The stratigraphic architecture of coastal plains is determined by the interactions between
local (eg fluvial processes and topography), regional (eg climate) and global (eg sea level) …

Sea-level fluctuations are a dominant mechanism that control coastal environmental
changes through time. This is especially the case for the successive regressions and …

This study presents the first in-depth analysis of properties, micromorphology, clay
mineralogy, magnetic susceptibility, and general properties of Quaternary paleosols from …

During Holocene sea-level rise, coastal areas became transitional environments as marine
incursion covered the land. Changing conditions resulted in dynamic depositional …

Seismic cross-sections and drillings, which were carried out as part of a larger research
program in the area of Dor on the southern Carmel coast of Israel, indicate that the young …

The late Quaternary history and systematics of slope erosion along a segment of the Central
Israeli Coastal Plain is examined in conjunction with a series of terminal Paleolithic …

The formation of short-lived backswamps along the Carmel coast of Israel coincides with the
rapid global sea-level rise during the late Pleistocene–early Holocene transition. The current …

Late Pleistocene–Holocene sequences in the southern Carmel coastal plain of Israel were
obtained from two cores, 12 and 16m deep, at the western and eastern longitudinal troughs …

The Lower Paleolithic Late Acheulian in the Levant marks a fascinating chapter in human
cultural and biological evolution. Nevertheless, many aspects of the Late Acheulian are still …

A series of submerged archaeological sites found on the continental shelf between Haifa
and Atlit indicate a continuous marine transgression between 8000 and 1500 yr BP The …