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The Gothic Mountains is a group of mountains, 32 kilometres (20 mi) long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier, Albanus Glacier, and Griffith Glacier. The mountains were first visited in December 1934 by the Byrd Antarctic Expedition (ByrdAE) geological party led by Quin Blackburn. The name was proposed by Edmund Stump, leader of a U.S. Antarctic Research Program (USARP) - Arizona State University geological party which made investigations here in the 1980-81 season. The mountains are composed of granites which have weathered to produce a series of spires and peaks reminiscent of a Gothic cathedral.[1]

Gothic Mountains
Gothic Mountains in Antarctica

Key mountains



Features


Geographical features include:


References


  1. "Gothic Mountains". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2010-10-17.
  2. "Altar Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2010-09-22.
  3. "Grizzly Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-02-28.
  4. "Mount Zanuck". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-03-20.
  5. "Zanuck East Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-03-20.

 This article incorporates public domain material from websites or documents of the United States Geological Survey.


На других языках


[de] Gothic Mountains

Die Gothic Mountains sind eine Gebirgsgruppe in der antarktischen Ross Dependency. Mit einer Ausdehnung von 32 km Länge liegen sie als Teil des Königin-Maud-Gebirges westlich des Watson Escarpment und werden vom Scott-, dem Albanus- und dem Griffith-Gletscher begrenzt.
- [en] Gothic Mountains

[fr] Chaîne Gothic

La chaîne Gothic (en anglais : Gothic Mountains) est un massif montagneux de la chaîne de la Reine-Maud, dans la chaîne Transantarctique, en Antarctique. Son point culminant est le mont Zanuck à 2 526 mètres d'altitude. Elle est comprise entre le glacier Scott à l'ouest et son affluent le glacier Albanus au nord et à l'est. Au sud-est, elle se rattache au plateau California de l'escarpement Watson.



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