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'GAZETTEER OF PERSIA. VOL. III. PART II: L to Z' [‎267r] (538/988)

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The record is made up of 1 volume (490 folios). It was created in 1918. It was written in English. The original is part of the British Library: India Office The department of the British Government to which the Government of India reported between 1858 and 1947. The successor to the Court of Directors. Records and Private Papers Documents collected in a private capacity. .

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SHA—SHA
886
In cases where the mineral has been more rapidly produced and the
centres of segregation numerous and close to one another, the resulting
nodules soon impinge on one another, unite and include in their interstices
as much as 50 or 60 per cent, of foreign matter. In some few cases lumps
of pure borate have been formed weighing as much as 30 to 40 lbs. when
dry and containing only a few per cent, of sand or earth.
Considerable areas are covered with firm gypsum, above which ulexite
has been deposited, but it is useless on account of the extreme difficulty
attending the separation of the flaky gypsum crystals.
Ulexite is never found at a greater depth than 1 foot and very rarely does
it exceed 8 inches. Much of the corroded mineral appears on the surface
and continues to a depth of 1 to 6 inches. The best mineral, however, is
always found beneath a layer of moist gypseous sand 3 to 4 inches in thick
ness and seldom reaches over 6 inches below. This 2 to 6 inches of ulexite
is never a solid mass but it is in reality a stratum of moist sandy material
containing the white nodules in larger or smaller quantity just like potatoes.
The Sohrab borate deposits .—A group of low hills lie between these deposits
and those of Deh-i-Shutoran.
In a hollow between the spurs of these hills is a branch of the main Kavir
and in this the borate is found. The total extent of the mineral-bearing
area is about 700 yards by 250 yards. The mineral is much more sparsely
distributed than at Deh-i-Shutoran.
Collecting the mineral. —Shovels and bags are the only tools necessary
for the work. Several men go ahead to find the good spots and others
follow and collect the lumps and nodules of borax. Three workmen are able
to oollect from 1 to kharver of borate a day (650 to 975 lbs.).
Drying. —The mineral is emptied on the ground by the people who bring
it. It is thus in a layer 2 to 3 inches thick, exposed to the sun for four or
five days, being turned once, when it is gathered and heaped against the
walls for dressing. The dressing is done by small boys and old men.
The borate contains about 30 per cent, water.
Refining as conducted by natives. —A quantity of crude soda, say 5 bat
mans (3'25 lbs. avoir.), is boiled three or four hours, after which the boiling
is discontinued to allow the mud to settle at the bottom of the boiler, from
which it is taken out with flat spoons. Then some 5 batmans of the
mineral slightly crushed is put in with the solution of soda and boiled.
An hour later the water is let off. When the boiling is stopped the mud
settles and leaves a clear solution of soda and borax in the boiler. This is
put into clay pots to rest 6 to 10 hours. A crust of soda forms at the top
whilst some forms a deposit at the bottom of the pots. The upper crust of
soda is removed and the solution is boiled again to evaporate the water.
What remains in the boiler is then taken out, made into round cakes and
left to dry. This refined borate is then ready for transport.
The great disadvantage of this system is the quantity of soda which still
remains in the refined product. Furthermore, the boiler, being made of
common thin copper sheets and occasionally only being thick wrought
copper boilers, the metal gets corroded and the refined borax becomes of a
greenish or brownish colour. The refined product also contains a small
admixture of mud or earthy substances.
3q

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Content

The item is Volume III, Part II: L to Z of the four-volume Gazetteer of Persia (Provisional Edition, 1917, reprinted 1918).

The volume comprises that portion of south-western Persia, which is bounded on the west by the Turco-Persian frontier; on the north and east by a line drawn through the towns of Khaniqin [Khanikin], Isfahan, Yazd, Kirman, and Bandar Abbas; and on the south by the Persian Gulf The historical term used to describe the body of water between the Arabian Peninsula and Iran. .

The gazetteer includes entries on towns, villages, districts, provinces, tribes, forts, dams, shrines, coastal features, islands, rivers, streams, lakes, mountains, passes, and camping grounds. Entries include information on history, geography, climate, population, ethnography, administration, water supply, communications, caravanserais, trade, produce, and agriculture.

Information sources are provided at the end of each gazetteer entry, in the form of an author or source’s surname, italicised and bracketed.

The volume includes an Index Map of Gazetteer and Routes in Persia (folio 491), showing the whole of Persia, with portions of adjacent countries, and indicating the extents of coverage of each volume of the Gazetteer and Routes of Persia , administrative regions and boundaries, hydrology, and major cities and towns.

The volume includes a glossary (folios 423-435); and corrections (Index to the sub-tribes referred to in the Gazetteer of Persia, Volume III, folios 436-488).

Printed by Superintendent Government Printing, India, Calcutta 1918.

Extent and format
1 volume (490 folios)
Physical characteristics

Foliation: the foliation sequence (used for referencing) commences at the front cover with 1, and terminates at the inside back cover with 492; these numbers are written in pencil, are circled, and are located in the top right corner of the recto The front of a sheet of paper or leaf, often abbreviated to 'r'. side of each folio. Pagination: the file also contains an original printed pagination sequence.

Written in
English in Latin script
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'GAZETTEER OF PERSIA. VOL. III. PART II: L to Z' [‎267r] (538/988), British Library: India Office Records and Private Papers, IOR/L/MIL/17/15/4/2, in Qatar Digital Library <https://www.qdl.qa/archive/81055/vdc_100034842569.0x00008b> [accessed 25 April 2024]

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