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Mount Vernon Harcourt, also unofficially known as Mount Harcourt, is a conical stratovolcano,[1] that rises over 1,535 meters,[1] making up part of the Hallett Peninsula extending into the Ross Sea about 375 mi (604 km) south of Mount Erebus, along with three overlapping shield volcanoes.[2]

Mount Vernon Harcourt
Mount Vernon Harcourt in 1964
Highest point
Elevation5,151 m (16,900 ft)[1]
Coordinates72°32′S 169°55′E[1]
Geography
Mount Vernon Harcourt
Hallett Peninsula, Antarctica
Geology
Age of rockOldest dated rock: 5.5 and 6.6 million years[2]
Mountain typeStratovolcano[2]

The mountain was discovered in January 1841 by Sir James Clark Ross and named by him for the Reverend William Vernon Harcourt, one of the founders of the British Association.[3]

Mount Vernon Harcourt is part of the Hallett Volcanic Province of the McMurdo Volcanic Group. Two dates have been obtained from the volcano's rock, roughly 5.5 and 6.6 million years in age. These samples are alkalic in composition.[2]


See also



References


  1.  This article incorporates public domain material from the United States Geological Survey document: "Mount Vernon Harcourt". (content from the Geographic Names Information System)
  2. "Mount Harcourt, Victorialand, Antarctica". Retrieved 23 July 2010.
  3. Mount Vernon Harcourt, New Zealand Gazetteer, retrieved 2019-04-02

На других языках


[de] Mount Vernon Harcourt

Mount Vernon Harcourt ist ein 1570 m hoher und auffällig kegelförmiger Berg an der Borchgrevink-Küste des ostantarktischen Viktorialands. Er ragt im südzentralen Teil der Hallett-Halbinsel auf.
- [en] Mount Vernon Harcourt



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