- Andesite line
The andesite line is the most significant regional
geologic distinction in thePacific Ocean basin. It separates themafic basalt icvolcanic rocks of the Central Pacific Basin from the partially submerged continental areas of morefelsic andesitic volcanic rock on its margins. The andesite line parallels thesubduction zone s and deepoceanic trench es around the Pacific basin. It is the surface expression of melting within and above the plunging subducting slab. It follows the western edge of the islands offCalifornia and passes south of the Aleutian arc, along the eastern edge of theKamchatka Peninsula , theKuril Islands , Japan, theMariana Islands , theSolomon Islands , andNew Zealand 'sNorth Island . The dissimilarity continues northeastward along the western edge of theAndes mountains of South America to Mexico, returning then to the islands off California. Indonesia, the Philippines, Japan, New Guinea, and New Zealand—all eastward extensions of the continental blocks of Australia and Asia—lie outside the andesite line.Within the closed loop of the andesite line are most of the deep troughs, submerged volcanic mountains, and oceanic volcanic islands that characterize the
Pacific basin . It is here that basaltic lavas gently flow out of rifts to build huge dome-shaped volcanic mountains whose eroded summits form island arcs, chains, and clusters. Outside the andesite line, volcanism is of the explosive type. ThePacific Ring of Fire runs parallel to the line and is the world's foremost belt of explosive volcanism.The term "andesite line" predates the geologic understanding of
plate tectonics . The term was first used in 1912 byNew Zealand geologistPatrick Marshall to describe the distinct structural and volcanologic boundary extending from east of New Zealand to Fiji and north of the New Hebrides and the Solomon Islands.References
* [http://www.dnzb.govt.nz/dnzb/default.asp?Find_Quick.asp?PersonEssay=3M44 Watters, W. A. 'Marshall, Patrick 1869 - 1950'. Dictionary of New Zealand Biography, updated 7 April 2006]
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