Morphology and modern functioning of chalky polygons in Obshchy Syrt; southeastern East European Plain
https://doi.org/10.31857/S0435428122030130
Abstract
Specific landscapes defined as chalky polygons can be found formed on chalky rocks under a continental climate across the south-east of the East European Plain. Theses landscapes are characterized by polygonal microrelief and spotting, outwardly resembling tundra medallions. Such landscape complexes are unique and practically not investigated. Our investigation showed a number of relict cryogenic features: polygonal relief with the polygon side averaging 5 m; ground wedges associated with hollow-like depressions between polygons; cryoturbation of soil profiles, and paleocryotextures. The results suggested the paleofrost genesis of chalky polygons. Chalky polygons were found to be a kind of relict cryogenic relief formed in the Valdai Cryochron in conditions of cryoarid climate, permafrost, frost cracking of soils and the growth of polygonalvein ice.
Keywords
About the Authors
A. G. RyabukhaRussian Federation
D. G. Polyakov
Russian Federation
I. D. Streletskaya
Russian Federation
I. V. Kovda
Russian Federation
References
1. Butakov G.P. Pleistotsenovyi periglyatsial Russkoi ravniny (Pleistocene Periglacial in the East of the Russian Plain). Kazan: Kazan University (Publ.), 1983. 143 p. (in Russ.)
2. Geograficheskii atlas Orenburgskoi oblasti (Geographical Atlas of the Orenburg Region). Orenburg: IS UB RAS (Publ.), 2020. 159 p. (in Russ.)
3. Kliment’ev A.I., Chibilev A.A., Blokhin E.V., and Groshev I.V. Krasnaya kniga pochv Orenburgskoi oblasti (The Red Data Book of Soils of the Orenburg Region). Yekaterinburg: UB RAS (Publ.), 2001. 294 p. (in Russ.)
4. Mikhno V.B. Melovye landshafty Vostochno-Evropeiskoi ravniny (Cretaceous Landscapes of the East European Plain). Voronezh: Petrovskii Skver (Publ.), 1993. 232 p. (in Russ.)
5. Popov A.I. Merzlotnye yavleniya v zemnoi kore (kriolitologiya) (Permafrost phenomena in the Earth’s crust (Cryolithology)). Moscow: MGU (Publ), 1967. 304 p. (in Russ.)
6. Problemy geoekologii i stepevedeniya (Problems of the Geoecology and the Steppe Science). Yekaterinburg: UB RAS (Publ.), 2010. Vol. 2. 364 p. (in Russ.)
7. Vandenberghe J., French H., Gorbunov A., Marchenko S., Velichko A., Jin H., Cui Z., Zhang T., and Wan X. The Last Permafrost Maximum (LPM) map of the Northern Hemisphere: permafrost extent and mean annual air temperatures, 25–17 ka BP. Boreas. 2014. Vol. 43. № 3. P. 652–666. https://doi.org/10.1111/bor.12070
8. Velichko A.A. Prirodnyi protsess v pleistotsene (Natural Process in the Pleistocene). Moscow: Nauka (Publ.), 1973. 256 p. (in Russ.)
9. Voskresensky S.S., Leontiev O.K., and Spiridonov A.I. Geomorfologicheskoe raionirovanie SSSR i prilegayushchikh morei (Geomorphological zoning of the USSR and adjacent seas). Moscow: Higher School (Publ.), 1980. 343 p. (in Russ.)
10. Chibilev A.A., Musikhin G.D., Pavleichik V.M., Petrishchev V.P., and Sivokhip Zh.T. Geologicheskie pamyatniki prirody Orenburgskoi oblasti (Geological Nature Monuments of the Orenburg Region). Orenburg: Book House (Publ.), 2000. 400 p. (in Russ.)
Review
For citations:
Ryabukha A.G., Polyakov D.G., Streletskaya I.D., Kovda I.V. Morphology and modern functioning of chalky polygons in Obshchy Syrt; southeastern East European Plain. Geomorfologiya. 2022;53(3):128-133. (In Russ.) https://doi.org/10.31857/S0435428122030130