|
Original Article |
Department of Earth Sciences, HB 6105, Dartmouth College, Hanover, NH 03755, USA (e-mail: W.B.Dade@Dartmouth.edu)
The geometries of alluvial fans and their upland catchments subject to known rates of basin subsidence V and upland precipitation P, respectively, are compared with predictions from a quantitative analysis of an idealized landscape. We find that the dimensionless ratio V/P explains systematic trends in relative fan size and source catchment relief previously reported from environmentally wide-ranging regions worldwide, and contributes to the interpretation of recently reported observations of fan-like phenomena on Mars.