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Vol 31
Pages:
48-52
Download volume:
RUS
Article
Geology

On the Origin of the “Chaos” of the Alupka Park

Authors:
I. F. Pustovalov
Date submitted:
1954-07-17
Date accepted:
1954-09-25
Date published:
1955-11-17

Abstract

Many works have been devoted to the geology of the Crimean Peninsula and the eruptive rocks developed here, most of which are based on personal observations of researchers. However, in a number of these works and in subsequent summaries of the Crimea to date, sometimes repeated incorrect conclusions of some researchers. Incorrect conclusions can be found both in specialized literature and in various reference books and guides for tourists and excursionists. Misconceptions include, in particular, the question of the formation of the chaos of Alupka Park, which is the subject of this article. In the light of these perceptions, the chaos is explained as the result of a grandiose collapse of eruptive rocks, moved a considerable distance down the slope from the place of its original occurrence.

Область исследования:
Geology
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References

  1. Borisyak A. A. About the rockfalls near Alupka in the Crimea. Collection of articles on geology in memory of I.V. Mushketov, St. Petersburg, 1905.
  2. Zaitsev A. M. Petrography of the Crimea. Yearbook of Geology and Mineralogy of Russia, 1908, vol. X, vol. 5-6; 1910, vol. XII, vol. 3-4, 7-8.
  3. Shcherbakov D. I. Green-stone rocks of Alupka. Izvestiya SPB. Polytechnic Institute, 1914, vol. XXIII.
  4. Luchitsky V. I. Petrographic Provinces of the USSR. Izd. of the Academy of Sciences of the USSR, 1936.
  5. Luchitsky V. I. Petrography of the Crimea. Regional Petrography. Izd. Institute of Geological Sciences, USSR Academy of Sciences, 1939, series 1, vol. 8.
  6. Meister A. K. Materials on petrography of the Crimea. Izvestiya Geologicheskogo Komiteta, 1908, vol. XXVII, No. 10.
  7. Pchelintsev V. F. From Yalta to Sevastopol. Guidebook of the Southern Excursion (Crimean ASSR) of the XVII International Geological Congress, 1937.

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