| 词条 | Barracouta Ridge |
| 释义 |
Barracouta Ridge ({{Coord|85|20|S|166|35|W|source:GNIS|display=inline,title}}) is a long jagged ridge which terminates on the north in Webster Knob. The ridge is an extension from the base of Mount Fridtjof Nansen into the head of Strom Glacier, Queen Maud Mountains. It was discovered and visited in 1929 by the geological party under Laurence Gould of the Byrd Antarctic Expedition, 1928–30, and was climbed by geologists of the Southern Party of the New Zealand Geological Survey Antarctic Expedition, 1963–64. The descriptive name applied by the Southern Party derives from the appearance of the toothlike pinnacle along the crest of the ridge, reminiscent of a Barracouta. References
2 : Nunataks of the Ross Dependency|Dufek Coast |
| 随便看 |
|
开放百科全书收录14589846条英语、德语、日语等多语种百科知识，基本涵盖了大多数领域的百科知识，是一部内容自由、开放的电子版国际百科全书。