Difference between revisions of "Subduction Zone"

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(New page: A '''Subduction zone''' is the place where two lithosphere plates come together, one riding over the other. Most volcanoes on land occur parallel to and inland ...)
 
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A '''Subduction zone''' is the place where two [[lithosphere]] plates come together, one riding over the other. Most [[volcano|volcanoes]] on [[land]] occur [[parallel]] to and [[inland]] from the [[boundary]] between the two plates. <ref>[http://vulcan.wr.usgs.gov/Glossary/volcano_terminology.html Glossary of Volcano and Related Terminology (Teacher's Packet)]</ref>
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A '''Subduction zone''' is the place where two [[lithosphere]] plates come together, one riding over the other. Most [[volcano]]es on [[land]] occur [[parallel]] to and [[inland]] from the [[boundary]] between the two plates.<ref>[http://vulcan.wr.usgs.gov/Glossary/volcano_terminology.html Glossary of Volcano and Related Terminology (Teacher's Packet)]</ref>
  
 
==References==
 
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[[Category:Geology]]

Latest revision as of 19:50, July 13, 2016

A Subduction zone is the place where two lithosphere plates come together, one riding over the other. Most volcanoes on land occur parallel to and inland from the boundary between the two plates.[1]

References