The most important section of quaternary deposits in the coastal plain of Israel has been recently described in a quarry near kibbutz Evron in the northern part of the country (Western Galilee Coastal plain, fig. 1) (1). Later, the quarry section was tied into an east-west transect across the northern coastal plain (2). The transect was shown (fig. 2) to include three soils (continental phases) intercalated between four layers of sandstone (ingressions). The existence in the vicinity of Evron of three superposed Acheulean assemblages renders the Evron transect of a prime importance for both prehistoric and geological-pedological studies. Investigations by the present authors have shown that the description given by Issar and Kafri was oversimplified. We intend to discuss the stratigraphy here, while the industries will be treated elsewhere (3).