| Abstract: | A flume study indicates that grainflow on slipfaces accounts for most cross-strata formed in unidirectional, shallow-water flows. The slipfaces studied were on small megaripples and delta-like steps (0.06-0.28 m high). During intermittent avalanching, at relatively low flow velocities, periods between avalanches were marked by grainfall onto the slipface, the intensity of which was greatest near the brink of the slipface and increased with current velocity. The lee eddy proved very significant in slipface processes by redistributing grainfall sediments and both promoting and impeding grainflow. -from Authors |
| Genre: | Article |
| ProdID: | 70014523 |
| Citation Author: | Hunter, R. E.; Kocurek, G. |
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| Citation End Page: | 394 |
| Citation Issue: | 3 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Sedimentary Petrology |
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| Citation Number Of Pages: | 8 |
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| Citation Search Results Text: | An experimental study of subaqueous slipface deposition.; 1986; Article; Journal; Journal of Sedimentary Petrology; Hunter, R. E.; Kocurek, G. |
| Citation Start Page: | 387 |
| Citation Volume: | 56 |
| Citation Year: | 1986 |
| Type: | citation/reference |
| Text: | An experimental study of subaqueous slipface deposition.; 1986; Article; Journal; Journal of Sedimentary Petrology; Hunter, R. E.; Kocurek, G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1986 00:00 -0600 |
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