| Abstract: | Hydrologic, geologic, geomorphic, and mass-balance data suggest that most of the approx. 30 000 playa lake basins on the Southern High Plains have developed by a combination of dissolution of caliche and piping of surface material into the unsaturated zone rather than by eolian processes as has generally been stated.-from Authors |
| Genre: | Article |
| ProdID: | 70014859 |
| Citation Author: | Wood, W. W.; Osterkamp, W. R. |
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| Citation End Page: | 230 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geological Society of America Bulletin |
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| Citation Number Of Pages: | 7 |
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| Citation Search Results Text: | Playa-lake basins on the Southern High Plains of Texas and New Mexico: Part II. A hydrologic model and mass-balance arguments for their development.; 1987; Article; Journal; Geological Society of America Bulletin; Wood, W. W.; Osterkamp, W. R. |
| Citation Start Page: | 224 |
| Citation Volume: | 99 |
| Citation Year: | 1987 |
| Type: | citation/reference |
| Text: | Playa-lake basins on the Southern High Plains of Texas and New Mexico: Part II. A hydrologic model and mass-balance arguments for their development.; 1987; Article; Journal; Geological Society of America Bulletin; Wood, W. W.; Osterkamp, W. R. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1987 00:00 -0600 |
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