Samakh Stream
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Samakh Stream
Samakh can mean: * Samakh, Tiberias, an depopulated former Palestinian village at the south end of the Sea of Galilee in Israel * Samekh Samekh (Phoenician ''sāmek'' ; Hebrew ''samekh'' , Syriac ''semkaṯ'') is the fifteenth letter of the Semitic abjads, including the Hebrew alphabet. Samekh represents a voiceless alveolar fricative . Unlike most Semitic consonants, the pro ...
, a letter in the Hebrew and various other Semitic alphabets {{Disambig ...
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Samakh, Tiberias
Samakh ( ar, سمخ) was a Palestinian people, Palestinian Arab village at the south end of Lake Tiberias (the Sea of Galilee) in Ottoman Galilee and later Mandatory Palestine (now in Israel). It was the site of Battle of Samakh (1918), battle in 1918 during World War I. Between 1905 and 1948, the town was an important stop on the Jezreel Valley railway and Hejaz railway, being the last effective stop in the Mandatory Palestine, British Mandate of Palestine (the station at Al-Hamma, Tiberias, al-Hamma was geographically isolated). It had a population of 3,320 Arab Muslims and Arab Christians in 1945.Appendix B - Non-Jewish Population within the Boundaries Held by the Israel Defence Army on 1.5.49 - as on 1.4.45, in accordance with Government of Palestine, ''Village Statistics, April, 1945'', p7 The town's inhabitants fled after Haganah forces captured the town on 3 March 1948, and the remainder left in the wake of an assault by the Golani Brigade against the Military of Syria, ...
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Sea Of Galilee
The Sea of Galilee ( he, יָם כִּנֶּרֶת, Judeo-Aramaic: יַמּא דטבריא, גִּנֵּיסַר, ar, بحيرة طبريا), also called Lake Tiberias, Kinneret or Kinnereth, is a freshwater lake in Israel. It is the lowest freshwater lake on Earth and the second-lowest lake in the world (after the Dead Sea, a saltwater lake), at levels between and below sea level. It is approximately in circumference, about long, and wide. Its area is at its fullest, and its maximum depth is approximately .Data Summary: Lake Kinneret (Sea of Galilee)
The lake is fed partly by underground springs, but its main source is the