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The Gorge of the Angitis River at “Stena Petras” Near the Alistrati Cave. A Magnificent Piece of Natural Architecture in Eastern Macedonia, Greece

  • Theodoros AstarasEmail author
Chapter

Abstract

The Angitis river principally drains the Drama basin and also the former marshes of Philippi. It then flows in the spectacular gorge called “Stena Petras”, just near the almost horizontal Alistrati caves and enters into the adjacent plain (basin) of Serres, where it joins the Strymon (Struma) river, discharging southwards to the Strymon gulf. The Angitis gorge and Alistrati caves are underlain by the Rhodope marbles. The outcrops of Alistrati marbles rise up to 273 m and are strongly jointed and fissured, mainly by NW-SE and NE-SW systems, with the NE-SW system being more dominant. Some faults oriented to NW-SE and NE-SW also occur in the marbles (Dimadis and Zachos, 1986).

Keywords

Drainage Line Fluvial Process Underground Tunnel Cave Entrance Small Meander 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. Astaras, T. 1982–1983. On the stream capture between the tributaries “Megalo Potami” and “Xiropotamos” of the Gallikos river. Geomorphological significance of stream captures to the study of fluvial placers and in general to landscape evolution of a certain area. Ann. Geol. Pays Hellen., 31: 725–740, Athens (in Greek with English summary).Google Scholar
  2. Astaras, T. 1988. A Karst Stream subterranean “autopiracy” of Angitis river flowing in the gorge of Stena Petras, near Alistraty, East Macedonia, Greece: A contribution to the evolution of the epigenetic valley of Angitis river. Ann. Geol. Pays Hellen., 33: 463–473.Google Scholar
  3. Bogli, A. 1964. Mischungskorrosion-ein Beitrag zum Verkastrungsproblem; Erdkunde, 18: 83–92.Google Scholar
  4. Dimadis, E. & Zachos, S. 1986. Geological map of Rhopope massif, Scale 1:200.000. Institute of Geology and Mineral Exploration (I.G.M.E.), Xanthi branch.Google Scholar
  5. Hellenic Army Geographical Service (H.A.G.S.) 1945, 1968, 1969. Topographic maps of Prosotsani and Drama, scale 1:50.000 (1969); and airphotos of approx. scale 1:45.000 (1945) and 1:55.000 (1968) Athens.Google Scholar
  6. Jennings, J., Brusch. J., Nicoll, S. & Spate, A. 1976. Karst stream self capture at London Bridge, Bura Creek, N.S.W., Aust. Geogr., 13: 238–249.CrossRefGoogle Scholar
  7. Jennings, J. 1985. Karst Geomorphology. Basil Blackwell, Oxford, UK: 88–94.Google Scholar
  8. Kaye, C. 1957. The effect of solvent motion on limestone solution. Journ. Geol., 65: 35–46.CrossRefGoogle Scholar
  9. Palmer, A. 1982. Geomorphic interpretation of karst features, Summary proceedings: 9. Thirtheent Annual Geomorphological Symposium (USA) (A continuation of SUNY Binghampton Geomorphology Symposium series), entitled “Groundwater as a Geomorphic agent” Troy, N.Y. (USA).Google Scholar
  10. Rhoades, R. & Sinacori, M. 1941. Pattern of ground-water flow and solution. Journ. Geol., 49: 785–94.CrossRefGoogle Scholar
  11. Symeonidis, N., Dilaras, G., Tsimbanis, E., Papadopoulos G. & Constantacatos E. 1977. The cave of Alistrati in Serres (Greece). Bull. Greek Speleol. Soc., 14: 64–81, Athens.Google Scholar
  12. Vavliakis, E., Psilovikos, A. & Sotiriadis, L. 1985. The epigenetic valley of Angitis river in relation with the evolution of the basins in Serres and Drama. I.G.M.E., Geol. and Geoph. Research, Special issue, 1986: 5–14. Athens.Google Scholar
  13. Whittow, J. 1986. Dictionary of Physical Geography. Penguin Books Ltd, England: 592.Google Scholar
  14. Williams, P. 1969. The geomorphic effects of ground water. In Chorley R. (ed.), Water, Earth and Man, London, Methuen & Co. Ltd: 269–284.Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2010

Authors and Affiliations

  1. 1.Department of Physical and Environmental Geography, School of GeologyAristotle University of ThessalonikiThessalonikiGreece

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