Abstract
ANYONE who has travelled by train along the coast of Palestine from Haifa to Ludd cannot have failed to notice, soon after rounding the northern point of Carmel, a low ridge of sandstone running roughly parallel with the railway line and the sea. It begins 5 km. to the south of Cape Carmel, and continues for approximately 32 km.
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GARROD, D., GARDNER, E. Pleistocene Coastal Deposits in Palestine. Nature 135, 908–909 (1935). https://doi.org/10.1038/135908b0
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DOI: https://doi.org/10.1038/135908b0
