KINNERET

KINNERET (Heb. כִּנֶּרֶת), moshavah in northern Israel, near the S.W. corner of Lake Kinneret, founded on Jewish Colonization Association (ICA) land in 1909 by settlers from Eastern Europe. The village developed at a slow pace, as the settlers frequently differed with the ICA (later pica ) administration. The land was transferred to the settlers only in 1944. After that their progress accelerated somewhat. In 1959 the moshavah received municipal council status. In 1968 it numbered 195 inhabitants, rising to 335 in the mid-1990s and 497 in 2002. In addition to intensive farming (mainly orchards), Kinneret set up a small hotel, a restaurant, and other tourist enterprises. The first experiments in lake fishing were made by Jewish fishermen on the shore by the moshavah. In the nearby "Kinneret Courtyard," where the kevuzah kinneret was founded previously, several nuclei of kibbutz settlements had their temporary camp before establishing their own villages in the region, e.g., afikim , ein gev , and Ma'agan. In the moshavah's graveyard, shared with nearby Kibbutz Kinneret, lie the remains of berl katznelson , Nahman Sirkin, moses hess , ber borochov , avraham harzfeld , the poet rachel , and naomi shemer . (Efraim Orni) KINNERET, LAKE KINNERET, LAKE (Heb. יָם כִּנְרֶת, Yam Kinneret, or םָי כִּנְרוֹת, Yam Kinnerot), freshwater lake in N.E. Israel. The Jordan enters it from the north and flows out from the south. Several names have been applied to the lake in the past, including "Sea of Chinneroth" or "Chinnereth" (Josh. 13:27; 12:3), "Water of   Gennesar" (I Macc. 11:67), and "Lake of Gennesareth" (Jos., Wars, 3:506), while in the New Testament it is called "the Sea of Galilee" or simply "the Sea" (Matt. 4:18; 17:27; John 6:1; etc.), and sometimes "the sea of Gennesareth" or "the sea of Tiberias" (Luke 5:1; John 6:1; 21:1). In talmudic sources it is usually called yammah shel Teveryah ("sea of Tiberias," Tosef. Suk. 3:9, etc.). The Arabs also called it Baḥr al-Ṭabariya. In Israel the biblical name Yam Kinneret has been revived. -Physical Data The lake occupies a section of the central Jordan Rift Valley. It covers an area of 64 sq. mi. (165 sq. km.). The level of the water surface, which varies considerably with the shift from rainy to drought years, averages 696 ft. (213 m.) below Mediterranean sea level. The water is deepest, 144 ft. (44 m.) on the average, northeast of the lake's center. The region of Lake Kinneret has a seismic character, borne out by hot mineral springs on its bottom and on its circumference. The lake was created in its present form when, in the recent geologic past, its bottom subsided more strongly than the area south of it, where diagonally posed young rock strata testify to an uplift which created a sill preventing the drainage of Jordan and other waters coming in from the north. Whereas the lake is thought to have originally been more or less rectangular, streams entering it, in addition to the Jordan itself, deposited alluvial material thus creating the Ginnesar Valley in the northwest and the Bethsaida (Buṭayḥa) Valley in the northeast and rounding off the north shore. At the same time, erosion at the Jordan's outflow in the south contributed to give the lake its present pear-like shape, with a north-south length of 15 mi. (23 km.) and a maximum east-west width of 10 mi. (16 km.). Alluvium deposited by the Yarmuk River in the south blocked the inflow of this watercourse into the lake and displaced the Jordan outflow to the southwest corner of the lake. Although the waters entering the lake are fresh, brackish springs at the lake bottom and near its shore raise its water salinity; strong evaporation in the region's hot climate further increases the water's salt content. Measurements taken in the 1950s and 1960s show oscillations in salinity ranging from 250 to 400 mm/liter chlorine content, again to be attributed to the varying amount of water entering the lake; the more water fills the lake, the better the saline bottom springs are plugged by its weight, causing a further reduction in salinity. -History Owing to its abundant water supply, warm climate, the fertile land in its vicinity, and the numerous fish in the lake, Lake Kinneret has attracted man since prehistoric times; in fact, the most ancient human remains and artifacts found in Ereẓ Israel come from ʿUbaydiyya not far from its shores. In Neolithic times the inhabitants of the Yarmuk valley adjoining the lake engaged in agricultural activities ("hoe" agriculture). In the Early Bronze Age some of the largest cities in Canaan were founded there, in particular, Bet Yeraḥ , a site of some 60 acres (250 dunams). The Via Maris (Maritime Route) which passed its shores contributed to the wealth of the riparian cities. Egyptian documents (Papyrus Anastasi I) mention the hot springs on its shores and their beneficent effects. In the Bible, Kinneret serves as a prominent boundary mark: it was the border of Sihon king of the Amorites (Deut. 3:17); its western shores were in the possession of Naphtali, whose cities of Hammath, Rakkath, and chinnereth were situated along its banks; most of the eastern shore belonged to Manasseh, and the tribe of Gad extended up to its southern end (Josh. 12:3; 13:27). In the time of David, Geshur held part of its northeastern coastline, and after the division of the monarchy the kings of Israel had to engage in combat with Aram for control of its eastern shore; in this the Omrid dynasty was most successful. In 732 B.C.E. Tiglath-Pileser III captured the area from Israel and assigned the western shore to the Assyrian province of Megiddo and the eastern to Karnaim (II Kings 15:29). The lands west of the lake were a royal estate in the Persian and Hellenistic periods. The Ptolemies established one of their administrative centers (Philoteria) along its shore. Part of the territory of the city of Susitha (Hippus) bordered on its eastern shore. Under the Hasmoneans the entire area was Jewish. In 30 B.C.E. Herod received Hippus and in 20 B.C.E. the Gaulan. His sons Antipas and Philip founded the cities of tiberias and Julias (bethsaida ) on the seashore. In the time of Herod Antipas the area around the sea was a main center of jesus ' activities. Under Roman rule the western shore (Tiberias) and part of the eastern (Gaulan) were Jewish while the rest was gentile. The entire lake was later included in the province of Palaestina Secunda; in Byzantine times many churches were built on its shores (e.g., Heptapegon, Capernaum, etc.). After the Arab conquest it remained in the same province which was renamed Jund al-Urdun (Jordan). The crusaders kept a firm hold on the western shore and fought repeatedly to gain control of the eastern (the Terre de Sueth). The Mamluks included the lake in the mamlaka (province) of Safed, and the Turks in the pashalik of Acre. Beginning from the first decade of the 20th century, Jewish settlements were founded on and near the lake's west and south shore (migdal , kinneret , deganyah , etc.). The frontier drawn between the British Mandate over Palestine and the French Mandate over Syria included the entire lake in the former territory, together with a 1.1–2.2 mi. (1.8–3.5 km.) broad strip on the southern half of the east coast and a tiny 32.8 ft. (10 m.) broad strip along the Bethsaida Valley in the northeast. Under the Mandate, the settlement chain was strengthened in the west and south, and the kibbutz ein gev set up in the east. It engaged, together with two other kibbutzim, in lake fishing and the development of pleasure-boat trips and tourism on the lake and in the area. After the 1948 War of Independence, the Israel-Syrian border remained unchanged, although the Ein Gev strip was declared a demilitarized area. More Jewish settlements (Ma'agan, ha-on , Tel Kaẓir in the south and east, almagor in the north) were added in the statehood period. Lake Kinneret was chosen as the National Water Carrier's principal reservoir, completed in 1964; the water   was lifted from the lake by the huge Eshed Kinnarot pumping station in its northwest corner. As the main source of water in Israel, the Kinneret's levels are of public interest. Its low level is 698 ft. (213 m.) below sea level, while its high level is 685 ft. (208.9 m.) below sea level. In dry years, when the low level is reached, pumping is stopped. In contrast, in rainy years, when the high level is reached the Deganyah dam is opened. After years of relative drought the abundant rains of 2003/2004 again brought the level to the high-water mark. Growing Syrian aggressiveness (attempts at setting up military positions on Israel territory near Ein Gev and in the Chorazin area, harassing of Israel fishermen, etc.) became one of the sources of friction building up the tension which led to the Six-Day War. The occupation of the dominating golan Heights by Israel in this war moved the border with Syria away from Lake Kinneret, which became an inland lake of Israel. The settlements around the Kinneret are mainly rural, while Tiberias serves as the urban center of the region. In 2003 the population of the Kinneret region was 96,000. -BIBLIOGRAPHY: Abel, Geog, 1 (1933), 163, 494–8; Picard, in: ZDPV, 55 (1932), 169ff.; Neumann, in: IEJ, 3 (1953), 246ff.; M. Schmorak, Atlas Yisrael (1961), V map 3; S. Yeivin and H. Hirschberg (eds.), Ereẓ Kinnerot (1950); EM, 4 (1962), 204–8. (Michael Avi-Yonah and Efraim Orni / Shaked Gilboa (2nd ed.)