The plateau edge of southern Oman is used as a natural laboratory to independently test apatite fi ssion-track analysis, (U-Th)/He dating, and stratigraphy as methods for quantifying post-rift erosion depths and lithospheric response at passive margins. A mappable unconformity between the Proterozoic basement and the low-conductivity, pre-rift sediment cover links residual buttes preserved at the coast to the escarpment, and therefore imposes tight limitations on parameter choices for modeling the Cenozoic topographic evolution. A mean geothermal gradient of ~33 °C km-1 ensures the best fi t between the thermochronologic data and the stratigraphically defi ned coast-to-scarp maximum denudation depth of ~1.75 km. With a lithospheric elastic thickness of 7 km, the resulting fl exural response generates a retreat and uplift of the escarpment associated with a seaward downwarp of the unconformity, made possible because denudation minima are inboard of the escarpment and sediment loading occurs offshore. This closed experiment confi rms the value of low-temperature thermochronology as a tool for quantifying long-term erosion, but also highlights the benefi ts of including independent stratigraphic information in terms of obtaining more plausible solutions. This study suggests that post-rift downwarping of eroded rift shoulders can occur, and may have not been commonly detected because low-temperature thermochronology data sets lack both suitable geologic data and intrinsic sensitivity.