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Abstract
Three sand units are recognized on the basis of bedforms, topographic expression, and soil development. Preliminary age limits for the three units, based on 26 numerical ages, are 22.5-9 ka, 8-1 ka, and 1.0-0.15 ka. The middle unit is the product of multiple episodes of eolian activity that are not yet accurately dated. Loess is widespread but thin (generally < 2.4 m). Three units - middle Pleistocene, late Pleistocene, and Holocene - are recognized on the basis of differences in soil-profile development and stratigraphic position. -from Author
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Spatial and temporal patterns of late Quaternary eolian deposition, eastern Colorado, USA |
| Series title | Quaternary Science Reviews |
| Volume | 14 |
| Issue | 2 |
| Year Published | 1995 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Quaternary Science Reviews |
| First page | 155 |
| Last page | 177 |
| Google Analytic Metrics | Metrics page |