Progressive changes in the morphology of fluvial terraces and scarps along the Rappahannock River, Virginia.
Earth Surface Processes and Landforms
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Abstract
Progressive geomorphic changes in the flight of fluvial terraces along the Rappahannock River, Virginia, provide a framework for analysing the effect of time on landforms. Indices of terrace preservation, especially drainage densities and area to perimeter ratios, show systematic changes with terrace age. Higher scarps tend to have steeper slopes and, for a given scarp height, older scarps tend to have gentler slopes. Depositional features such as bars and channels with 1-3m of relief are preserved on terraces on the order of 105 yr old.-from Author
Suggested Citation
Colman, S.M., 1983, Progressive changes in the morphology of fluvial terraces and scarps along the Rappahannock River, Virginia.: Earth Surface Processes and Landforms, v. 8, no. 3, p. 201-212, https://doi.org/10.1002/esp.3290080303.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Progressive changes in the morphology of fluvial terraces and scarps along the Rappahannock River, Virginia. |
| Series title | Earth Surface Processes and Landforms |
| DOI | 10.1002/esp.3290080303 |
| Volume | 8 |
| Issue | 3 |
| Publication Date | July 18, 2006 |
| Year Published | 1983 |
| Language | English |
| Publisher | Wiley |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Earth Surface Processes and Landforms |
| First page | 201 |
| Last page | 212 |