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- Golubkina_(crater) abstract "Golubkina is a crater on Venus.Golubkina is characterized by terraced inner walls and a central peak, typical of large impact craters on the Earth, Moon and Mars. The terraced inner walls form at late stages in the formation of an impact crater, due to collapse of the initial cavity formed by the meteorite impact. The central peak forms due to rebound of the inner crater floor.The smoothness of the floor may be due to pounding of volcanic lava flows in the crater floor. The rough, blocky morphology of the crater ejecta and the sharp terraced crater wall suggest that this feature is relatively young.".
- Golubkina_(crater) diameter "28000.0".
- Golubkina_(crater) location Venus.
- Golubkina_(crater) thumbnail Golubkina_f.jpg?width=300.
- Golubkina_(crater) wikiPageID "4674510".
- Golubkina_(crater) wikiPageRevisionID "579888630".
- Golubkina_(crater) caption "Radar image of Golubkina combining high and low resolution data".
- Golubkina_(crater) diameter "28.0".
- Golubkina_(crater) eOrW "E".
- Golubkina_(crater) eponym Anna_Golubkina.
- Golubkina_(crater) hasPhotoCollection Golubkina_(crater).
- Golubkina_(crater) latitude "60.3".
- Golubkina_(crater) longitude "286.5".
- Golubkina_(crater) nOrS "N".
- Golubkina_(crater) subject Category:Impact_craters_on_Venus.
- Golubkina_(crater) type GeologicalFormation109287968.
- Golubkina_(crater) type ImpactCratersOnVenus.
- Golubkina_(crater) type Object100002684.
- Golubkina_(crater) type PhysicalEntity100001930.
- Golubkina_(crater) type VolcanicCrater109472413.
- Golubkina_(crater) type YagoGeoEntity.
- Golubkina_(crater) type YagoPermanentlyLocatedEntity.
- Golubkina_(crater) type Crater.
- Golubkina_(crater) type NaturalPlace.
- Golubkina_(crater) type Place.
- Golubkina_(crater) type Wikidata:Q532.
- Golubkina_(crater) type Place.
- Golubkina_(crater) type Location.
- Golubkina_(crater) comment "Golubkina is a crater on Venus.Golubkina is characterized by terraced inner walls and a central peak, typical of large impact craters on the Earth, Moon and Mars. The terraced inner walls form at late stages in the formation of an impact crater, due to collapse of the initial cavity formed by the meteorite impact. The central peak forms due to rebound of the inner crater floor.The smoothness of the floor may be due to pounding of volcanic lava flows in the crater floor.".
- Golubkina_(crater) label "Golubkina (crater)".
- Golubkina_(crater) label "Golubkina (cratère)".
- Golubkina_(crater) label "戈卢布金娜撞击坑".
- Golubkina_(crater) sameAs Golubkina_(cratère).
- Golubkina_(crater) sameAs m.03hfvzj.
- Golubkina_(crater) sameAs Q3110331.
- Golubkina_(crater) sameAs Q3110331.
- Golubkina_(crater) sameAs Golubkina_(crater).
- Golubkina_(crater) wasDerivedFrom Golubkina_(crater)?oldid=579888630.
- Golubkina_(crater) depiction Golubkina_f.jpg.
- Golubkina_(crater) isPrimaryTopicOf Golubkina_(crater).