Implications of 36Cl exposure ages from Skye, northwest Scotland for the timing of ice stream deglaciation and deglacial ice dynamics
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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.

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