Alluvial sequences in central Israel reveal a history of climatic and landscape changes from Chalcolithic through Byzantine times. These are closely related to social and historical events at Tel Lachish. The deposits indicate a moister climate during initial settlement in the Chalcolithic period and Early Bronze Age. Rapid floodplain buildup in MB I suggests an instability in the drainage system corresponding to widespread abandonment of Levantine cities, including Lachish. A dry period of wadi incision followed. This lasted until a phase of colluvial deposition in the Late Iron Age, which apparently resulted from neglected agricultural terraces after the Assyrian destruction of Israelite Lachish. A later fill accompanied Byzantine settlement and may be related to an amelioration in climate.
No takes yet. Share an insight, caveat, or question.
Arlene M. Rosen (1986) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: