Les blocs d'estran a Saint-Fabien-sur-Mer, estuaire maritime du Saint-Laurent, Quebec.

Abstract

Boulders, up to 5 m in diameter, are found on marine postglacial deposits of thick clay. As there is no evidence of glacial drift in the area, and as the boulders overlay fine marine sediments of postglacial age, drift ice can be considered as the principal agent of transportation and deposition. -from Author