@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_00000279	rdf:type	owl:Class .
@prefix xsd:	<http://www.w3.org/2001/XMLSchema#> .
@prefix rdfs:	<http://www.w3.org/2000/01/rdf-schema#> .
ns1:ENVO_00000279	rdfs:label	"saline pan"^^xsd:string ;
	rdfs:subClassOf	ns1:ENVO_00000017 ,
		ns1:ENVO_01000296 .
@prefix obo:	<http://www.geneontology.org/formats/oboInOwl#> .
ns1:ENVO_00000279	obo:hasDbXref	"Geonames:L.SALT"^^xsd:string ,
		"SWEETRealm:SaltFlat"^^xsd:string ,
		"TGN:21506"^^xsd:string ,
		"TGN:21459"^^xsd:string ,
		"EcoLexicon:salt_pan"^^xsd:string ;
	obo:hasExactSynonym	"salt pan"^^xsd:string ,
		"SALT PAN"^^xsd:string ;
	obo:hasRelatedSynonym	"salt flat"^^xsd:string ,
		"salt area"^^xsd:string ;
	ns1:IAO_0000115	"A flat expanse of ground covered with salt and other minerals, usually shining white under the sun. A salt pan is formed where water pools. A saline pan would be a lake or a pond if it were located in a climate where the rate of water evaporation were not faster than the rate of water precipitation, i.e., if it were not in a desert. If the water is unable to drain into the ground, it remains on the surface until it evaporates, leaving behind whatever minerals were dissolved. Over thousands of years, the minerals (usually salts) accumulate on the surface."^^xsd:string ;
	obo:hasOBONamespace	"ENVO"^^xsd:string ;
	obo:id	"ENVO:00000279"^^xsd:string .