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- Q3050115 subject Q8179598.
- Q3050115 subject Q9112603.
- Q3050115 abstract "El Negrillar is a volcanic field in the Andes. Located west of the Cordón de Púlar, it generated cinder cones and andesitic lava flows. The volcanic field may be of Holocene age. Parts of the Socompa debris avalanche overlie the field. The cones have volumes of less than 0.1 cubic kilometres (0.024 cu mi) and lava flows are thin and branch out dendritically. Lava flows are up to 100 metres (330 ft) thick and overlie the Salín Formation. The origin of the more basic lavas of this field has been explained with olivine differentiation.".
- Q3050115 elevation "3500.0".
- Q3050115 otherName "Negros de Aras".
- Q3050115 thumbnail El_Negrillar.jpg?width=300.
- Q3050115 wikiPageWikiLink Q1806785.
- Q3050115 wikiPageWikiLink Q181908.
- Q3050115 wikiPageWikiLink Q22693.
- Q3050115 wikiPageWikiLink Q25445.
- Q3050115 wikiPageWikiLink Q422765.
- Q3050115 wikiPageWikiLink Q519105.
- Q3050115 wikiPageWikiLink Q5456.
- Q3050115 wikiPageWikiLink Q8179598.
- Q3050115 wikiPageWikiLink Q9112603.
- Q3050115 elevationM "3500".
- Q3050115 name "El Negrillar".
- Q3050115 otherName "Negros de Aras".
- Q3050115 point "-24.18 -68.25".
- Q3050115 type Mountain.
- Q3050115 type Place.
- Q3050115 type Location.
- Q3050115 type Mountain.
- Q3050115 type NaturalPlace.
- Q3050115 type Place.
- Q3050115 type Thing.
- Q3050115 type SpatialThing.
- Q3050115 type Q8502.
- Q3050115 comment "El Negrillar is a volcanic field in the Andes. Located west of the Cordón de Púlar, it generated cinder cones and andesitic lava flows. The volcanic field may be of Holocene age. Parts of the Socompa debris avalanche overlie the field. The cones have volumes of less than 0.1 cubic kilometres (0.024 cu mi) and lava flows are thin and branch out dendritically. Lava flows are up to 100 metres (330 ft) thick and overlie the Salín Formation.".
- Q3050115 label "El Negrillar".
- Q3050115 lat "-24.18".
- Q3050115 long "-68.25".
- Q3050115 depiction El_Negrillar.jpg.
- Q3050115 name "El Negrillar".