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File 1450/1919 ‘Mesopotamia & Kurdistan: Geological Reports on’ [189v] (401/522)
The record is made up of 1 volume (244 folios). It was created in 1 Dec 1917-26 Jun 1922. 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. .
Transcription
This transcription is created automatically. It may contain errors.
2
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waters of the Tigris and Euphrates discharge into the Gulf) it is 345 miles in a
straight line and 500 miles or more by river, and to either of the possible
oilfields of Hit or the Persian frontier is an additional 100 miles. This factor
is of primary importance in any consideration of the development of these
oilfields.
PAET 3.—STRATIGRAPHY.
(4) Introductory Remarks .—The rocks exposed in the whole of the region
traversed are of Tertiary age ranging from Oligocene to Recent; they are
divided into the following groups :—
Mesopotamian Alluvium
Alluvial Deposits
Koweit Series
Bakhtiari Series .
Pars Series
U pper G roup ■)
Middle ,, >-
Lower ,, )
Asmari Limestone Series
Recent.
»
Pliocene or post-Pliocene.
Pliocene.
Miocene.
Oligocene.
(5) Asmari Limestone Series .—The Asmari Limestone of Hit is a moder
ately hard amorphous pure white apparently easily weathered limestone, it is
first seen in quantity three or four miles up stream from the town where its
gleaming white appearance is very striking and accounts for its being termed,
locally “marble”. With the white variety are interstratified bands of hard
compact fine grained homogeneous limestone of greyish color, which break with
a conchoidal fracture and are identical with the usual type of this limestone in
the Bakhtiari country, ino fossils were observed here but in parts of the
Bakhtiari country this limestone contains many Nummulites. As is usual in
such formations shales are associated with the limestones in Persia, and here
they may be expected at any depth. As the limestone is lying horizontal and
the country is generally flat, nowhere was a thickness much above 50 feet
exposed, and the same 50 feet all the time, so that although we know something
of the lithological characters of these particular horizons, there is at present no
means of judging thickness or ascertaining where the shale groups lie.
{ ^ ie Asmari Limestone of Hit was in the preliminary report called the
“ Euphrates Limestone ” as from lithological characteristics alone it was by no
means certain that it represented a facies of the Asmari Limestone, but it was
subsequently discovered that the Mesopotamian Expeditionary Eorce were
quarrying what appears to he undoubted Asmari Limestone at fi point half way
between Samawah on the Euphrates and Nejef, or near the Ham mar Lake, and
with this additional evidence it seems certain that the limestone at Hit belongs
to the Asmari Series. Near the town of Hit a somewhat porous variety of ti e
limestone contains cavities up to 1 inch in diameter half filled with liquid
bitumen and a bituminous impregnation completely permeates it in many
places.
{6) The Lower Fars Group .—The Lower Ears is the most striking rock
group exposed .in the district, and not the least important since in it we find the
oil of the Persian frontier foothills. It is composed essentially of gypsum and
clay ^shales with sandstones and shelly limestones. The gypsum beds occur up
to 15 feet in thickness, sometimes pure, sometimes with^ a large admixture of
sandy clay. . The sandstones are fine grained, porous and in thin bands only
with a certain amount of calcareous cementing matrix. The intercalated clays
and shales are of dark to bright red color and would be impervious to water or
oil. . The whole group with its white bands of gypsum and red clays has a most
distinctive appearance and may be recognised miles away.
The precise nature of the junction between the Asmari Limestone and the
Lower Ears cannot be said to have been satisfactorily determined as yet. In
the South Gulf region near Lingeh, Lo wer Ears beds lie w T ith marked uncon-
tormabiLty on the upturned edges of an Oligocene Nummulitic limestone
^iuch perhaps might be correlated with the Asmari Limestone, but this is npt
About this item
- Content
This volume contains correspondence, memoranda, reports, telegrams and maps and geological drawings, regarding the geological examination of regions in Mesopotamia and the prospect of petroleum [oil] in these areas.
Included in the volume are the following reports:
- ‘MESOPOTAMIA GEOLOGICAL REPORTS No. 7-11’ (‘No. 7’ is crossed out and replaced with ‘No. 8’), 1920 (ff 9-22)
- ‘GEOLOGICAL REPORT (Mesopotamia) No. 7 NOTES ON THE UNDERGROUND WATER RESOURCES OF NORTHEN MESOPOTAMIA’, 1920 (ff 25-31)
- ‘GEOLOGICAL REPORT (Mesopotamia) No. 6 NOTES ON ZAKHO AND DOHUK [Duhok]’, 1920 (ff 41-44)
- ‘MESOPOTAMIA GEOLOGICAL REPORT 1919’, 1920 (ff 57-109)
- ‘REPORT OF THE BITUMINOUS DEPOSIT NEAR KIFRI’, 1919 (f 114)
- ‘GEOLOGICAL REPORT (Mesopotamia) No 5. THE KIFRI DISTRICT’ (ff 115-116)
- ‘GEOLOGICAL REPORT (Mesopotamia) No 4. RECONNAISSANCE REPORT ON THE COUNTRY ON THE RIGHT BANK OF THE RIVER TIGRIS BETWEEN BAIJI AND MOSUL’, 1919 (ff 122-129)
- ‘GEOLOGICAL REPORT (Mesopotamia) No 3. RECONNAISSANCE REPORT ON THE EUPHRATES VALLEY BETWEEN HILLAH AND HIT’, 1919 (ff 131-143)
- ‘GEOLOGICAL REPORT (Mesopotamia) No 2. PRELIMINARY NOTES ON THE JABAL HAMRIN’, 1919 (f 143)
- ‘GEOLOGICAL REPORT (Mesopotamia) No 1 ON THE DISTRICT OF QAIYARAH [Al Qayyarah]’, 1919 (ff 146-151)
- ‘APPENDIX. Translation of a Captured Document. Report of a Tour to the Coal Area and Petroleum Springs in the Zone of the Sixth L. of C. Inspectorate’, 1919 (ff 156-158)
- ‘No 13. Notes on the Jabal Gilabat [Qilabat] between Chinchal-al-Kabir and Qarah Tappah’, 1919 (f 164)
- ‘No 14. Notes on the Jabal Hamrin between Qarah Tappah and Table Mountain’, 1919 (ff 164v-167)
- ‘No. 10. Notes on the Geology of the Country between Tazah Khurmatu and Tauq [Tukhama Khulu]’, 1919 (ff 182-185)
- ‘REPORTS ON THE PROSPECTS OF PETROLEUM IN THE BAGHDAD WILAYAT [Vilayet]’, 1918 (ff 187-201)
- ‘Report No 9. Oil in the Kirkuk Anticline’, 1919 (ff 204-205)
- ‘No 3. Report on the Prospects of Obtaining Oil in the Jab-al-Khanuqah, S.E. of Sharqat [Ash Sharqat]’, 1918 (f 207)
- ‘No 4. Prospects of Obtaining Oil in the Jab-al-Qaiyarah and its continuation, the Jab-al-Najmah’, 1919 (ff 208-209)
- ‘No 5. Possibilities of Obtaining Oil in the Jab-al-Mishrak [Al Mishraq] and Country West of Hammam Ali [Hammam al Ali]’, 1919 (ff 210-211)
- ‘No 6. The Country between Mosul and Quwair [Al Kuwayr] on the Greater Zab, and its Prospects as Oil-producing Territory’, 1919 (ff 211v-212)
- ‘Report No 7. Sulphur near the Confluence of the Greater Zab with the Tigris’, 1919 (f 213)
- ‘No 8. Prospects of Obtaining Oil in the Quwair Dome’, 1919 (ff 213-214)
- ‘Appendix to Report No. 4, on the Jab-al-Qaiyarah Oil-field’, 1919 (f 214v)
- ‘Report on the prospects of obtaining Oil in the Jabal-Hamrin and Jabal- Makhul between Tikrit and Sharqat’, 1918 (ff 217-218)
- ‘Odd Notes on the Country between Tikrit and the Jabal-Hamrin and Jabal Makhul’, 1918 (ff 219-220)
- ‘PRELIMINARY REPORT ON THE PROSPECTS OF PETROLEUM IN THE BAGHDAD WILAYAT’, 1918 (ff 233-236).
Also included in the volume are the following maps and geological drawings:
- ‘TO ACCOMPANY GEOLOGICAL REPORT MESOPOTAMIA No 8’, 1920 (f 20)
- ‘To ACCOMPANY GEOLOGICAL REPORT MESOPOTAMIA No 8 ON THE SULAIMANIYAH DISTRICT’, 1920 (f 21)
- ‘TO ACCOMPANY GEOLOGICAL REPORT MESOPOTAMIA No: 7a. THE WATER RESOURCES OF THE MANDALI-BADRAH DISTRICT’, 1920 (f 30)
- ‘GEOLOGICAL REPORT (MESOPOTAMIA) No 7 NOTES ON THE UNDERGROUND WATER RESOURCES OF NORTHERN MESOPOTAMIA’, 1920 (f 31)
- ‘TO ACCOMPANY GEOLOGICAL REPORT No 6’, 1920 (f 44)
- ‘TRANSVERSE SECTION. JABAL HAMRIN’ (f 88)
- ‘Diagrammatic Section across Jabal Hamrine [Hamrin] in the Table mountain area, shewing [showing] relationship of Pos Tertray [Post-Tertiary] Gravel to the Tertainis [Tertiaries]’ (f 168)
- ‘Red Clay & Sandstone Series Transverse section across Jabal Gilbat’ (f 169)
- ‘QĀRAH TAPPAH’, 1918 (f 170)
- ‘CHINCHĀL-TALISHĀN’, 1918 (f 172)
- ‘SHAHRABĀN’, 1917 (f 174)
- ‘MANSURĪYAH AL JABAL’, 1918 (f 176)
- ‘1 Diagrammatic Section N[orth]. of the Tuz Khurmatu’ (f 183)
- ‘2 Diagrammatic Section oposite [ sic ] Sulaiman Beg, just N[orth]. of the stream’ (f 183)
- ‘3 Diagrammatic Section oposite [ sic ] Sulaiman Beg just S[outh]. of the Stream’ (f 183v)
- ‘Transverse Section across Jabal Nasaz near Gil’ (f 185)
- ‘GEOLOGICAL MAP OF NAFT KHANA DISTRICT OF MESOPOTAMIA’ (f 198)
- ‘THE PETROLEUM DEPOSITS OF HIT’ (f 199)
- ‘GEOLOGICAL RECONNAISSANCE IN N.E. MESOPOTAMIA’ (f 200)
- ‘SECTION FROM SHAHRABAN TO CHAH SURKH [Chiya Surkh]’ (f 201)
- Transverse Section Maps of Jabal Hamrin and Jabal Makhul (f 220).
The volume comprises internal correspondence between British officials of different departments. The principal correspondents are: the Civil Commissioner, Baghdad; the Under-Secretary of State, 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. ; the Political Agent A mid-ranking political representative (equivalent to a Consul) from the diplomatic corps of the Government of India or one of its subordinate provincial governments, in charge of a Political Agency. , Baghdad; officers of the Imperial Mineral Resources Bureau; and officers from the Petroleum Department.
The volume includes a divider which gives the subject number, the year the subject file was opened, the subject heading, and a list of correspondence references by year. This is placed at the back of the correspondence.
- Extent and format
- 1 volume (244 folios)
- Arrangement
The volume’s contents are arranged in approximate chronological order from the rear to the front of the volume.
- Physical characteristics
Foliation: the foliation sequence (used for referencing) commences at the inside front cover with 1 and terminates at the inside back cover with 246; 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. A previous foliation sequence, which is also circled, has been superseded and therefore crossed out.
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- English in Latin script View the complete information for this record
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- Reference
- IOR/L/PS/10/815
- Title
- File 1450/1919 ‘Mesopotamia & Kurdistan: Geological Reports on’
- Pages
- front, back, spine, edge, head, tail, front-i, 2r:19v, 22r:29v, 32r:43v, 45r:87v, 89r:167v, 177r:182v, 184r:184v, 186r:197v, 202r:219v, 221r:245v, back-i
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- East India Company, the Board of Control, the India Office, or other British Government Department
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- Open Government Licence