the north American plate is the plate that covers most of north America
divergent boundary
North American Plate and the Pacific Plate.
The North America and Caribbean plates meet at a transform plate boundary. This type of boundary is characterized by plates sliding past each other horizontally, causing earthquakes along the boundary.
The North American-Eurasian Plate boundary.
North America and South America have edges that are not all plate boundaries. The boundary between North and South America is known as the Central American Subduction Zone, where the Cocos Plate is subducting beneath the Caribbean Plate.
The two convergent boundaries on the largest plate, the Pacific Plate, are the boundary with the North American Plate along the west coast of North America, and the boundary with the Philippine Sea Plate in the western Pacific Ocean.
The North American Plate and the Caribbean Plate are on a transform boundary. This boundary is known as the North American-Caribbean Plate boundary, where the plates slide past each other horizontally. This motion results in frequent earthquakes in the region.
No, the east coast of the United States is in the middle of the of the North American plate. The eastern most part of the North American plate boundary is in the middle of the Atlantic Ocean in an area known as the Mid-Atlantic Rift. The north western coast of North America (Oregon, Washington, Canada and Southern Alaska) are subduction zones.
The Pacific Plate and the North American Plate are the names of those two plates.
The plate boundary near New York is the North American Plate boundary. This boundary is a divergent boundary, meaning that the North American Plate is moving away from the Mid-Atlantic Ridge, which runs along the eastern coastline of the United States.
The plate boundary along the coast of California is a transform boundary where the Pacific Plate and the North American Plate slide past each other horizontally, causing earthquakes. In contrast, the plate boundary along the west coast of South America is a convergent boundary where the Nazca Plate subducts beneath the South American Plate, leading to volcanic activity and mountain building.
Klyuchevskaya Sopka is on the Kamchatka Peninsula in Russia and is located near the boundary of the North American Plate and the Pacific Plate. This boundary is a convergent boundary, specifically a subduction zone where the Pacific Plate is being subducted beneath the North American Plate.