Nemesis Glacier (70°32′S 67°30′E / 70.533°S 67.500°E / -70.533; 67.500) is a large glacier which flows northeast through the center of the Aramis Range, Prince Charles Mountains. Discovered in January 1957 by ANARE (Australian National Antarctic Research Expeditions) southern party under W.G. Bewsher, and named after Homer's Nemesis because considerable difficulty was experienced in traversing the region due to the glacier.

• List of glaciers in the Antarctic
• Glaciology

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• Ian C. W. Fitzsimons, The Metamorphic Histories of some Proterozoic Granulites from East Antarctica, January 1991
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• Hultzsch, N., Wagner, B., Diekmann, B., & White, D. (2008), Mineralogical implications for the Late Pleistocene glaciation in Amery Oasis, East Antarctica, from a lake sediment core., Antarctic Science, 20(2), 169–172. https://doi:10.1017/S0954102007000880

• Nemesis Glacier on USGS website
• Nemesis Glacier on AADC website
• Nemesis Glacier on SCAR website
• Nemesis Glacier long term updated weather forecast

•  This article incorporates public domain material from "Nemesis Glacier". Geographic Names Information System. United States Geological Survey.