Abstract:
An integrated multi-analytical approach has been performed to ceramic fragments from the
archaeological site of Tell el-Far‘ah North, West Bank, dated back to the Early Bronze Age IB
(3300-3100/ 3000 BC). The main objective of this thesis is to make a comparison between Um
Hammad ware and common wares through the investigation of mineralogical and chemical
composition, technological aspects and the provenance of raw materials. Mineralogical,
petrographic and chemical analyses are applied by means of Optical Microscopy (OM), X-Ray
Powder Diffraction (XRPD) and Scanning Electron Microscopy Coupled with Energy
Dispersive Spectroscopy (SEM-EDS), Fourier Transform Infrared Spectroscopy (FTIR-ATR)
and Inductively Coupled Plasma Mass Spectrometry (ICP-MS). The application of mineralogical
and chemical analyses indicate that the ceramics were produced using calcareous clays with
inclusions of sedimentary calcareous rock fragments, calcite, iron oxides and quartz. Two basic
fabrics, A-calcite and B-calcareous, have been identified according to the presence or absence of
coarse and angular calcite crystals. Moreover, two different clays, clay α and clay β, have been
identified based on the presence or absence of microfossils. The optical activity of the matrix
and the presence of calcareous inclusions indicate a maximum firing temperature lower than 850
°C and in the range 700–850 °C for those ceramics showing an initial decarbonation process of
calcareous inclusions.
The pictographic results suggested that the nature of the inclusions supports a local supply of
raw materials. In line with this, the ICP-MS analysis highlights that the same concentrations of
the trace elements Zn, Cu, Ni, Co, and Ba from the samples are related to same sources of
calcareous clay raw materials utilized. Moreover, the comparison between the Um Hammad and
common wares type of ceramic materials shows that there is a distinctive mineralogical
composition difference between the two types in addition to the morphological and
ornamentation difference
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