Biblical Geography and HistoryKent, Charles Foster
History
Biblical Geography and History
Kent, Charles Foster
Bible -- Geography; Palestine -- History
=Gilead.= South of the Yarmuk the black basalt of the Jaulan yields to
the light limestone of the west-Jordan. The entire territory of Gilead
more closely resembles the western hills of Palestine than does any
other part of the east-Jordan region. On the broad rolling uplands of
eastern Gilead there are large grain fields and the soil is
cultivated at many other points. In the Roman period great cities, of
which Gerasa^{(44)} was the chief, testified to the rich productivity
of this region, but for the most part it is the paradise of the
herdsmen and the shepherd. It is a land of deep valleys, rounded
hills, and frequent springs. On the northwest many small streams cut
their way to the Jordan valley. The roads run up and down steep
inclines where the flocks and the herds cling to the sloping
hillsides. Groves of noble oaks cover the hilltops and reveal the
strength inherent in the soil.
=The Jabbok and Jebel Osha.= The dominant factor in southern Gilead is
the River Jabbok.^{(45)} It rises among the hills not far from the
Moabite border, only eighteen miles from the Jordan, and then flows
northeast, past the old Ammonite capital. Thence it completes the half
circle, cutting its way through the Gileadite hills to the Jordan. At
some points its channel is between two and three thousand feet below
the level of the plateau. It is a joyous river, rippling in flashes of
sunlight over the rocks, through green glades and tangles of oleanders
and rushes, a type of this happy, picturesque land of the shepherd.
The centre of the half circle described by the Brook Jabbok is the
Jebel Osha, the highest peak in Gilead. From its height of three
thousand five hundred and ninety-five feet, practically all of Gilead
is spread to the north and south and east like a great variegated
carpet.
=Southern Gilead.= In southern Gilead the trees become fewer and fewer
until south of Jebel Osha they almost disappear. In spring-time the
fields are green with grass and grain, but in summer they become
parched and brown. The wadies in the south, such as Wady Nimrin and
Wady Heshbân, avail little for irrigation, since their channels are
far beneath the level of the surrounding plateau. The region as a
whole begins to take on something of the sombre color of the Dead Sea
region which lies in the depths below.
Public-domain text, read in full here on John Shaqi.
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