Two million years of climate-driven cave-sediment aggradation and valley incision in the southern Ozark Plateau from Fitton Cave, northern Arkansas, USA
(2025). Two million years of climate-driven cave-sediment aggradation and valley incision in the southern Ozark Plateau from Fitton Cave, northern Arkansas, USA, Quaternary Research, 1-24, Cambridge University Press, 10.1017/qua.2025.14
Climate,Geochronology,Karst,Landscape Evolution,Speleogenesis