Winston County Ms Arrests 2020, What Happened To Charlie Griffin Wicked Tuna, Industrial Attachment Vacancies In Zimbabwe 2022, How To Help A Bird That Almost Drowned, Used Golf Carts For Sale Near Peachtree City, Ga, Articles E

It is a layer of solid rock that has so much pressure and heat the rocks can flow like a liquid. Some of our most famous mountain ranges have been formed as a result of Continental-Continental Convergence! In order for a collision to be successful by resulting in a chemical reaction, A and B must collide with sufficient energy to break chemical bonds. Also, 90% of all earthquakes take place here. Continental crust is too buoyant to subduct. Rising at the border of Tibet and Nepal, Mount Everest formed from a tectonic smashup between the Indian and Eurasian tectonic plates tens of millions of years ago. But the crust is too thick for magma to get through. Convergent boundaries occur where tectonic plates collide, which takes place where two oceanic plates meet, where two continental plates meet or where an oceanic plate meets a continental plate. If the magma chamber does not solidify before it reaches the surface, it might lead to a volcanic eruption at the surface, leading to the formation of a volcano. The World Ocean is the name for the collective group of oceans on the planet. The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate. Oceanic Plate Crust Density, Tectonics & Boundaries | What is a Continental Plate? Review Visit the Interactive Plate Boundary Map to explore satellite images of these three areas. The formation of the Himalayan and Tibetan Plateau is a result of a continental-continental plate boundary. When a convergent boundary occurs between two oceanic plates, one of those plates will subduct beneath the other. Magma rises into and through the other plate, solidifying into granite, the rock that makes up the continents. To use this website, please enable javascript in your browser. C) entire earth had polar conditions at the . Science, 14.11.2019 16:28, . Other Words from collision Synonyms Choose the Right Synonym Example Sentences Learn More About collision. What additional items could we add to make this model more realistic? These are determined by the area or location on the earths crust where the boundaries are formed. subducted. Found a content error? There are three important parts to collision theory, that reacting substances must collide, that they must collide with enough energy and that they must collide with the correct orientation. Imagine the world is like an egg, with a shell that is cracked all over. 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. 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. At convergent plate boundaries, oceanic crust is often forced down into the mantle where it begins to melt. continental. At a convergent boundary, plates collide and as such are sometimes called "destructive" boundaries because they . 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. What is formed at continental continental plate boundaries? 2011-01-19 04:03:05. Paleomagnetism Evidence & Analysis | What is Paleomagnetism? Oceanic/Oceanic Oceanic/Continental Show. Since the oceanic plate is denser than the continental plate, it is pushed or subducted under the continental plate. I love to write and share science related Stuff Here on my Website. The Crafty Science Teacher. Well-known examples of continental volcanic arcs are the Cascade Mountains in the Pacific Northwest [ 63] and the Western Andes Mountains in South America [ 64 ]. These cookies will be stored in your browser only with your consent. The western coast of South America is a very good example of an oceanic to continental convergent boundary where the Nazca plate is colliding (and being subducted beneath) the South American plate. The remnants of subducted oceanic crust remain beneath the continental convergence zone. The impact of the colliding plates can cause the edges of one or both plates to buckle up into a mountain ranges or one of the plates may bend down into a deep seafloor trench. This convergent boundary has a trench and mantle wedge and frequently, a volcanic arc. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. Oceanic-Continental Convergence. Pacific Ring of Fire This is the most famous boundary because it's the most active seismic area in the world. Convergent boundaries between continental plates are a bit different than oceanic/oceanic and oceanic/continental mashups. The Himalayas were born as a result of the collision between two continental plates (the Indo-Australian Plate and the Eurasian plate) at the convergent boundary between these plates. C) Paleomagnetic reversals. SCIENCE. These cookies ensure basic functionalities and security features of the website, anonymously. There is usually a deep ocean trench off the coast of the continent. 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. Precipitation Reaction Examples in Real Life. Oceanic plates are denser due to being made from basalt rock and thus will sink, or subduct, under continental plates, which are made of granitic rocks. This forms a trench on the oceanic side, and volcanoes and mountains on the continental side. 4.8. Answers: 3 Get Iba pang mga katanungan: Science. Examples in the World One more example is the Cascade Mountain Ranges. Visit the Interactive Plate Boundary Map to explore satellite images of divergent boundaries between continental plates. The Himalaya Mountain Range is the best active example of this type of plate boundary. Is Clostridium difficile Gram-positive or negative? Manage Settings I am currently continuing at SunAgri as an R&D engineer. Study Resources. The different ways the pieces move are like the three types of boundaries: A convergent boundary is a location where two tectonic plates move towards each other. Where can you find an example of this type of 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. Convergent plate boundaries are locations where lithospheric plates are moving towards one another. Start by rolling out two flat sections of clay, each of a different color. The tectonic plates of the lithosphere are not static in nature but are constantly moving towards and away from each other. It does not store any personal data. 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. Our goal is to make science relevant and fun for everyone. 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. What is continental continental convergent boundary? When two continental plates converge, they smash together and create mountains. 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. Oceanic plates are exactly as they sound - the plates below the oceans. This typically happens at oceanic-continental boundaries and oceanic-oceanic boundaries. { "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. The Juan de Fuca oceanic plate is subducting beneath the westward moving North American Continental plate. Continental lithosphere is too buoyant to subduct deeply, so rather than a subduction zone and trench these boundaries encompass a thick mess of folded, piled-up crust. Continent-Continent Convergent Plate Boundaries Loading. An example is the where the Indian sub continent collides with the Asian continent. In geology, continental collision is a phenomenon of plate tectonics that occurs at convergent boundaries. Along a convergent boundary two lithospheric plates collide against each other. Litho is from the Greek word lithos, meaning stone. The amazing Himalaya Mountains are the result of this type of convergent plate boundary. Although they can generally be found under land or water respectively, continental and oceanic plates are actually categorized by their geological makeup. Since two continental plates are colliding, subduction becomes questionable as the difference in density between the plates is usually quite low. from the University of Wisconsin-Madison. This can result in one plate sinking under the other, or the two plates colliding to push the lithosphere upwards. Are All Supplementary Angles Linear Pairs? The Mid-Atlantic Ridge divides Iceland and is the boundary between the North American and Eurasian tectonic plates . 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. In the early stages of this type of boundary, the cones will be deep beneath the ocean surface but later grow to be higher than sea level. When two oceanic plates collide, ocean trenches and volcanoes can form. Oceanic-Oceanic Convergence. What is a convergent boundary and give an example? To the west, the Alps grew in similar fashion via the collision of the African and Eurasian plates. This page will be removed in future. (5) $2.00. This range formed from continent-continent collisions in the time of Pangaea. What is the difference between c-chart and u-chart? So, it is pushed down or subducted beneath the other plate which is warmer and younger. The tectonic plates are of two types: the oceanic plates, and the continental plates. Other features of an oceanic/oceanic convergent boundary are the forearc basin between the trench and the island arc and the backarc basin on the opposite side of the arc. Follow the instructions below and then answer the analysis questions to evaluate your work. Divergent boundaries are formed where two plates pull apart from each other (the most famous example is the Mid-Atlantic Ridge, where the North American and Eurasian plates diverge). Instead, subduction might happen to some extent if the heavier lithosphere below the crust might break free from it due to the forces of friction and pressure created at the convergent boundary. The other two zones being the deep-ocean basins and mid-ocean ridges. The Himalayas (Figure below) are the world's tallest mountains. Out of the two, the older or colder plate will be denser. The two main types of tectonic plates are oceanic and continental. The Appalachian Mountains are the remnants of a larger mountain range. A) plants were distributed to current locations by ancient glacial ice sheets. D) poles were at the equator at times in the geologic past. Science, 28.10.2019 16:29, elaineeee. Students should expect for the clay to collide together, forming a mountain range similar to those that occur when two continental plates collide. Transform Fault Boundaries & Examples | What is a Transform Fault? Fold mountains are created where two or more of Earths tectonic plates are pushed together. Learn the definition of a convergent plate boundary and explore the different types of convergent boundaries, where they occur, and see detailed examples. An example of data being processed may be a unique identifier stored in a cookie. But instead of resting on liquid-y egg yolk, these plates float on a sea of hot magma, something you'd only actually see in rare events like volcanoes. The Earth's crust is split, like an eggshell, into many sections called tectonic plates. Subduction Zones & Processes | What is Subduction? Functional cookies help to perform certain functionalities like sharing the content of the website on social media platforms, collect feedbacks, and other third-party features. When two continental plates collide, large mountain ranges form. Convergent boundary types include oceanic/oceanic, oceanic/continental and continental/continental. Ethan Shaw is an independent naturalist and freelance outdoors/nature writer based in Oregon. Magma chambers that reach the surface break through to form a volcanic eruption cone. The ranges lie in a subduction zone making them very unusual since these are high mountains. Two locations are marked within the rift valley of East Africa . What is the example of divergent boundary? There are several landforms and features that can develop at convergent plate boundaries. Its boundaries border other plates such s the Philippine, North American, Nazca, Indian-Australian, Cocos, Juan de Fuca, and Pacific plates. succeed. The collision of two continental plates occurs when a sea becomes narrower until both plates collide. Which plate sinks into the mantle? A convergent boundary might also feature two oceanic plates. The buoyant magma chambers begin a slow ascent through the overlying materials, melting and fracturing their way upwards. Plates can diverge or slide past one another; where they collide, they form tumultuous convergent boundaries, where one plate is either destroyed hence the alternate term destructive plate boundaries or jams up against the other. Which country, continent, or ocean? The subduction also forms volcanos and islands as the magma moves to the surface. Facts about Convergent Boundaries 10: a continental-continental plate boundary. oceanic crust, the outermost layer of Earths lithosphere that is found under the oceans and formed at spreading centres on oceanic ridges, which occur at divergent plate boundaries. What are the differences between a male and a hermaphrodite C. elegans? Evidence of Plate Tectonics | Overview, Plate Motion & Theory. Continental collision is a phenomenon of the plate tectonics of Earth that occurs at convergent boundaries. Seafloor Spreading Theory & Facts | What is Seafloor Spreading? These mountain ranges are located in South America. The Alps are some of the most majestic mountains around. flashcard sets. copyright 2003-2023 Study.com. They formed from the collision of the Nazca and South America plates. Thus, at convergent boundaries, continental crust is . B) plants probably were tolerant of both tropical and polar conditions. What do you see at a continent-continent convergent plate boundary? Wiki User. The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate. They create many of the mountain ranges, volcanos, and even earthquakes that occur on Earth. Its a ring covering 15 countries which include New Zealand, Papa New Guinea, Indonesia, Philippines, United States, Japan, Chile, Canada, Russia, Guatemala, and Peru. Examples of accreted terranes are found in southeast Alaska and northern Washington state. When two tectonic plates approach each other, subduction zones might be created at the convergent boundary between these two tectonic plates. Performance cookies are used to understand and analyze the key performance indexes of the website which helps in delivering a better user experience for the visitors. Earthquakes and volcanoes can reveal a lot about plate boundaries. Want a front-row seat to some tension-packed seismic action on earth? An error occurred trying to load this video. The consent submitted will only be used for data processing originating from this website. Indian and Eurasian plates. Convergent oceanic-oceanic boundary. Found a content error? One of them is Mount Everest which is the earths highest mountain. Tectonic Plates Overview & Types | Tectonic Plates Definition, Divergent, Convergent, & Transform Plate Boundaries, Evidence for the Mechanism of Continental Drift. At a convergent boundary between oceanic and continental lithosphere, the oceanic plate will always subduct, which will cause earthquakes and form volcanic arcs. Among the major zones of the ocean floor, the continental margin is ranked as one of the three major zones. Petrushka: A Ballet by Igor Stravinsky | Music, Rhythm & Analysis. Chemistry, 21.06.2019 17:40 . Oceanic-continental subduction occurs when an oceanic plate dives below a continental plate. 2.4.3. This model is very simple and misses the other layers, such as the mantle inside the Earth. When were Appalachian mountains formed? This was an ocean-continent boundary in which the oceanic plate was subducted under the continental plate. Here the oceanic plate of Juan de Fuca is subducting beneath the North American continental plate that is moving in a westward direction. Ocean-Continent Convergent Plate Boundaries ( Read ) | Earth Science | CK-12 Foundation Ocean-Continent Convergent Plate Boundaries Covers ocean-ocean and ocean-continent convergent plate boundaries, including the creation of volcanic arcs and earthquakes. As the plate slides to greater depths of about 100 km below the surface of the Earth, it comes into contact with the relatively hotter environment of the mantle. It's a ring covering 15 countries which include New Zealand, Papa New Guinea, Indonesia, Philippines, United States, Japan, Chile, Canada, Russia, Guatemala, and Peru. North American Tectonic Plates | Facts, Movement & Locations. The amazing Himalaya Mountains are the result of this type of convergent plate boundary. Continental collision is a variation on the fundamental process of subduction, whereby the subduction zone is destroyed, mountains produced, and two continents sutured together. In convergence there are subtypes namely: Contributor: Hobart KingPublisher, Geology.com. As one plate bends and subducts under the other, it melts into the asthenosphere, and a deep trench forms. Answer - 1. The intense compression can also cause extensive folding and faulting of rocks within the two colliding plates. Instead, it collided with Eurasia, compressing the landscape and thrusting it upward into mountains. The North Andean Plate is a continental plate that is located in the northern portion of South America in Ecuador, Colombia, and Venezuela. Convergent Boundary. Create your account. What is the example of convergent plate boundary? Effects found at a convergent boundary between continental plates include: intense folding and faulting; a broad folded mountain range; shallow earthquake activity; shortening and thickening of the plates within the collision zone. The presence of mechanically vulnerable layers like a layer of salt in such deposits speeds up the process of folding. When two oceanic plates meet, they form large trenches underwater. Features associated with a subduction zone include: Mountain ranges develop from all types of convergent boundaries. Although the Earth feels stationary, in actuality the lithosphere is always moving, and eventually, that movement can create large geological changes. Vernacular Region: Meaning, Examples, & FAQs. The continents of Africa, South America, Australia and Antarctica were originally part of a large supercontinent called Gondwanaland. Create your account, 26 chapters | Plate Boundaries and Features Google Form. This cookie is set by GDPR Cookie Consent plugin. The different types of boundaries will result in different geographic features as described in the sections below. The characteristics that describe convergent boundaries are subduction, where one plate sinks under another, and collision, where two plates crash together.