Transliterated Name | Source | Name |
---|---|---|
Teleilat Ghassul | Arabic | |
Tuleilat el-Ghassul | Arabic | |
Tulaylât al-Ghassûl | Arabic |
Tuleilat el-Ghassul is a large settlement (c. 50 a. in area) dating from the Late Neolithic and Chalcolithic periods. The site, c. 295 m below sea level, is made up of a group of small mounds and is situated in the lower Jordan Valley, about 5 km (3 mi.) northeast of the Dead Sea. The site was initially discovered in the 1920s, by A. Mallon and a team from the Pontifical Biblical Institute in Jerusalem. During this early phase of research, the investigators were primarily concerned with identifying the five cities of the plain mentioned in Genesis 14 and tentatively identified Ghassul with one of them. Following the first excavations, from 1929 to 1938, it became clear that Tuleilat el-Ghassul represented a new pre-Bronze Age culture in the country's archaeological history. The first to suggest ascribing this culture to the Chalcolithic period was W. F. Albright, and by the mid-1930s its distinct material culture made Tuleilat el-Ghassul the type site for this period.
The initial excavations by the Pontifical Biblical Institute revealed four major superimposed strata (I-IV, earliest to latest), separated from one another by layers of ash, wind-blown and other sediments. The maximum depth of the cultural deposits reached approximately 5 m. The most perplexing problem associated with these deep stratigraphic excavations was the lack of change observed in the material culture assemblage. This homogeneity led the researchers to interpret the four strata as representing a single culture, which R. Neuville named Ghassulian, a term that became synonymous with the Chalcolithic period in this country. To tackle the stratigraphic problem anew, the Pontifical Biblical Institute resumed excavations in 1960, under the direction of R. North, but was unsuccessful in demonstrating any technological development. In 1967, the third and most recent phase of excavation was initiated by B. Hennessy, under the aegis of the British School of Archaeology in Jerusalem. These excavations (1967 and 1975-1978) focused on providing a reliable stratigraphy and sequence of settlement on the site's various mounds; stratigraphically relating the individual mounds to one another; obtaining a large exposure of the earliest settlement phase; collecting paleoenvironmental data; establishing an absolute chronology for the site, using radiocarbon methods; and relating the site to surrounding settlements assumed to be contemporary. Since the early excavations, numerous regional cultures dating to the Chalcolithic period have been found in Israel and Jordan, limiting the value of the term Ghassulian to the site and its immediate environs
Excavation of Ghassul (see Vol. 2, pp. 506–511) was renewed in the 1990s with three seasons conducted by a team from Sydney University (Australia) led by S. Bourke. The work consisted of several small soundings on some of the hillocks that make up the site. All remains date from the Chalcolithic period, but analysis of the finds is only in a preliminary stage. The limited nature of the soundings meant that large areas of coherent architecture were not uncovered. Rather, multiple phases (sometimes up to 10) of partial houses and courtyards with pits and silos were discerned. Aside from the usual tools and ceramics at the site, another small fragment of a painted wall fresco was found.
Tuleilat el-Ghassul is the largest Chalcolithic site in the country and provides new evidence concerning the local evolution of this culture beginning in the Late Neolithic period. Although previously viewed as the type site for the Chalcolithic, very few copper objects have been found at the site. No evidence of metal production was found in the recent excavations and only a few copper axes were recovered in the Pontifical Biblical Institute's investigations. Recent radiocarbon dates and the pottery from the earliest phase suggest an affinity to the Pottery Neolithic at Jericho, Middle and Late Neolithic Byblos, and Neolithic sites in the southern Beqa'a in Lebanon. While general similarities exist between Ghassul and the Beersheba Valley sites, the relationship between these cultures is more complex than previously thought. This is due to the lack of radiocarbon dates from the upper levels at Ghassul, the virtual absence of a metal industry at the site, and the need for more provenance studies to trace interregional relations during this period. Recent excavations at Gilat show that this site has more affinities with Ghassul. Although Tuleilat el-Ghassul has been investigated for over sixty years now, scholars have still not explained why it grew into one of the largest late fifth-to fourth-millennia sites in the Levant.
We have come to the conclusion that all the walls and hearths can be divided into two classes that belong to levels IV A and B respectively, although we must admit that they really form one whole (Koeppel 1940:53).The joint British School of Archaeology in Jerusalem and University of Sydney (BSAJ/USyd) work was more careful in its stratigraphic investigation and provided new insights. Hennessy's first season distinguished ten building phases and broad exposures revealed carefully excavated floor deposits which tell us much more about the daily activities of the site's inhabitants. It was noted that earthquake faulting had disrupted stratigraphy so that some areas were not able to be effectively investigated.
13 A catalogue of the ceramics and other finds was later attempted by Lee (1973) although this has remained unsatisfactory due to the lack of firm stratigraphy.
14 Almost all of the non-registered finds from the 1994-7 excavations are held in store at the University of Sydney, N.S.W. Australia. Material from the Hennessy excavations is split between Sydney (which has the large bulk of material), the British School of Archaeology at Jerusalem (BSAJ), the British Museum (BM), the Nicholson Museum, Sydney, the Amman Citadel Museum and the Salt Museum, Jordan. Registered small finds from the 1994-1997 seasons were divided 70:30 to Jordan.
Through the various years of excavation, an area of over 10,500 sq m was exposed. Although the earlier excavators defined four main phases, the precision of Hennessy's more recent excavations defined ten major building phases separated by camp-floor occupations. The latter occurrences are interpreted as occupational subphases when the site was reconstructed for resettlement following periods of destruction. The entire sequence, labeled phases A through I, contains over one hundred successive floor levels. Although there is a paucity of reports concerning the recent excavations, the preliminary studies show technological development for the pottery and, to a limited extent, for the flint industries. The recent excavations also suggest that frequent seismic activity in the Jordan Valley caused the destruction of numerous settlements found in the archaeological sequence. Hennessy's excavations show no continuity for the Chalcolithic settlement into the subsequent Early Bronze Age, but there is a degree of continuity from the Late (Pottery) Neolithic period not noted by the original excavators. The following table equates the original four major phases (I-IV) with Hennessy's:
a number of earthquake splits [fissures in the floor]in an area that
was probably the entranceto a structure whose corner is manifest in walls J and K. See Fig. 3.9 for the plan and Plates III.16 and III.17 for photos.
23 This means that when the present author began work, a large amount of pottery had to set aside because it was not clear to which phase it belonged. This problem has only affected the ceramics from AII.
an earthquake/subsidence split [fissure]on the interior of Wall 4b. See Fig. 3.10 for the plan.
The area under walls G and F (phase A) is earthquake disturbed. He also shows apparent earthquake fissures on a nearby floor. See Fig. 3.11 for the plan. A radiocarbon date was obtained from a sample taken from a posthole under wall I with the context number AII 107.3/4 ( Lovell, 2001:25 n. 25). Weinstein (1984:334) supplied the following results from radiocarbon dating of this sample.
Provenance | Material | 14C date BP | 14C date BCE | CRD-1σ date | Lab no. | Refs and Remarks |
---|---|---|---|---|---|---|
Teleilat el- Ghassul Area AII p.107.3 and 4 |
Wood | 6430 ± 180 | 4480 | 5540-5195 BCE | SUA-736 | Unpub; pers commun, J B Hennessy |
23 This means that when the present author began work, a large amount of pottery had to set aside because it was not clear to which phase it belonged. This problem has only affected the ceramics from AII.
25 A radiocarbon date was calculated from a sample (SUA 736) taken from a posthole with the context number AII 107.3/4 (Weinstein 1984:334) . This posthole is visible in the section. See chapter 5 for further details.
Damage Type | Location | Image(s) | Comments |
---|---|---|---|
Fractures folds and popups on irregular pavements ? |
entrance to a structure outside the corner of walls J and K
Fig. 3.9
Composite plan of Area A, phase C Lovell (2001) |
Plate III.16
AII, phase C walls J & K looking east. (Photo TG Project) Lovell (2001)
Plate III.17
AII, phase C, walls J, K, L & M at end 1967, note area of sondage to north (Photo TG Project) Lovell (2001) |
|
Damage Type | Location | Image(s) | Comments |
---|---|---|---|
Displaced Wall ? | inside of wall 4b
Fig. 3.10
Composite plan of Area A, phase B Lovell (2001) |
|
Damage Type | Location | Image(s) | Comments |
---|---|---|---|
Fractures folds and popups on irregular pavements ? |
area under walls G and F
Fig. 3.11
Composite plan of Area A, phase A Lovell (2001) |
|
A. Mallon and R. Koppel, annual excavation reports, in Biblica (!930-1938)
id. et al.,
Teleilat Ghassull, Rome 1934
Ghassul2, Rome 1940
R. North, Ghassul1960 Excavation Report, Rome
1961
R. North, Biblica40 (1959), 541-555
id., ADAJS-9 (1964), 68-74
id., SHAJ l (1982), 59-
66
B. Hennessy, RB 75 (!968), 247-250
id., Levant l (1969), 1-24
id., SHAJ I (1982), 55-58
E. D.
Stockton, Levant 3 (1971), 80-81
J. R. Lee, "Chalcolithic Ghassul" (Ph.D. diss., Hebrew Univ. of
Jerusalem 1973)
C. Elliott, PEQ 109 (1977), 3-25
id., Levant 10 (1978), 37-54;1. A. Sauer, BA 42(1979),
9
P.M. Schwartzbaum et al., Third International Symposium on Mudbrick (Adobe) Preservation, Ankara
1980, 177-200
D. 0. Cameron, The Ghassulian Wall Paintings, London 1981
American Archaeology in
the Mideast, 150
G. Dollfus, MdB 46 (1986), 5-6
T. E. Levy, BA 49 (1986), 82-108
id. and A. Holl,
Archeologie Europeenne 29 (1988), 283-316
I. Gilead, Journal of World Prehistory 2 (1988), 397-443
id.
(andY. Goren). RASOR 275 (1989), 5-14
Khouri, Antiquities, Amman 1988, 81-85
Weippert 1988
(Ortsregister)
Akkadica Supplementum 7-8 (1989), 230-241
Y. Goren, Mitekufat Ha'even 23 (1990),
100*-112*
B. Rothenberg, University of London. Institute for Archaeo-Metallurgical Studies Newsletter
17 (1991), 1-7.
Teleilat Ghassul Project, Sydney University: Ghassul Archaeozoological Report 1995–
1997 Seasons, by L. D. Mairs, 1997
Teleilat Ghassul Petrography 1995–1996, by W. I. Edwards, 1997;
Teleilat Ghassul Shell 1994–1997, A First Listing, by D. S. Reese, 1997
Ghassul Archaeobotany Report,
1997 Season, by J. Meadows, 1998
Teleilat Ghassul: A Large Village on the Periphery of Egyptian Trade,
by J. L. Lovell, 1998
S. A. Scham, Pastoralism and the Emergence of Sociopolitical Complexity in the
Chalcolithic Period, Teleilat Ghassul, Jordan (Ph.D. diss.), Washington, DC 1999
J. L. Lovell, The Late
Neolithic and Chalcolithic Periods in the Southern Levant: New Data from the Site of Teleilat Ghassul,
Jordan (Monographs of the Sydney University Teleilat Ghassul Project 1
BAR/IS 974), Oxford 2001
ibid.
(Reviews) Paléorient 28/2 (2002), 148–155. — BASOR 331 (2003), 69–71. — Mitekufat Ha’even 33 (2003),
218–224
JNES 64 (2005), 143–144. — NEAS Bulletin 50 (2005), 61–62.
B. Rothenberg, IAMS Studies 17 (1991), 6–7
S. Sadeh & R. Gophna, Mitekufat Ha’even 24 (1991),
135–148
J. B. Hennessy, ABD, 2, New York 1992, 1003–1006
id., OEANE, 5, New York 1997, 161–163;
J. Perrot, EI 23 (1994), 100*–111*
S. J. Bourke (et al.), ADAJ 39 (1995), 31–63
44 (2000), 37–91
id., AJA
99 (1995), 509–510
100 (1996), 518–520
103 (1999), 493–494
id., Orient Express 1996, 41–43
2000,
52–54
id., The Prehistory of Jordan II, Berlin 1997, 395–418
id., SHAJ 6 (1997), 249–260
id. Radiocarbon 43 (2001), 1217–1222 (et al.)
46 (2004), 315–323 (et al.)
id., Egypt and the Levant, London 2002,
152–164
id., PEQ 134 (2002), 2–27
id., Paléorient 30/1 (2004), 179–182
D. O. Cameron, Bolletino del
Centro Camuno di Studi Preistorici 28 (1995), 114–120
P. L. Seaton, Trade, Contact and the Movement of
Peoples in the Eastern Mediterranean (J. B. Hennessy Fest.
Mediterranean Archaeology Suppl. 3
eds. S.
J. Bourke & J. -P. Descoeudres), Sydney 1995, 27–30
S. Scham, ACOR Newsletter 8/1 (1996), 4
id., AJA
101 (1997), 507–508
id., BA 60 (1997), 108
id., Dept. of Pottery Technology, Leiden University, Newsletter
16–17 (1998–1999), 85–105
id. (& Y. Garfinkel), BASOR 319 (2000), 1–5
A. Enea, Contributi e Materiali
di Archeologia Orientale 7 (1997), 163–176
L. Quintero & I. Kohler-Rollefson, The Prehistory of Jordan II,
Berlin 1997, 567–574
G. O. Rollefson, ibid., 567–574
A. Von den Driesch, ibid., 511–556
R. G. Khouri,
Jordan Antiquity Annual, Amman 1997–1998, no. 13
E. B. Banning, NEA 61 (1998), 188–237
66 (2003),
4–21
id., ICAANE, 1, Roma 2000, 1503–1514
J. L. Lovell, PEQ 130 (1998), 176
id., Australians Uncovering Ancient Jordan: 50 Years of Middle Eastern Archaeology (ed. A. Walmsley), Sydney 2001, 31–42;
M. Blackham, Levant 31 (1999), 19–64
Y. Garfinkel, Neolithic and Chalcolithic Pottery of the Southern
Levant, Jerusalem 1999
G. Philip & O. Williams-Thorpe, ICAANE, 1, Roma 2000, 1383
S. P. Tutundzic,
Glasnik: The Journal of the Serbian Archaeological Society 17 (2001), 77–88
I. Gilead, Beer Sheva 15
(2002), 103–128
A. H. Joffe, AASOR 58 (2003), 45–67.