| 词条 | Charybdis Icefalls |
| 释义 |
The Charybdis Icefalls ({{Coord|70|51|S|161|10|E|source:GNIS|display=inline,title}}) are a large group of crevassed icefalls in the lower portion of Harlin Glacier, where it descends notably to join the Rennick Glacier at Victoria Land in Antarctica. The feature is nourished in part by the Lovejoy Glacier which flows eastward parallel to the Harlin Glacier's north side and coalesces with it before reaching the icefalls. It was first mapped by the United States Geological Survey (1962–63) and the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1963–64), and named by the latter after Charybdis, the fearsome whirlpool monster of Greek mythology. The icefalls lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. References
3 : Icefalls of Antarctica|Landforms of Victoria Land|Pennell 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。