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Revisiting the time of the last mass straightening bends on the upper Kama

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The scientists investigating channels and palaeographers still do not have a clear answer to the question when the last mass channel directional change processes started on the upper Kama and its tributaries. Distinct morphometrical parameters of numerous ox-bows, now located along relatively straight channel parts and at the same time absence of imperforation (ageing) signs do not allow to makes unambiguous conclusions about the duration of directional straightening of the river and major restructuring of the floodplain-channel complexes. Finding the answer to this question included: a) the analysis of historical documents and local folklore that mention change in the location (removal) of the Kama channel; b) comparison of the degree of the Kama ox-bows imperforation and peat overgrowing with the standard peat accumulation rates under the conditions of taiga landscapes. According to the results of complex analysis the following suggestion has been made – the beginning of the last mass straightening bends of the upper Kama was in the second half the Subatlantic period.
Rocznik
Strony
53--59
Opis fizyczny
Bibliogr. 34 poz., rys.
Twórcy
  • Perm State National Research University, Perm, Russia
  • Perm State National Research University, Perm, Russia
Bibliografia
  • 1. Borzenkova I.I., Budyko M.I. Ed., 1992. Climate change in the Cenozoic era. Gidrometeoizdat, St. Petersburg.
  • 2. Buravskaya M.N., Golubev Yu.V., Marchenko-Vagapova T.I., 2012. Partition of oxbow deposits in the outcrop of Sedkyrkesch (middle stream of the Vychegda river) based on a comprehensive analysis. Proceedings of Komi scientific center of the RAS Ural Department 2 (10), 84-97.
  • 3 Burov G.M., 1969. On search of ancient wooden objects and fishing equipment in the oxbow peatlands of lowland rivers. Brief Reports of the Institute of Archaeology, USSR Academy of Sciences 117, 130-134.
  • 4. Chagin G.N., 1999. History in memory of Russian peasants of the Middle Urals in the middle of 19th – early 20th century. Perm. University Press Perm.
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  • 6. Chalov R.S., 2011. Channel Study: theory, geography, and practice. V. 2. Morphodynamics of river channels. M. KRASAND.
  • 7. Chalov R.S., Chernov A.V., 1996. Kama basin zoning on factors and forms of channel processes display in medium and large rivers. Issues of Physical Geography and Geoecology of the Urals. Perm State University. Perm, 10-20.
  • 8. Chernov A.V., Harrison L.M., 1981. Paleogeographic analysis of the development of channel deformations wide of floodplain rivers in the Holocene (a case study of the upper and middle Ob). Bulletin of Moscow Society of Naturalists, Geology 5 (4), 97-108.
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  • 10. Dmitriev A., 1889. The Collection of historical articles and materials mainly about Perm Region, Issue 1. P.F. Kamensky’s Typography, Perm.
  • 11. Gening V.F., 1988. Ethnic history of the Western Urals at the turn of A.D. (Pyanoborskaya epoch of III century BC. II century A.D.). Nauka, Moscow.
  • 12. Inisheva L.I., Kobak K.I., Turchinovich I.E., 2013. The development of waterlogging process and accumulation rate of carbon in wetland ecosystems in Russia. Geography and natural resources 3, 60-68.
  • 13. Kargapolova I.N., 2006. Reaction of river channels on conductivity change and anthropogenic influence over the past century: Author’s abstract. Geography. Moscow State University Press, Moscow.
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  • 15, Krivoshchekov I.J., 1914. Geography and Statistics Dictionary of Cherdynsk district of Perm province. Edition of Cherdynsk uezd zemstvo. Electro- Typography „Trud”, Perm.
  • 16. Kurochkina M.V., 2011. Oral history of Kama villages in the system of local and family folklore (a case study of contemporary records). [Electronic resource] URL: http://elar.urfu.ru/bitstream/10995/20291/1/dc3-2011-17. pdf (access date: 15.01.2014)
  • 17. Makhinov A.N., 2006. Modern relief formation under alluvial accumulations. Dalnauka, Vladivostok.
  • 18. Maksimov E.V., 1995. Rhythms on Earth and in Space. Izdat Sant Petersburgskowo Universyteta, St. Petersburg.
  • 19. Nazarov N.N., 2009. Drainage variability and channel processes in Prikamye. 24 Plenary interuniversity coordination meeting on the problem of erosion, fluvial and mouth processes. ASU Press, Barnaul, 155-157.
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  • 24. Oborin V.A., 1967. Orel-town as the Russian defensive pivot in the Prikamye of 16th-17th centuries. Scholarly Notes of Perm University 10 (3), 23-36.
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  • 29. Spirin L.N., Shmyrov V.A., 1984. Main features of the Holocene tectonics and paleogeography of the Perm Pre-Urals. Physical and geographical foundations for development and distribution of productive forces of nonblack soil Urals. Perm University Press, Perm, 107-112.
  • 30. Surmach G.P., 1992. Relief formation, forest-steppe zone formation, modern erosion and anti-erosion measures.VNIALMI, Volgograd.
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  • 33. Zawadzky A.S., Kargapolova I.N., Chalov R.S., 2002. Stages of free bends development and their hydrological and morphological analysis. Vestnik MGU, Ser. Geography 2, 17-22.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-ac0e5920-ef02-4d57-ac5c-78070deb0ddf
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