Plate Tectonics Earth Science Explosion Movement in narrow zones along plate boundaries causes most earthquakes. most seismic activity occurs at three types of plate boundaries—divergent, convergent, and transform. as the plates move past each other, they sometimes get caught and pressure builds up. when the plates finally give and slip due to the increased pressure, energy is. Plate tectonics drive the reshaping of continents. inch by inch, this accounts for incredibly long distances over millions of years. continents collide creating a supercontinent cycle. then, they detach again into a new configuration. all the result of convergent, divergent, and transform plate boundaries.
Convergent Boundary The melted rock rises into and through the overlying plate as magma, often forming a chain of volcanoes parallel to the plate boundary. powerful earthquakes are common along these boundaries. the pacific ring of fire is an example of a convergent plate boundary. two plates sliding past each other forms a transform plate boundary. one of the. For example, sections of earth’s crust can come together and collide (a “convergent” plate boundary), spread apart (a “divergent” plate boundary), or slide past one another (a “transform” plate boundary). each of these types of plate boundaries is associated with different geological features. In a simplified model, there are three major types of tectonic plate boundaries: convergent, divergent, and transform. convergent plate boundaries let’s first look at convergent plate boundaries, which can be broken down into three subcategories, depending on the type of crusts involved. Divergent boundaries; convergent boundaries. exercise 10.4 a different type of transform fault; exercise 10.5 getting to know the plates and their boundaries; image descriptions; media attributions; continental drift and sea floor spreading became widely accepted around 1965 as more and more geologists started thinking in these terms.
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