<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:skos="http://www.w3.org/2004/02/skos/core#" xmlns:gcmd="https://gcmd.earthdata.nasa.gov/kms#" xmlns:dcterms="http://purl.org/dc/terms/" xml:base="https://gcmd.earthdata.nasa.gov/kms/concept/">
  <gcmd:gcmd>
    <gcmd:termsOfUse>https://cdn.earthdata.nasa.gov/conduit/upload/5182/KeywordsCommunityGuide_Baseline_v1_SIGNED_FINAL.pdf</gcmd:termsOfUse>
    <gcmd:keywordVersion>23.6</gcmd:keywordVersion>
    <gcmd:schemeVersion>2026-03-19T10:41:57.720Z</gcmd:schemeVersion>
    <gcmd:viewer>https://gcmd.earthdata.nasa.gov/KeywordViewer/scheme/sciencekeywords/a91a00f7-05ed-4633-9fac-1772a48b6342</gcmd:viewer>
  </gcmd:gcmd>
  <skos:Concept rdf:about="a91a00f7-05ed-4633-9fac-1772a48b6342">
    <skos:broader rdf:resource="c16bda61-353b-4668-af2f-bbb98785b6fa"/>
    <skos:prefLabel xml:lang="en">CONTINENTAL MARGINS</skos:prefLabel>
    <gcmd:reference gcmd:text="Alyn C. Duxbury, Alison B. Duxbury, and Keith A. Sverdrup.  An Introduction to the World&apos;s Oceans. 6th edition. McGraw-Hill Higher Education, 2000." xml:lang="en"/>
    <skos:definition xml:lang="en">The ocean floor from the shore of a continent to the abyssal plain.  Thecontinent margin is the zone separating the continents from the deep-seabottom, usually subdivided into the continental shelf, slope, and rise.  
They are two basic types of continental margins: passive, or Atlantic, marginsand active, or Pacific, margins.  Passive margins have little seismic orvolcanic activity and form when continents are rifted apart, creating a newocean basin between them.  Active margins are tectonically active and are mostoften associated with plate convergence and subduction.</skos:definition>
    <skos:inScheme rdf:resource="https://gcmd.earthdata.nasa.gov/kms/concepts/concept_scheme/sciencekeywords"/>
  </skos:Concept>
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