Wind-abraded rocks (ventifacts) are common coastal features associated geomorphically with beaches, estuary mouths and sand dunes. This paper compares evidence for ventifaction from similar coastal settings in Donegal (Ireland) and Oregon (USA) and considers their implications for coastal sediment dynamics. Ventifacts on a bedrock platform at Gweebarra Bay, Donegal, show pit and groove ventifact styles and are estimated to have formed over some < 2500 years. Ventifacts on a boulder jetty (built 1892–1901) on the Oregon coast, USA, show similar grooves and pits. Winds above the threshold for sand transport and possible abrasion are present for 28–30% of the time at both locations. Based on depth of rock loss, wind abrasion rates on the Oregon coast are 0.24–0.95 mm yr−1, two orders of magnitude greater than in Donegal. Coastal sediment fluxes on these coasts since the late Pleistocene have responded to sea-level fluctuations and changes in onshore sediment supply. Sediment systems are presently less dynamic than in the past, and some coastal geomorphic features may be largely relict.