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The aquifer goes down to the Mediterranean Sea, beginning in the south and descending towards north-western Israel. [5] The water recharges in the West Bank mountains and ends in the springs of the Yarkon River at Antipatris , and Taninim Springs on the coastal plain of the Mediterranean.
The following is a partial list of aquifers around the world. ... Yarkon-Taninim Aquifer, also known as Mountain Aquifer (Israel-Palestine) Europe
The Yarkon River, also Yarqon River or Jarkon River [1] (Hebrew: נחל הירקון, Nahal HaYarkon; Arabic: نهر العوجا, Nahr al-Auja), is a river in central Israel. The source of the Yarkon ("Greenish" in Hebrew) is at Tel Afek (Antipatris) , north of Petah Tikva .
The Mountain Aquifer consists of three basins: The Western Aquifer , in Israel called the Yarkon-Taninim Aquifer , [ 7 ] is the largest one, with an annual safe yield of 362 million cubic metres (mcm), based on average annual estimate, (of which 40 mcm are brackish).
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Aquifers of the United States Withdrawal rates from the Ogallala Aquifer.. This is a list of some aquifers in the United States.. Map of major US aquifers by rock type. An aquifer is a geologic formation, a group of formations, or a part of a formation that contains sufficient saturated permeable material to yield significant quantities of water to groundwater wells and springs.
The North-Eastern Aquifer, in Israel called the "Gilboa-Bet She'an Aquifer" or "Schechem-Gilboa Aquifer", [47] has an annual safe yield of 145 mcm (of which 70 mcm are brackish). Almost 100% of its water comes from precipitation falling within the West Bank area, but then flows underground in a northerly direction into the Bisan (Bet She'an ...
Wadi Qana (Arabic: وادي قانا, romanized: wādī qānā, Hebrew: נחל קנה, romanized: Nahal Qana) [a] is a wadi with an intermittent stream meandering westwards from Huwara, south of Nablus, in the West Bank, Palestine, down to Jaljulia in Israel, from where it flows into the Yarkon River, of which it is a tributary.