Page 63 - Bible Geography and Near East Studies
P. 63

Several mountain ranges run the length of
                                                        the country. In the northeast, the basalt
                                                        landscapes of the Golan Heights, formed by
                                                        volcanic eruptions in the distant past, rise as
                                                        cliffs overlooking the Hula Valley.

                                                        The hills of Galilee, largely composed of soft
                                                        limestone and dolomite, ascend to heights
                                                         ranging from 1,600 to 4,000 feet (500 to 1,200 m.) above
                 Mount Hermon (Photo: S. Lederhendler)   sea level. Small perennial streams and relatively ample
                                                         rainfall keep the area green all year round. Many residents
               of Galilee and the Golan are engaged in agriculture, tourism-related enterprises, and light industry.

               The Jezreel Valley, separating the hills of Galilee from those of Samaria, is Israel's richest agricultural
               area, cultivated by many cooperative communities (kibbutzim and moshavim). The rolling hills
               of Samaria and Judea (the West Bank) present a mosaic of rocky hilltops and fertile valleys, dotted with
               groves of age-old, silver-green olive trees. The terraced hillsides, first developed by farmers in ancient
               times, blend into the natural landscape. The population is concentrated mainly in small urban centers
               and large villages.


                      The Negev, comprising about half of Israel's

                      land area, is sparsely inhabited, its population
                      supported by an agricultural and industrial
                      economy. Further south, the Negev becomes an
                      arid zone characterized by low sandstone hills
                      and plains, abounding with canyons and wadis
                      in which winter rains often produce flash floods.

               Continuing southward, the region gives way to an area
               of bare craggy peaks, craters, and rock-strewn plateaus,
               where the climate is drier, and the mountains are            The Negev (Photo: S. Lederhendler)
               higher. Three erosive craters, the largest of which is
               about 5 miles (8 km) across and 21 miles (35 km) long,
               cut deeply into the earth's crust, displaying a broad range of colors and rock types.

               At the tip of the Negev, near Eilat on the Red Sea, sharp pinnacles of gray and red granite are broken by
               dry gorges and sheer cliffs, with colorful layers of sandstone glowing in the sunlight.
















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