Page 210 - Records of Bahrain (2)(ii)_Neat

536 Records oj Bahrain

}G ADMINISTRATION REPORT OK THE PKR8IAN Gfl.K POLITICAL

banked is some 22 yards across by 40 long-, is as clear as crystal with a
slightly green tint and vcr}r beautiful.
It holds a shoal or two of large fish and many water-tortoises. It is
not perfectly sweet, and this applies to
• NnmeoftwoYlUngc*, n jnilcorso nearly all the wells, the drinking water
apnrt, ontho top of tbo circlo of for connoisseurs being brought on camels
c l " from the wells of the Umm Koefik and
Hnnnini, said to bo 20 fathoms deep, in the hills of Rifd-a*.
The water is conducted from these various wells by ordinary unbanked
channels, the larger of which have come to look like natural streams.
'Where it i9 necessary to raise it, this is' done from wells by the ordinary
skin-bucket let do.wu over a pulley, and walked up to the cistern level by
cattle pulling down an incline from channels, generally by leverage of a
date-trunk lightly swung by ropes to a frame and balanced at one end
by a basket of earth, into which it is inserted, so that little exertion is
required to lift up the water.
The Jebel Dukhan, as I said above, seems to be of a sort of lime­
stone. I found some fossil shells upon it. The surrounding cliffs were,
where I saw them, I think, of sandstone; but they are generally limestone,
and this stone was enormously quarried from here, I take it to build the
dead houses under the tumuli.
On nearing the coast, white dusty ground, the cerecloth of dead
t I nppend r *Vetch of ouo group races and habitations, intrudes c\ery*
cf tlie-e, prolally the largest on tbe where as if to enforce attention, and
ipaud.
mighty mounds,f bare of vegetation,
tower above the palm groves.
The map gives a very slight idea of this most noticeable feature.
Mass upon mass, mound upon mound, these mounds stretch on in endless
chains all round the slope that falls from the cliffs to the sea, clinging
more particularly perhaps to the higher ground, but found in separate
clusters near the coast itself.
The parent group is perhaps that at Ali,J a modern village, but
X Se« map. other large ones are to be found at many
places, noticeably those in the Bilad-i-
Kadim, the red ones on the left of the high road to Rifd-a, and the chain
of five or six large ones facing the northern sea near the village of Sirabd,
which arc ouly some out of very many groups, all more or less worthy of
notice. I shall have to recur again to these monuments later on.
Salt in considerable quantity is said to be obtainable at the southern
5 Pliny.—Houm» built of «fossil end of the island, (as also, I am told, on
I00* or the adjacent mainland.) Compare Strabo ■
r^^;iiruof.tc::;g^4. “o£ the houscB built [o£
pregnated with ult). these parts and “ mended with-salt water
douches."
On this subject an Arab from the mainland assured me that in one
place, where they now quarry salt, the remains of old buildings and
pillars are often seen.
ZVee# and Plant*,-— Foremost amongst the trees is, of course, the date,
and some of the date-gardens are extremely fine. Many however are
going and gone to ruin, the result of bad government on the part of the
oliaikh, and indeed in some places that were once flourishing gardens
not a bearing tree remains.