@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_00000489	rdf:type	owl:Class .
@prefix xsd:	<http://www.w3.org/2001/XMLSchema#> .
@prefix rdfs:	<http://www.w3.org/2000/01/rdf-schema#> .
ns1:ENVO_00000489	rdfs:label	"palsa"^^xsd:string ;
	rdfs:subClassOf	ns1:ENVO_00000176 ,
		_:b1217208 .
@prefix obo:	<http://www.geneontology.org/formats/oboInOwl#> .
ns1:ENVO_00000489	obo:hasDbXref	"Wikipedia:Palsa"^^xsd:string ;
	obo:hasExactSynonym	"palsa bog"^^xsd:string ;
	obo:hasRelatedSynonym	"wetland"^^xsd:string ;
	ns1:IAO_0000115	"A low oval elevation in areas with permafrost, frequently peat bogs, where a perennial ice lens has developed within the soil. A palsa consists, similarly to a pingo, of an ice core and overlying soil materials, in case of a palsa usually boggy soil. Palsas are characteristically found in areas with discontinuous permafrost and in such areas bay be the only reliable surface evidence of permafrost. A palsa needs large quantities of water for the formation of its ice core (i.e. ice lens), which is why they frequently emerge from and are bound by boggy soils, which can store enormous quantities of water in their pores. Palsas develop particularly in moorlands and are therefore also named palsamoors."^^xsd:string ;
	obo:hasOBONamespace	"ENVO"^^xsd:string ;
	obo:id	"ENVO:00000489"^^xsd:string .
_:b1217208	rdf:type	owl:Restriction ;
	owl:onProperty	ns1:BFO_0000051 ;
	owl:someValuesFrom	ns1:ENVO_01000279 .