Mount

East of the Jordan the Anti-Lebanon, stretching south, terminates in the hilly district called Jebel Heish, which reaches down to the Sea of Gennesareth. South of the river Hieromax there is again a succession of hills, which are traversed by wadies running toward the Jordan. These gradually descend to a level at the river Arnon, which was the boundary of the ancient trans-Jordanic territory toward the south.

The composition of the Palestinian hills is limestone, with occasional strata of chalk, and hence the numerous caves, some of large extent, found there.