Location of Tepe Gawra
The site of Tepe Gawra is located in the in the Ninawa Plain in the piedmont of the Zagros Mountains. The site is roughly a kilometer and a half to the south of the town of Fadiliyah, and about the same distance from the ancient Assyrian city of Dur Šarukin (Khorsabad) to its east. Tepe Gawra is located in a well-watered plain with several spring fed streams running through the site or near it. This condition encouraged settlement across time resulting in a long sequence of occupation at the site. Today most of the springs that were near Fadiliyah are dry as a result of tapping into the water table with deep wells and pumps.
History of Work at the site and its Significance
Tepe Gawra has long been seen as an essential site for late prehistoric and early historic periods, not only in Iraq but for the region in its entirety. Despite the significance of Tepe Gawra, there hasn’t been work carried out at the site since the 1930’s. The work conducted at the site by Speiser (1935) and Tobler (1950) has revealed a long occupational sequence dating from the Halaf period to the mid second millennium BC. The sequence has very few short-lived gaps in occupation and as such has become a chronological anchor for the region, especially for late prehistory (Halaf, Ubaid, and Uruk/LC). Analytical work carried out by Abu al-Soof (1974), and more recently, Rothman (2002), has expanded our understanding of the Northern Uruk period and has been key to developing the modern Late Chalcolithic (LC1-LC5) chronological scheme (Rothman ed. 2001; Schwartz 2001).
Despite its small size (roughly 2-3 ha. at its base extent), Tepe Gawra has been the hallmark site for the development of complexity during the Ubaid and Late Chalcolithic periods in the ancient Near East. Excavations at the site revealed a local development of a sophisticated infrastructure manifest in construction of temples, monumental architecture, and elaborate administrative practices. The site throughout its occupation shows an involvement in far flung networks connecting it with Highland Anatolia and the Zagros mountains, with connections as far afield as Afghanistan. These connections were seen in the high concentration of objects made of exotic materials such as obsidian, lapis lazuli, carnelian, copper, gold, and silver (Rothman 2002: 8), in addition to the presence of imported utilitarian and luxury ceramics (Abu Jayyab 2019; Rothman and Blackman 2003). The households at Tepe Gawra were also shown to be involved in multiple craft activities such as woodwork, textile production, elaborate administration, stone tool manufacture, and the production of high-end ceramic wares (see Rothman 2002; Rothman and Blackman 2003).
All together the main mound of the site has furnished evidence of highly specialized activities (administration, exchange, and craft production) with very little evidence of agricultural implements and farming practices. This phenomenon is unique as this degree of specialization was only attested at larger contemporary sites that combined specialized activities with extensive farming practices (e.g. Tell Brak reaches over 100 ha during this period). This situation necessitated that the inhabitants of Tepe Gawra relied on an external source for food. Rothman suggested that a functional segregation between sites existed in the piedmont or the foothills during this time (Rothman 2002: 5). He saw that the site of Tepe Gawra was a ‘center’ at the top of a specialized hierarchical network. Within this network Gawra served as an administrative, religious, and craft hub (Rothman 2002: 5-6). In support of the notion of a center, Frangipane argues that the landscape played a role in limiting urbanism in the piedmont around Tepe Gawra where the terrain may have restricted the expansion of agriculture beyond its natural limit restricting the region from producing enough agricultural surpluses to support a large conglomeration (Frangipane 2009: 135).
Research Aims
There is no doubt as to the significance of Tepe Gawra within the region but was the site truly interdependent as part of a large regional network for subsistence? That is, was the site serving a special function that excluded it from food production? There remains a debate as to whether or not there was a lower Chalcolithic period town around Tepe Gawra. Algaze notes (1993: 71-72) – based on personal communication with Gibson – that the mound was surrounded by a lower town. If this was true then the high mound would have been the acropolis of a larger town that still remains systematically unexplored. Rothman did not reject the idea of the presence of a lower town, however he remained skeptical with the absence of empirical data (Rothman 2002: 19).