Abstract
Question Thegeologic formations of the study area, limestone and chalky limestone belong to upper Oxfordian and lower Kimeridgian. Two springs; Fontbout (70 l/s) and Favray (300 l/s) are situated in this area. Those two springs are witness to the existence of a water reservoir of important volume. The similarity of the results of their hydro-chemical analysis shows that they belong to the same aquifer. The direction of water flow in the studied area is NW–SE, the springs are located in the s...
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
