Travels in Syria and the Holy Land

by John Lewis Burckhardt

OM KEIS.

[p.270]May 5th.—I took a guide from hence to shew me to Om Keis, which, I was told, was inhabited by several families. I there intended to pass the night, and to proceed the next day to Feik, a village on the E. side of the lake of Tabaria. In half an hour from Hebras we passed the spring Ain el Terab [Arabic], in a Wady, which farther to the north-westward joins the Wady Szamma, and still lower down unites with the Wady Sheriat el Mandhour. At one hour and a quarter to our right was the village Obder [Arabic], on the banks of Wady Szamma, which runs in a deep ravine, and half an hour farther north-west, the village Szamma [Arabic]. The inhabitants of the above villages cultivate gardens of fruit trees and all kinds of vegetables on the side of the rivulet. The villages belong to the district of Kefarat. To the left of our route extends a country full of Wadys, called the district of Serou [Arabic], to the southward of which begins that of Wostye [Arabic]. At one hour and a half to our left, distant half an hour, we saw, in the Serou, the village Faour [Arabic]. Between Hebras and Szamma begins the Wady el Arab [Arabic], which continued to the left parallel with our route; it is a fertile valley, in which the Arabs Kelab and others cultivate a few fields. There are several mills on the water-side. Our route lay W. by N. and W.N.W. across the Kefarat, which is uneven ground, rising towards the west, and is intersected by many Wadys. At the end of three hours and a quarter we reached Om Keis [Arabic].

Om Keis is the last village to the west, in the district of Kefarat; it is situated near the crest of the chain of mountains, which bound the valley of the lake of Tabaria and Jordan on the east. The S. end of the lake bears N.W. To the N. of it, one hour, is the deep Wady called Sheriat el Mandhour, which is, beyond a doubt, the Hieromax of the Greeks and Jarmouk of the Israelites.

To the south, at the same distance, flows the Wady el Arab,

[p.271]which joins the Sheriat in the valley of El Ghor , not far from the junction of the latter with the Jordan. I am doubtful to what ancient city the ruins of Om Keis are to be ascribed.[It was probably Gamala, which Josephus describes as standing upon a mountain bordered by precipices. Gadara appears from the authorities of Pliny and Jerom to have been at the warm baths, mentioned below, on the north side of the Sheriat el Mandhour; Gadara Hieromiace praefluente. Plin. Nat. Hist. l.i.c.18. Gadara, urbs trans Jordanem contra Scythopolin et Tiberiadem, ad orientalem plagam, sita in monte, ad cujns radices aquae calidae erumpunt, balneis super aedificatis,—Hieron. in Topicis.]

At Om Keis the remains of antiquity are very mutilated. The ancient town was situated round a hill, which is the highest point in the neighbourhood. To the east of the hill are a great number of caverns in the calcareous rock, some of which have been enlarged and rendered habitable. Others have been used as sepulchral caves. Great numbers of sarcophagi are lying about in this direction: they are all of black stone, which must have been transported from the banks of the river below: the dimensions of the largest are nine spans in length by three in breadth; they are ornamented with bas-reliefs of genii, festoons, wreaths of flowers, and some with busts, but very few of them are of elegant wor[k]manship. I counted upwards of seventy on the declivity of the hill. On the summit of the hill are heaps of wrought stones, but no remains of any important building: on its west and north sides are the remains of two large theatres, built entirely of black stone. That on the W. side is in better preservation than the other, although more ruined than the theatres at Djerash. The walls and the greater part of the seats yet remain; a tier of boxes intervenes between the rows of seats, as at Djerash, and there are deep vaulted apartments beneath the seats. There are no remains of columns in front of either theatre. The theatre on the north side of the hill, which is in a very dilapidated state, is remarkable for its great depth,

[p.272]caused by its being built on a part of the steepest declivity of the hill; its uppermost row of seats is at least forty feet higher than the lowest; the area below the seats is comparatively very small. From these two theatres the principal part of the town appears to have extended westwards, over an even piece of ground at the foot of the hill; its length from the hill was at least half an hour. Nothing is at present standing; but there are immense heaps of cut stones, columns, &c. dispersed over the plain. A long street, running westward, of which the ancient pavement still exists in most parts, seems to have been the principal street of the town. On both sides there are vast quantities of shafts of columns. At a spot where a heap of large Corinthian pillars lay, a temple appears to have stood. I here saw the base of a large column of gray granite. The town terminates in a narrow point, where a large solid building with many columns seems to have stood.

With the exception of the theatres, the buildings of the city were all constructed of the calcareous stone which constitutes the rock of every part of the country which I saw between Wady Zerka

SHERIAT EL MANDHOUR.

[p.273]and Wady Sheriat. In Djebel Adjeloun, Moerad, and Beni Obeid, none of the basalt or black stone is met with; but in some parts of El Kefarat, in our way from Hebras to Om Keis, I saw alternate layers of calcareous and basaltic rock, with thin strata of flint. The habitations of Om Keis are, for the greater part, caverns. There is no water but what is collected in reservoirs during rains; these were quite dried up, which was the occasion, perhaps, of the place having been abandoned, for we found not a single inhabitant.