geo.wikisort.org - MountainsThe 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]
Mountains in Antarctica
Gothic Mountains in Antarctica
Key mountains
- Altar Peak (86°4′S 150°23′W) is a peak (1,780 m) located 1 nautical mile (1.9 km) east-southeast of Mount Harkness. The feature was first visited in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. The descriptive name was suggested by Edmund Stump, leader of a United States Antarctic Research Program (USARP)-Arizona State University geological party which studied this peak, 1987-88.[2]
- Grizzly Peak (86°00′S 150°00′W) is a peak rising to 2,200 m on the southwest flank of Mount Zanuck. The feature was visited in December 1934 by the Byrd Antarctic Expedition geological party and was included in "Darryl Zanuck Mountain." The granite of this peak is highly jointed and fairly bristles with small spires, suggestive of the coat of a grizzly bear.[3]
- Mount Zanuck (85°58′S 151°10′W) is a mountain about 8 kilometres (5 mi) long surmounted by three sharp peaks in an east-west line, the highest of which rises to 2,525 metres (8,284 ft). The feature stands at the south side of Albanus Glacier at the point where the latter joins Scott Glacier. Discovered by Byrd on the Byrd Antarctic Expedition flight to the South Pole in November 1929. The mountain was visited in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. Named by Byrd for Darryl F. Zanuck, official of Twentieth Century-Fox Pictures, who assisted the Byrd Antarctic Expedition, 1933–35, in assembling motion-picture records, and later supplied the United States Antarctic Service (USAS), 1939–41, with motion-picture projectors.[4]
- Zanuck East Peak (85°57′S 150°53′W) is the easternmost of the three high peaks that rise from Mount Zanuck massif. The peak was discovered and mapped by the geological party of the Byrd Antarctic Expedition, 1933–35, led by Quin Blackburn. The name was applied in association with Mount Zanuck by members of New Zealand Geological Survey Antarctic Expedition (NZGSAE) who climbed the peak in the 1969-70 season.[5]
Features
Geographical features include:
References
- "Gothic Mountains". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2010-10-17.
- "Altar Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2010-09-22.
- "Grizzly Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-02-28.
- "Mount Zanuck". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2008-03-20.
- "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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