The debris flows in the Lozenska Mountain from Subboreal and Subatlantic periods

R. Kenderova, Nadezhda Kecheva
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Abstract

This research was conducted in June 2020 in connection with carrying out rescue archaeological excavations of a site recorded during the construction of the Sofia Ring Road, in the northern foothills of the Lozenska Mountain. On the basis of sedimentological studies of cultural layers, the flow of two mudflows with a southeast-northwest direction were proven at different depths. The discovered archaeological artefacts, mainly fragmented ceramic vessels, help to date these two flows through the Subboreal and the lower Sub-Atlantic. The first, located deeper than the modern surface flow, is dated after the 2nd millennium BC. (i.e., from the Subboreal). The second is the shallower stream, after the Roman era, II–IV centuries AD. (i.e., Sub-Atlantic). Both flowed into the Iskar River. Nowadays. it is difficult to determine their exact location. The archaeological sites from the two streams brought artifacts located in a south/southwest direction, closer to the northern slope of the Lozenska Mountain.
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亚滨海和亚大西洋时期洛岑斯卡山脉的泥石流
这项研究是在2020年6月进行的,与对洛赞斯卡山北麓索非亚环路建设期间记录的遗址进行的救援考古发掘有关。在文化层沉积学研究的基础上,证实了两种不同深度的东南-西北方向的泥流。发现的考古文物,主要是破碎的陶瓷容器,有助于确定亚北方和亚大西洋下游的两次流动的日期。第一个位于比现在的地表流更深的地方,可以追溯到公元前2000年之后。(即来自亚北方)。第二个是较浅的河流,在罗马时代之后,公元2 - 4世纪。(即亚)。两者都流入伊斯卡河。如今。很难确定它们的确切位置。来自两条河流的考古遗址将文物定位在南/西南方向,更靠近Lozenska山的北坡。
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