Abstract
The freshwater of the Judea Group aquifer that recharges on the crest of the Judea and Samria Mountain ridge flows east and west, defining two groundwater basins. At the foothills of both basins the freshwater encounters ancient saline or brackish water. The mode of interaction between the two water bodies within each basin is different, although both eventually discharge as brackish spring system. We describe these systems and identify the source of the higher salinity end members.
Original language | English |
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Article number | 07008 |
Journal | E3S Web of Conferences |
Volume | 98 |
DOIs | |
State | Published - 7 Jun 2019 |
Externally published | Yes |
Event | 16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Russian Federation Duration: 21 Jul 2019 → 26 Jul 2019 |
ASJC Scopus subject areas
- General Environmental Science
- General Energy
- General Earth and Planetary Sciences