Issue 10
Issue 10
Ashkawta Rash(ئەشکەوتە ڕەش) is a Palaeolithic cave site located. 35 km northwest of the city of Slemani, near the Bazian Gates.
The Shahrizor Plain is one of the ideal fields for tracking the transition from Neolithic village life in the Fertile Crescent to Urbanisation which occurred in Mesopotamia because of its geographical location connecting the mountainside valleys along the Zagros and the downstream Diyala River that flows into the Tigris. Our field project aims to obtain archaeological materials to unveil this process. Following the first excavations at Shakar Tepe conducted in 2019, we excavated two additional areas at this site in 2023, including one of the three satellite mounds that were newly identified around the main mound. The cultural remains of the Late Halaf settlement uncovered from Operation B at Shakar Tepe II date back to approximately 5600–5400 calBC. On the other hand, Operation C at Shakar Tepe I yielded a thick deposit of the Late Chalcolithic occupations dated to ca. 3800–3600 calBC. The recovered materials fill the time ranges in the late prehistoric chronology of the site and will contribute to our understanding of the historical role of this region in the transition from Neolithisation to Urbanisation.
In the late third and early second millennium bc, the large plain known today as the Shahrizor and its surrounding region, located in the province of Suleymaniyah in Iraqi Kurdistan, likely formed an important region of the kingdom of Simurrum (Fig. 31.1; Altaweel et al. 2012). For much of the remaining second millennium bc and into the irst two centuries of the irst millennium bc, the region was a contested border zone between northern and southern Mesopotamian kingdoms or became splintered into small kingdoms.
Issue 10