Temperature-composition-depth relationship in Rift Valley hot springs: Hammat Gader, northern Israel

Avraham Starinsky*, Amitai Katz, Dov Levitte

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

22 Scopus citations

Abstract

The Hammat Gader (El-Hamma) springs constitute a rift valley hot-spring system. The five springs which belong to this complex are distinguished by temperatures of 25, 28, 36, 42 and 50°C and salinities of between 700 and 1400 mg/l. With one exception, the salinity of the spring waters increases with temperature. A model is presented which explains the chemical composition of the individual springs by mixing of an ancient, Ca-chloridic, rift brine with present-day meteoric waters. The water temperatures are dictated by the regional geothermal gradient, which is calculated for the investigated area from deep-drilling data. The model is in good accordance with previously published isotopic and rare-gas data. A model suggested earlier for the Hammat Gader springs is examined, discussed and rejected on geochemical, spatial and hydrogeological grounds.

Original languageEnglish
Pages (from-to)233-244
Number of pages12
JournalChemical Geology
Volume27
Issue number3
DOIs
StatePublished - Nov 1979

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