What boundary is between the Cocos Plate and the Caribbean plate?

What boundary is between the Cocos Plate and the Caribbean plate?

The Cocos Plate is bounded by several different plates. To the northeast it is bounded by the North American Plate and the Caribbean Plate. To the west it is bounded by the Pacific Plate and to the south by the Nazca Plate….

Cocos Plate
Type Minor
Approximate area 2,900,000 km2
Movement1 north-east
Speed1 67 mm/year

Is the Cocos Plate and Caribbean Plate convergent or divergent?

(The Cocos Plate is a subducting plate where it converges with the Caribbean Plate.) These interactions are what are responsible for earthquakes, oceanic trenches, mountains, and volcanoes. To learn more, check out these Science NetLinks resources: Tsunamis: Know What To Do!

What type of plate boundary is the Caribbean islands?

The northern boundary of the Caribbean plate with the North American plate is a transform plate boundary, as seen in the image above. The North American plate and the Caribbean plate are sliding past each other there.

Is the Caribbean plate convergent divergent or transform?

In the Caribbean Sea, the U. S. Virgin Islands lie along a transform plate boundary where the small Caribbean Plate moves eastward past the oceanic part of the North American Plate.

Is Iceland a convergent boundary?

Iceland lies on the Mid Atlantic Ridge, a divergent plate boundary where the North American Plate and the Eurasian Plate are moving away from each other. As the plates pull apart, molten rock or magma rises up and erupts as lava creating new ocean crust.

Which plate is not adjacent to the Caribbean Plate?

On the western edge of the plate is a continuous subduction zone where the Cocos, Panama, and North Andean Plates are all converging with the Caribbean Plate. The Cocos Plate is subducting beneath the Caribbean Plate, while the Caribbean Plate is subducting below both the Panama Plate and the North Andean Plate.

How do continental plates behave at a divergent plate boundary?

In divergent boundaries, plates are moving away from each other; in convergent boundaries, plates are moving toward each other; and in transform boundaries, plates are sliding past each other. The type of crust on each plate determines the geologic behavior of the boundary (Figure 1.1).

Are there volcanoes on the Caribbean plate?

In contrast, the Caribbean Plate farther east overrides the North American Plate, creating the island arc of the Lesser Antilles with its active volcanoes. There are currently no active volcanoes in Puerto Rico and the Virgin Islands; the last volcanoes were active approximately 30 million years ago.

What kind of plate boundary runs across Iceland convergent?

The Iceland hotspot and mighty geological phenomena Iceland sits spanning the Mid-Atlantic Ridge tectonic plate boundary which separates the Eurasian and the North American plates. The ridge, an underwater mountain chain, extends about 16,000 km along the north-south axis of the Atlantic Ocean.

What are the boundaries of the Caribbean Plate?

The Caribbean Plate. Presently, there are strike-slip faults along the North and Southeast boundaries of the Caribbean Plate, allowing eastward movement relative to the North and South American Plates. In particular, the Northern boundary is left-lateral, while the Southern boundary is right-lateral (Mann, 1999).

Where is the Cocos Plate and the Caribbean Plate?

The Cocos Plate in the Pacific Ocean is subducted beneath the Caribbean Plate, just off the western coast of Central America. This subduction forms the volcanoes of Guatemala, El Salvador, Nicaragua, and Costa Rica, also known as the Central America Volcanic Arc.

Where are Puerto Rico and Hispaniola located on the plate?

Puerto Rico, the Virgin Islands to its east, and eastern Hispaniola to its west, are located on an active plate boundary zone between the North American Plate and the northeast corner of the Caribbean Plate (Figure 1).

How is Venezuela related to the Caribbean Plate?

This boundary is in part the result of transform faulting along with thrust faulting and some subduction. The rich Venezuelan petroleum fields possibly result from this complex plate interaction.