File 1450/1919 ‘Mesopotamia & Kurdistan: Geological Reports on’ [64r] (142/522)
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.
3
uplift. An intere^ing point is that it appears that the present drainage system of the hills dates
hack to a penod prior to the deposition of the coral limestone. With regard to the peculiar
subsi lary ome on the crest of the anticline, we are unable to determine at present, to which
period ot earth movement it owes its origin.
PROSPECTS OF THE DISTRICT.
wer ^ fortunate in having the opportunity of examining this district first, as apart from
ar ^ seepages actual drilling had been done, and although the wells are only
shallow, their result is of great value in forming an opinion of the prospects of obtaining good
production in the district.
To arrive at a conclusion the following points must be considered
(a) The existence of oil-bearing beds. —Messrs. Bucking & Porro state that they are unable to
find a continuous oil horizon and therefore do not consider the prospects of the
country as a whole to be very promising. They base this opinion largely on an examin
ation of the complete section of the Lower Ears Beds in the Kara Tchok Mountains
(about 20 miles east of Qaiyarah), where no trace of oil-bearing beds could be found.
As a parallel example, the San Felipe Beds of Mexico, where they crop out, shew
practically no signs of containing oil, yet the largest wells occur in these beds, where
they are overlaid by the Mendez Marls. The seepages of Qaiyarah, also those of
Kirkuk and Fatha (on the Tigris) are in the lower part of the Lower Fars ; also the
result of the wells, drilled only 150—170 feet lower than the seepages, shew that there
are oil-bearing beds in this formation. Taking into consideration the large number of
seepages existing over a large area of Mesopotamia, we conclude that the Lower Fars
Series is an oil-bearing formation of great extent.
(b) The presence of an impervious covering or “cap-rock .”—As will be seen from the attached
succession of beds of the Lower Fars Series, the beds above the highest oil-bearing
horizon are gypsum and marl. At the crest of the anticline only about 80 feet of
these beds overlie it and it is estimated that the total thickness of the Lower Fars
underlying the surface here is not more than 400—500 feet. Gypsum and marl are
suitable as a cap rock, but it is impossible to say whether there is sufficient. It
should be borne in mind that the folding has been gentle, the rocks shew no sign of
fracturing and no trace of faulting. Also no oil, asphalt or graphamite has been seen
in any other part of the Lower or Upper Fars. We, therefore, incline to the view
that the covering of gypsum and marl has been sufficient to preserve the oil.
(c) Geological structure .—As shewn in para. 5 the structure is that of a very elongated dome,
which, on account of its shape and great extent, is considered favourable for the
accumulation of oil.
With regard to the area from which oil may have accumulated into this dome ; the nearest
anticline to the south is at least 20 miles away and to the north some 12 miles. The area
between on both sides is occupied by beds of the Upper Fars Series forming synclines.
Thus the area from which oil can have migrated to accumulate in the anticlinal area is
very great.
*.
(d) The result of the wells .—From the map and sections it will be seen that the wells are
located about \\ miles from the crest of the anticline and some 800—1,000 yards from
the axis. They are therefore located in an unfavourable position. Yet these wells
although they only penetrate some 150 feet into the oil-bearing part of the formation
could be made to yield a production of perhaps 30—-40 tons a day.
The evidence of the wells may, therefore, be considered as a favourable indication.
Taking all these points into consideration, we are of the opinion that the prospects of obtaining
a good production in this district, are favourable.
A. H. NOBLE.
R. DuB. EVAlNS.
Baghdad, 8th June, 1919.
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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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- File 1450/1919 ‘Mesopotamia & Kurdistan: Geological Reports on’
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- 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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