Convergent Boundary. This is a high activity area that can also literally get too hot to touch! (b) Ol Doinyo Lengai volcano and the East African Rift Valley in Tanzania Convergent Boundaries. Volcanoes are formed at three locations on the crust of the Earth: at convergent boundaries, divergent boundaries, and hot spots. As one plate bends and subducts under the other, it melts into the asthenosphere, and a deep trench forms. My thesis aimed to study dynamic agrivoltaic systems, in my case in arboriculture. The cookie is used to store the user consent for the cookies in the category "Other. 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Where do convergent boundaries occur? What is the shape of C Indologenes bacteria? These cookies track visitors across websites and collect information to provide customized ads. What is a continental continental divergent boundary? Effects that are found at this type of plate boundary include: a zone of progressively deeper earthquakes; an oceanic trench; a chain of volcanic islands; the destruction of oceanic lithosphere. Oceanic-oceanic convergent: a collision between two plates composed of oceanic lithosphere. 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. Study Resources. Further Reading: Geomorphic Processes The Origin And The Evolution Of The Earth Both regions are vulnerable to severe earthquakes associated with this intense plate collision. 55) The East Africa Rift Valleys are an example of _____ plate boundary. At a convergent boundary between oceanic and continental lithosphere, the oceanic plate will always subduct, which will cause earthquakes and form volcanic arcs. The Earth Machine: The Science of a Dynamic Planet; Edmond A. Mathez, James D. Webster, The Geological Society: Convergent Plate Boundaries, U.S. Geological Survey: Convergent Plate Boundaries, U.S. Geological Survey: Accretionary Wedge. It has a length of about 40,000 kilometers. Continental/Continental: The Himalayas - The Geological Society All rights reserved. In a subduction zone, the plates colliding can push the less dense plate upwards, forming mountains. 10 Facts about Convergent Boundaries - Fact File The magma that escapes during subduction can also form new crust and mountain ranges. It has been suggested that the next supercontinent will form in 200-250 million years, so we are currently about halfway through the scattered phase of the current supercontinent cycle. The Himalayan range is a classic example of fold mountains formed in this manner.