Minor plate · oceanic and continental crust

Caribbean Plate

The Caribbean Plate lies beneath the Caribbean Sea and carries much of Central America and the Greater and Lesser Antilles. Its edges combine long transform faults to the north and south with subduction zones on its east and west sides.

Area
2.96 million km²
Share of Earth
0.6%
Size rank
16 of 52
Avg boundary speed
1.9 cm/yr
Map showing the location of the Caribbean Plate and its neighbors Caribbean North Andes Panama Cocos Open on interactive map

Boundaries of the Caribbean Plate

8,998 km of boundary in total: 47% convergent, 12% divergent, 41% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
North American Plate Transform Oceanic transform fault, Continental rift 3,508 km 1.7-1.8 cm/yr
South American Plate Convergent Subduction zone, Continental transform fault 2,270 km 1.6-2.0 cm/yr
North Andes Plate Convergent Subduction zone, Continental rift 1,397 km 1.1-1.3 cm/yr
Panama Plate Convergent Continental collision zone, Oceanic convergent boundary 1,277 km 1.1 cm/yr
Cocos Plate Convergent Subduction zone 546 km 7.1-8.0 cm/yr

Where it is and what it carries

The Caribbean Plate covers about 3 million square kilometers, or 0.58% of Earth’s surface. Most of it lies beneath the Caribbean Sea, but it also carries land. All of Honduras, Nicaragua, El Salvador, Jamaica, Haiti, the Dominican Republic and Puerto Rico sit on it, along with the islands of the Lesser Antilles such as Barbados, Saint Lucia and Grenada. About half of Trinidad and Tobago and a quarter of Costa Rica are also on the plate, while Cuba lies almost entirely on the North American Plate to the north.

Its crust is mixed. The central Caribbean floor is an oceanic plateau, much thicker than normal ocean crust. The Central American part, including Honduras and Nicaragua, is continental and volcanic arc crust.

What happens at its edges

The northern edge, 3,508 km long, is a transform boundary with the North American Plate, with an average relative speed of about 1.7 cm/yr. It runs from the Motagua Fault in Guatemala, through the Cayman Trough, where a short spreading center opens new seafloor, and along strike-slip faults through Jamaica and Hispaniola to the Puerto Rico Trench.

The eastern edge is the Lesser Antilles subduction zone. Here Atlantic seafloor of the North American and South American plates sinks beneath the Caribbean Plate. The southern edge, shared with South America at about 1.9 cm/yr, turns into transform faults that cross northern Venezuela and Trinidad. Farther west, the plate meets the North Andes Plate at about 1.2 cm/yr, where Caribbean seafloor slowly underthrusts northern Colombia, and the Panama Plate at about 1.1 cm/yr along the North Panama Deformed Belt.

The western edge is the fastest. At the Middle America Trench, the Cocos Plate subducts beneath El Salvador and Nicaragua at about 7.6 cm/yr.

Earthquakes

The dataset lists 92 earthquakes of magnitude 6.5 or larger on the plate since 1900, none of magnitude 8. The largest was the 1946 Dominican Republic earthquake (M7.76) near Samana Bay, which produced a deadly tsunami. Several others reached M7.7, including the 1943 earthquake north of Puerto Rico, the 1992 Nicaragua tsunami earthquake, the 2001 El Salvador earthquake and the 2020 Jamaica earthquake in the Cayman Trough. In 2025 an M7.6 earthquake struck south of the Cayman Islands. The 2010 Haiti earthquake (M7.0) was smaller but far deadlier, because it hit close to a crowded capital.

Volcanoes

The plate holds 59 volcanoes in the dataset, in two arcs. In the west, Cocos Plate subduction feeds the Central American Volcanic Arc, including Masaya, Telica, San Cristobal and Momotombo in Nicaragua and San Miguel in El Salvador. In the east, the Lesser Antilles arc includes La Soufriere on Saint Vincent, which erupted in 2021, the submarine volcano Kick ’em Jenny north of Grenada, and Soufriere Hills on Montserrat. Mount Pelee on Martinique destroyed the town of Saint-Pierre in 1902.

Countries on the Caribbean Plate

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

Largest earthquakes on the Caribbean Plate

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

Volcanoes on the Caribbean Plate

The Smithsonian Global Volcanism Program lists 59 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

What caused the 2010 Haiti earthquake?

The 2010 Haiti earthquake (M7.0) struck near the Enriquillo-Plantain Garden fault zone, part of the boundary where the Caribbean Plate slides east past the North American Plate. Stress from this slow sideways motion built up on faults in southern Haiti until they ruptured beneath densely populated areas near Port-au-Prince.

Where did the Caribbean Plate come from?

Most geologists think the Caribbean Plate formed in the Pacific and moved east into the gap between North and South America over the past several tens of millions of years. Much of its interior is an unusually thick oceanic plateau built by huge volcanic outpourings in the Late Cretaceous. A minority view holds that it formed close to where it is today, and the debate is not fully settled.

Why are there volcanoes in the Lesser Antilles?

Atlantic seafloor belonging to the North and South American plates sinks beneath the eastern edge of the Caribbean Plate. Water released from the sinking slab melts the mantle above it and feeds a chain of volcanoes from Saba to Grenada, including Soufriere Hills on Montserrat, Mount Pelee on Martinique and La Soufriere on Saint Vincent.

Is Puerto Rico on the Caribbean Plate?

In the PB2002 model, yes. Puerto Rico sits near the northern edge of the Caribbean Plate, just south of the Puerto Rico Trench. Some geologists treat Puerto Rico and the Virgin Islands as a small separate block caught in the boundary zone between the Caribbean and North American plates.

How big is the Caribbean Plate?

The Caribbean Plate covers about 2.96 million km² (1.14 million sq mi), roughly 0.6% of Earth's surface. That makes it the 16th largest of the 52 plates in the PB2002 model.

How fast does the Caribbean Plate move?

Measured against its neighbors, the Caribbean Plate moves at an average of 1.9 cm/yr (0.8 in/yr) along its boundaries. The fastest motion is against the Cocos Plate, where relative speeds reach 8.0 cm/yr on a convergent boundary.

What countries are on the Caribbean Plate?

Countries mostly on the Caribbean Plate: Nicaragua, Honduras, Dominican Republic, Haiti, El Salvador, Jamaica, Puerto Rico, Trinidad and Tobago and 7 more. Countries partly on it: Costa Rica, Guatemala, Venezuela, France and Cuba. Shares are measured by land area using Natural Earth outlines.

What plates border the Caribbean Plate?

The Caribbean Plate shares boundaries with 5 plates: the North American Plate (transform), the South American Plate (convergent), the North Andes Plate (convergent), the Panama Plate (convergent), the Cocos Plate (convergent).

All 52 tectonic plates