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400 online dating method pdf

Its mountains—Carmel, Gilboaʿ, Aybāl (Ebal), and Al-Ṭūr (Gerizim)—are lower than those of Upper Galilee, while its basins, notably those of the ʿArrābah Plain and Nāblus, are wider and more gently contoured than their equivalents in Judaea.Samaria is easily approached from the coast across the Plain of Sharon and from the Jordan by the Fāriʿah valley.The maritime plain connects with Esdraelon by the pass of Megiddo and several lesser routes between the mountain spurs of Carmel and Gilboaʿ.Galilee is better-watered and more thickly wooded than that of Samaria or Judaea.After Roman times the name had no official status until after World War I and the end of rule by the Ottoman Empire, when it was adopted for one of the regions mandated to Great Britain; in addition to an area roughly comprising present-day Israel and the West Bank, the mandate included the territory east of the Jordan River now constituting the Hashimite Kingdom of Jordan, which Britain placed under an administration separate from that of Palestine immediately after receiving the mandate for the territory.The name Palestine has long been in popular use as a general term to denote a traditional region, but this usage does not imply precise boundaries.The strategic importance of the area is immense: through it pass the main roads from Egypt to Syria and from the Mediterranean to the hills beyond the Jordan River.Settlement depends closely on water, which is almost never abundant.

Farther southward the lowland opens out rapidly into the Plain of Sharon, about 8 miles (13 km) wide and extending south to the latitude of Tel Aviv–Yafo.The Negev, a desertlike region, is triangular in shape with the apex at the south.It extends from Beersheba in the north, where 8 inches (200 mm) or more of precipitation falls annually and grain is grown, to the port city of Elat on the Red Sea, in the extremely arid south.Precipitation, which arrives in the cool half of the year, decreases in amount in general from north to south and from the coast inland.Perennial rivers are few, and the shortage of water is aggravated by the porous nature of the limestone rocks over much of the country.

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