The city of JerusalemConder, C. R. (Claude Reignier)
History
The city of Jerusalem
Conder, C. R. (Claude Reignier)
Jerusalem -- Antiquities; Jerusalem -- History
The excavations at the spring showed that a large tank or pool probably
once existed before the cave. The overflow from the cave was also
carried away by the aqueduct, and perhaps brought round to tanks still
existing below Siloam south-west of the pool. If this work was really
ancient, representing the “brook that flowed through the midst of the
earth”[87] even before Hezekiah’s tunnel was made, it is an argument in
favour of the view that the upper city of Jerusalem was the original
Jebusite stronghold.
[Sidenote: EN-ROGEL]
The earliest reference to any feature of Jerusalem topography is the
notice of the spring called En-rogel, on the boundary between Judah and
Benjamin east of the Valley of Hinnom. The meaning of the name has
been differently conjectured,[88] but if the true rendering be “spring
of the water channel,” it would seem that an aqueduct must have existed
at En-rogel when the Book of Joshua was written; and the topographical
evidence in that book indicates a date earlier than the time of Isaiah
and Hezekiah, thus favouring the conclusion that the aqueduct in front
of the cave is ancient.
En-rogel has, it is true, been placed in quite another position.
Brocardus, in the thirteenth century, supposed it to be the well at
the junction of the Kidron and Hinnom valleys which Christians called
“Nehemiah’s Fountain,” in connection with the apocryphal legend of a
fire fountain which was in Persia and not at Jerusalem at all.[89] The
Moslems called it the “Well of Job,” from a legend of the fountain
which sprang up when Job stamped on the ground[90]--perhaps confounding
Job with Joab, since En-rogel was near the “Stone Zoheleth” where Joab
proclaimed Adonijah king. But a well is not a spring, and Zoheleth is
supposed by M. Clermont-Ganneau to be the rock still called _Zahweileh_
(“the slippery”), close to the village of Silwân, and opposite the
cave spring already described, which is the only spring on this side
of Jerusalem. Neither Josephus nor any ancient pilgrim speaks of the
well in question before 1184 A. D., when it was cleared out. There is
no doubt that this well is ancient, but how old it is not easy to say.
It is now 125 feet deep, and at 113 feet below the surface the old
well-shaft rises from a rock-cut cave below. After the rains, in March,
when the Kidron is full of water beneath the surface, a stream here
rises to the surface, and flows down the valley for some distance. West
of the well is a remarkable aqueduct, with another rock reservoir fed
by two channels. This aqueduct is 90 feet below the rock surface, and
runs south for 600 yards. It was discovered by Sir Charles Warren in
1869, and he suggests that this may be the “brook that flowed through
the midst of the earth” which has been noticed above. These works were
evidently intended for the storage of the winter rain waters; but, on
the other hand, the description of the tunnel, with its flights of
Public-domain text, read in full here on John Shaqi.
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