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'IRAQ AND THE PERSIAN GULF' [‎90v] (185/862)

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The record is made up of 1 volume (430 folios). It was created in 1944. 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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mfh:
114
GEOLOGY AND DESCRIPTION OF THE LAND
Zab is that one range, the Ghara Dagh, plunges downwards after
entering the Khabur basin, so that the Khabur is deflected round it
instead of passing through it, its place and that of the Av-i-Sarka
trough being taken on the west by the broad plain of Zakho which
greatly increases accessibility.
The Khabur enters Iraq at 37 0 22' N., 43 0 10' E., and for 14 miles
carves a winding course through the hard calcareous rocks of the
frontier ranges. The gorge walls rise steeply from the river bed and
the current is swift. Avalanches sweep both sides in winter and early
spring; and from February to June the river can only be crossed by
wicker bridges at two places, Nazdur and Chalki, or by raft. The
mountain crests east of the gorge are nearly 4,000 feet above the bed
(c. 2,500 ft.), and two summits exceed 7,000 feet above sea-level
(Mamleshkeri, 7,906 ft.; Zinnar, 7,379 ft.); nomad herdsmen can only
cross in summer. The frontier ranges between the Khabur and the
Hazil are not much easier, but there are more tracks.
The Khabur valley opens out for a short distance about 4 miles
below Chalki where a stream enters from the east after draining the
wooded Barwar-i-Bala depression which leads to the Great Zab above
the Baiznur gorge; but it soon closes in at the Gerago-Bilijan defile
by which it passes the western end of the Ser Amadia. Then the
landscape opens out again as the river picks up the Av-i-Sarka which
enters from a fertile well-wooded valley to the east, 5 to 8 miles wide.
The Khabur is now deflected westwards by the declining folds of the
Ghara Dagh, biting into its northern foot and cutting off a low foot
hill. Fifteen miles west of the Av-i-Sarka the Av-i-Rogarm enters
the left bank and the Khabur meets the Jabal Bakhair. The landscape
opens out on the right bank to the broad treeless but grassy plain of
Zakho, 5 to 10 miles wide, with its rich clay soil and overlying gravel.
The river’s left bank is cut in the gravel scree of Jabal Bakhair’s out
lying spurs. Zakho stands on an island in the river, connected by
bridges with the banks; an old high-pitched Turkish bridge spans
the river just above the village; the Khabur widens and shoals below.
Until June the current may be strong, but a month later the river may
be forded at several places; at one ford about 4 miles below Zakho the
river in the low-water season has been recorded as 80 yards wide,
2^ feet deep, and with a current of 3 miles an hour. In flood-time
Zakho is the starting-point of rafts (kelleks) which pass down the
Tigris to Mosul.
A number of torrent beds score the Zakho plain to the north; some
are perennial. The Hazil, which forms the boundary, cuts across the

About this item

Content

The volume is titled Iraq and the Persian Gulf The historical term used to describe the body of water between the Arabian Peninsula and Iran. (London: Naval Intelligence Division, 1944).

The report contains preliminary remarks by the Director of Naval Intelligence, 1942 (John Henry Godfrey) and the Director of Naval Intelligence, 1944 (E G N Rushbrook).

There then follows thirteen chapters:

  • I. Introduction.
  • II. Geology and description of the land.
  • III. Coasts of the Persian Gulf The historical term used to describe the body of water between the Arabian Peninsula and Iran. .
  • IV. Climate, vegetation and fauna.
  • V. History.
  • VI. People.
  • VII. Distribution of the people.
  • VIII. Administration and public life.
  • IX. Public health and disease.
  • X. Irrigation, agriculture, and minor industry.
  • XI. Currency, finance, commerce and oil.
  • XII. Ports and inland towns.
  • XIII. Communications.
  • Appendices: stratigraphy; meteorological tables; ten historical sites, chronological table; weights and measures; authorship, authorities and maps.

There follows a section listing 105 text figures and maps and a section listing over 200 illustrations.

Extent and format
1 volume (430 folios)
Arrangement

The volume is divided into a number of chapters, sub-sections whose arrangement is detailed in the contents section (folios 7-13) which includes a section on text-figures and maps, and list of illustrations. The volume consists of front matter pages (xviii), and then a further 682 pages in the original pagination system.

Physical characteristics

Foliation: the foliation sequence (used for referencing) commences at the front cover with 1, and terminates at the inside back cover with 430; 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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'IRAQ AND THE PERSIAN GULF' [‎90v] (185/862), British Library: India Office Records and Private Papers, IOR/L/MIL/17/15/64, in Qatar Digital Library <https://www.qdl.qa/archive/81055/vdc_100037366478.0x0000ba> [accessed 22 March 2025]

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