What Are the Three Different Types of Convergent Boundaries?

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One type of tectonic plate boundary -- a boundary separates the large plates composing Earth's surface -- is the convergent boundary. Tectonic plates are in constant, although extremely slow, movement. Their movements cause land to separate, islands to form, mountains to rise, water to cover land and earthquakes to occur. Convergent boundaries are classified according to what occurs when two plates intersect.

Tectonic Plate Boundaries

The effects of the sliding plates can be seen along the San Andreas fault.
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As the plates of the earth move, three types of tectonic plate boundaries occur. Divergent boundaries occur when two plates move in opposite directions, such as the pulling apart of North and South America from Europe and Africa, which, according to the U.S. Geological Survey, happens at a rate of 25 km every million years. Transform fault boundaries occur when two plates are sliding past each other, as with the San Andreas fault in California. This type of boundary produces earthquakes. The third type of plate boundary is the convergent boundary, which forms when two plates meet head on.

Oceanic-Continental Convergence

Andes mountains with volcanic action resulted from this convergence.
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This convergence boundary is the result of two plates colliding. The oceanic plate gives way to the continental plate. The result is a submerged oceanic plate that sinks slowly, ultimately some of it breaking into small pieces. The small pieces later rise suddenly to the top and cause earthquakes. The continental plate, having risen over the oceanic plate, pushes up to form mountain ranges such as the Andes in South America and the Cascades in North America. According to the U.S. Geological Survey, this convergence produces some of the earth's most powerful volcanoes.

Oceanic-Oceanic Convergence

The Hawaiian islands are volcanic.
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When two oceanic plates converge, one is pushed under the other one. The result is the deep trenches seen in the oceans, particularly the Pacific Ocean. These trenches, like the Marianas Trench in the Pacific (which is deeper than the world's highest mountain is high), form undersea volcanoes. Lava and debris from the volcano pile up and accumulate until it rises above sea level to form an island volcano.

Continental-Continental Convergence

The top of the earth.
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When two continental plates converge, neither can push the other beneath it. The result is a buckling effect at the point of collision. The earth is pushed up in both plates, but the most dramatic effect occurs in the middle. Over a long period of time, large mountains form, such as the Himalayas and Mount Everest, the world's highest mountain. The two plates pushing each other create mountain ranges and high plateaus.

References

About the Author

Robert Alley has been a freelance writer since 2008. He has covered a variety of subjects, including science and sports, for various websites. He has a Bachelor of Arts in economics from North Carolina State University and a Juris Doctor from the University of South Carolina.

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