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  • Calcrete-coated remnants of landslide debris and alluvial deposits are exposed along the hillslopes of the Soreq drainage, Judea Hills, Israel. These remnants indicate that a transition from landslide-dominated terrain to dissolution-controlled
  • of landslide activity in the drainage. The ages of a younger landslide remnant, alluvial terrace, and alluvial fan, all situated only a few meters above the present level of the active streambed indicate that since 688 the Soreq base level had stabilized
  • 2013