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Morton, G. H. The Geology of the Country around Liverpool.. Ed. 2. Water Supply, pp. 170-180. 8vo. Lond.

Pearson, H. W. Some of the Water-Bearing Strata and Wells sunk in same. With special reference to Wells in the New Red Sandstone Formation. Proc. Bristol Nat. Soc. vol. vi. pt. iii. pp. 327-341.

Shore, T. W. Springs and Streams of Hampshire. Papers Hants Field Club, vol. ii. pt. i. pp. 33-58.

Thompson, Professor S. P. On the Sources of the River Aire. Rep. Brit. Assoc. for 1890, pp. 821, 822.

Whitaker, W., F. J. Bennett, and S. B. J. Skertchly. Appendix ii. Well Sections, pp. 110-119 of Memoirs of the Geological Survey. England and Wales. The Geology of Parts of Cambridgeshire and Suffolk. (Ely, Mildenhall, Thetford.) 8vo. Lond.

Whitaker, W. and A. H. Green. London County Council. London Water Supply Enquiry. Preliminary Report on the possibility of obtaining a Supply of Water for London within the Thames Basin. 8vo. Lond. Pp. 20, plate (section). Privately printed.

1892.

Anon. Waterworks, Shropshire and Montgomery Counties Lunatic Asylum. [Account of Well.] Engineer, vol. lxxiii., p. 379.

Barclay, T. The Future Water Supply of Birmingham. (Refers to the present supply from Wells. With remarks and sections by H. JOHNSON.) 8vo. Birmingham and London.

De Rance, C. E. Further Notes on Triassic Borings. Trans. Manch. Geol. Soc. vol. xxi. pp. 477–488.

On the Underground Waters of Lincolnshire. Proc. Yorksh. Geol. Soc. vol. xii. pt. i. p. 22.

Frankland, Dr. P. What is the Importance of Magnesia in Drinking Water Trans. 7 Internat. Congr. Hygiene, vol. v. pp. 82-87.

Grover, J. W. An Explanation of the London Water Question. Trans. Surveyors' Inst. vol. xxiv. p. 195.

Hopkinson, J. The River Colne and the Swallow-holes at Potterells. Trans. Herts. Nat. Hist. Soc. vol. vi. pt. 7, pp. xxix-xxxii.

Hopkinson, J., and others. (Remarks on lowering of water-level, in

a Discussion.) Ibid. p. xxxix.

Latham, B. The Influence of Ground-Water upon Health.

7 Internat. Congr. Hygiene, vol. vii. pp. 145-148.

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Lobley, J. L. The Supply of Water to London in the Near and Distant Future. 8vo. Lond. Reprinted, with Additions, from the County Council Times.

Marley, John. On the Cleveland and South Durham Salt Industry. Trans. Fed. Inst. M. Eng. [? Trans. N. Engl. Eng.], vol. xxxix. pp. 91124, pts. liv. lv.

Platnauer, H. M. Notes on Two Borings [Strensall, Hanby Road]. Ann. Rep. Yorksh. Phil. Soc. for 1891, pp. 77–79.

Tate, T. Notes on Recent Borings for Salt and Coal in the Tees District. Quart. Journ. Geol. Soc. vol. xlviii. pp. 488-495.

Whitaker, W. Some Essex Well-sections. (Part iii.) Essex Naturalist, vol. vi. pp. 47-60.

Borough of King's Lynn. Water Supply for the Town.

Pp.

Report on the Best Source for a 8. 8vo. Lynn. Reprinted, with

Reports by J. Mansergh and E. J. Silcock, in 'Borough of King's Lynn. Information respecting the Proposed New Water Scheme.' 8vo. Lynn.

1893.

Willoughby, Dr. E. F. The Water Supply of Maritime Towns. Trans. 7 Internat. Congr. Hygiene, vol. vii. pp. 140–143.

1893.

Report of the Royal Commission appointed to inquire into the Water Supply of the Metropolis. 4 pts. Fol. Lond.

Bothamley, C. H. The Mineral Waters of Askern in Yorkshire. Journ. Chem. Soc. vol. lxiii. pp. 685-696.

De Rance, C. E. Results of the Salt Union Boring at Marston, near Northwich. Trans. Manch. Geol. Soc. vol. xxii. pts. ix. x. pp. 269-302. Evans, Sir John. Hertfordshire and its Water Supply. Herts Illustrated Review, no. 1 (5 pages).

Goodchild, J. G. Notes on the Water Supply of Edenside. Trans. Cumb. Assoc. no. xvii. pp. 43-51.

Hodson, G. A Consideration of some of the Conditions requisite for obtaining Underground Water Supplies, Illustrated by a description of the Works for supplying Long Eaton and Melbourne (Derbyshire), and Castle Donington (Leicestershire.) Trans. Assoc. Munic. County Eng. vol. xix. Reprinted. 8vo. Loughborough. Pp. 39; 9 plates.

Jukes-Browne, A. J. On some Recent Borings through the Lower Cretaceous Strata in East Lincolnshire. Quart. Journ. Geol. Soc. vol. xlix. pp. 467-478.

Mansergh, J. Borough of Tunbridge Wells. Water Supply. Report (Geological Report, by W. Topley, at end). 8vo. Tunbridge Wells. Palmer, P. H. To the Chairman and Members of the Water Committee of the Corporation of Hastings. Brede Valley Water Scheme. Pp. 11. Fol. Hastings.

Thresh, Dr. J. C. The Shallow and Deep Well Waters of Essex. Essex Naturalist, vol. vii. pp. 28-40, 43-45.

Valon, W. A. M. Inaugural Address of the President. [Largely concerned with Water from the Chalk.] Soc. Eng.

Whitaker, W. On Maps showing the Area of Chalk available for Water Supply in the London Basin. Trans. San. Inst. vol. xiii. pp. 243253. An abstract in Trans. 7 Internat. Congr. Hygiene, vol. vii. p. 144 (1892).

Local Geology from a Sanitary Standpoint [Portsmouth]. Trans. Sanitary Inst. vol. xiii. pp. 266-271.

Whitaker, W. (and others). Memoirs of the Geological Survey. England and Wales. The Geology of South-Western Norfolk and of Northern Cambridgeshire. 8vo. Lond. (Springs. Water, pp. 147–153. Wells, 154-164.)

Whitaker, W., and H. B. Woodward. Notes of some Somerset Wells. Proc. Bath Field Club, vol. vii. no. 4, pp. 340-345.

Wills, C. Notes on an Outbreak of Typhoid Fever [? near Shireoaks Colliery. Note on water, and analysis, pp. 140, 141]. Public Health, vol. v. no. 5, p. 139.

Winwood, Rev. H. H. On some Deep-Well Borings in Somerset and elsewhere. Proc. Bath Field Club, vol. vii. no. 4, pp. 335-340.

W[orth], R. N. [Note of Boring at Plymouth.] Trans. Devon. Assoc. vol. xv. pp. 173, 174.

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Anon. Remarkable Overflowing Artesian Well [Bourn, Lincolnshire]. Engineer, vol. lxxvii. pp. 23, 24.

Elworthy, T. The Hastings Water Supply Past and Present. Pp. 8, map. 8vo. Hastings.

Fritton, G. W. The Waters of the Arden: a sketch of its Springs, Wells, Rivers, Lakes, Pools, and Marshes, within the basin of the Avon. Proc. Warwicksh. Field Club for 1893, pp. 19-36.

Hodson, G. Epsom Local Board of Health. Report . Water Supply. Pp. 29. Fol.

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Suffolk County Lunatic Asylum. Report on the Protection of the Water Supply . . . accompanied by Reports of Dr. E. Frankland and Dr. G. Thresh. Pp. 29. Fol.

Hull, Prof. E. Artesian Boring at New Lodge, near Windsor Forest (Berks). Quart. Journ. Geol. Soc. vol. 1. pp. 152-155.

Palmer, P. H. Hastings Corporation Waterworks. Brede Valley Scheme. Pp. 23. Fol. Hastings.

Pendlebury, W. H. Chemistry of Dover Water. S. E. Naturalist, vol. i. pt. iv. pp. 107–114.

Topley, W. Borough of Tunbridge Wells. Water Supply. Water Supply. Report. Pp. 4. 8vo. Tunbridge Wells.

Whitaker, W., and A. J. Jukes-Browne. On Deep Borings at Culford and Winkfield, with Notes on those at Ware and Cheshunt. Quart. Journ. Geol. Soc. vol. 1. pp. 488-514.

Tunbridge Wells. Temporary Association for Promoting the Utilisation of our Surplus Water Supply. Pp. 16. 8vo. Tunbridge Wells. (Gaugings of Springs.)

Which Recommendation of Mr. Mansergh will the Burgesses Vote for if the Town is Polled-Penbury Spring Water, or Ashdown Surface Water? (Issued by the Temporary Association.) Pp. 32. 8vo. Tunbridge Wells. (Gaugings of Springs.)

1895.

Barwise, Dr. S. The Mountain Limestone as a Source of Underground Water. Public Health, vol. vii. pp. 416, 417.

Hull, Prof. E. On 'The Water Supply of the Borough of St. Helens, Lancashire, from Wells in the New Red Sandstone.' Trans. San. Inst. vol. xv. pt. iv. pp. 578-585. Discussion, pp. 596-603.

Peirce, W. G. Inaugural Address. (Refers to Water from Chalk.) Trans. Soc. Eng.

Whitaker, W. On the Chalk of the London Basin in regard to Water Supply. (Reprinted from Rep. R. Comm. Metrop. Water Supply, with small additions.) Geol. Mag. dec. iv. vol. ii. pp. 360–366.

Some Surrey Wells. Trans. Croydon Micr. Nat. Hist. Club, 1894-95, pp. 132-150.

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Cetiosaurus Remains.—Report of the Committee, consisting of Professor A. H. GREEN (Chairman), Mr. JAMES PARKER (Secretary), the EARL of DUCIE, Professor E. RAY LANKESTER, and Professor H. G. SEELEY, appointed to examine the Ground from which the Remains of the Cetiosaurus in the Oxford Museum were obtained, with a View to determining whether other parts of the same Animal remain in the Rock.

THE Committee have to report that from unavoidable circumstances no satisfactory conclusion has as yet been arrived at.

During the Easter vacation, when excavations might have been made, their Chairman, Professor A. H. Green, was prevented by illness from taking any active part, and therefore no orders could be given for actual operations in the way of digging. Several visits, however, have been made to the spot and information obtained; and, further, full permission has been obtained from Lord Valentia, the owner of the land, to make such excavations as are required, and co-operation from his agent has also been promised.

The quarry where the bones were found is in a slope facing the north, and to the south of the spot where it has been ascertained they lay, further excavations would be attended with much difficulty, as the ground rises rapidly some 20 feet and is surmounted by a wall, on the other side of which there is a high road, and excavations might endanger its stability.

On the western side, where it was thought most advisable to excavate, it was at the last moment discovered that some two or three years previously some excavations had been undertaken with the same object, but without success, and then filled up again. As to reopening and extending these, a decision cannot be come to till further particulars as to what was done are obtained and the men found who were employed. On the eastern side there is perhaps more chance of success, but the ground here also has at some time been evidently much broken up.

Meanwhile, however, the opening of a quarry about 350 yards to the south has disclosed the circumstances that the sandy bed, which contained the bones of the Cetiosaurus and which also contains much carbonaceous matter, is continued in this direction. The pit where the bones were found is on the northern edge of a promontory round which the Cherwell river runs, and the quarry lately opened is practically on the south edge of the same promontory. The bed is of the same thickness, namely, from 6 to 12 inches, and appears from the measurements at present taken to be almost exactly at the same level in each spot, and in each case resting upon some 20 feet of limestone beds belonging to the Great Oolite. Most of these beds are very hard and more or less fossiliferous, but one or two very soft. One soft bed, about 6 feet below this sandy parting, is crowded with Terebratula maxillata. This bed is found in one or two other sections not far distant, and forms a definite datum line in the several sections for comparison.

Above the sandy parting, in both the Cetiosaurus pit and the newly opened pit, there is a bed of about 4 feet of shale, immediately followed by the hard slabs and slaty beds of the Forest Marble.

This 6 to 12 inch sandy bed, with the carbonaceous matter in which the bones were found, may be certainly taken as the line of demarcation

between the Great Oolite and the Forest Marble; and though there is no trace of unconformity (the beds being all practically horizontal), the sudden change in lithological character points to a marked change of physical circumstances, in which the surface, if not actually becoming dry land, must have become nearly so, to be followed again by the shales and the marine beds of the Forest Marble.

This change may perhaps account for so many bones of one individual animal being found together and comparatively so little worn by any movement whatever.

Some 400 yards to the east, and about the centre of the promontory, large quarries are open, which pass through 25 feet of the Cornbrash and Forest Marble, apparently reaching the shales which rest on the sandy parting referred to, as shown in the other sections. Though there is no reason to anticipate that any of the bones of this particular animal may have been drifted in this direction, it is thought advisable to make an excavation or so at the place with the view of ascertaining exactly how far the particular sandy parting is extended.

In the uncertainty as to which was the best spot where to set the excavations going, the Chairman felt he was not justified in drawing any money on account of the grant of 201.; but now that permission has been granted and several observations and measurements made and inquiries set on foot, the Committee would request that the grant may be renewed, so that the inquiries and observations may be continued, and that at the first favourable opportunity some trial holes may be made, partly with a view of being satisfied that no further remains of that animal exist near the spot where the others were found, partly also of determining somewhat further than has been done the circumstances under which those remains were deposited in that spot, and the relation of the bed in which they occur to the Great Oolite below and the Forest Marble above.

Photographs of Geological Interest in the United Kingdom.-Sixth Report of the Committee, consisting of Professor JAMES GEIKIE Chairman), Professor T. G. BONNEY, Dr. TEMPEST ANDERSON, the late Dr. VALENTINE BALL, Mr. JAMES E. BEDFORD, Professor W. BOYD DAWKINS, Mr. EDMUND J. GARWOOD, Mr. J. G. GOODCHILD, Mr. WILLIAM GRAY, Mr. ROBERT KIDSTON, Professor T. MCKENNY HUGHES, Mr. A. S. REID, Mr. J. J. H. TEALL, Mr. R. H. TIDDEMAN, Mr. W. W. WATTS, Mr. H. B. WOODWARD, and Mr. OSMUND W. JEFFS (Secretary). (Drawn up by the Secretary.)

APPENDIX

1. Schedule of the Collection of Photographs II-List of Photographs illustrating Geological Papers

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413

YOUR Committee have the honour to report that during the past year 161 photographs have been received, thus bringing up the number registered since the commencement of their operations to a total of 1,216. Particulars of the new additions are, as heretofore, given in this Report. By far the greater number of these are the work of Mr. Godfrey Bingley, of Leeds, to whom the Committee are indebted for much valuable assistance. They desire to record their thanks to the following donors of photographs and others who have rendered aid in various ways: Professor

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