@prefix rdf:	<http://www.w3.org/1999/02/22-rdf-syntax-ns#> .
@prefix ns1:	<http://purl.obolibrary.org/obo/> .
@prefix owl:	<http://www.w3.org/2002/07/owl#> .
ns1:ENVO_00000274	rdf:type	owl:Class .
@prefix xsd:	<http://www.w3.org/2001/XMLSchema#> .
@prefix rdfs:	<http://www.w3.org/2000/01/rdf-schema#> .
ns1:ENVO_00000274	rdfs:label	"continental rise"^^xsd:string ;
	rdfs:subClassOf	ns1:ENVO_00002000 ,
		_:b1216509 .
@prefix obo:	<http://www.geneontology.org/formats/oboInOwl#> .
ns1:ENVO_00000274	obo:hasDbXref	"TGN:23110"^^xsd:string ,
		"FTT:534"^^xsd:string ,
		"Wikipedia:Continental_rise"^^xsd:string ,
		"Geonames:U.CRSU"^^xsd:string ;
	obo:hasExactSynonym	"continental rise"^^xsd:string ;
	ns1:IAO_0000115	"The continental rise is below the continental slope, but landward of the abyssal plains. Its gradient is intermediate between the slope and the shelf, on the order of 0.5-1. Extending as far as 500 km from the slope, it consists of thick sediments deposited by turbidity currents from the shelf and slope. Sediment cascades down the slope and accumulates as a pile of sediment at the base of the slope, called the continental rise."^^xsd:string ;
	obo:hasOBONamespace	"ENVO"^^xsd:string ;
	obo:id	"ENVO:00000274"^^xsd:string .
_:b1216509	rdf:type	owl:Restriction ;
	owl:onProperty	ns1:BFO_0000050 ;
	owl:someValuesFrom	ns1:ENVO_01000298 .