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Gaprindashvili, M., Tsereteli, E., Gaprindashvili, G., & Kurtsikidze, O. (2021). Landslide and Mudflow Hazard Assessment in Georgia. In F. L. Bonali, F. Pasquaré, Mariotto, & N. Tsereteli (Eds.), Building Knowledge for Geohazard Assessment and Management in the Caucasus and other Orogenic Regions (pp. 265-279). Springer.
https://doi.org/10.1007/978-94-024-2046-3_14

has been cited by the following article:

• TITLE: Field and Laboratory Study of Accumulated Debrisflow-Forming Solid Mass Sediment on the Example of River Chokheltkhevi (Mtskheta-Mtianeti Region, Georgia)

  AUTHORS: Zurab Varazashvili, Zurab Kakulia, George Gaprindashvili, Goga Chakhaia, Irakli Ramishvili

  KEYWORDS: Georgia, Geology, Debrisflow, Mudflow, Laboratory

  JOURNAL NAME: Journal of Geoscience and Environment Protection, Vol.12 No.6, June 27, 2024

  ABSTRACT: The paper presents the results of the field and laboratory research carried out in the Chokheltkhevi river basin, according to which the sediment-forming solid mass accumulated in the bed of the Chokhelthkhevi river was recorded and its granulometric and chemical composition, as well as physical-mechanical characteristics, were studied. Based on the results of the research, it can be said that in the debrisflow channel of the Chokheltkhevi River, coarse and sandy-clay soils are mainly accumulated, which represent an unstable mass for the expected debrisflow in the gorge, which, together with other geological, hydrological and climatic factors, helps to increase the scale of the expected ecological danger. According to the results of the laboratory research, it can be concluded that the soil accumulated in the drainage channel is low in ion concentration, and the humus content in it is minimal, which indicates the possibility of easy displacement of the solid mass accumulated in the drainage channel and, accordingly, the risk of a catastrophic debrisflow.