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Antonio Sagona, The Archaeology of the Caucasus From Earliest Settlements to the Iron Age .pdf
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216

Encounters Beyond the Caucasus

confusing, whereas others are more than adequate and still very much in use. The range includes the ‘Eneolithic culture of Trans-Caucasia’;‘Shengavit culture’, focusing on a key site in Armenia; the ‘Karaz culture’, used by Turkish archaeologists for the Anatolian assemblages; the ‘East Anatolian Early Bronze Age’ and ‘The Culture of North East Anatolia’; the ‘Yanik culture’, stressing the role of north-western Iran; the ‘Outer Fertile Crescent Culture’; the ‘Dagestan-Palestinian Archaeological Area’, according special importance to the tradition’s northern and southern extremities; ‘Khirbet Kerak Ware’, a regional assemblage from the Levant found clustered in northern Israel and the West Bank; and ‘Red-Black Burnished Ware’ used to describe the ceramics of Amuq Phase H and, increasingly, the repertoire in the Turkish Upper Euphrates region, especially by the Italian researchers at Arslantepe.8 In this study, I have retained the designation Kura-Araxes.

BORDERS AND FRONTIERS

More than 700 Kura-Araxes sites, from the tradition’s fledgling appearance to its latest expressions, have been documented, and many hundreds more are likely to augment this number in the future, as neglected highland areas are intensively surveyed (Figure 5.2).9 This includes work in the southern Caucasus where, despite a very active archaeological tradition during the Soviet period, little systematic field walking and recording has been undertaken.The KuraAraxes tradition is at home in the tangle of mountains and inter-montane valleys between the Caucasus and the Taurus ranges. After the Late Chalcolithic period, the immense highland zone of eastern Anatolia and north-western Iran was swiftly embraced by the material culture of the Kura-Araxes. As will be discussed, what prompted this dispersal is unclear, but most would now agree that it involved in part the migration of kin-based communities who moved as far south as the Sea of Galilee.10 Western Georgia, however, remained

8Shengavit culture (Baiburtian 1938; Sardarian 1967); Karaz culture (Koşay and Turfan 1959;Yalçın 2011, 2012. Işıklı, 2011, who re-investigated the material from Karaz, prefers the ‘Early Trans-Caucasian Culture’); the East Anatolian Early Bronze Age (Burney 1958); the Culture of North East Anatolia (Lamb 1954); theYanik Culture (Dyson 1965); Dagestan-Palestinian Archaeological Area (Areshian 2005: 72, n.7); the Outer Fertile Crescent culture (Kelly-Buccellati 1979); Khirbet Kerak Ware (Albright 1926: 27);

for a detailed report on the early excavations at Tel Bet Yeraḥ (Khirbet el-Kerak), see Greenberg et al. 2006; and for a final report on the Tel Beth-Shean deposits, Mazar 2012; Red Black Burnished Ware (Braidwood and Braidwood 1960; Palumbi 2008).

9For a detailed gazetteer, see Sagona 1984, vol. 2, which has been updated by Batiuk (2005: 295–415). Amongst the publications that have extended the cultural boundaries of the Kura-Araxes culture province or revealed significant concentrations in specific areas, see Young 2004; Fahimi 2005; Badalyan and Avetisyan 2007; Piller 2010.The map

in Kushnareva (1997: 46–8, fig. 18) is useful, but outdated. 10 Greenberg et al. 2015.

N

0 - 1000 m

 

1000 - 2000

 

2000 - 3000

Black sea

 

6

8

 

7

9

 

 

2

 

 

3

Murat

 

4

 

 

 

5

 

 

1

050 km

 

 

39

 

40

 

 

 

 

38

 

 

 

 

 

37

Kura

 

48

10

 

36

41

47

 

11

35

42

 

46

 

 

 

45

 

 

34

 

43

 

River

 

 

 

 

44

 

 

 

 

 

 

 

12-14

 

32

 

49

 

 

 

33

 

 

 

15

 

31

 

 

 

 

16

 

30

 

Lake Sevan

 

 

27

29

 

 

 

A

28

 

 

 

26

 

 

 

 

raxes

 

 

 

25

24

 

 

 

 

River

 

 

 

 

 

 

 

 

17

 

23

 

 

 

 

 

 

 

 

 

 

 

50

 

 

Lake

 

 

 

22

 

 

Van

 

 

 

 

18

Lake Urmia

21

19

20

51

River

 

 

 

217

1

Arslantepe

12-14

Keti I, II, III

2

Pulur (Sakyol)

15

Karnut I

3

Taşkun Mekvii

16

Talin

4

Tepecik

17

Köhne Shahar (Ravaz)

5

Norşuntepe

18

Haftavan Tepe

6

Karaz

19

Giljar Tepe

7

Pulur

20

Geoy Tepe

8

Güzelova

21

Yanik Tepe

9

Sos Höyük

22

Kul Tepe (Hadishahr)

10

Abastumani

23

Kültepe (Nakhichevan)

11

Chobareti

24

Ovçular Tepesi

 

 

25

Mukhanat Tapa

 

 

26

Shengait

 

 

27

Mokhra Blur

 

 

28

Garni

 

 

29

Elar

 

 

30

Aparan III

 

 

31

Tsaghkahovit

 

 

32

Gegharot

 

 

33

Kosi Choter

 

 

34

Grmakhevistavi

 

 

35

Ozni

 

Caspian

36

Beshtasheni

 

37

Kvatskhelebi

 

sea

38

Khizanaant Gora

 

 

39

Natsargora

 

 

40

Gudabertka

 

 

41

Samshvilde

 

 

42

Tetri Tskaro

 

 

43

Ghaitmazi

 

 

44

Dangreulis Gora

 

 

45

Koda

 

 

46

Kiketi

 

 

47

Didube

 

 

48

Badaani

 

 

49

Baba Dervish 1-3

 

 

50

Kohne Pasgah Tepesi

 

 

51

Velikent

Figure 5.2. Map showing the main Early Bronze Age sites in the southern Caucasus and neighbouring lands (drawn by C. Jayasuriya).

218

Encounters Beyond the Caucasus

unaffected by this expansion, for reasons discussed further on, and the formidable Greater Caucasus Mountains, though traversable, acted as an effective barrier to the settlement of the Eurasian steppes to the north.

Within this divided landscape, these pioneering farming groups are today represented by mound sites, mostly small hamlets between 1 and 2 ha in size. These have only one or two periods of occupation and are almost never sandwiched between the cultural debris of other periods. Shengavit in the Ararat Plain, with its 3.5 m deposit and 6 ha spread, is an exception.11 Sites with similarly deep deposits are located on the fringe of the Ararat Plain or in Nakhichevan and the middle Araxes Valley, around Lake Urmia, where Yanik Tepe and Gijlar Tepe are found, or in the Turkish Upper Euphrates region, where the co-mingling of several cultural traditions has been attested.

Kura-Araxes communities settled at a range of altitudes, from coastal plain (not well populated) along foothills and valley floors to the highlands proper, reaching lofty heights around 2,000 m above sea level. In this sense, they followed the pattern already set by the bearers of the Chalcolithic Sioni tradition. Stephen Batiuk concluded that geography can account in part for the choice of land, and that most Kura-Araxes communities preferred valley floors and foothills, within the 400–600 mm isohyet zone of precipitation, the most conducive for rain-fed agriculture.12 Although human activity during the Holocene period has dramatically changed the physical landscape of the Near East, especially the woodlands, broad ecological niches can still be discerned. Outside the Caucasus, the clear majority of Kura-Araxes communities (76 per cent) preferred territories with arable land suited to farming. Only a very small proportion (15 per cent) of sites are located in pastureland, and even fewer (1.3 per cent) in areas of rough grazing.13 While this patterning could reflect the ‘invisibility’ of transhumant sites, evidence is mounting that the communities of the KuraAraxes opted for territories that were well suited to a low-risk, mixed farming economy. Even so, we should bear in mind the difference between herd mobility and community mobility. It is possible, for instance, that a fully sedentary agricultural community practised transhumance, the seasonal migration of the livestock and a few herders between higher and lower pastures.

Georgia

The north and north-eastern boundary of the Kura-Araxes culture province is defined by the mountains of Dagestan, Chechnia, and Ingushetia. In

11Simonyan and Rothman 2015: 12.

12An isohyet is a line connecting points on a map that have the same amount of rainfall. Batiuk (2005: 79–80) groups sites according to quantity of Kura-Araxes material culture: predominant (class 1), substantial amount coexisting with other ware types (class 2), in the minority (class 3), and funerary sites (class 4).

13Batiuk 2005: 83–4; fig. 7, table 3.

Borders and Frontiers

219

Dagestan, most of the sites are positioned along the narrow coastal littoral, such as Velikent, north of Derbent, with a few following the watercourses up into the foothills.14 From the adjacent territory of north Ossetia down to the districts around Kutaisi there is another cultural frontier, namely that between the Kura-Araxes and the Maikop traditions, where Sachkhere represents the pre-eminent site.

Interestingly, most of western Georgia, drained by the rivers Rioni and Inguri and their tributaries, has no Kura-Araxes sites. This boundary could simply stem from an aversion to the wetlands of western Georgia, where the rich red soil, mild temperatures, and high precipitation nurtures sub-tropical vegetation within a system of marshes and lagoons.A social explanation, however, is more likely. Indigenous communities in this triangular wedge of land, who pursued their own distinctive cultural trajectory throughout the Bronze Age (the so-called Proto-Colchian, Chapter 10), quite possibly posed a formidable barrier that thwarted the expansion of Kura-Araxes values. There are a few sites in the eastern half of western Georgia, to be sure, which do bear Kura-Araxes affinities and show some form of co-existence. The site of Qanobili near Abastumani, for instance, is a striking example of a boundary site, comprising a mixture of Kura-Araxes elements intermingled with those of the Zemo (Upper) Imereti cave cultures.15

In Georgia,there are several settlement nodes,specifically along the lowlands of the Kura River (Shida and Kvemo Kartli). Significant settlements in the environs of the modern towns of Urbnisi and Gori include the stratified sites of Berikldeebi, Kvatskhelebi, Khizanaant Gora, Natsargora, and Gudabertka.16 Other locations are dotted across the plain, with a good number strung along the Liakhvi River, which cuts through South Ossetia to meet the Kura River. Further east, sites are located in the narrow valley of the Aragvi River, especially around Dusheti.17 In Kvemo Kartli, the early settlements of Didube and Treligorebi are situated on opposite banks of the Kura River within the environs of Tbilisi; both were discovered as part of modern building operations.18 Further south in the plain of Marneuli, fed by the Khrami and Algeti Rivers, we have a number of significant villages – Ghaitmazi, Dangreuli Gora, Kiketi, and Koda.19

14Gadzhiev et al. 2000; Magomedov 2006; Kohl and Magomedov 2014.

15Pkhakadze et al. 1982.

16Dshawachischwili 1998 (Berikldeebi); Dzhavakhishvili and Glonti 1962 (Kvatskhelebi); Kikvidze 1972 (Khizanaant Gora); Puturidze and Rova 2012b (Natsargora); Mindiashvili et al. 2012 (Gudabertka).

17Gogochuri 2008.

18Kiguradze and Sagona 2003 (Didube);Abramishvili and Gotsiridze 1978 (Treli).

19Glonti 1975 (Ghaitmazi and Dangreuli Gora); Pkhakadze 1963 (Kiketi); Pkhakadze 1976 (Koda).