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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. 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. Big mountains! Paleomagnetism Evidence & Analysis | What is Paleomagnetism? This makes it descend or get subducted under the Caribbean Plate. Convergent continental-continental boundary. A convergent boundary, or destructive boundary, is where two plates are moving towards each other and colliding. 4.6 Convergent Plate Boundaries - Introduction to Oceanography The continents of Africa, South America, Australia and Antarctica were originally part of a large supercontinent called Gondwanaland. Fold mountains are created where two or more of Earths tectonic plates are pushed together. When two continental plates collide, large mountain ranges form. What happens at a continental oceanic convergent boundary? Continent-Continent Convergence, Formation of the Himalayas Two locations are marked to show this type of plate boundary - the Cascade volcanoes along the Washington-Oregon coast of North America and the Andes mountain range on the western margin of South America. 3.3: Convergent Boundaries - Geosciences LibreTexts