The Late Halafian Lithic Industry of Tell Kashkashok I, the Upper Khabur, Syria

Q4 Social Sciences
Orient Pub Date : 2018-09-30 DOI:10.5356/orient.53.1
Y. Nishiaki
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引用次数: 2

Abstract

This paper presents the flaked flint and obsidian assemblages excavated in 1990 from Tell Kashkashok I, northeast Syria. Albeit a small collection selected from limited excavations, they represent one of the rare Halafian lithic assemblages that help define the lithic craft tradition of the Syrian Jazireh during this period. The analysis shows that the assemblages belong to the Late Halafian industry characterized by the common use of the following: imported raw materials, elaborate techniques for blank production including pressure debitage, snapped rectangular blades and crescent-shaped flake-blades with backed edges for sickle elements, bifacial knives made on tabular flint, and the rare manufacturing of burins. The literature survey reveals that these traits are recognized in the Early-Middle Halafian and the Late Pottery Neolithic industries of the Syrian Jazireh, suggesting that the Halafian lithic tradition of the region was established through indigenous cultural development. At the same time, the survey reveals that they do not occur in the neighboring regions as a package but in different combinations by regions. Future research into those regionally different patterns would provide a means to interpret the complex Halafian cultural dynamics from a perspective not examined in prior research that emphasized pottery analysis.
上哈布尔,叙利亚,Tell Kashkashok I的晚期哈拉菲石器工业
本文介绍了1990年在叙利亚东北部Tell Kashkashok I发掘的片状燧石和黑石组合。尽管它们是从有限的挖掘中挑选出来的一小部分,但它们代表了罕见的哈拉菲石器组合之一,有助于定义这一时期叙利亚贾兹雷的石器工艺传统。分析表明,这些组合属于晚期哈拉菲亚工业,其特点是以下方面的共同使用:进口原材料、精细的坯料生产技术,包括压力脱苦、用于镰刀元件的折断矩形刀片和带背边缘的新月形薄片刀片、用板状燧石制成的双面刀,以及罕见的墓葬制造。文献调查显示,这些特征在叙利亚贾兹雷的早中哈拉菲和晚陶器新石器时代工业中得到了认可,这表明该地区的哈拉菲石器时代传统是通过土著文化发展建立起来的。同时,调查显示,它们并不是作为一个整体出现在邻近地区,而是按地区以不同的组合出现。未来对这些区域不同模式的研究将提供一种手段,从以前强调陶器分析的研究中没有考察过的角度来解释复杂的哈拉菲文化动态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Orient
Orient Social Sciences-Development
CiteScore
0.20
自引率
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