Cosmogenic nuclide dating of glacial erratics on Blomstrandhalvøya, North west Spitsbergen. The project also involves detailed Quaternary mapping of the island, in order to give context to the interpretation of Cosmogenic ages, and the overall rate and magnitude of deglaciation in Kongsfjorden following the Last Glacial Maximum. This will aid the modelling of the Svalbard-Barents Sea Ice Sheet deglaciation by providing ground-truthing and deglaciation chronology in a key location.