Skip to Main Content
U.S. Forest Service
Caring for the land and serving people

United States Department of Agriculture

Home > Search > Publication Information

  1. Share via EmailShare on FacebookShare on LinkedInShare on Twitter
    Dislike this pubLike this pub
    Author(s): Bradley Suther; David Leigh; George Brook
    Date: 2011
    Source: Southeastern Geology 48(2):73-93
    Publication Series: Scientific Journal (JRNL)
    PDF: View PDF  (851.14 KB)

    Description

    An optically-stimulated luminescence (OSL) and radiocarbon chronology is presented for fluvial terraces of the Little River, a tributary to the Cape Fear River that drains 880 km2 of the Sandhills Province of the upper Coastal Plain of North Carolina. This study differs from previous work in the southeastern Atlantic Coastal Plain in that numerical age estimates are provided for all terraces in the valley of mappable extent by direct dating of fluvial sediments. The Little River valley contains a floodplain and five fluvial terraces with average heights above modern river bed level that range from 3.0 m (T1) to 29.0 m (T5b). Dating indicates the floodplain has a late Holocene (1.3 ± 0.3 ka) to historical age while terraces range in age from 9.9 ± 2.0 ka (T1) to 94.0 ± 15.9 ka (T5b). Age separation of the six fluvial surfaces is corroborated by distinct differences in soil morphology and chemistry. Terrace heights above modern river level and terrace ages indicate a long-term net incision rate of 0.29 mm/yr during the last 100 ka. This rate is nearly an order of magnitude higher than late Pleistocene uplift rates reported for the Cape Fear River valley in the 1980s, based on age estimates for the Wando Formation. However, the 0.29 mm/yr rate is consistent with OSL and radiocarbon dates reported from terraces in the adjacent Pee Dee River valley. Together, these data refine the ages assigned to fluvial facies of the Wando terrace and suggest it is composed of multiple fluvial deposits with a wide range of late Pleistocene ages. The long-term net incision rate of the Little River is consistent with the range of neotectonic uplift rates reported for this region. Scrutiny of the inter-terrace ages indicates that Little River terraces may reflect short-term aggradation in response to periodic climate-mediated increases in sediment supply that is compensated by longterm incision in response to neotectonic uplift.

    Publication Notes

    • You may send email to pubrequest@fs.fed.us to request a hard copy of this publication.
    • (Please specify exactly which publication you are requesting and your mailing address.)
    • We recommend that you also print this page and attach it to the printout of the article, to retain the full citation information.
    • This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.

    Citation

    Suther, Bradley E.; Leigh, David S.; Brook, George A. 2011. Fluvial terraces of the Little River Valley, Atlantic Coastal Plain, North Carolina. Southeastern Geology 48(2):73-93.

    Related Search


    XML: View XML
Show More
Show Fewer
Jump to Top of Page