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Vol 48 Iss. 2
Pages:
134-136
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RUS
Article

Plastic Landslides of the Kakheti Ridge

Authors:
R. Z. Khatashvili
Date submitted:
1964-08-28
Date accepted:
1964-10-26
Date published:
1965-05-05

Abstract

Displacements of earth masses, called landslides, are very widespread on the territory of Georgia. There is almost no region where landslide phenomena would not bring harm to the national economy, annually destroying tens of thousands of hectares of arable land and pastures, forests, destroying railroads and highways.The most characteristic is the landslide region of the Kakheti Range - the watershed of the Iori and Alazani valleys. The northern part of the region starts from the Borbala Mountain and extends meridionally across the fold structures of the B. Caucasus. The southern part - the Tsiv-Gomborski ridge - starts from Akhmet village and runs parallel to the pan-Caucasian extension of the folds ...

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References

  1. Janelidze A.I. Tbilisi Landslides and Their Geological Significance. Reports of the Scientific Session of the Tbilisi University, No. 1, 1947.
  2. Janelidze A. I. About the Late Quaternary Conglomerates Formation of the Kakheti Ridge. Reports of the Academy of Sciences of Georgia. Communications of the AS of the Georgian SSR, vol. X, No. 2, 1949.
  3. Karstens I.E. Materials to the paleogeography of the Kakheti Ridge and the Alazani River Valley. Proc. Neft. geol.-prospecting institute, series B, vol. 47, 1934.
  4. Tsereteli D. History of relief development and paleogeography of the Alazani River valley. Vesti. Academy of Sciences of Georgia. SSR, vol. XV, No. 7, 1954.
  5. Maruashvili L. I. Geomorphologic sketch of the Gombor or Kakheti Range in eastern Georgia. Proc. of Vakhushti Institute of Geography, vol. VI, 1955.
  6. Changoshvili G. Z. Landslides of the north-eastern slope of the Gombor Ridge. Theses of reports of the VI scientific conference of post-graduate students and young researchers of the AS of the Georgian SSR.
  7. PH of the AS of Georgia. SSR, 1955.

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