GROUNDWATER BEHAVIOR IN THE CENTRAL PART OF YEREVAN CITY

Authors

  • Zh. A. Achoyan Chair of Hydrogeology and Engineering Geology, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2012.46.3.029

Keywords:

outcrop cone, lava flow, water contour map, groundwater monitoring

Abstract

Conducted short-time groundwater monitoring in the central part of Yerevan, especially in the section between stations named "Yeritasardakan" and "Zoravar Andranik" indicated that groundwater table is shallow and interferes with metro. For a rational reconstruction of the metro first the water table level should be lowered. To maintain the level of groundwater at relatively low depths it is required to develop and implement the necessary engineering measures.

Downloads

Published

2012-12-10

How to Cite

Achoyan, Z. A. (2012). GROUNDWATER BEHAVIOR IN THE CENTRAL PART OF YEREVAN CITY. Proceedings of the YSU C: Geological and Geographical Sciences, 46(3 (229), 29–35. https://doi.org/10.46991/PYSU:C/2012.46.3.029

Issue

Vol. 46 No. 3 (229) (2012)

Section

Geology

License

Copyright (c) 2012 Proceedings of the YSU

Creative Commons License

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