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Propagation of coastal slope deformations at Taukliman, Bulgaria

Propagation de deformations de pente littorales a Taukliman, Bulgarie

  • 26e Congrès Géologique International Paris, France, 7–17.07.1980
  • Published:
Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur Aims and scope Submit manuscript

Summary

In a coastal region of high seismicity a giant block-type slope deformation is being propagated in sliding cycles due to the action of creep in a bed of clay, deep under a brittle rock platform.

Résumé

La déformation géante de pente en blocs se propage en cycles de glissements par une action de fluage au fond du plateau rocheux dans une rayon sismique.

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References

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Author information

Authors and Affiliations

  1. Institute of Geology and Geotechnics, Engineering Geology Dept., Czechoslovak Academy of Sciences, Boční II, 141 32, Praha 4, CSSR

    Košťák B.

  2. Geotechnical Laboratory of the Bulgarian Academy of Science, Academician Georgi Bončev, Bl. II, 1113, Sofia, Bulgaria

    Avramova-Tačeva Elka

Authors
  1. Košťák B.
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  2. Avramova-Tačeva Elka
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Additional information

In memoriamProfessor Bojan Kamenov (Nov. 22, 1979), who discussed first the deformation at Taukliman (Kamenov et al. 1969, 1977) and promoted the joint research of Czechoslovak and Bulgarian Academies of Sciences in this field (Kamenov, Pašek et al. 1973), so that the first proof of the present activity of the deformation could be given (Košťák, Avramova-Tačeva 1977).

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Košťák, B., Avramova-Tačeva, E. Propagation of coastal slope deformations at Taukliman, Bulgaria. Bulletin of the International Association of Engineering Geology 23, 67–73 (1981). https://doi.org/10.1007/BF02594728

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