‘Atiqot 76, 2013
PetrograPhic examination of medieval Pottery from tiberias
anastasia shaPiro
Thirteen samples of pottery, unearthed during
the salvage excavation of a medieval-period
building in Tiberias (see Stern, this volume),
were chosen for petrographic examination
(Table 1). All sampled vessels date to the
Crusader-period occupation of the building
(Phases 3 and 4; see Stern, this volume).
The thin-sections were prepared and
examined under a polarizing microscope at
magniications from ×20 to ×200. Descriptions
of the thin-sections were provided with the
aid of charts and tables (Whitbread 1986:80).
The following parameters were examined:
mineralogy and approximate amount of siltsized material and optical properties of the
matrix; mineralogy of non-plastics and their
volume in the sherd;1 grain size, shape and
sorting. Firing temperature was estimated
according to mineralogical changes.
The aim of the current study was to prove
or refute visually determined similarities of
the selected material to wares found at ‘Akko,
and, when different from the ‘Akko material,
determine their possible provenance.
As some of the samples discussed here are
visually similar to the fabrics found at ‘Akko,
deined as ‘Beirut’ and ‘Acre’ Wares (Shapiro
2012:104–107), special attention was paid
to these. The thin-sections were compared to
those of similar wares from ‘Akko, with the
results presented below. The geological settings
of the site vicinity were also considered.
Table 1. List of Thin-Sections
Sample
No.
Locus
Basket
Vessel
Fig. No. (see Stern,
this volume)
Provenance
1
111
1022/5
Cooking pot
7:2
Beirut Ware
2
111
1022/6
Cooking pot
7:3
Beirut Ware
3
111
1022/7
Bowl
7:4
Beirut Ware
4
107
1023/5
Jar
12:1
Tiberias vicinity
5
107
1015/1
Jar
12:2
Tiberias vicinity
6
103
1010/2
Baking dish
12:3
Beirut Ware
7
107
1023/4
Cooking pot
12:4
Beirut Ware
8
103
1014/1
Cooking pot
12:5
Beirut Ware
Beirut Ware
9
107
1020/2
Bowl
12:7
10
107
1020/1
Bowl
12:8
Beirut Ware
11
102
1005/1
Bowl
13:4
Acre Ware
12
106
1009/7
Bowl
13:5
Acre Ware
13
103
1007/1
Cooking pot
12:6
Northern Israel
210
anastasia shaPiro
PetrograPhic results
Beirut Ware
Five cooking vessels (Samples 1, 2, 6–8) and
three bowls (Samples 3, 9 and 10) belong to
a homogenous petrographic group. They are
all characterized by a ferruginous, shalerich matrix, with a large amount of siltsized quartz. One bowl’s (Sample 3) matrix
is slightly more calcareous than the other
samples. Sand-sized quartz inclusions are
poorly sorted subrounded-to-angular grains,
0.1–0.5 mm large, comprising up to 11% of the
sherd’s volume, suggesting its classiication
as temper. Opaque rounded ore particles,
varying from minute (0.02 mm) to sand
sizes, and ferruginous shale fragments are
present in small amounts. Chert, and possibly
extremely eroded basalt grains, are sporadic
if any. Based upon the optical properties of
the matrix, iring temperature is estimated at
800–850°C. Some of the samples (6–9) have
cracks inside, which are oriented parallel to
the surfaces of the vessels. Temper-and-matrix
composition of the samples is very similar to
the examined Beirut Ware within the ‘Akko
collection, for which the Lower Cretaceous
formations outcropping at the Mount Hermon
foothills, Transjordan and the southern
Lebanon Range were suggested as sources
of raw materials (Waksman et al. 1999:7–8;
Stern and Waksman 2003:173–175; Waksman
et al. 2008; Shapiro 2012). As basalt does not
crop out in Transjordan, this area should be
excluded from the list of possible origins of
these vessels.
Acre Ware
Two bowls (Samples 11 and 12) produced the
same thin-sections. They have a ferruginous,
slightly calcareous matrix containing silt-sized
quartz. Most of the tempers are well-rounded
to subangular quartz grains, partially oriented
parallel to the vessels’ surface. Plagioclase
and chert are present sporadically. Temper
constitutes 5–15% of the sherd’s total volume.
A considerable number of internal cracks are
oriented parallel to the surfaces of the vessel.
The surface of the bowl (0.01–0.05 mm) is
vitriied, as well as the groundmass of the sherd,
which has vitriied spots and some rounded
air bubbles that have vitriied inner surfaces.
This effect can be a result of the presence of
sea-salts in the paste, indicating that seashore
sand and seawater were involved in preparing
the paste for pottery production (Rice 1987:88;
Orton, Tyers and Vince 1993:115–116; Shapiro
2012:104–105). Firing temperature is estimated
at 750–800°C, based on the absence of
carbonate material and optical passivity of the
clay. Comparison with the examined medieval
pottery from ‘Akko showed that these two
bowls are petrographically identical to Acre
Ware, which was manufactured in ‘Akko or
nearby, utilizing upper Pleistocene formations
of the vicinity as raw materials. Red hamra
clay (distributed along the entire coastal plain
between ‘Akko and Nahariyya) was used as
matrix, with coastal sand, characteristic of the
shore south of ‘Akko (personal observations),
providing tempering material (Bentor 1966;
Dan et.al. 1975; Sneh, Bartov and Rosensaft
1998). Seawater was used in preparing the
paste, giving the effect of surface vitriication
(Shapiro 2012).
Tiberias Ware
Two jars (Samples 4 and 5) have a
foraminiferous marl matrix, where the
foraminifera compose 12–15% of the volume
of the sherd. Some silt-sized to ine sand-sized
(0.1 mm large) plagioclase and olivine grains
are present. Additional sand-sized particles
(0.2–0.5 mm large) of quartz and eroded basalt
grains are present in small numbers (1–2 per
section) in each section, as well as chalk and
mud balls. Firing temperature is estimated at
750ºC, due to the stage of decomposition of
the carbonate material of microfossils. The
iring was executed in an oxidized atmosphere
which gave the sherd a light brown (tan) color.
Possible sources of nearby raw materials are:
(1) the marl of the Bira formation, cropping
out only a few kilometers to the north, and on
PetrograPhic examination of medieval Pottery from tiberias
a hill southwest of Tiberias (Sneh 2008); and
(2) Taqiya marl, which can be found about 2
km to the north of Tiberias, between Giv‘at
Hanamala and Majdala Beach (Sneh 2008).
Basalts are common in the vicinity of Tiberias,
and their sporadic presence can point to very
accurate mining and careful preparation of
pastes. Plagioclase and olivine grains present in
the sherds derived from eroded basalt as well.
A pottery kiln, which may be part of a larger
industrial area, was revealed in southern
Tiberias (Stern 1995). The kiln, dating to the
Early Islamic period, yielded vessels of a buff
to tan shade. Although the pottery inds were
not analyzed, its external appearance leads us
to suggest that the same source of raw material
served for these vessels and for the jars
examined here.
Other Fabrics
One cooking pot (Sample 13) has a ferruginous
slightly silty matrix, to which rounded, rather
well-sorted quarts sand was added in small
amounts as temper. The sand composed about
10–12% of the sherd’s volume, and its grains
are 0.5–0.7 mm on average. Due to the optically
passive clay minerals, iring temperature can
be estimated at 800ºC. The mineralogical
composition of this sherd does not allow us
to determine its exact provenance, although
nothing suggests that the source would not be
somewhere in northern Israel.
conclusions
The examined pottery assemblage forms
three petrographic groups, two of which are
represented by two samples only. One sherd did
not fall into any of these petrographic groups.
Two groups share petrographic features with
two groups of medieval pottery from ‘Akko,
and were therefore labeled with the same
names: Beirut Ware and Acre Ware, which
indicate their provenance.
Beirut-Ware vessels (both cooking and table
ware) are frequently unearthed at medieval sites
in Israel and abroad (Avissar and Stern 2005:6–
211
9, 19–22, 91–94, 96–99, Pls. II:1–3, VI:1–5, 8,
XXVI, XXVII), although their provenance is
usually termed Lebanese (Stern and Waksman
2003:169–170, 173–175; Shapiro 2012).
Acre Ware, represented by two bowls, is
rarely found outside of ‘Akko, where they were
manufactured (Stern and Waksman 2003:168–
169, 173–175; Shapiro 2012). It is therefore
surprising to encounter this ware so far from its
place of origin. Further careful reading of the
medieval pottery assemblages and petrographic
examination of similar Acre Ware samples
may shed light on whether these vessels were
exclusively domestic in nature or whether they
were traded as well and if so, how distant was
their distribution?
The inal group is represented by two jars, for
which the Tiberias vicinity was suggested as the
most possible provenance. The examination of
microfauna (foraminifers) revealed that Taqiya
marl was most likely used for these vessels.
Although this marl is widespread in Israel
(Bentor 1966:72–73) and was frequently used
for pottery production in ancient times (Goren
1995:302; Glass et al. 1993:278), it is suggested
here that the examined jars were manufactured
in Tiberias or its very close vicinity, based
on two pieces of evidence. First, the basalt,
plagioclase and olivine grains present in the
thin-section originate in basalt formations,
and these are present in and around Tiberias.
Secondly, a visual examination of the pottery
from the above-mentioned kiln (Stern 1995)
suggests that the same fabric was in use in
Tiberias some four centuries earlier. Although
no analysis was conducted on the vessels
found in the kiln, it is reasonable to propose
that the source of raw material was the same
for both cases. Examples of prolonged use of
the same source of clay for pottery production
over hundreds and even thousands of years of
human history are known (Goren 1995:303;
Glass et al. 1993:277; Shapiro, forthcoming).
Further petrographic analysis of the pottery
vessels from the kiln may help support or refute
this preposition.
212
anastasia shaPiro
Finally, a single cooking pot, not belonging
to these petrographic groups, did not provide
enough petrographic information to determine
anything other than an origin in northern Israel.
note
1
The non-plastic materials within the ceramic body
are termed “temper” in cases when the quantities
present could have been added by the potter (i.e., 5%
or more).
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