2020
DOI: 10.1007/978-3-030-51148-7_4
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General Information and Hydrogeology of the Mediterranean and Dead Sea Coastal Aquifers and Their Relation with Their Base Level

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Cited by 3 publications
(3 citation statements)
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“…Its composition has evolved from predecessor lakes during late Neogene-Quaternary, subsequent fresh-water inflow and evaporation [22]. Its main tributary is the Jordan river, but also numerous ephemeral streams, wadis, aquifers, and submarine springs provide inflow to the lake [23]. The main groundwater bearing formations in the proposed Geopark area are the shallow alluvial aquifer of the Lisan formation of Tertiary and Quaternary origin, the mostly karstified limestone of the Amman-Wadi Es Sir aquifer of the Belqa and Ajlun groups of the Upper Cretaceous, the limestone/marl formations of the Ajlun group, the Kurnub sandstone aquifer of the Lower Cretaceous and parts of the Zarqa group of Triassic-Jurassic age as well as parts of the Ram (Disi) fossil groundwater aquifer of Cambrian origin [24,25].…”
Section: The Dead Sea and Its Surroundingsmentioning
confidence: 99%
See 1 more Smart Citation
“…Its composition has evolved from predecessor lakes during late Neogene-Quaternary, subsequent fresh-water inflow and evaporation [22]. Its main tributary is the Jordan river, but also numerous ephemeral streams, wadis, aquifers, and submarine springs provide inflow to the lake [23]. The main groundwater bearing formations in the proposed Geopark area are the shallow alluvial aquifer of the Lisan formation of Tertiary and Quaternary origin, the mostly karstified limestone of the Amman-Wadi Es Sir aquifer of the Belqa and Ajlun groups of the Upper Cretaceous, the limestone/marl formations of the Ajlun group, the Kurnub sandstone aquifer of the Lower Cretaceous and parts of the Zarqa group of Triassic-Jurassic age as well as parts of the Ram (Disi) fossil groundwater aquifer of Cambrian origin [24,25].…”
Section: The Dead Sea and Its Surroundingsmentioning
confidence: 99%
“…In the last decades, however, the human and natural impact has accelerated the changes in the natural system, leading to a rapid decline in the water level of the lake (Figure 2, based on satellite images from [28,29]). The shorelines of the lake suffer from an increase in natural hazards related to desertification and erosion, such as sinkholes, landslides, salt storms and flash floods, all of these are prominent examples that caused life and economic loss [23,[30][31][32][33][34][35][36] recently. The sad highlight in this context is the flash floods of Wadi Ma'in and Wadi Musa that caused high death tolls in Jordan in October 2018 [37].…”
Section: The Dead Sea and Its Surroundingsmentioning
confidence: 99%
“…The Dead Sea is located in the Jordan Rift Valley at 430 meters (1,410 feet) below sea level, it is the lowest point on Earth's surface, with a salinity of 342 grams per liter, which is roughly ten times saltier than the ocean, additionally, the Dead Sea is also the saltiest body of water on Earth and has a depth of 300 meters, making it the deepest hypersaline lake [1] [2] The Jordan River and a number of other smaller tributaries feed the Dead Sea [3]. The Dead Sea's water level has been dropping for ages, though.…”
Section: Introductionmentioning
confidence: 99%