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2. Cilt - Kültür ve Turizm Bakanlığı

2. Cilt - Kültür ve Turizm Bakanlığı

2. Cilt - Kültür ve Turizm Bakanlığı

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of any associable cultural finds, dating this building is based on indirectevidence: the small collection of pottery mixed in with the foundation gra<strong>ve</strong>l,and its stratigraphic context within the OP. U sequence. They would assignthis massi<strong>ve</strong> construction to Period 5 (late sixth - early fifth century B.C.), yetanother phase previously attested only in OP. E/H 23 .The imposing proportions of this Period 5 building argue for a publicand/or military function. The mound’s current south slope corresponds toits location and steepness in antiquity, according to a series of Middle IronAge retaining walls built against it (sounding ST); and the building’s southernfoundations 124, because wider (w = 1.40 m.) than the others, would suit asexterior wall for a fortress or fortified enclosure. Kinet’s Period 5 coincidedwith the onset of Achaemenid Persian interests in Cilicia, a region weakenedby Neo-Babylonian deportations earlier in the sixth century, and open to thefounding of Persian military outposts 24 . OP. U’s Period 5 building wouldreflect this policy in architectural terms.Below this building and its intrusi<strong>ve</strong> construction techniques, earlier LateIron (Periods 6-7) and Middle Iron (Periods 8-9) deposits were reco<strong>ve</strong>red onlyfrom the soundings ST and DS. They included thick le<strong>ve</strong>lling fills known fromother trenches at the start of Periods 7 (se<strong>ve</strong>nth c. B.C.) and 8 (later eighthcentury B.C.), when site-wide renewal projects were undertaken. Period 8’sfill, associated with a Neo-Assyrian installation at Kinet, was richly packedwith sherds of late Middle Iron Age type from Period 9 destruction debris:painted Cypro-Cilician wares, Black-on-Red, and Late Geometric Greekimports (Pendant Semi-Circle skyphoi) (Fig. 15). Earlier Middle Iron types(Periods 11 and 10) preceded them down another 1.5 m.The earliest cultural deposits were poorly characterized, since soundingDS 177/180 was at this depth reduced to 3 m 2 , half of its initial size. Its limitedsherd sample may date to Kinet’s Early Iron Period 12; and an underlyingwall, at the base of the sounding, to Kinet’s final Late Bronze Period 13.2(below a non-architectural sequence of ca. <strong>2.</strong>5 m.). These attributions arehighly tentati<strong>ve</strong>. If correct, corresponding le<strong>ve</strong>ls on the west slope were indeedslightly elevated (by ca. 1.2 m.) abo<strong>ve</strong> the rest of the mound. This topographicaspect of the Late Bronze mound was already suggested by a sharp incline inthe eastern part of OP. E/H. It recei<strong>ve</strong>d some support from OP. U’s lowestle<strong>ve</strong>ls this season.23 Gates 1999: 323-325.24 Gates 1999; Casabonne 2004.360

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