We present new 36Cl exposure ages from southern Skye, northwest Scotland.
Deglaciation of a marine terminating ice stream that drained the BIIS occurred by 17.6 ± 1.3 ka.
Offshore bathymetry reveals a moraine delimiting a pre-Younger Dryas readvance.
Dated to 15.2 ± 0.9 ka and occurred at the same time as a regional scale readvance.