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The
Thesprotia Expedition
2004 - 2005
2006
2007
Field survey
Trial excavations
2008
2009
2010

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THE THESPROTIA EXPEDITION
A Regional,
Interdisciplinary Survey Project
in Northwestern Greece
The preliminary
results of the archaeological work conducted during the fourth season of the
Thesprotia Expedition are as follows.
Continued
survey and prospecting
The fourth
consecutive field season of the Expedition consisted of intensive field survey,
a geo-archaeological survey, geophysical prospecting, and taking of
palynological samples from lakes in the region, as well as trial excavations at
three sites.
This was the last
field season in which the intensive field survey was continued. The total area
covered by the intensive survey in four years amounts to ca. 4 km2.
The area surveyed in 2007 was located on the actual valley bottom to the east of
the Kokytos river. We identified a total of 13 new places of special interest
(indicated by PS), most of which are to be considered as sites. This brings the
total number of places of special interest documented by us within the 4 km2
to 49, which corresponds to roughly 12 sites per km2.
Among the places
of special interest documented this year was a cluster of Middle to Upper
Palaeolithic lithics (PS 45) as well as a Mesolithic site producing a large
spectrum of tools and flakes (PS 43). We also documented several sites dating to
the Classical to Hellenistic period with black glazed pottery and loomweights as
well as coarse ware and roof tiles (PS 37, PS 44, PS 46, PS 48 and PS 49). One
of them, PS 46, which lies only some hundred metres away from the Early Iron Age
site PS 36 (cf. AR 2006 - 2007), also produced some Early Iron Age sherds and some
Early Roman terra sigillata. Finally we found one Middle Roman site (PS 41), two
Late Roman sites (PS 38, PS 39) and at least one Early Modern site (PS 47).
The
geo-archaeological survey continued along the same lines as in 2006 with e.g.
further coring at Mavromandilia of Prodromi. The Early Iron Age through
Classical finds made at PS 31 and PS 36, as well as at a third place explored by
the 32nd Ephorate, all seem to belong to one and the same site located next to
several springs and a small stream once flowing into the Kokytos river. The
geophysical prospecting with magnetometer and georadar continued. The most
interesting finds were once again made next to the Early Christian basilica of
Zervochori, where the magnetometer survey revealed a large square building,
measuring at least 25 x 30 m and probably belonging to the same village located
next to the basilica which was partly uncovered already last year.
This year the
palynological team, under direction of Henk Kars and Sjoerd Kluiving from VU
University in Amsterdam, began its work by coring in the lakes of Prontani,
Chotkova and Kalodiki. The most interesting results regarding climate
reconstruction and geomorphology were obtained from the Kalodiki lake at Morphi.
According to the C-14 dates, the timescale of the analysis of the calcareous
gyttja layer is set to a minimum of 40,000 14C yrs BP. The pollen
sequence correlation suggests a possible Middle to Late Pleistocene dating of
the
calcareous gyttja sediment. It seems that in that period the basin was
enclosed and the surrounding hills were most likely vegetated. These conditions
prevented the occurrence of erosion and provided the conditions for accumulation
of an undisturbed sedimentological sequence, which is an ideal archive for
regional climate and environmental reconstruction. These ideal conditions
changed with the activation of the alluvial fans and the subsequent erosion of
the lacustrine deposits. It is suggested that this event is related to the
dramatic climate change from the Pleistocene to the Holocene period.
Trial
excavations
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