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Abstract

The Appalachian Highlands consist of the Piedmont, Blue Ridge, Valley and Ridge, and Appalachian Plateau physiographic provinces (Fenneman, 1938) (Fig. 1). The Interior Low Plateau province is also included with this discussion of the Appalachian Highlands. The Quaternary geology of the unglaciated Appalachians is challenging because of the complexity of its montane landscapes and limited datable deposits. Surficial deposits in the Appalachians are difficult to date by radiocarbon because of relatively low sedimentation rates that, together with a high oxidation rate, result in poor preservation of organic material except below the water table. Only a handful of numerical dates older than late Wisconsin exist from deposits of alluvium and colluvium. Moreover, alluvial terraces, as well as colluvial deposits, are generally discontinuous in distribution, poorly exposed, and have considerable soil and vegetation cover, hindering reliable stratigraphic and morphologic correlation. Beyond the range of radiocarbon dating, correlation is even more tentative owing to postdepositional erosion and dissection of geomorphic surfaces, and to the lack of numerical-age-dating techniques applicable to these surficial deposits. Tephra are unknown.

Knowledge of late Quaternary climatic changes in the Appalachian region, from palynological study and radiocarbon dating of lacustrine and peat deposits, is relatively more advanced than stratigraphie investigations. Sinkholes formed in carbonate terrains provide continuous paleoenvironmental and paleovegetation records extending back through middle Wisconsin time. This paleoecological knowledge provides a tentative framework for interpreting landscape development during the Quaternary. However, well-dated palynological sequences from lacustrine sites commonly cannot be correlated directly with nonlacustrine

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