/neg"ev/, n.
a partially reclaimed desert region and district in S Israel, bordering on the Sinai Peninsula. 4700 sq. mi. (12,173 sq. km). Cap.: Beersheba.
Also, Negeb /neg"eb/.

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or Ha-Negev

Desert region, southern Israel.

Bounded by the Sinai Peninsula and the Jordan Rift Valley, it has an area of about 4,700 sq mi (12,200 sq km). It was a pastoral region in biblical times and an important source of grain for the Roman Empire. After the Arab conquest of Palestine (7th century AD), it was left desolate, and for more than 1,200 years it had only a small population of Bedouin. Modern agricultural development began with three kibbutzim in 1943; others were founded after World War II (1939–45), when irrigation projects were initiated. Assigned to Israel in the partition of Palestine in 1948, it was the scene of clashes between Israeli and Egyptian forces in 1948–49. It is the site of many preplanned Israeli settlements, including the port city of Elat, Israel's outlet to the Red Sea. Beersheba is an important administrative centre. The region produces grain, fruit, and vegetables; mineral resources include potash, bromine, and copper.

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▪ desert region, Israel
also spelled  Negeb,  Hebrew  Ha-negev 
 (The Southland), arid region, southern part of Israel, occupying almost half of Palestine west of the Jordan, and about 60 percent of Israeli territory under the 1949–67 boundaries. The name is derived from the Hebrew verbal root n-g-b, “to dry,” or “to wipe dry.” Triangular shaped with the apex at the south, it is bounded by the Sinai Peninsula (west) and the Jordan Rift Valley (east). Its northern boundary, where the region blends into the coastal plain in the northwest, Har Yehuda (the Judaean Hills) in the north, and the Wilderness of Judaea (Midbar Yehuda) in the northeast, is indistinct. Many use an arbitrary line at about 30°25′ north latitude for the northern boundary. Within these limits, the Negev has an area of about 4,700 sq mi.

      Geologically, the area is one of northeast–southwest folds, with many faults. Limestones and chalks predominate. A unique feature is the large elongate makhteshim, or erosion craters, surrounded by high cliffs. These were created by the erosion of upward-folded strata (anticlines), combined with horizontal stresses. The largest of these are Makhtesh Ramon, 23 mi (37 km) long and up to 5 mi wide, and ha-Maktesh ha-Gadol (The Great Crater), about 9 mi long and up to 4 mi wide. The floors of these craters expose chalks, marls, and gypsums, geologically much older than the walls or surrounding plateaus.

      Biblical references such as Psalms 126:4 (“Restore our fortunes, O Lord, like the water-courses in the Negeb”) point to the semi-arid character of the region from early recorded times. The Negev should not, however, be considered a desert as such; in the Beersheba area (altitude about 800 ft [250 m]), rainfall varies from 8 in. (200 mm) to 12 in. in some years. The latter amount permits unirrigated grain farming. Precipitation decreases to the south; the central Negev plateau (altitude 820–3,395 ft [250–1,035 m]) receives 3–4 in.; rainfall is negligible at Elat at the southern tip. The amount of rainfall varies considerably throughout the region from year to year. Flash flooding is common in the winter rainy season. Most of the rugged region is heavily dissected by wadis, or seasonal watercourses.

      Remains of prehistoric and early historic settlements are abundant. Flint arrowheads of the Late Stone Age (c. 7000 BC) and implements of the Copper and Bronze ages (c. 4000–1400 BC) have been found on the central Negev plateau. The Negev was a pastoral region in biblical times, but the Nabataeans, a Semitic people centred in what is now Jordan, developed techniques of terracing and of conserving winter rains, which made the Negev a thriving agricultural area. It was an important granary of the Roman Empire. After the Arab conquest of Palestine (7th century AD), the Negev was left desolate; for more than 1,200 years it supported only a meagre population of nomadic Bedouin.

      Modern agricultural development in the Negev began with three kibbutzim (collective settlements) in 1943; others were founded just after World War II, when the first large-scale irrigation projects were initiated. After the creation of the State of Israel (1948), the importance of development of this large portion of the country was realized. Under the National Water Plan pipelines and conduits bring water from northern and central Israel to the northwestern Negev, which has almost 400,000 ac (more than 160,000 ha) of fertile loess soils. Irrigation, combined with the area's year-round sunlight, produces fine crops of grain, fodder, fruits, and vegetables. Double-cropping is not uncommon.

      Exploitation of mineral resources has accompanied agricultural development. Potash, bromine, and magnesium are extracted at Sedom (q.v.), at the southern end of the Dead Sea; copper is mined at Timnaʿ (q.v.); there are large deposits of ball clay and glass sand for the ceramic and glass industries; phosphate works have been established at Oron and Zefaʿ, and natural gas fields at Rosh Zohar.

      Urbanization has come in the wake of modern settlement; Beersheba (q.v.), “capital of the Negev,” is the largest city in Israel not in the environs of Tel Aviv–Yafo, Jerusalem, or Haifa. Planned cities in the Negev include Aradʿ (founded 1961), Dimona (1955), and the port-city of Elat (settled 1949; qq.v.), Israel's outlet to the Red Sea.

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Universalium. 2010.

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