Volcanic strata in the Skaftafell region, southeast Ireland, record a seque
nce of at least 16 glacial and interglacial intervals since 5 Ma. Two compo
site sections of 2 to 2.8 km thickness have been constructed from multiple,
overlapping, cliff profiles. The timing of alternating sequences of subaer
ial lava flows, pillow basalts, and hyaloclastite deposits is provided by m
agnetostratigraphic mapping and K-Ar radiometric dating. We find that the f
requency and intensity of glaciations increased significantly at ca, 2.6 Ma
, and particularly since 0.8 Ma, amplifying topographic relief in this area
from <100 m to 2 km. These changes correlate with increases in global ice
volume, ice-rafted debris, and development from local to regional glacial c
onditions in the North Atlantic.