This territory is shut in on every side by lofty mountains, offshoots of Mount Cyllene and the Aroanian chain; and it is about 7 miles (12 km) in length and the same in breadth.
In order to convey the waters of this river in a single channel to the katavóthra, the inhabitants at an early period constructed a canal, 50 stadia in length, and 30 feet (9 m) in breadth.
The canal of Heracles, however, could not protect the valley from the danger to which it was exposed, in consequence of the katavóthra becoming obstructed, and the river finding no outlet for its waters.
[7] Pausanias evidently refers to the yellow border which is still visible upon the mountains and around the plain: but in consequence of the great height of this line upon the rocks, it is difficult to believe it to be the mark of the ancient depth of water in the plain, and it is more probably caused by evaporation; the lower parts of the rock being constantly moistened, while the upper are in a state of comparative dryness, thus producing a difference of colour in process of time.
Pliny the Elder says that the calamity had occurred five times;[8] and Eratosthenes related a memorable instance of such an inundation through the obstruction of the katavóthra, when, after they were again opened, the water rushing into the Ladon and the Alpheius overflowed the banks of those rivers at Olympia.
[14] Pausanias describes the two roads which led westward from Pheneus around a mountain – that to the right or northwest leading to Nonacris and the supposed river Styx, and that to the left to Cleitor.
The road to Cleitor ran at first along the canal of Heracles, and then crossed the mountain, which formed the natural boundary between the Pheneatis and Cleitoria, close to the village of Lycuria.
The road passed from the Orchomenian plain to that of Pheneus through a narrow ravine (φάραγξ); in the middle of which was a fountain of water, and at the further extremity the village of Caryae.
The mountains on either side were named Oryxis (Ὄρυξις), and Sciathis (Σκίαθις), and at the foot of either was a subterraneous channel, which carried off the water from the plain.