PALEORELIEF AND ESTIMATION OF GROUND WATER FLOW OF THE SELAVMASTARA WATERSHED (SOUTH-WESTERN AND SOUTHERN VERSANTS OF ARAGATS MASSIF)

Authors

  • R. S. Minasyan Chair of Geophysics, YSU, Armenia
  • V. P. Vardanyan Chair of Geophysics, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2008.42.2.133

Keywords:

Selavmastara River, paleorelief, Aragats Massif, natural ground water flow

Abstract

New data concerning paleorelief of the Selavmastara River watershed (South-Western and Southern versants of Aragats Massif). Relationships between paleo and recent watersheds, as well as distribution of ground water flow have been discovered. Following directions of ground water flow are singled out: Haykadzor–Souser–Arteni, Haykadzor–Bagravan–Arteni, Areg–Talin, Shgharshik–Ashnak and Davtashen–V. Bazmaberd. According to general water-balance calculations the natural ground water flow of the Selavmastara watershed is estimated up to 4.33 m3/day, out of which the concentrated flow is about 2.4–2.9 m3/day.

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Published

2008-05-07

How to Cite

Minasyan, R. S., & Vardanyan, V. P. (2008). PALEORELIEF AND ESTIMATION OF GROUND WATER FLOW OF THE SELAVMASTARA WATERSHED (SOUTH-WESTERN AND SOUTHERN VERSANTS OF ARAGATS MASSIF). Proceedings of the YSU C: Geological and Geographical Sciences, 42(2 (216), 133–136. https://doi.org/10.46991/PYSU:C/2008.42.2.133

Issue

Vol. 42 No. 2 (216) (2008)

Section

Geology

License

Copyright (c) 2008 Proceedings of the YSU

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This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

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