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History of Phoenicia by George Rawlinson
page 8 of 539 (01%)
from the 380, and the length of Phoenicia along the Mediterranean shore
must be regarded as not exceeding three hundred miles.

The width varied from eight or ten miles to thirty. We must regard
as the eastern boundary of Phoenicia the high ridge which forms the
watershed between the streams that flow eastward toward the Orontes,
Litany, and Jordan, and those that flow westward into the Mediterranean.
It is difficult to say what was the _average_ width, but perhaps it may
be fairly estimated at about fifteen miles. In this case the entire area
would have been about 4,500 square miles.

The tract was one of a remarkably diversified character. Lofty mountain,
steep wooded hill, chalky slope, rich alluvial plain, and sandy shore
succeeded each other, each having its own charm, which was enhanced by
contrast. The sand is confined to a comparatively narrow strip along the
seashore,[14] and to the sites of ancient harbours now filled up. It is
exceedingly fine and of excellent silicious quality, especially in the
vicinity of Sidon and at the foot of Mount Carmel. The most remarkable
plains are those of Sharon, Acre, Tyre, Sidon, Beyrout, and Marathus.
Sharon, so dear to the Hebrew poets,[15] is the maritime tract
intervening between the highland of Samaria and the Mediterranean,
extending from Joppa to the southern foot of Carmel--a distance of
nearly sixty miles--and watered by the Chorseas, the Kaneh, and other
rivers. It is a smooth, very slightly undulating tract, about ten
miles in width from the sea to the foot of the mountains, which rise up
abruptly from it without any intervening region of hills, and seem to
bound it as a wall, above which tower the huge rounded masses of Ebal
and Gerizim, with the wooded cone, on which stood Samaria, nestling at
their feet.[16] The sluggish streams, several of them containing water
during the whole of the year, make their way across it between reedy
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