Gennesareth to the Dead Sea, where the depression reaches its lowest
point, and the land, rising into a ridge, separates the Jordan valley
from the upper end of the Gulf of Akabah. The Jordan valley divides
Palestine, strongly and sharply, into two regions. Its depth, its
inaccessibility (for it can only be entered from the highlands on either
side down a few steep watercourses), and the difficulty of passing
across it (for the Jordan has but few fords), give it a separating power
almost equal to that of an arm of the sea. In length above a hundred
miles, in width varying from one mile to ten, and averaging some five
miles, or perhaps six, it must have been valuable as a territory,
possessing, as it does, a rich soil, abundant water, and in its lower
portion a tropical climate.

On either side of the deep Jordan cleft lies a highland of moderate
elevation, on the right that of Galilee, Samaria, and Judsea, on the
left that of Ituraea, Bashan, and Gilead. The right or western highland
consists of a mass of undulating hills, with rounded tops, composed of
coarse gray stone, covered, or scarcely covered, with a scanty soil, but
capable of cultivation in corn, olives, and figs. This region is
most productive towards the north, barer and more arid as we proceed
southwards towards the desert. The lowest portion, Judaea, is
unpicturesque, ill-watered, and almost treeless; the central, Samaria,
has numerous springs, some rich plains, many wooded heights, and in
places quite a sylvan appearance; the highest, Galilee, is a land of
water-brooks, abounding in timber, fertile and beautiful. The average
height of the whole district is from 1500 to 1800 feet above the
Mediterranean. Main elevations within it vary from 2500 to 4000 feet.
The axis of the range is towards the East, nearer, that is, to the
Jordan valley than to the sea. It is a peculiarity of the highland that
there is one important break in it. As the Lowland mountains of Scotland