Summary
The present work characterizes the reactivation of existing landslides and formation of new ones on the shores of the Angara reservoir; it describes different types of deformations in the superficial deposits and bedrock; the role of erosion is estimated.
Résumé
L’article décrit les caractères de la réactivation des glissements de terrain existants et de la formation de nouveaux glissements de terrain sur les rives des retenues d’eau de l’Angara. Il décrit divers types de déformations qui affectent les roches meubles et le bedrock; il évalue le rôle de l’érosion.
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References
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TRZHTSINSKII YU.B. — BUDZ M.D. — ZARUBIN N.E. (1969): Opolzni, seli, termokarst v Vostochnoi Sibiri i ikh inzhenernogeologicheskoe znachenie (in Russian). Nauka, Moscow, 134 p.
TRZHTSINSKII YU.B. (1974) : Rutschungen und Böschungsdeformationen in Flusstälern Ostsibiriens. Zschr. für geologische Wissenschaften, 2,4, Berlin, 457–465.
BRATSKOE VODOKHRANILISCHE. INZHERNERNAYA GEOLOGIYA TERRITORII (1963), (in Russian). Nauka, Moscow, 247 p.
UST-ILIMSKOE VODOKHRANILISCHCHE. PODZEMNYE VODY I INZHENERNAYA GEOLOGIYA TERRITORII (1975), (in Russian). Nauka, Novosibirsk, 211 p.
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Institute of the Earth’s Crust, Lermontova 128, 664033 Irkutsk-33, USSR.
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Trzhtsinskii, Y.B. Landslides along the Angara reservoirs. Bulletin of the International Association of Engineering Geology 17, 42–43 (1978). https://doi.org/10.1007/BF02634674
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DOI: https://doi.org/10.1007/BF02634674