Accretion (geology)
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Accretion is a process by which sediment is added to a tectonic plate. When two tectonic plates collide, one of the plates may slide under the other. This process is called subduction. The plate which is being subducted (the plate going under), is floating on the asthenosphere and is pushed up and against the other plate, which will often be scraped by the subducted plate. This scraping causes sediment to come off the subducted plate and form a mass of rocks called the accretionary wedge, which attaches itself to the subducting plate (the top plate).
[edit] Evidence
Continental plates are formed of rocks that are very noticeably different from the rocks that form the ocean floor. The ocean floor, is usually composed of basaltic rocks that make the ocean floor denser than continental plates. In places where plate accretion has occurred, land masses may contain the dense, basaltic rocks that are usually indicative of oceanic lithosphere. In addition, a mountain range that is distant from a plate boundary suggests that the rock between the mountain range and the plate boundary is part of an accretionary wedge.
[edit] Examples
This process is present in many places, but especially around the Pacific Rim, including the western coast of North America, the eastern coast of Australia, and New Zealand. New Zealand consists of areas of accreted rocks which were added on to the Gondwana continental margin over a period of many millions of years. The western coast of North America is made of accreated island arcs. The accreted area stretches from the Rocky Mountains to the Pacific coast.
[edit] Resources
- Robert, Ballard D. Exploring Our Living Planet. Washington D.C.: The National Geographic Society, 1983.
- Sattler, Helen Roney. Our Patchwork Planet. New York: Lee & Shepard, 1995.
- Watson, John. "This Dynamic Planet." US Geological Survey. 6 December. 2004 [1]
