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Plunket Point (85°5′S 167°6′E) is a conspicuous rock point marking the northern end of the Dominion Range and the confluence of the Beardmore and Mill Glaciers. Discovered by the British Antarctic Expedition (1907–09) and named for Lord Plunket, at that time Governor of New Zealand.

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

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[de] Plunket Point

Der Plunket Point ist ein Felssporn in der antarktischen Ross Dependency. Am Nordende der Dominion Range markiert er den Ort des Zusammenflusses von Beardmore- und Mill-Gletscher.

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- [en] Plunket Point

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