Ruben Willaert bvba, Afdeling archeologie; J. De Gryse & J. Ooms
Additional contextual information
site code: LE-06-HPL; CAI code: 1999; feature S45, filling of the partially conserved kiln (tile/rooftile level); this tile fragment was probably not a product of the kiln
Oxidized red fabric; redbrown (PPL), dark brown and yellow/orange brown (XP).
Heterogeneous matrix, non-calcareous with medium to high optical activity.
- ca. 60-75%
Inclusions
Quartz (++; cf: mono, r, medium - coarse sand; ff: mono, poly, r-sr, very fine to fine sand; bimodal), sedimentary rock detritus (+-; ff, possible quartz arenite), chert/flint (+-; ff & cf), muscovite mica (+-; el, ff), feldspars (--; orthoclase, microcline), glauconite (+-; red in PPL, r, ff), pyroxene (--; r, ff), O/Fe (+; ff & cf), semi-plastics/clay pellets (+; various compositions*)
The coarse fraction varies from coarse to medium sand, the fine fraction from fine sand to very fine sand. Coarse fraction grains are generally rounded, fine fraction grains are generally rounded to subrounded. Bimodality of quartz population, iron oxides and semi-plasics/clay pellets (possibly natural). Overall the fabric is moderately to poorly sorted.
- ca. 20-30%
Voids
Small planar voids and larger vughs with good alignment parallel to the edge, no infill. Drying cracks in and around semi-plastics/clay pellets.
- ca. 5-10%
Diagnostic features
The fabric is characterized by a heterogeneous oxidized matrix with medium to high optical activity and low porosity. Dominant quartz inclusions with common sedimentary rock detritus, chert/flint, muscovite mica, glauconite, opaques/iron oxides and semi-plastics/clay pellets of various compositions, and rare feldspars and pyroxene. Bimodality in quartz population, unclear if it represents a natural sandy fraction or an added temper. The various plastic inclusions most likely result from poor mixing of various clays or clay layers, or can represent a temper of dried and/or fired material. Overall moderately to poorly sorted.
Additional information
*Semi-plastics/clay pellets: 1. iron-rich semi-plastics; 2. iron-poor clay zones; 3. reduced zone (grey) rich in quartz; 4. argillaceous/grog inclusions: oxidized, orange body color in PPL, dark yellow in XP, medium to high optical activity, very fine matrix (ca. 80-90%) with monocrystalline quartz (+; r-sr), muscovite mica (-; el), iron oxide (-); clear boundaries, rounded, neutral optical density, concordant features); similar to inclusions in A0011. Most likely the result of poor mixing of two clays or a clay with layers consisting of different compositions. Possible addition of dried or fired material (n°3 & 4 = grog temper?).
De Gryse J. & Ooms J. 2007 Archeologisch onderzoek op het A. Smetsplein (Leuven). Onuitgegeven opgravingsverslag Ruben Willaert Bvba. Afdeling archeologie, Damme: 67.
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