@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> .
@prefix ns0: <http://rdf-vocabulary.ddialliance.org/xkos#> .

<http://www.irandoc.acir/onto/irandoc/SWEETT20120>
  skos:prefLabel "فوران آتشفشانی"@fa, "volcanic eruption"@en ;
  a <http://www.irandoc.ac.ir/onto/irandoc-meta/Concept>, skos:Concept ;
  skos:narrower <http://www.irandoc.acir/onto/irandoc/SWEETT17512> .

<http://rdf-vocabulary.ddialliance.org/xkos#Definitions> rdfs:label "تعاریف"@fa, "Definitions"@en .
<http://www.irandoc.acir/onto/irandoc/SWEETT17512>
  skos:broader <http://www.irandoc.acir/onto/irandoc/SWEETT20120> ;
  skos:prefLabel "فوران پلئه‌ای (نوعی فوران آتشفشانی)"@fa, "peleean eruption"@en ;
  ns0:Obsolete "false" ;
  ns0:Definitions "In a Peléan eruption or nuée ardente (glowing cloud) eruptions a large amount of gas, dust, ash, and lava fragments are blown out of a central crater, fall back, and form avalanches that move downslope at speeds as great as 160 km per hour. These eruptions are usually associated with silicic magmas. A name for some pyroclastic flows is nuée ardente (French for ‘glowing cloud’); this was first used to describe the disastrous 1902 eruption of Mount Pelée on Martinique.[3] These pyroclastic flows glowed red in the dark. [Wikipedia]" ;
  a <http://www.irandoc.ac.ir/onto/irandoc-meta/Concept>, skos:Concept .

ns0:Obsolete rdfs:label "منسوخ"@fa, "Obsolete"@en .