We analysed 1593 basalt artefacts from the Halawa Dune Site, on the easternmost part of Moloka'i Island, for a combination of geochemical and technological attributes to expose different reduction strategies related to basalt adze production and rejuvenation. West Moloka'i is well known as a location where many outcrops were quarried to make adzes, but the island's east side has not been widely perceived as a location where adzes were produced in significant quantities in the prehistoric economy. We infer, however, through large-scale geochemical non-destructive energy-dispersive X-ray fluorescence (EDXRF) analyses, combined with technological analyses, that the majority of adzes at the Halawa Dune Site were manufactured from local resources, supporting a predominantly localised pattern of adze production and use. Approximately one third of the adze debitage clearly related to use and rejuvenation (DA) is made from non-local sources, but does not represent a heavy reliance on the full range of quarries on West Moloka'i, and may also include samples derived from other islands or archipelagos.