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Vol 48 Iss. 2
Pages:
134-136
Download volume:
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 do not cause harm to the national economy, annually destroying tens of thousands of hectares of arable land and pastures, forests, and railways 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 Mount Borbala and extends meridionally across the fold structures of the Greater Caucasus. The southern part – the Tsiv Gombori ridge – starts from Akhmeta village and runs parallel to the general Caucasian strike of the folds ...

Область исследования:
(Archived) Without section
Funding:

None

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References

  1. Janelidze A. I. Tbilisi Landslides and Their Geological Significance. Doklady nauchnoy sessii Tbilisskogo universiteta, No. 1, 1947.
  2. Janelidze A. I. About the Late Quaternary Conglomerates Formation of the Kakheti Ridge. Soobshcheniya Akademii Nauk Gruzinskoy SSR, vol. X, No. 2, 1949.
  3. Karstens I. E. Materials to the paleogeography of the Kakheti Ridge and the Alazani River Valley. Trudy Neftyanogo geologo-razvedochnogo instituta, series B, vol. 47, 1934.
  4. Tsereteli D. History of relief development and paleogeography of the Alazani River valley. Vestnik Akademii Nauk Gruzinskoy SSR, vol. XV, No. 7, 1954.
  5. Maruashvili L. I. Geomorphologic sketch of the Gombor or Kakheti Range in eastern Georgia. Trudy Instituta geografii imeni Vakhushti, vol. VI, 1955.
  6. Changoshvili G. Z. Landslides of the north-eastern slope of the Gombor Ridge. Tezisy dokladov VI nauchnoy konferentsii aspirantov i molodykh nauchnykh rabotnikov AN Gruzinskoy SSR. Izdatel'stvo Akademii Nauk Gruzinskoy SSR, 1955.

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