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The east coast of South America along the Atlantic Ocean is a passive continental margin. This means that it is not located along a tectonic plate boundary where significant tectonic activity such as earthquakes or volcanic eruptions occur. The passive margin formed when South America separated from Africa during the opening of the South Atlantic Ocean.
Eldfell is located on a divergent plate boundary, specifically along the Mid-Atlantic Ridge on the island of Heimaey in Iceland.
The boundary between the Pacific Plate and the North American Plate is a transform boundary. At this boundary, the plates slide past each other horizontally, causing frequent earthquakes along the boundary. This boundary is known as the San Andreas Fault.
Tectonic plates come together at convergent boundaries. Some examples include the boundary between the Pacific Plate and the North American Plate along the west coast of the United States, where the plates are converging and creating the Cascade Range of mountains. Another example is the boundary between the Indian Plate and the Eurasian Plate, where the plates are colliding and creating the Himalayas.
A plate is not classified as convergent, divergent, or transform, a plate boundary i.e. a boundary between plates is. All three types of plate boundary can be found along the edges of the North American plate.
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.
Canada is on the North American plate, the eastern part of this plate extends to the mid-Atlantic ridge, however this is far from Canada. The western coast of Canada is a subduction zone for the most part with a small amount of the Queen Charolette fault towards the north. The subduction zone is called the Cascadia subduction zone.
The West Coast of Central America is located along a convergent plate boundary where the Cocos Plate is subducting beneath the North American Plate. This subduction zone has led to the formation of the Central American Volcanic Arc and the occurrence of frequent earthquakes in the region.
The plate boundary that is found along the coast of California is the San Andreas fault system that runs in a northwest- southwest direction I think that's the answer
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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.
In plate tectonics, a convergent boundary, also known as a destructive plate boundary (because of ... 1 Descriptions; 2 Convergent margins ... An example of a continental-oceanic subduction zone is the area along the western coast of South.
Convergent
Pinnacles National Monument is located along the boundary of the Pacific Plate and the North American Plate. The monument showcases unique geological features formed by volcanic activity along this plate boundary.
The east coast of South America along the Atlantic Ocean is a passive continental margin. This means that it is not located along a tectonic plate boundary where significant tectonic activity such as earthquakes or volcanic eruptions occur. The passive margin formed when South America separated from Africa during the opening of the South Atlantic Ocean.
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
The Nazca and Antarctic plates share a convergent tectonic boundary where the Nazca Plate is subducting beneath the Antarctic Plate. This results in volcanic activity and the formation of the Andes mountain range along the western coast of South America.