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Convergent Boundary ocean-ocean with subduction picture

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Convergent Boundary ocean-ocean with subduction picture

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all information in big paragraph

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all information is in big paragraph

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All information is in big paragraph

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Transform Boundaries are formed when two tectonic plates can move past one other in opposite directions. The movement is mostly horizontal, although the plates do not move smoothly, instead they slowly scrape against one another, which then causes energy to build. Then suddenly they shift releasing energy. These movements break or distort rock. An example of a Transfrom Boundary is the San Andreas Fault, however most Transform Boundaries are found on the Ocean floor. The Earth feature that occurs as a result of this pate movement is Earthquakes The definition of a Transform Boundary is: Convection currents move 2 plates (ocean/continental) in opposite directions or in the same direction at different speeds. At Transform Boundaries lithosphere is neither created nor destroyed. Many Transform Boundaries are found on the sea floor, where they connect segments of diverging mid-ocean ridges. Here is a link to a video about Transform Boundaries https://www.youtube.com/watch?v=Wp-hZ0QCoQY

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Divergent boundaries occur along spreading centers where plates are moving apart and new crust is created. This new crust is generated as the plates move away from each other. An example of an divergent boundary, which is one of the most known is the Mid-Atlantic Ridge. The Mid-Atlantic Ridge is located straight down the middle of the North America, South America, Europe, and Africa. The definition of a divergent boundary ocean-ocean(seafloor spreading) is, Convection currents pull the 2 ocean plates apart.Hot, less dense magma rises in the middle, cools and hardens, pushing the old seafloor out. There are also continental-continental divergent boundaries. The plates in this boundary are moving away from each other. The defintion of this boundary is: Convection currents pull convectional plates apart. Magma rises in the middle, cools, hardness, then sinks, forming a valley. Eventually fills in with ocean water and becomes seafloor spreading.Here is a link to a youtube video so that you can learn more about divergent boundaries. https://www.youtube.com/watch?v=FK1s1-OJ5BE

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Convergent Boundaries are locations where lithospheric plates are moving towards one another. The plate collisions that occur in these areas can produce earthquakes, volcanic activity, and crustal deformation. Ann example of a convergent boundary is along the west coast of South America between the Nazca Plate and the South American Plate. Convergent Boundaries also can create islands.There are also Convergent Boundaries with and without subduction. These boundaries include, Convergent Boundary ocean-continental with subduction, Convergent Boundary ocean-ocean with subduction, and continental-continental No subduction. The defintion of a convergent boundary ocean-continental with subduction is: convection currents cause denser ocean plate to dive under continental plate, ocean plate melts, forms magma and magma rises forming volcanoes. The features of Earth that occur at this boundary as a result of plate movement are, Ocean Trenches, Volcanoes, and Mountains. The definition of a Convergent Boundary ocean-ocean with subduction is: convection currents cause 2 plates to move towards each other. One plate is always older, colder, and move denser and dives under. The feature of Earth that occurs at this boundary as a result of this plate movement is Ocean Trenches and Volcanic Islands. An example of where on Earth this boundary exists is the Aleutian Islands. The next Convergent Boundary is continental-continental No subduction, the definition is: convection currents cause plates to move towards each other. Both plates are the same density therefore no subduction occurs. The 2 plates crumble up. the feature of Earth that occurs as a result of this plate movement is mountains. An example on Earth of where this type of boundary exists at the Himalayan Mountain.
Here is a link to  a video to learn more about Convergent Plate Boundaries and what they are and how they occur. Also to learn more about Convergent Boundaries with and without subduction.
https://www.youtube.com/watch?v=Y0eWnOZpSpQ.