Millstones from Revne at Bukovyna

IF 0.3 4区 历史学 0 ARCHAEOLOGY
S. Gorbanenko, Mykola Ilkiv, Liubomyr Mykhailyna, Bohdan Ridush
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Abstract

In the article stones from light hand millstones from Revne group of settlements of the 8th — 10th centuries left by the Slavs — bearers of the Raiky archaeological culture are published (fig. 1; 2). The lithological composition of rocks was determined. The millstones were made of two types of rocks: 1 — organogenic-detrital limestone, layered, cavernous, grayish-yellow (fig. 3: 1, 2); 2 —organogenic detrital limestone, massive, finely cavernous, yellowish-gray (fig. 3: 3). Such rocks are typical for the area of Revne agglomeration. This confirms the local origin of the raw materials (fig. 4). The rocks can be easily processed with iron tools. At the same time, they are strong enough and not prone to fracture and small fracturing. An average density of limestone is 2.7 g/cm3. Millstones are widely known from the materials of the Raiky culture sites (fig. 5). Probably, in all cases, local raw materials were used. On this background mention of the finds of grain graters occurs in scientific literature less often. In the materials of Revne agglomeration of the 8th — 10th centuries grain graters are unknown. Discovered millstones are divided into «spoilage» or blank (fig. 3: 1), bed stone (fig. 3: 2) and runner stone (fig. 3: 3). There is a sufficient basis for the general reconstruction of a light hand millstone. It consists of archaeological finds (stones and occasionally other parts made of iron and wood), ethnographic and iconographic data (fig. 6). All these sources were qualitatively analysed by R. S. Minasyan and he proposed his own classification. Today, we consider his work to be the most generalizing and reliable basis for descriptive reconstruction of the millstone. However, the classification itself is not quite user-friendly. Therefore, we offer systematization as a combination of main features. It is presented in a tabular form (fig. 7). According to the proposed systematization, the millstones from Revne can be characterized as ІІ.2.A—B — bed stone with a hole and a wooden pin (not preserved), with runner stone and rind (not preserved), with a hole for a handle of indeterminate length (not preserved).
来自Revne在Bukovyna的Millstone
在文章中,斯拉夫人留下的8世纪至10世纪Revne定居点的轻型手工磨石中的石头——Raiky考古文化的传承者发表了(图1;2)。岩石的岩性成分已确定。磨石由两种类型的岩石组成:1-有机碎屑石灰岩,层状,洞穴状,灰黄色(图3:1,2);2-有机质碎屑石灰岩,块状,细海绵状,黄灰色(图3:3)。这种岩石是Revne凝聚区的典型岩石。这证实了原材料的当地来源(图4)。用铁工具可以很容易地加工这些岩石。同时,它们足够坚固,不容易破裂和小破裂。石灰石的平均密度为2.7g/cm3。磨石从Raiky文化遗址的材料中广为人知(图5)。可能,在所有情况下,都使用了当地的原材料。在这种背景下,科学文献中很少提及谷物磨碎机的发现。在8-10世纪的Revne凝聚材料中,谷物磨碎机是未知的。发现的磨石分为“变质”或空白(图3:1)、床石(图3:2)和转轮石(图3:3)。轻型手工磨石的一般重建是有充分依据的。它包括考古发现(石头,偶尔还有其他铁和木制成的部分)、人种学和图像学数据(图6)。R.S.米纳相对所有这些来源进行了定性分析,并提出了自己的分类。今天,我们认为他的作品是对磨石进行描述性重建的最普遍和最可靠的基础。然而,分类本身并不十分方便用户。因此,我们将系统化作为主要特征的组合。它以表格形式呈现(图7)。根据所提出的系统化,Revne的磨石可以被描述为?.2.A-B——带孔和木钉的床石(未保存),带转轮石和外皮的(未保存的),带不确定长度的把手孔的(未保留的)。
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
ARCHAEOLOGY
ARCHAEOLOGY ARCHAEOLOGY-
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