Article · Wikipedia archive · Last revised Jun 27, 2026

Evans Ice Stream

The Evans Ice Stream is a large ice stream draining from Ellsworth Land, between Cape Zumberge and Fowler Ice Rise, into the western part of the Ronne Ice Shelf. Mills Glacier flows adjacently into the ice stream from the southwest side. The feature was recorded on 5 February 1974 in Landsat imagery. It was named by the UK Antarctic Place-Names Committee for Stanley Evans, a British physicist who, starting in 1961, developed apparatus for radio echo sounding of icecaps and glaciers from aircraft; he carried out upper atmosphere research at Brunt Ice Shelf, 1956–57.

Last revised
Jun 27, 2026
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Evans Ice Stream
Location of Evans Ice Stream in Antarctica
Typeice stream
LocationEllsworth Land
Coordinates76°00′S 78°00′W / 76.000°S 78.000°W / -76.000; -78.000
Thicknessunknown
TerminusFilchner-Ronne Ice Shelf
Statusunknown

The Evans Ice Stream is a large ice stream draining from Ellsworth Land, between Cape Zumberge and Fowler Ice Rise, into the western part of the Ronne Ice Shelf. Mills Glacier flows adjacently into the ice stream from the southwest side.1 The feature was recorded on 5 February 1974 in Landsat imagery. It was named by the UK Antarctic Place-Names Committee for Stanley Evans, a British physicist who, starting in 1961, developed apparatus for radio echo sounding of icecaps and glaciers from aircraft; he carried out upper atmosphere research at Brunt Ice Shelf, 1956–57.2

See also

See also

Further reading

Further reading

External links
References

References

 This article incorporates public domain material from "Evans Ice Stream". Geographic Names Information System. United States Geological Survey.

76°S 78°W / 76°S 78°W / -76; -78