Fadous-Kfarabida

2700 - 2200 BCE

Jar

Lebanon/Northern Coast

Early Bronze Age III

Transport/Storage

All samples of this fabric are composed of a clay-rich groundmass, rich in microcrystalline calcite, which in most cases has an optically active crystallic b-fabric. Less commonly, a highly sintered optically inactive fabric is noted, indicating a relatively high firing temperature. Of Fabric 2 (Badreshany et al 2019), six sub-fabrics (A–F) could be differentiated by an increasing degree of coarseness, and variations in quartz and calcareous minerals. Sub-fabric 2A is distinguished by the presence of sub- to well-rounded, moderate to coarse, sand-sized quartz (10–15%), and moderately occurring sub- to well-rounded, medium to coarse, sand-sized limestone (10–15%). The limestone is generally not fossiliferous.

Lebanon/Biqa Valley/Northern Coast/Jurassic–Middle Cretaceous Limestones Alluvial Colluvial