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Subject Item
_:vb1217213
rdf:type
owl:Axiom
obo:hasDbXref
Wikipedia:Obsequent_stream
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n3:IAO_0000115
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A stream whose course follows the original relief, but at a lower level than the original slope (e.g., flows down a course determined by the underlying strata in the same direction). These streams develop later and are generally a tributary to a subsequent stream.