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- Slalama_Slope abstract "Slalama Slope (72°31′S 3°25′W) is a steep ice slope on the northeast side of Borg Mountain, in the Borg Massif of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Slalama (the slalom). This article incorporates public domain material from the United States Geological Survey document "Slalama Slope" (content from the Geographic Names Information System).".
- Slalama_Slope wikiPageID "29629379".
- Slalama_Slope wikiPageRevisionID "492617359".
- Slalama_Slope hasPhotoCollection Slalama_Slope.
- Slalama_Slope subject Category:Ice_slopes_of_Queen_Maud_Land.
- Slalama_Slope subject Category:Princess_Martha_Coast.
- Slalama_Slope point "-72.51666666666667 -3.4166666666666665".
- Slalama_Slope type GeologicalFormation109287968.
- Slalama_Slope type IceSlopesOfQueenMaudLand.
- Slalama_Slope type Object100002684.
- Slalama_Slope type PhysicalEntity100001930.
- Slalama_Slope type Slope109437454.
- Slalama_Slope type YagoGeoEntity.
- Slalama_Slope type YagoPermanentlyLocatedEntity.
- Slalama_Slope type SpatialThing.
- Slalama_Slope comment "Slalama Slope (72°31′S 3°25′W) is a steep ice slope on the northeast side of Borg Mountain, in the Borg Massif of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Slalama (the slalom). This article incorporates public domain material from the United States Geological Survey document "Slalama Slope" (content from the Geographic Names Information System).".
- Slalama_Slope label "Slalama Slope".
- Slalama_Slope sameAs m.0fpj7wb.
- Slalama_Slope sameAs 6625500.
- Slalama_Slope sameAs Q7538531.
- Slalama_Slope sameAs Q7538531.
- Slalama_Slope sameAs Slalama_Slope.
- Slalama_Slope lat "-72.51666666666667".
- Slalama_Slope long "-3.4166666666666665".
- Slalama_Slope wasDerivedFrom Slalama_Slope?oldid=492617359.
- Slalama_Slope isPrimaryTopicOf Slalama_Slope.