The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
This town is named in Scripture Elath or Eloth; in the Septuagint
Ailath, and Ailôn; Ailas, Aeila, or Aila by the Greeks; Ælana by the
Romans; and Ailah by the Arabians: it is described in 1 Kings ix. 26,
as "on the _shore_ of the _Red Sea_ in the land of Edom;" and in 2
Chron. viii. 17, "at the _sea-side_ in the land of Idumea." From
Procopius, in the 6th century, we learn the following exact
account,[5] which agrees very well with the site of those
_mounds_--"the eastern limits of _Palæstina_ (including of course that
part of the peninsula which he elsewhere relates[6] was called
_Palæstina Tertia_), reach along the Red Sea. On the shore is placed
the town _Aïlas_, where, the sea ending, it is contracted into a very
narrow bay."
Footnote 5: _Procopii_ de Bell. Pers., lib. i., cap. 19.
Footnote 6: _Procop._ de Ædificiis Justiniani, lib. v., cap, 8.
Tom. ii. Edit. _Par._ 1663.
Edrisi, in the 12th century, terms the steep descent from the Desert
El Tyh by El Nakb to Akaba--"Akaba Ailah"--_i.e._, the "Descent of
Ailah;" and Makrisi, in the 14th century, as cited by Burckhardt (p.
511), speaks of "the _Akaba_, or steep mountain _before Aila_."
Consequently, I take it to be correct that these _mounds_ indicate the
former position of _Elath_,[7] on the shore of the Sea of Edom or
Idumea--an arm of the Red Sea.
Footnote 7: Ailah was in the middle ages considered (Robinson,
i., p. 252, and Lepsius' Tour, p. 20), as _Elim_, the sixth
station of the Israelites after they passed the Red Sea. But I
apprehend that the error very likely arose from the word Ailam
occurring in the _Alexandrine MS._, (2 Kings xvi. 6; and 2 Chron.
viii. 17), for Ailath, which is used in the LXX., in those
verses. So Ailam had here been _mistaken_ for Aileim, _Elim_, the
word which is found in Exodus, xvi. 1; of the LXX.
At a short distance from them, but westward, a large space, like a
marsh, seemed to be impregnated with _nitre_, which is left incrusted
in some spots upon their surface. From hence, going up the extensive
valley El Araba, it is found to be full of sand drifts, with here and
there a few trees scattered about; the torrents, after rain, flow
along the west side, and their waters, which are _not absorbed_ by the
_sand_, enter the sea at the north-west angle. The width of this part
of the Wadi is near 5 miles, but in advancing farther to the north it
becomes wider. The mountains on the east are high--from 2000 to 2500
feet; being of _granitic_, or rather _porphyritic_ formation, they are
highly picturesque, and have fine, lofty, jagged peaks: but those on
the west, which are _sandstone_ and _chalk_, are lower; rising to
about a level with the desert El Tyh, they do not exceed 1500, or in
places 1800 feet in elevation.
Public-domain text, read in full here on John Shaqi.
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