Characterization of Wet Pine Flats on Mineral Soil in the Southeastern United StatesWet (hydric) flats include wetlands on mineral soils. In the southeastern United States wet pine flats occur on the subdued and poorly dissected interfluvial marine terraces of the coastal plain. Hydric conditions have developed on these interfluvial flats primarily in response to abundant rainfall and slow drainage associated with a landscape of low relief. Based on the extent of hydric soils mapped in each state, wet flats may comprise 20-30 percent of the coastal plain landscape from southeastern Virginia to southeastern Texas. Wet flats on mineral soils are primarily associated with poorly drained sandy and loamy Ultisols and Alfisols (mostly Aquults and Aqualfs, respectively), but also are associated with various Spodosols, Inceptisols, and Mollisols. Wet Pine Flats are characterized by an open savanna of shade-intolerant forbs and graminoids with widely scattered pines. Guidebooks Web Date: October 1997 |