This cookie is set by GDPR Cookie Consent plugin. The best place to see two continental plates converging is in the Himalayas. Accessibility StatementFor more information contact us [email protected] check out our status page at https://status.libretexts.org. What is a real world example of convergent boundaries? This magma is not a liquid - it's actually solid, but under the incredible pressures beneath the Earth's crust, even solids flow like honey. 5 Perfect Social Commentary Examples in Human History, 10 Vestigial Structures Examples in Animals. Visit the Interactive Plate Boundary Map to explore satellite images of these three areas. The Crafty Science Teacher. The geological features that are formed at convergent plate boundaries include volcanoes, volcanic arcs, mountains (especially in arcs), oceanic trenches, and island arcs. SCIENCE 0373C0. The asthenosphere is a layer (zone) of Earths mantle lying beneath the lithosphere. The Panama Plate, a continental plate, is located in Panama and is currently moving northward, colliding with both the South America plate and the Cocos plate. These mountains were formed as a result of the collision between the Eurasian Plate and the Indo-Australian Plate at the convergent boundary. The purpose of this activity is to . His primary interests from both a fieldwork and writing perspective include landscape ecology, geomorphology, the classification of ecosystems, biogeography, wildlife/habitat relationships, and historical ecology. 3) Fossils of ancient polar plants are currently found near the equator because the ________. What is the ring of fire and where is it located? 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. Convergent Plate BoundariesAccreted Terranes - Geology (U.S - NPS The amazing Himalaya Mountains are the result of this type of convergent plate boundary. 5 Convergent Boundary Examples - The Boffins Portal At the beginning of the age of dinosaurs (during the Triassic Period, about 230 million years ago), the continents were arranged together as a single supercontinent called Pangea. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. Click the image to enlarge or view the MP4 movie (MP4 Video 30.3MB Dec20 11). flashcard sets. At continental-oceanic or oceanic-oceanic boundaries, the plates are different densities, and one sinks under the other. 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. When a convergent boundary occurs between two oceanic plates, one of those plates will subduct beneath the other. Paleomagnetism Evidence & Analysis | What is Paleomagnetism? The formation of volcanoes at such sites is explained below as an answer to the question: How Do Volcanoes Form At Convergent Boundaries? About 225 million years ago, India was a large island still situated off the Australian coast, and a vast ocean (called Tethys Sea) separated India from the Asian continent. What two types of plates come together at continent-continent convergent plate boundaries? An example of this is found at the boundary between the South American continental plate and the Nazca oceanic plate. If one plate was less dense, it would sink beneath the other, forming volcanoes or island arcs. As a result of this, dramatic seismic events can follow like earthquakes, volcanic eruptions, or deformation of the crust. The Himalayan Mountains are an example of: a. continent-continent convergent boundary b. divergent boundary c. transform boundary d. rift movement along divergent boundary Mount St. Helens, Mount Rainier, and other active volcanoes along the Cascade Ranges are examples of: a. ocean-ocean convergent boundaries The subducting plate is heated as it is forced deeper into the mantle, and at a depth of about 100 miles (150 km) the plate begins to melt. This is a great activity for students to review the movement, geological features, crust type, and boundaries and how they are associated with each other. This results in the creation of magma chambers at the subduction zones which might ultimately lead to volcanic eruptions and the formation of volcanic island chains in the ocean. Boundaries are the types of connections between tectonic plates. Which country, continent, or ocean? What are at least 3 effects of the oceanic plate/continental plate convergent boundary? At convergent plate boundaries, oceanic crust is often forced down into the mantle where it begins to melt. Just like these cracked pieces of eggshell, the entire outer crust of the Earth is broken down into sections, called tectonic plates. At convergent plate boundaries, oceanic crust is often forced down into the mantle where it begins to melt. The Continental margins consume about 28% of the area of the ocean. Continental collision is a variation on the fundamental process of subduction, whereby the subduction zone is destroyed, mountains produced, and two continents sutured together. Draw upon what you've learned from this lesson on convergent boundaries when it's time to: To unlock this lesson you must be a Study.com Member. The cracks in the egg are boundaries between plates. 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 sunken plate gets heated in the mantle causing it to melt. The Earths lithosphere, composed of the outer crust and the rigid, uppermost section of the mantle, is divided into mobile segments called tectonic plates on which the oceans and continents ride. . 2.4 Convergent Boundaries - Dynamic Planet: Exploring Geological Copyright 2023 . Which type of plate boundary did the clay mimic? Northward migration of India Note that this figure is a simplification and does not take into account the huge amount of crustal shortening that would have occurred in both the Eurasian and Indian plates. This cookie is set by GDPR Cookie Consent plugin. Convergent Boundary. Contributor: Hobart KingPublisher, Geology.com. Although they can generally be found under land or water respectively, continental and oceanic plates are actually categorized by their geological makeup. Oceanic-Continental Convergence. The types are ocean-ocean, ocean-continent, and continent-continent. A subduction zone is an area where one plate sinks underneath another. Legal. An example of data being processed may be a unique identifier stored in a cookie. A convergent boundary marks the area where two tectonic plates collide or meet each other. Continental Margin - Explanation, Types and FAQs - VEDANTU They create many of the mountain ranges, volcanos, and even earthquakes that occur on Earth. Answers: 1 Show answers Another question on Chemistry. The formation of the Himalayan and Tibetan Plateau is a result of a continental-continental plate boundary. Science, 28.10.2019 16:29, elaineeee. What Is The Difference Between Catholic And Christian? The magma that escapes during subduction can also form new crust and mountain ranges. Effects of a convergent boundary between an oceanic and continental plate include: a zone of earthquake activity that is shallow along the continent margin but deepens beneath the continent; sometimes an ocean trench immediately off shore of the continent; a line of volcanic eruptions a few hundred miles inland from the shoreline; destruction of oceanic lithosphere. The subduction also forms volcanos and islands as the magma moves to the surface. 4.6 Convergent Plate Boundaries - Introduction to Oceanography The new magma (molten rock) rises and may erupt violently to form volcanoes, often building arcs of islands along the convergent boundary. See answer (1) Best Answer. This is a difficult boundary to draw. { "5.01:_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.02:_Wegener_and_the_Continental_Drift_Hypothesis" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.03:_Magnetic_Polarity_Evidence_for_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.04:_Bathymetric_Evidence_for_Seafloor_Spreading" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.05:_Magnetic_Evidence_for_Seafloor_Spreading" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.06:_Seafloor_Spreading_Hypothesis" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.07:_Plate_Tectonics-_Challenge_1" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.08:_Earth\'s_Tectonic_Plates" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.09:_Tectonic_Plate_Motions" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.10:_Theory_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.11:_Divergent_Plate_Boundaries_in_the_Ocean" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.12:_Divergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.13:_Transform_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.14:_Plate_Tectonics-_Challenge_2" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.15:_Ocean-Continent_Convergent_Plates" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.16:_Ocean-Ocean_Convergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.17:_Continent-Continent_Convergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.18:_Continental_Margins" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.19:_Supercontinent_Cycle_and_Pangaea" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.20:_Intraplate_Activity" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.21:_Plate_Tectonics-_Challenge_3" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, { "00:_Front_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "01:_The_Nature_of_Science" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Introduction_to_Earth_Science" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_Planet_Earth" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Earth\'s_Minerals_and_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Geological_Activity_and_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Geological_Activity_and_Volcanoes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Earth\'s_Fresh_Water" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Earth\'s_Oceans" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Atmospheric_Processes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Weather" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:_Climate" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13:_Weathering_and_Soils" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "14:_Erosion_and_Deposition" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "15:_Understanding_Earth\'s_History" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "16:_Earth\'s_History" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "17:_Evolution_and_Populations" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "18:_Ecosystems" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "19:_History_of_Life_on_Earth" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "20:_Earth\'s_Energy" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "21:_Earth\'s_Materials" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "22:_The_Solar_System" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "23:_Beyond_the_Solar_System" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "zz:_Back_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, 5.17: Continent-Continent Convergent Plate Boundaries, [ "article:topic", "showtoc:no", "program:ck12", "authorname:ck12", "license:ck12", "source@https://flexbooks.ck12.org/cbook/ck-12-middle-school-earth-science-flexbook-2.0" ], https://k12.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fk12.libretexts.org%2FBookshelves%2FScience_and_Technology%2FEarth_Science%2F05%253A_Plate_Tectonics%2F5.17%253A_Continent-Continent_Convergent_Plate_Boundaries, \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}\) \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} \)\(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\) \(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\)\(\newcommand{\AA}{\unicode[.8,0]{x212B}}\), 5.16: Ocean-Ocean Convergent Plate Boundaries, source@https://flexbooks.ck12.org/cbook/ck-12-middle-school-earth-science-flexbook-2.0, status page at https://status.libretexts.org.