Microplate · oceanic crust

Juan Fernandez Plate

Also called the Juan Fernandez Microplate

The Juan Fernandez Plate is a small oceanic microplate in the southeast Pacific, near the point where the Pacific, Nazca and Antarctic plates meet. It sits between spreading ridges and rotates as the surrounding plates pull apart.

Area
97,681 km²
Share of Earth
<0.1%
Size rank
48 of 52
Avg boundary speed
8.8 cm/yr
Map showing the location of the Juan Fernandez Plate and its neighbors Juan Fernandez Open on interactive map

Boundaries of the Juan Fernandez Plate

1,239 km of boundary in total: 27% convergent, 70% divergent, 3% transform. Speeds are relative motion between the two plates, from the PB2002 model.

Neighboring plate Boundary type Main features Shared length Relative speed
Nazca Plate Convergent Oceanic convergent boundary, Mid-ocean spreading ridge 551 km 1.0-11.2 cm/yr
Pacific Plate Divergent Mid-ocean spreading ridge, Oceanic convergent boundary 528 km 5.6-20.2 cm/yr
Antarctic Plate Divergent Mid-ocean spreading ridge, Oceanic transform fault 160 km 3.5-7.4 cm/yr

Where it is and what it carries

The Juan Fernandez Plate, also called the Juan Fernandez Microplate, covers about 98,000 square kilometers, or 0.02% of Earth’s surface. It lies in the southeast Pacific Ocean, between about 31° and 35° south, along the East Pacific Rise. It sits near the triple junction where the Pacific Plate, the Nazca Plate and the Antarctic Plate meet.

It is made entirely of young oceanic crust under deep water and carries no islands. It is one of the smallest plates in the PB2002 model.

What happens at its edges

On its western side, the plate spreads away from the Pacific Plate along a 528 km boundary at about 13.5 cm/yr on average. This is part of the East Pacific Rise and one of the fastest spreading boundaries on Earth.

On its eastern side, the plate meets the Nazca Plate along a 551 km boundary. Part of it is spreading ridge, and part of it is compressional, where the rotating block pushes against the Nazca Plate. The average relative speed is about 5.3 cm/yr, but it varies widely along the boundary because the microplate rotates.

In the south, a short boundary of about 160 km with the Antarctic Plate is mostly spreading ridge, with an average relative speed of about 5.3 cm/yr.

Why geologists separate it

Ship surveys of seafloor depth and magnetic stripes revealed two spreading ridges here with a rotating block between them. That block moves independently of the three large plates around it, which is why plate models such as PB2002 list it separately. Like the Easter Plate to the north, it shows how unstable triple junctions on very fast ridges can break off small pieces of seafloor.

Because it is small and remote, its exact boundaries and rotation rate are less certain than those of large plates.

Earthquakes

The dataset lists four earthquakes of magnitude 6.5 or larger on the plate since 1900, all far out at sea. The largest was an M7.0 earthquake in 2014 on the southern East Pacific Rise, followed less than an hour later by an M6.6 event nearby. Others were an M6.9 in 1925 and an M6.7 in 2021. The plate has no named volcanoes in the dataset, though new oceanic crust forms constantly along its spreading ridges.

Countries on the Juan Fernandez Plate

No country sits mainly on the Juan Fernandez Plate. Its surface is almost entirely ocean floor.

Largest earthquakes on the Juan Fernandez Plate

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

EarthquakeMagnitudeYearDepth
southern East Pacific Rise M7.0 2014 17 km
Easter Island region M6.9 1925 10 km
southern East Pacific Rise M6.7 2021 10 km
southern East Pacific Rise M6.6 2014 10 km

Frequently asked questions

Are the Juan Fernandez Islands on the Juan Fernandez Plate?

No. The Juan Fernandez Islands, which belong to Chile, sit on the Nazca Plate roughly 3,000 km east of the microplate, much closer to the Chilean coast. The microplate shares their name because both lie at about the same latitude in the southeast Pacific.

How did the Juan Fernandez Plate form?

It formed at a triple junction where three fast-spreading ridges meet. Where ridges join like this, one ridge tip can grow into older seafloor and trap a block between two spreading centers. The trapped block then rotates on its own, becoming a microplate.

Is the Juan Fernandez Plate related to the Easter Plate?

They formed in a similar way. Both are rotating microplates on the East Pacific Rise between the Pacific and Nazca plates. The Easter Plate lies farther north, while the Juan Fernandez Plate sits near the junction with the Antarctic Plate.

How big is the Juan Fernandez Plate?

The Juan Fernandez Plate covers about 97,681 km² (37,715 sq mi), roughly <0.1% of Earth's surface. That makes it the 48th largest of the 52 plates in the PB2002 model.

How fast does the Juan Fernandez Plate move?

Measured against its neighbors, the Juan Fernandez Plate moves at an average of 8.8 cm/yr (3.5 in/yr) along its boundaries. The fastest motion is against the Pacific Plate, where relative speeds reach 20.2 cm/yr on a divergent boundary.

What countries are on the Juan Fernandez Plate?

No country sits mainly on the Juan Fernandez Plate; it is almost entirely ocean floor. The nearest land is part of the neighboring plates.

What plates border the Juan Fernandez Plate?

The Juan Fernandez Plate shares boundaries with 3 plates: the Nazca Plate (convergent), the Pacific Plate (divergent), the Antarctic Plate (divergent).

All 52 tectonic plates