First it is complex and second, it is poorly understood when compared to the other types of plate boundaries. Quick Tips Ocean-Continent Convergent Plate Boundaries Loading. The cookie is set by the GDPR Cookie Consent plugin and is used to store whether or not user has consented to the use of cookies. Oceanic-Continental Convergent Boundaries by amelie creekmore - Prezi Examples of continent-continent convergent boundaries are the collision of the India Plate with the Eurasian Plate, creating the Himalaya Mountains, and the collision of the African Plate with the Eurasian Plate, creating the series of ranges extending from the Alps in Europe to the Zagros Mountains in Iran. The subduction also forms volcanos and islands as the magma moves to the surface. Two plates slide past each other. In this activity, you're going to be modeling a convergent boundary out of clay. The Andes Mountain Range and the south west side of South America are some of the examples of oceanic-continental boundaries. When an ocean plate meets a continental plate at close to a straight line ( 180 degrees) the result is a subduction zone. A convergent boundary occurs when two tectonic plates move towards each other. This cookie is set by GDPR Cookie Consent plugin. What is an example of oceanic-continental boundary? - Answers Even though this boundary involves the same type of lithosphere, one of the plates will still subduct beneath the other. To complete this activity, you'll need at least two colors of modeling clay and a clean, flat surface to work on. Material that is liquified under the pressure is pushed upwards, forming underwater volcanoes which can create islands. I am currently continuing at SunAgri as an R&D engineer. The Indian plate still maintains its movement northward at 67 mm each year. They are formed from the subduction of oceanic plates. Continent-Ocean Convergence, Formation of Fold Mountains

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