Johns Knoll

Johns Knoll (

71°59′S 7°59′E / 71.983°S 7.983°E / -71.983; 7.983Coordinates: 71°59′S 7°59′E / 71.983°S 7.983°E / -71.983; 7.983) is a crevassed ice knoll (apparently the ice surface reflection of the underlying rock) in the lower part of Vinje Glacier in Queen Maud Land, Antarctica. It was mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Johnsbaen (John's sunken rock) for , a radio technician with the expedition.^[1]

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 This article incorporates public domain material from the United States Geological Survey document: "Johns Knoll". (content from the Geographic Names Information System)