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Two types of convergent boundaries are where Ocean plates meet Continental plates creating subduction zones and where two continental plates meet. Subduction zones and Continent to Contient resulting in Mountain formation. One example of a subduction zone is the Pacific coast South America. The Pacific plate is converging with the South ...
The location of a convergent boundary stays reasonably constant. When an ocean plate converges with a continental plate. The Ocean plate is driven down creating a subduction zone. The subduction zone often creates an ocean trench at the point the two plates meet. The continental plate is pushed upward as the ocean plate is pushed under the continental plate. The longer the motion bringing the ...
A convergent boundary occurs when one plate slips under, or converges with another. If two forces are acting on two separate objects pushing them toward each other, one object will slide under while the other over. The two plates do not simply crush each other. Usually the plate with the greatest density slips on top of the plate with the lower density. Often the convergence of plates results ...
The mid-Atlantic ridge that is slowly pushing North America away from Europe. The mid-Atlantic ridge lies mostly in the middle of the Atlantic Ocean and is the classic example of a divergent plate boundary. This tells us that a couple of large mantel plumes are at work below the Earth's surface and these are gradually pulling the crust apart. It is where the ancient content of Pangea used to ...
The main plate boundaries are convergent, divergent, and transform. 1. A convergent boundary happens when two plates are moving towards each other: one plate is subducted below another or mountains are formed. 2. A divergent boundary happens when two plates are moving away from each other. 3. A transform boundary happens when two plates move away from a divergent plate boundary. India and Asia ...
An example of this is where India and Asia collide forming the Himalayas. The third types is a transverse fault where two plates run into each other at an angle or almost side by side. The San Andreas fault in Southern California is an example of this type of convergent fault. Two tectonic plates are moving toward each other and collide ...
Good examples include the Western Pacific (with its deep-sea trenches and volcanoes) and the Himalayan Mountain Range (a product of the Indian plate pushing northward to Asia). Divergent Boundary Balancing out convergent boundaries, divergent boundaries happen when two plates separate or "split-apart".
An oceanic plate goes under a continental plate and causes volcanism on the continental plate. This occurs because the continental plate is less dense. An example of oceanic slab subduction would be the Andes mountains of South America, which run along the western side of that continent. Mountain ranges can form when two continental plates ...
All subduction boundaries are convergent boundaries but not all convergent boundaries are subduction zones. A subduction zone is where an ocean crust meets a continental crust. The ocean crust is pushed under the continental crust creating a subduction zone and a deep ocean trench. This is a converging boundary. There is also the possibility of an ocean crust connected to a continental crust ...
A convergent boundary causes extremely powerful earthquakes and eruptions. A convergent boundary is where one of the plates, usually a oceanic plate, is subducted beneath a continental plate. This plate boundary is seen on the West coast of South America causing the Andes. Often, seawater and minerals get caught up in the subduction zone, which can cause a build up of pressure and leads to the ...