example of continental continental convergent boundary

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The intense compression can also cause extensive folding and faulting of rocks within the two colliding plates. The number of mountains this tall in the Himalayas is impressive. They float on currents in the underlying asthenosphere based on heating and cooling patterns of magma. Create your account. Both regions are vulnerable to severe earthquakes associated with this intense plate collision. An example of this is found at the boundary between the South American continental plate and the Nazca oceanic plate. Which type of plate boundary did the clay mimic? Continental plates are the part that lies above sea level, but again, the real definition is that the crust is made of granite and other felsic rocks. When two continental plates converge, they smash together and create mountains. In fact, the collision continues to this day -- the Himalayas are still growing! copyright 2003-2023 Study.com. The buoyant magma chambers begin a slow ascent through the overlying materials, melting and fracturing their way upwards. Just like these cracked pieces of eggshell, the entire outer crust of the Earth is broken down into sections, called tectonic plates. The lithosphere of the Earth that includes the crust and the uppermost mantle is not continuous in nature but is subdivided into several pieces called tectonic plates. In convergence there are subtypes namely: Arrange the tectonic plates end to end to create a boundary. At these colliding, compressing boundaries, rocks and debris are warped and folded into rocky outcrops, hills, mountains, and entire mountain ranges. The Appalachian Mountains resulted from ancient convergence when Pangaea came together. e.g., a lithospheric mantle and an oceanic crust. The subduction zone eventually becomes inactive The two continents become welded together as they are compressed together over time. Fold mountain ranges form at convergent plate boundaries. continental. Japan, the Aleutian Islands, and the Eastern Caribbean islands of Martinique, St. Lucia, and St. Vincent and the Grenadines are examples of islands formed through this type of plate boundary. The Karakoram Range is part of the Himalayas. What is formed at continental continental plate boundaries? When an ocean plate meets a continental plate at close to a straight line ( 180 degrees) the result is a subduction zone. Convergent Boundary. 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. Precipitation Reaction Examples in Real Life. 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. Examples in the World Another example of the oceanic-continental convergent boudaries is the Washington-Oregon coastline of the US. Use the resource below to answer the questions that follow. Wiki User. The Pacific Ring of Fire is an example of a convergent plate boundary. Fragments of crust or continent margin sediments might be caught in the collision zone between the continents, forming a highly deformed melange of rock. The different types of boundaries will result in different geographic features as described in the sections below. When one of the plates is an oceanic plate, it gets embedded in the softer asthenosphere of the continental plate, and as a result, trenches are formed at the zone of subduction. When two oceanic plates meet, they form large trenches underwater. A semi-solid, such as marshmallows, slime or putty, could be used as that material and the plates could be something more solid, such as cardboard or paper, to represent the crust. ILTS Science - Physics (116): Test Practice and Study Guide, ORELA General Science: Practice & Study Guide, ILTS TAP - Test of Academic Proficiency (400): Practice & Study Guide, NYSTCE English Language Arts (003): Practice and Study Guide, ILTS Social Science - History (246): Test Practice and Study Guide, ILTS School Counselor (235): Test Practice and Study Guide, ILTS Social Science - Geography (245): Test Practice and Study Guide, ILTS Social Science - Political Science (247): Test Practice and Study Guide, Praxis Family and Consumer Sciences (5122) Prep, Praxis Biology and General Science: Practice and Study Guide, Praxis Biology: Content Knowledge (5236) Prep, Create an account to start this course today. Examples of this boundary in the World Famous Himayla Mountain Range.With Continental drift over millions of years the Indian plate collides with the Eurasian plate forming mountains. She is also certified in secondary special education, biology, and physics in Massachusetts. The Caribbean Plate, which is an oceanic plate, is subducting under the North Andean Plate, forming extensive volcanos in the area. Before collision, both plates would have extended much further than their current boundaries: some 2500 km of India's continental crust was either subducted beneath Asia or squashed and . What causes mountain ranges to rise at convergent plate boundaries? Necessary cookies are absolutely essential for the website to function properly. When two continental plates collide, the impact is so significant that the material in the subduction zone is pushed upwards. The pressure and friction is great enough at these boundaries that the material in the Earth's mantle can melt, and both earthquakes and volcanoes happen nearby. 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