By C. Serruya (auth.), C. Serruya (eds.)
Fauna and vegetation oflakes are an integrative results of nearby earlier heritage and current environmental elements. within the Lake Kinneret zone the place Prehistoric guy witnessed the final tectonic readj ustments of the Rift Valley, geological occasions don't belong in basic terms to the distant previous yet nonetheless strongly impact the lacustrine atmosphere. it truly is for this reason essential to provide an in depth photograph of the nearby heritage and limnological positive factors of the lake (Parts I and II) earlier than describing its planktic and benthic com munities (Parts III and IV) and the Vertebrate fauna of the lake and its atmosphere (Part V). The trophic relationships among groups are past the scope of a Monograph and feature hence no longer been studied intimately yet basically pointed out sometimes. it really is intentional that guy and his penetration into the Kinneret zone were taken care of on a only zoological foundation. It underlines the truth that guy, as the other dwelling organism, is a part of the environment and governed by means of its legislation and that his actions have an automated feed again on his surroundings. despite the fact that, against this with different residing organisms, guy is ready to 'utilize' the lakes and their watersheds for his profit if, via acceptable administration, he minimizes the dangerous impression of his actions. this can be the most goal of the study conducted shortly on Lake Kinneret and its watershed and in brief defined partly VI.
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Additional info for Lake Kinneret
Paper 84: 337-366. Picard, L. 1970. Further reflections on graben tectonics in the Levant, Int. Upper Mantle proj. Sci. Rep. 7: 249-267. Picard, L. & U. Baida. 1966. Stratigraphic position of the Ubeidiya formation. Proc. Isr. Acad. Sci. Hum. 4: 1-8. Rosenberg, E. 1960. Geologische Untersuchungen in den Naftali-Bergen. Mitt. E. T. H. Zurich C. 80. Saltzman, U. 1964. Geology of the Tabgha-Huquq-Migdal region. M. Sc. thesis Hebrew Univ. Jerusalem. (in Hebrew). Schulman, N. 1959. Geology of central Jordan Valley.
Conf. NE African and Levantine Pleistocene prehistory. Dallas. 65 p. Horowitz, A. 1974. The Late Cenozoic stratigraphy and paleogeography of Israel. Institute of Archaeology, Tel Aviv University. 187 p. , G. Siedner & O. Bar Yosef. 1973. Radiometric dating of the Ubeidiya formation, Jor· dan Valley, Israel. Nature. 242: 186-187. Lartet, L. 1869. La Geologie de la Palestine (These) Paris. 292 p. Michelson, H. 1972. The hydrology of southern Golan Heights. Water Planning for Israel Ldt. (T AHAL) Tel Aviv.
Standard climatological measurements at Tiberias were resumed in 1939 and continued at a new site in the upper town (-110 m MSL) from 1942 to 1962. Routine measurements at Ein Gev were resumed in 1951. Measurements at Ginosar on the western shore (32° 51'N, 35° 31'E,-205 m MSL) are available from 1958. Rainfall measurements are also available from some twenty lakeside sites, a few of which also record evaporation from class A pans and windrun. In 1968, the Kinneret Limnological Laboratory set up a meteorological station at Tabgha where air temperature and barometric pressure are recorded.