the Mid-Ocean Ridge.
Sometimes plate boundaries coincide with those of the continental landmass, the majority do not. Subduction zones such as those around the Pacific are located offshore and influence the shape of South America - the Chile-Peru trench, Alaska, Japan etc. In the Atlantic it is the opening of the Atlantic that is mirrored by South America and Africa, whilst the Mediterranean Sea is dying as Africa slowly pushes into Europe.
Convergent plate boundaries.
The three subtypes of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental. At oceanic-continental boundaries, such as the Nazca Plate subducting beneath the South American Plate, volcanic mountain ranges like the Andes are formed. At oceanic-oceanic boundaries, like the Pacific Plate subducting beneath the North American Plate, island arcs such as the Aleutian Islands are created. Finally, at continental-continental boundaries, such as the collision of the Indian Plate with the Eurasian Plate, large mountain ranges like the Himalayas are formed.
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
The three types of convergent boundaries are when two plates meet and two oceanic plate meet, or where an oceanic and continental plate meet.the three types of convergent boundaries are continent boundaries , continent - ocean boundaries, and last but not least............. ocean boundaries
Convergent plate boundaries.
The three subtypes of convergent plate boundaries are oceanic-continental, oceanic-oceanic, and continental-continental. At oceanic-continental boundaries, such as the Nazca Plate subducting beneath the South American Plate, volcanic mountain ranges like the Andes are formed. At oceanic-oceanic boundaries, like the Pacific Plate subducting beneath the North American Plate, island arcs such as the Aleutian Islands are created. Finally, at continental-continental boundaries, such as the collision of the Indian Plate with the Eurasian Plate, large mountain ranges like the Himalayas are formed.
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active continental margin
active continental margin
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
The two types of convergent boundaries are oceanic-continental and continental-continental. At oceanic-continental convergent boundaries, an oceanic plate subducts beneath a continental plate, leading to volcanic activity and the formation of mountain ranges. In contrast, at continental-continental convergent boundaries, two continental plates collide, resulting in the uplift of mountain ranges without significant subduction. These interactions are responsible for significant geological features and seismic activity.