Following are 3 examples of different tectonic settings of convergent plate boundaries. The convergent plate boundaries that occur on continents are the collisional mountain belts. In particular, it is proved that there exists a unique solution continuous on the closure of the domain for a given sequence of convergent boundary values. Where is a convergent plate boundary In the ocean basins, convergent plate margins are marked by deep trenches in the sea floor. The plates are usually motionless because of the resistance of the other. These plates don't move in slow motion in the way you would think. This is called a transform plate boundary.
This type of convergent boundary is similar to the Andes or the Cascade Range in North America.Īlong offshore to the east of southern Taiwan, different stages of subduction and collision occur simultaneously along strike of the convergent boundary. As the North American plate is sliding north, it is encountering resistance from the Pacific plate sliding south. The AFB has been formed because of the subduction process near the Andaman-Sumatra convergent boundary. Locating at the boundary between the Philippine Sea Plate to the East and the Eurasian Plate to the West, the island of Taiwan was formed at a complex convergent boundary between the two plates. Japan's dealing with a single convergent boundary, but San Francisco is staring down multiple faults, and the ones that matter are transform faults.
Yet from northern California into the Pacific Northwest is a subduction zone, a convergent boundary where the oceanic plate dives beneath the continental plate of North America. He attributed the quake to the subduction of the Philippine Sea Plate under the Eurasian Plate at their convergent boundary. The Cyprian Arc represents the convergent boundary between the Anatolia Block to the north and the Africa Plate to the south. How dangerous is a convergent plate boundary?Ĭonvergent boundaries are more dangerous than divergent and transform fault boundaries due to the threat of a major earthquake, an explosive volcanic eruption, tsunamis or a mountain landslide.The tectonics underlying the Sunda arc are a type of plate boundary known as a convergent boundary. The collision of tectonic plates can result in earthquakes, volcanoes, the formation of mountains, and other geological events. The next type is Oceanic-Oceanic Convergence.Īlso know, what happens at a convergent boundary?Ī convergent plate boundary is a location where two tectonic plates are moving toward each other, often causing one plate to slide below the other (in a process known as subduction). The first type of convergent boundary is Oceanic-Continetal Convergence. Here the Nazca Plate is subducting beneath the South American plate.Īdditionally, what are the 3 types of convergent boundaries and what do they cause? There are three types of convergent boundaries each with its own consequences. The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate. The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate. Just so, where are convergent boundaries located in the world? Convergent boundaries can also form islands. The collision of this oceanic and continental plate was how the Andes Mountains were formed. Therefore at many convergent plate obstacles, there are continental volcanic arcs, or volcanic island arcs.
This allows hot magma from deep within the earth to get up into the cracks. Examples of Convergent Boundaries The West Coast of South America is a convergent boundary between the Nazca Plate and the South American Plate. At a convergent boundary, one plate sub-ducts beneath some other.
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