Microplate · oceanic and continental crust

Panama Plate

The Panama Plate is a small plate carrying most of Costa Rica and Panama, the narrow land bridge between North and South America. The Cocos Plate subducts beneath its Pacific side, feeding Costa Rica's volcanoes and frequent strong earthquakes.

Area
273,735 km²
Share of Earth
<0.1%
Size rank
37 of 52
Avg boundary speed
3.0 cm/yr
Map showing the location of the Panama Plate and its neighbors Panama North Andes Open on interactive map

Boundaries of the Panama Plate

2,593 km of boundary in total: 78% convergent, 3% divergent, 20% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
Caribbean Plate Convergent Continental collision zone, Oceanic convergent boundary 1,277 km 1.1 cm/yr
Cocos Plate Convergent Subduction zone 533 km 7.1-7.9 cm/yr
Nazca Plate Transform Oceanic transform fault, Oceanic convergent boundary 512 km 4.0-4.0 cm/yr
North Andes Plate Transform Continental transform fault, Continental collision zone 271 km 1.3-1.4 cm/yr

Where it is and what it carries

The Panama Plate covers about 274,000 square kilometers, or 0.05% of Earth’s surface. It holds 94.5% of Panama and 75% of Costa Rica, including San Jose, the Nicoya Peninsula and the Panama Canal. It also extends offshore into the Pacific and the Caribbean.

Its crust is mixed. The isthmus is built mainly from volcanic arc rock that grew on top of oceanic crust and thickened over time. Geologists often call it the Panama Block or Panama Microplate, and its boundaries with the Caribbean and North Andes plates are broad fault zones.

What happens at its edges

The northern edge faces the Caribbean Plate along a 1,277 km boundary that moves at about 1.1 cm/yr. Offshore, this boundary is the North Panama Deformed Belt, a zone of thrust faults where Caribbean seafloor is pushed beneath the isthmus.

The southwestern edge is the southern end of the Middle America Trench. Here the Cocos Plate subducts beneath Costa Rica and western Panama at about 7.5 cm/yr. The Cocos Ridge, a thick volcanic ridge on the Cocos Plate, collides with southern Costa Rica and helps raise the Talamanca Range.

To the south, the Panama Fracture Zone forms a transform boundary with the Nazca Plate at about 4 cm/yr. In the east, the plate meets the North Andes Plate near the border with Colombia, at about 1.3 cm/yr. This collision is slowly pushing the isthmus into northwestern South America.

Earthquakes and volcanoes

The dataset lists 44 earthquakes of magnitude 6.5 or larger on the plate since 1900. The largest was an M7.7 earthquake in Panama in 2026. Costa Rica had the 1991 Limon earthquake (M7.6) on the Caribbean side and the 2012 Nicoya earthquake (M7.6) on the Pacific side, along with an M7.59 event in 1939 near Atenas. Western Panama had an M7.5 earthquake in 1934 near Burica.

The plate holds seven volcanoes in the dataset, nearly all in Costa Rica. Poas and Turrialba, near San Jose, have erupted in recent years. Arenal was continuously active for decades until about 2010, and Irazu last erupted in 1977. In Panama, Volcan Baru (3,474 m) is the country’s highest peak. East of Baru, Cocos subduction gives way to the Panama Fracture Zone, and the active volcanic arc ends.

Countries on the Panama Plate

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

Largest earthquakes on the Panama Plate

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

Volcanoes on the Panama Plate

The Smithsonian Global Volcanism Program lists 7 Holocene volcanoes on this plate. The most recently active:

See all volcanoes on the live map

Frequently asked questions

When did the Isthmus of Panama form?

The isthmus grew from a chain of volcanic islands as the Panama arc moved toward South America. Most studies place the final closure of the seaway between the Pacific and the Caribbean at about 3 million years ago, though some researchers argue for an earlier date. Closure changed ocean currents and allowed land animals to cross between the Americas.

Is the Panama Plate separate from the Caribbean Plate?

In the PB2002 model, yes. Earthquakes and GPS measurements show that the Panama region moves differently from the main Caribbean Plate, with a belt of thrust faults, the North Panama Deformed Belt, between them. Some textbooks still include the area in the Caribbean Plate, and geologists often call it the Panama Block or Panama Microplate.

What caused the 1991 Limon earthquake?

The 1991 Limon earthquake (M7.6) struck Costa Rica's Caribbean coast. It came from thrust faulting along the northern edge of the Panama Plate, where it pushes against the Caribbean Plate. The quake lifted parts of the coastline out of the sea, exposing coral reefs.

How big is the Panama Plate?

The Panama Plate covers about 273,735 km² (105,690 sq mi), roughly <0.1% of Earth's surface. That makes it the 37th largest of the 52 plates in the PB2002 model.

How fast does the Panama Plate move?

Measured against its neighbors, the Panama Plate moves at an average of 3.0 cm/yr (1.2 in/yr) along its boundaries. The fastest motion is against the Cocos Plate, where relative speeds reach 7.9 cm/yr on a convergent boundary.

What countries are on the Panama Plate?

Countries mostly on the Panama Plate: Panama and Costa Rica. Countries partly on it: Colombia. Shares are measured by land area using Natural Earth outlines.

What plates border the Panama Plate?

The Panama Plate shares boundaries with 4 plates: the Caribbean Plate (convergent), the Cocos Plate (convergent), the Nazca Plate (transform), the North Andes Plate (transform).

All 52 tectonic plates