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The unnavigable Jordan River forms the northern portion of the borders between Israel and Jordan and between the West Bank and Jordan. The river flows through the Sea of Galilee (166 sq km/64 sq mi), which provides many species of fish and supplies more than half of Israel’s fresh water. The Jordan empties into the Dead Sea (1,020 sq km/394 sq mi), a highly saline lake supplying many important minerals. Parts of the Dead Sea lie in Israel, Jordan, and the West Bank. The Sea of Galilee and the Dead Sea lie below sea level; the shore of the Dead Sea is the lowest point on the Earth’s surface. Projects by Israel and Jordan to divert water from the Jordan River for irrigation and other uses have caused the level of the Dead Sea to drop. In 1996 the level was 408 m (1,339 ft) below sea level. Other principal rivers are the Yarqon, which runs through Tel Aviv-Yafo, and the Qishon River (Nahr al Muqaţţa‘), which reaches the Mediterranean Sea near Haifa. The coastline of Israel, including the country’s western edge on the Mediterranean Sea and its southern tip on the Red Sea, stretches for 273 km (170 mi). Apart from limited sections of cliffs rising 10 to 40 m (30 to 120 ft), the coast has few headlands or indentations; much of it is low-lying and backed by sand dunes. Haifa, a natural harbor in the northern part of the country, and Ashdod, an artificial deepwater port to the south, serve as the main seaports on the Mediterranean. The port of Elat on the Gulf of Aqaba provides Israel’s only access to the Red Sea, making it extremely important to the country’s shipping interests.
Although much of Israel’s desert regions contain poor soils, the northern Negev, the coastal plains, and the interior valleys provide patches of productive soils. An estimated 18 percent of Israel’s land is used for crops or orchards. Most cultivable soils in Israel require irrigation and careful management; of 3,920 sq km (1,514 sq mi) under cultivation, 44 percent is irrigated. The Dead Sea contains valuable minerals such as potash, bromine, and magnesium, all of which are exploited mainly for export. The Negev contains deposits of many minerals, including copper, phosphate, bromine, and clay. Small quantities of oil and natural gas are also mined from areas near the Dead Sea and south of Tel Aviv-Yafo.
Israel has a typical Mediterranean climate with cool, rainy winters and warm, dry summers. Temperatures vary considerably with elevation, exposure to the sea, and predominant winds. January is normally the coldest month and August the warmest. In upland regions such as Jerusalem, January temperatures average 9°C (48°F) while August temperatures average 24°C (75°F). In the coastal plains, including Haifa and Tel Aviv-Yafo, January averages 12°C (54°F) and August averages 25°C (77°F). The highest and lowest elevations are subject to extremes: Frost occurs a few days a year in mountainous inland regions, while summer temperatures can reach the upper 30°s C (lower 100°s F) in the Jordan Valley and in southern desert regions. About 70 percent of annual precipitation falls as rain between November and February. Amounts of rain decrease from north to south and from west to east. The upper Galilee receives about 1,000 mm (about 40 in) of rain annually; the Judean Hills, about 700 mm (about 30 in); and most of the Negev, about 100 mm (about 4 in). Elat, the driest spot in Israel, receives only 25 mm (1 in) annually. Snow falls occasionally in higher parts of the hills during the coldest months. Frequent summer droughts, especially in the southern desert regions, make extensive irrigation a necessity. Heavy rains in these and other areas can cause flooding and erosion.
As a small country experiencing rapid population growth and industrialization, Israel faces serious air and water pollution as well as problems disposing of solid and hazardous waste. The government is taking steps to tackle these problems, such as requiring catalytic converters for vehicles, phasing out the use of leaded gasoline, initiating rehabilitation programs for polluted streams, conducting environmental impact assessments for industry, and supervising the production, handling, and disposal of hazardous substances.
The estimated population of Israel in 2007, including residents of the Golan Heights and East Jerusalem, was 6,426,679. Population density, including the area of the Golan Heights and East Jerusalem, was 316 persons per sq km (819 per sq mi). Israel is one of the most urbanized countries in the world. Some 92 percent of the population lives in communities of more than 2,000 people, and over half of Israel’s population lives in the metropolitan areas of its three largest cities, Jerusalem, Tel-Aviv-Yafo, and Haifa. More than one-third of the world’s Jewish population lives in Israel, where they make up 82 percent of the people. Arabs, most of whom are Muslims, make up almost the entire remainder of the population. Because the birth rate is greater for Arabs than for Jews, the Arab proportion of the population more than doubled between 1950 and the late 1990s.
© 1993-2008 Microsoft Corporation. All Rights Reserved.
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© 2008 Microsoft
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