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To the south, Lower Galilee—with its highest peak, Samaria, the region of the ancient kingdom of Israel, is a hilly district extending from the Plain of Esdraelon to the latitude of Ramallah.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.The term Palestine has been associated variously and sometimes controversially with this small region, which some have asserted also includes Jordan.

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The region (or at least a part of it) is also known as the Holy Land and is held sacred among Jews, Christians, and Muslims.

Since the 20th century it has been the object of conflicting claims of Jewish and Arab national movements, and the conflict has led to prolonged violence and, in several instances, open warfare.

The Jordan Valley is a deep rift valley that varies in width from 1.5 to 14 miles (2.5 to 22 km).

In its northern section the bed of the drained Lake Ḥula and of Lake Tiberias (the Sea of Galilee) are blocked by natural dams of basalt.

Settlement depends closely on water, which is almost never abundant.

Precipitation, which arrives in the cool half of the year, decreases in amount in general from north to south and from the coast inland.

Farther northward the Plain of Esdraelon (ʿEmeq Yizreʿel), formed by subsidence along lines of faults, separates the hills of southern Galilee from the mountains of Samaria.

The plain, 16 miles (26 km) wide at most, narrows to the northwest, where the Qishon River breaks through to the Plain of ʿAkko, and to the southeast, where the Ḥarod River—which rises at the Spring of Ḥarod—has carved the plain into the side of the Jordan Valley.

Galilee is better-watered and more thickly wooded than that of Samaria or Judaea.

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