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Divergent boundary information


Continental-continental divergent/constructive boundary
Oceanic divergent boundary: mid-ocean ridge (cross-section/cut-away view)

In plate tectonics, a divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. Divergent boundaries within continents initially produce rifts, which eventually become rift valleys. Most active divergent plate boundaries occur between oceanic plates and exist as mid-oceanic ridges.[1][2]

Current research indicates that complex convection within the Earth's mantle allows material to rise to the base of the lithosphere beneath each divergent plate boundary.[3] This supplies the area with huge amounts of heat and a reduction in pressure that melts rock from the asthenosphere (or upper mantle) beneath the rift area, forming large flood basalt or lava flows. Each eruption occurs in only a part of the plate boundary at any one time, but when it does occur, it fills in the opening gap as the two opposing plates move away from each other.

Over millions of years, tectonic plates may move many hundreds of kilometers away from both sides of a divergent plate boundary. Because of this, rocks closest to a boundary are younger than rocks further away on the same plate.

  1. ^ Langmuir, Charles H.; Klein, Emily M.; Plank, Terry (2013). "Petrological Systematics of Mid-Ocean Ridge Basalts: Constraints on Melt Generation Beneath Ocean Ridges". Mantle Flow and Melt Generation at Mid-Ocean Ridges. Geophysical Monograph Series. pp. 183–280. doi:10.1029/GM071p0183. hdl:10161/8316. ISBN 9781118663875.
  2. ^ Sinton, John M.; Detrick, Robert S. (1992). "Mid-ocean ridge magma chambers". Journal of Geophysical Research. 97 (B1): 197. Bibcode:1992JGR....97..197S. doi:10.1029/91JB02508.
  3. ^ Toshiro Tanimoto; Thorne Lay (November 7, 2000). "Mantle dynamics and seismic tomography". Proc. Natl. Acad. Sci. U.S.A. 97 (23): 12409–10. Bibcode:2000PNAS...9712409T. doi:10.1073/pnas.210382197. PMC 34063. PMID 11035784.

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occur mainly in areas where the crust is being extended such as a divergent boundary. Earthquakes associated with normal faults are generally less than...

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