| Abstract: | A large avalanche (21 square kilometers) at the Apollo 17 landing site moved out several kilometers over flat ground beyond its source slope. If not triggered by impacts, then it was as "efficient" as terrestrial avalanches attributed to air-cushion sliding. Evidently lunar avalanches are able to flow despite the lack of lubricating or cushioning fluid. |
| Genre: | Article |
| ProdID: | 70010988 |
| Citation Author: | Howard, K. A. |
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| Citation End Page: | 1055 |
| Citation Issue: | 4090 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Avalanche mode of motion: Implications from lunar examples; 1973; Article; Journal; Science; Howard, K. A. |
| Citation Start Page: | 1052 |
| Citation Volume: | 180 |
| Citation Year: | 1973 |
| Type: | citation/reference |
| Text: | Avalanche mode of motion: Implications from lunar examples; 1973; Article; Journal; Science; Howard, K. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Mon, 1 Jan 1973 00:00 -0600 |
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