| 词条 | Institute Ice Stream |
| 释义 |
| child = | name = Institute Ice Stream | other_name = | photo = | photo_alt = | photo_caption = | map = Antarctica | map_width = | map_alt = | map_caption = Location of Institute Ice Stream in Antarctica | type = | location = Queen Elizabeth Land | coordinates = {{coord|82|S|75|W|region:AQ|format=dms|display=inline}} | coords_ref = | area = | length = | width = | thickness = unknown | elevation_max = | elevation_min = | terminus = Filchner-Ronne Ice Shelf | status = unknown | embedded = }} The Institute Ice Stream ({{Coord|82|S|75|W|source:GNIS|display=inline,title}}) is an ice stream flowing north into the Ronne Ice Shelf, Antarctica, southeast of Hercules Inlet. The feature was traversed by the United States Antarctic Research Program (USARP) Ellsworth–Byrd Seismic Party, 1958–59, and the USARP – University of Wisconsin Seismic Party, 1963–64. It was delineated by the Scott Polar Research Institute – National Science Foundation – Technical University of Denmark airborne radio echo sounding program, 1967–79, and in association with Foundation Ice Stream and Support Force Glacier, named after the Scott Polar Research Institute, Cambridge, England. See also
References}}{{usgs-gazetteer|id=7326}}{{Portalbar|Antarctica|Geography}}{{Glaciers in the Antarctic}}{{QueenElizabethLand-geo-stub}}{{Glaciology-stub}} 2 : Ice streams of Queen Elizabeth Land|Filchner-Ronne Ice Shelf |
| 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。