduction has nearly stopped.

Why is the Shetland Plate separate from the Antarctic Plate?

The Bransfield Strait between the South Shetland Islands and the Antarctic Peninsula is an active rift. Because the islands are pulling away from the peninsula, they behave as a separate block, and PB2002 treats that block as its own microplate. Its motion is slow, so some models leave it as part of the Antarctic Plate.

How big is the Shetland Plate?

The Shetland Plate covers about 72,215 km² (27,882 sq mi), roughly <0.1% of Earth's surface. That makes it the 49th largest of the 52 plates in the PB2002 model.

How fast does the Shetland Plate move?

Measured against its neighbors, the Shetland Plate moves at an average of 1.0 cm/yr (0.4 in/yr) along its boundaries. The fastest motion is against the Antarctic Plate, where relative speeds reach 1.0 cm/yr on a divergent boundary.

What countries are on the Shetland Plate?

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

What plates border the Shetland Plate?

The Shetland Plate shares boundaries with 2 plates: the Antarctic Plate (divergent), the Scotia Plate (convergent).

All 52 tectonic plates