The article presents findings of complex interdisciplinary researches of a group of sopkas in the Plakun terrain feature. The monument is part of the Staroladozhky archaeological complex located in Volk- hovsky district, Leningrad region, 120 km east of St. Petersburg. The sopkas are one of the main landmarks of the region. They are high steep embankments 11 – 30 m in diameter and 3 – 8 m high. They date back to the 8th – 10th centuries. The ethnicity of their makers is uncertain. Historiographical data suggest that the monu- ment consisted of 6 sopkas divided into clusters 3 embankments each. In 1955, the southernmost sopka was excavated for demolition. In 2022 – 2023, scheduled scientific researches and Russian Science Foundation Grant No. 23-18-00515 implied an aerial laser scanning of the monument territory. The area was scanned at the attitude of 70 – 90 m with a DJI Matrice 300 RTK drone and an L1 LiDAR from a DJI D-RTK ground station. The coordinates are referenced in LCS-47 Zone 2 with Spectra Epoch 50 GNSS receiver and amended by Geospider survey station network. The findings allow to distinguish a range of small hills in two groups of remaining sopkas. The standard presentation of Digital Elevation Model (DEM) clearly distinguishes 5 remaining large rounded embankments and piles of the excavated southernmost one. However, the research matches several relief color gradations. The study combines several DEM copies in QGIS geographic information system. Consequently, it is revealed that the chain of remaining embankments includes 4 rounded elevations. 3 of them resemble ploughed embankments. In 2023, two identified elevations were studied with OKO-2 ground penetrating radar equipped with a probe antenna which radiates 100 and 700 MHz pulses. The research involves gridding the area of the alleged lost ploughed sopkas and one apparent embankment. The profiles of the site were double-scanned. The radargrams reveal common structure features in the hills and sopka such as contrast mound foundations, heterogeneous centers, multi-layered structures and local depressions in the top layer around 0.5 meters thick. The findings suggest that 3 out of 4 hills can be viewed as demolished embank- ments of a sopka burial. The fourth one requires additional research.
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