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‹Better GutenbergWater Supply: Sinking and Boring WellsChapter VII β€” Examples of Wells Executed, and of Districts Supplied… · 8 of 9Contents›

Water Supply: Sinking and Boring Wells

by Ernest Spon

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Chapter VII Examples of Wells Executed, and of Districts Supplied by Wells

Permian Strata

Durham.β€”Large quantities of water are pumped from the lower Permian sandstone beneath the magnesian limestone of this county, and are used for the supply of the towns of Sunderland, South Shields, Jarrow, and many villages. The quantity, calculated by Daglish and Foster to reach five millions of gallons a day, is obtained from an area of fifty square miles overlying the coal measures. The water-level has not been lowered in the rock by these operations. Along the coast it is that of mean tide, and inland rises to a level of 180 feet. In the coal measures below there is little water, and that little is saline. Sedgwick gives the strata as red gypseous marls, 100 feet; thin bedded grey limestone, 80 feet; red gypseous marls, slightly salt, 200 feet; magnesian limestone, 500 feet; marl slate, 60 feet; lower red sandstone, 200 feet.

Coventry.β€”Warwickshire. The town is supplied with 750,000 gallons of water a day from two bore-holes made in the bottom of the reservoir. The bore-holes are respectively 6 inches and 8 inches diameter, and 200 feet and 300 feet deep. The town is situated on the Permian formation, but Latham states that the supply is procured from the red sandstone, and, from observations made, it has been found that the two bore-holes yield water at the rate of 700 gallons a minute.

Trias Strata

Birkenhead.β€”There are here several deep wells belonging to the Tranmere Local Board, the Birkenhead Commissioners, and the Wirral Water Company, yielding together about 4,000,000 gallons a day. Figs. 222, 223, show a section and plan of the No. 2 or new engine well at the Birkenhead Waterworks. The shaft is 7 feet diameter for 105 feet, with a bore-hole 26 inches for 35 feet, 18 inches for 16 feet, 12 inches for 99 feet, and 7 inches for 150 feet, or a total depth from surface of 405 feet. The water-level is about 95 feet from surface when the engine is not at work. At the upper water-level, shown in the 26-inch hole, the yield was at the rate of 1,807,400 gallons in twenty-four hours, at the lower level at the rate of 2,000,000 gallons in the same time. At the water-level indicated in the 7-inch bore, water was met with in large quantities. The old engine well is almost identical.

Figs. 224, 225, are a section and plan, and Fig. 226 enlarged parts of the well at Aspinall’s brewery, Birkenhead. It consists of a shallow shaft 5 feet in diameter and steined, continued by means of iron cylinders 3 feet 3 inches in diameter and 50 feet in depth. When sand with much water of poor quality was met with, a series of lining tubes was introduced from the point A A, the space between these and the cylinders being filled with concrete. The tubes were discontinued at the sandstone, and the lowest portion of the hole, 3 inches in diameter, is unlined. The water overflows.

Figs. 227, 228, are a section and plan of the well at Cook’s brewery, Birkenhead. The shaft is 6 feet diameter, lined with 9-inch steining, and is 66 feet deep. At 29 feet from surface it is enlarged for the purpose of affording increased storage room for the water. There is a 16-inch pipe at bottom of shaft 49 feet deep, continued by a 12-inch bore-hole 13 feet into the red sandstone. The water-level is 27 feet from the surface of the ground.

Birmingham.β€”Out of the 7,000,000 gallons a day supplied to the town in 1865 by the Waterworks Company, 2,000,000 were derived from wells in the new red sandstone. In that year an Act was passed authorizing the sinking of several new wells, whereby the quantity may be greatly increased.

Burton-on-Trent.β€”Fig. 229 is a section of the well at the London and Colonial Brewery. Extraordinary precautions were taken in constructing this well to obtain the water from the lower strata perfectly free from admixture with that from above. There is a steined shaft within which is an iron cylinder, and this again is lined with brick steining backed with concrete. The bore-hole, 182 feet deep and 4 inches diameter, is lined throughout with copper tubes. At the top the bore-hole is surrounded with a short tube upon which a thread is cut, so that, if necessary, a pipe may be screwed on and up to surface. The water rises to within 6 feet 3 inches of the level of the ground. Fig. 230 is an enlarged section of the arrangements at the top of the bore-hole, and Fig. 231 an enlarged section of the pipe joints.

Crewe.β€”Cheshire. A very plentiful supply of water for the supply of the town and works of Crewe is obtained from a well sunk in the new red sandstone. The water is said to be very pure, and from the analysis of Dr. Zeidler it appears that there are only 6Β·10 grains of solid matter to the gallon.

Leamington.β€”The well in this town is situated at the foot of Newbold Hill, and is 5 feet in diameter and sunk to a depth of 50 feet. At the bottom of the well a bore-hole, part of the way 18 inches and the remainder 12 inches in diameter, is carried down 200 feet. It passes through alternating beds of marl and sandstone, and the surface water met with has been bricked or puddled out. The yield is about 320,000 gallons in twenty-four hours. Previously to this well being made, a trial boring, of which Figs. 232, 233, are sections, was made. This boring was lined with iron tubes 9 inches in diameter for 17 feet, inside this 8 inches in diameter for 22 feet 9 inches, and within this again a 5-inch tube. It was continued by a 5-inch bore reduced to 41⁄2 inches, and at bottom to 3 inches.

Liverpool.β€”The oldest wells are at Bootle, to the north of the town; these consisted in the first instance of three lodges or excavations in the rock, covering about 10,000 feet super and about 261⁄2 feet deep. These were covered with timber or slate roofs, and in them 16 bore-holes were sunk, of various diameters and at depths ranging from 13 feet to 600 feet. In 1850 the yield of one of these bore-holes was 921,192 gallons in twenty-four hours, and the total yield in the same time only 1,102,065.

The water was collected in the lodges and conveyed by a tunnel 255 feet to a well 8 feet in diameter and 50 feet deep, from which it was pumped. The yield of the Bootle well in 1865 was 643,678 gallons a day. Since this time a new well of oval form, 12 feet by 9 feet and 108 feet deep, has been sunk, and at its completion the yield rose to 1,575,000 gallons a day, but it has again diminished considerably.

The Green Lane wells were commenced in 1845, the surface being 144 feet above the sea-level and their depth 185 feet, or 41 feet below the sea-level. Headings extend in all about 300 feet from the shafts in various directions, three separate shafts being carried up to the surface. At first the yield was 1,250,000 gallons a day. A bore-hole, 6 inches in diameter, was then driven to a depth of 60 feet from the bottom of the well, when the yield increased to 2,317,000 gallons. In June, 1856, the bore-hole was widened to 9 inches and carried down 101 feet farther, when the yield amounted to its present supply of over 3,000,000 gallons a day.

The large quantity of water yielded by the Green Lane well is probably due to the existence of a large fault which is considered to pass in a north-westerly direction by the well. In 1869 a bore-hole, 24 inches in diameter at the top and diminishing to 18 inches in diameter, was sunk from the bottom of a new shaft, 174 feet deep, to a depth of 310 feet, and the additional quantity of water derived from the new hole was about 800,000 gallons a day.

The Windsor Station well is of oval form, 12 feet by 10 feet and 210 feet deep, with a length of headings of 594 feet, and a bore-hole 4 inches in diameter and 245 feet deep. The yield is 980,000 gallons a day.

The Dudlow Lane well is also oval, 12 feet by 9 feet, and is sunk to a depth of 247 feet from the surface of the ground. Headings have been driven from the bottom of the well for a total distance of 213 feet, and an 18-inch bore-hole has been sunk to a depth of 196 feet from the bottom of the well, which is chiefly in a close hard rock, with occasional white beds from which the water is mainly obtained. The yield is nearly 1,500,000 gallons a day.

The total weekly supply from wells in Liverpool is upwards of 41,000,000 gallons, and there are also a great number of private wells drawing water from the sandstone, and their supply may be roughly estimated at 30,000,000 gallons a week.

Longton, Staffordshire.β€”The Potteries obtain a portion of their supply from a series of wells at Longton, which are shown in the diagrammatic sectional plan, Fig. 234. The well marked No. 1 is 12 feet in diameter, and 135 feet deep in the new red sandstone. When finished the water rose to within 35 feet from the surface. The cost of the first 45 feet was 3l. 10s. a yard; of the second 45 feet, 6l. 10s. a yard; and the third 45 feet, 9l. a yard. When this well was 36 feet down, a large quantity of water was met with, so a heading was driven at that depth in the direction of No. 2 well; this, after 30 feet, passed through a fault which drained off the water, and the sinking of No. 1 was proceeded with. After the engine had been erected and pumping some short time, it was proposed to drive headings from the bottom; but owing to the pumps taking up so much room in the shaft, there was not space enough for sinking operations to be carried on, and No. 2 well was therefore sunk for convenience sake, at the cost of about 30s. a yard. When No. 2 was down 54 feet, a trial bore-hole 3 inches diameter was put down, and water rose in a jet about 3 feet high. The well was then continued to the level of No. 1, and a heading, 39 feet long, driven between the two shafts. No. 2 has now a 12-inch bore-hole at bottom, down 54 feet.

Headings have also been driven W. and N. of No. 2 well, at a cost of 30s. a yard. The western heading is 213 feet long, driven with a slight rise, and gave much water. There are two headings N., running in the direction of the railway, one over the other. The lower was driven level with the bottom of the shaft, but no water met with; the upper is 36 feet from the surface, and is intended to carry away surplus water down to a line of earthenware pipes which are led along the railway to a low-level reservoir.

In the eastern heading there is a rise of 4 feet, owing to the nature of the strata; and after it had been driven 510 feet, well No. 3 was sunk for ventilation and for drawing out material. A bed of very hard sandstone, 63 feet long, was passed, cost 4l. 10s. a yard, and beyond came marl, in which driving cost 45s. a yard. This heading was continued 330 feet beyond No. 3, and an air-hole 3 inches diameter put down 126 yards deep, but no water was met with. The bed of hard sandstone was also found in driving the lower N. heading, which was discontinued after going into it some 5 or 6 feet. The yield from these wells is about 600,000 gallons a day, and recently a new bore-hole at No. 3 well, when down 350 feet, gave some 380,000 gallons a day additional.

Leek.β€”The Potteries waterworks have also wells at the Wallgrange Springs, near Leek; these rise from the conglomerate beds, and are stated to yield 3,000,000 gallons daily. The water from these springs is pumped into Ladderidge reservoir, and is distributed from thence into the town of Newcastle-under-Lyme and the Potteries.

Middlesborough.β€”The Figs. 235 to 238 are sections and plans of a well at the works of Messrs. Bolckow and Vaughan, Middlesborough, made under the direction of S. C. Homersham, C.E. A trial hole was first put down to a depth of 398 feet 6 inches, and a shaft afterwards sunk by Messrs. Docwra and Son to that depth, through alternating beds of clay, sand, gypsum, and sandstone. At the bottom of the shaft a bore-hole of 18 inches diameter throughout was made with Mather and Platt’s apparatus to a depth of 1312 feet; the first 1160 feet of which were through new red sandstone interspersed with beds of clay, white sandstone, red marl, and gypsum. Next came 40 feet of gypsum, hard white sandstone, and limestone; and the remaining 100 feet were through red sandstone, pure salt rock, occasional layers of limestone, and then salt rock to the bottom. The gross time spent in sinking this bore-hole was 510 days, or an average of 2 feet 5 inches a day.

Ross, Herefordshire.β€”The well at the Alton Court Brewery is shown in Figs. 239, 240. The shaft, 5 feet in diameter and 27 feet deep, is steined with 9-inch brickwork for a distance of 17 feet. At the bottom is a 12-inch bore-hole 100 feet 9 inches deep, unlined. The water is abundant. At level of the bore a heading, 6 feet high, 5 feet wide, and 27 long, has been driven, to afford storage room.

Wolverhampton.β€”This town is partially supplied from wells sunk in the new red sandstone. There are two shafts, 7 feet in diameter and 300 feet deep, a heading 459 feet long, and in this a boring of 390 feet. The yield when first completed was 211,000 gallons a day.

St. Helens, Lancashire.β€”Supplied with about 570,000 gallons daily from two wells, each 210 feet deep, in the new red sandstone. Each well has a bore-hole at the bottom.

Oolitic Strata

Northampton.β€”The well at the waterworks is sunk and bored 253 feet 3 inches in the lias. The shaft is steined with brickwork and iron cylinders in the following order: for 16 feet 9 inches in depth the well is 7 feet 6 inches in diameter, lined with brickwork; at this depth two cast-iron cylinders 5 feet 6 inches diameter are introduced, which are again succeeded by 9-inch brickwork, commencing at 5 feet 6 inches internal diameter and widening out to 7 feet 6 inches in diameter. The bottom of the shaft is floored with bricks at a distance of 120 feet from surface. At this point the bore-hole commences, and for the first 31 feet it is lined with 14-inch pipes, which rise into the shaft 5 feet above the floor. The remaining portion of the bore-hole, 102 feet, is 9 inches diameter.

Swanage, Dorset.β€”The section and plan, Figs. 241, 242, are of a well at Swanage, sunk 60 feet and bored 53 feet, the lining tube rising 8 feet into the shaft, which is 5 feet 6 inches in diameter, and lined with 9-inch steining. The strata passed through are clays and limestones, and may perhaps be referred to the Purbeck beds. At first this well yielded little or no water, but it now gives a sufficient supply.

Cretaceous Strata

Bishop Stortford.β€”The waterworks and well are situate west of the town, near the farm buildings known as Marsh Barns. The shaft is 160 feet deep, the bore-hole 140 feet. The following is a section of the strata;β€”

Feet.
Boulder Clay17
London Clay, 54 feet;β€”
Brown Clay14
Black Clay2
Black Sandy Loam, with iron pyrites12
Black Clay, with lignite11
Dark Grey Sand, with large pieces of sandstone and shells15
Reading Beds, 451⁄2 feet;β€”
Black Clay2
Brown Clay20
Light Brown Sand01⁄2
Variegated Sand18
Brown Clay4
Flints and Pebbles1
To Chalk1161⁄2
Chalk1831⁄2
Total300

The water rises to within 140 feet of the surface of the ground. The yield is 10,000 gallons a minute; only 25 gallons a minute from the bore; the rest from the headings driven north and south respectively at a depth of 154 feet.

Braintree.β€”The well sunk for the Local Board is in a field near Pod’s Brook. The shaft is 8 feet in diameter, steined with 9-inch steining, and carried down 55 feet, the remainder of the well being bored. Strata;β€”

Drift, 14 feet;β€”Feet.
Sandy Gravel5
Drift Clay9
London Clay, 136 feet;β€”
Clay, with sand, shells, and septaria, the bottom part more sandy126
Dark Sand, with a few shells, yielding much water10
Reading Beds, 45 feet;β€”
Mottled Plastic Clays, getting more sandy lower down, and with specks of chalk44
Coarse Black Sandy Clay1
Thanet Sand (?), 33 feet;β€”
Light-coloured Sands, firm and hard, getting darker and more friable lower down20
Light-coloured Sands, firm, changing to coarse and dark13
To Chalk228
Chalk, with much water, rising to about 12 feet from the surface17
Total245

The level of the ground is 140 feet above the sea-level; water stands 29 feet deep; yield about 11,500 gallons an hour.

Brighton.β€”This town has always been supplied from wells sunk in the chalk. One well is sunk near the Lewes Road, and has a total length of 2400 feet of headings driven in a direction parallel with the sea, and at about the coast-level of low water. These headings intercept many fissures and materially add to the yield.

A second well was sunk in 1865, at Goldstone Bottom, and headings driven to the extent of about a quarter of a mile across the valley parallel to the sea.

Goldstone Bottom is a naturally formed basin in the chalk, the lowest side of which, nearest the sea, is more than 60 feet higher than the middle or bottom of the basin. The water is obtained as at Lewes Road, from fissures running generally at right-angles to the coast-line, but they are of much larger size and at far greater distances from each other; whereas at the Lewes Road well it is rare that 30 feet of headings were driven without finding a fissure, and the yield of the largest was not more than 100 to 150 gallons a minute. At Goldstone nearly 160 feet were traversed without any result, and then an enormous fissure was pierced which yielded at once nearly 1000 gallons a minute; and the same interval was found between this and the next fissure, which was of a capacity nearly as large. The total length of the headings at Goldstone Bottom is 13,000 feet. The yield from each well is about 3,000,000 gallons daily.

Chelmsford.β€”The well belonging to the Local Board of Health, situated at Moulsham, yields about 95,000 gallons of water a day. It is sunk for 200 feet; the rest bored. Water overflowed at first, but now that the well is in use and pumped from, the water only rises to 76 feet from the surface. The following strata were pierced;β€”

Feet. In.
Black Soil (Mould)3 0
Drift, 631⁄2 feet;β€”
Yellow Clay2 6
Gravel12 6
Quicksand44 6
Sand, with stones4 0
London Clay, 1861⁄2 feet;β€”
Clay104 0
Clay, with sand50 0
Dark Sand12 6
Clay Slate (? septaria)0 9
Clay and Shells4 0
Clay Slate (? septaria)0 3
Dark Sand and Clay9 6
Sand and Shells4 0
Pebbles1 6
Woolwich Beds;β€”
Sand7 0
Red Clay12 0
Clay and Sand64 0
Dark Thanet Sand30 0
To Chalk366 0
Chalk, 202 feet;β€”
Chalk88 0
Rubble1 0
Chalk113 0
Total568 0

Cheshunt, New River Company.β€”Situate at the engine-house between the two reservoirs. The well is 171 feet deep, and is steined partly with brickwork and partly with iron cylinders. For 12 feet in depth the well is 11 feet 6 inches in diameter, and steined with 14-inch brickwork; for a farther depth of 44 feet it is 9 feet diameter, and steined with 9-inch brickwork; of the 44 feet, 41 feet are lined with cast-iron cylinders, 8 feet diameter, which are also carried to a depth of 105 feet from the surface. There are fifteen cylinders of this size in use, and they are succeeded by others 6 feet 10 inches diameter, of which there are six in use; these are again succeeded by two cylinders 6 feet diameter. The whole of the cylinders are 6 feet in depth. The bottom of the last cylinder is 118 feet from the surface, at which point they rest upon a foundation of 9-inch brick steining 7 feet in depth. At the bottom of the 6-feet cylinders the well widens out in the form of a cone 12 feet 6 inches diameter at the floor, which is 26 feet below the bottom of the 6-feet cylinder. In the centre of the well a bore-hole, 3 inches diameter and 27 feet deep, was made, and the well is provided on the floor-level with headings.

Section of Strata.Feet. In.
Surface Earth1 6
Gravel8 0
London Clay, 47 feet;β€”
Blue Clay45 0
Yellow Clay2 0
Reading Beds, 51 feet;β€”
White Sand12 0
Dark Sand39 0
To Chalk107 6
Chalk63 6
Total171 0

Dorking, Surrey, obtains its water supply from a well sunk into the outcrop of the lower greensand, at the south side of the town. The shaft is 11 feet in diameter and 160 feet deep, steined with 9-inch work laid dry. The yield is not more than 30 gallons a minute, owing to the unfortunate position of the well, but might be considerably increased if suitable means were adopted.

Harrow Waterworks.β€”The well is situate 430 yards to the west of the church. The surface of the ground is 226 feet above the Ordnance datum. There is a shaft for 1931⁄2 feet; the rest is a bore. In a bed of dark red sand 144 feet down, the water was very foul. Strata;β€”

Feet. In.
Light Blue Clay, with light-coloured stone19 11
Brown Clay, with white stone54 11
Dark Mottled Clay15 0
Similar Clay, with dark and green sand4 0
The same, very hard3 0
The same, very hard, and dark sand2 0
Lighter-coloured Hard Clay5 0
The same, and dark sand6 0
Large Pebbles0 6
Clay and Sand5 0
Light Blue Clay0 4
Light-coloured Stone, with red and blue spots1 3
Mottled Clays7 11
Yellow, Light Blue, and Green Clay1 0
Dark Green Clay, with black veins and spots5 0
Blue Clay1 6
Very Hard Brown, Yellow, and Blue Clay4 0
Light Brown Running Sand, with water2 6
Hard Mottled Clays6 6
Light Brown Dead Sand8 8
Black Peat, with dark pebbles0 6
Brown and Green Gravel, with flints3 2
Green Clay0 4
To Chalk158 6
Chalk, with beds of flint 4 to 15 inches in thickness, 15 to 24 inches apart; 3951⁄2 feet down, from surface, a bed of flint 6 feet thick254 0
Total412 6

Water rises to a height of 125 feet below the surface. The yield is about 190 gallons a minute.

Highbury, Middlesex.β€”Well at the residence of H. Rydon, Esq., New Park. Figs. 243 to 245. The shaft is 4 feet 6 inches diameter, and 136 feet deep, steined with 9-inch work set in cement. The bore was commenced with a 12-inch hole, but the character of the ground was such that the successive reductions in size, shown in the enlarged section of the lining tubes, Fig. 245, had to be made. When in the chalk the bore was continued some 48 feet unlined. The strata passed were;β€”

Gravel3feet.
London Clay, 111 feet;β€”
Blue Clay110β€ž
Claystone1β€ž
Reading and Thanet Sand, 85 feet;β€”
Mottled Clay25β€ž
Coloured Sand60β€ž
To Chalk199β€ž
Chalk50β€ž
Total249β€ž

Kentish Town.β€”This well was sunk under the supposition that as the outcrop of the subcretaceous formations was continuous around the margin of the cretaceous basin surrounding and underlying the London tertiaries, except at the eastern border, those subcretaceous formations would be found under London, just as they actually were at Paris. This proved to be the case until the gault was passed, when a series of sandstones and clays was encountered, occupying the place of the lower greensand, but evidently of older geological character, and having many of the features of the new red sandstone.

The surface of the ground, Fig. 246, is 174 feet above Thames high-water mark. There is a shaft for 539 feet; the remainder being bored. The following detailed account of the strata is due to Prestwich.

London Clay, 236 feet;β€”Feet.In.
Yellow Clay306
Blue Clay, with septaria2056
Reading Beds, 611⁄2 feet:β€”
Red, Yellow, and Blue Mottled Clay376
White Sand, with flint pebbles06
Black Sand, passing into the bed below20
Mottled Green and Red Clay10
Clayey Sand30
Dark Grey Sand, with layers of clay96
Ash-coloured Quicksand66
Flint Pebbles16
Thanet Sand, 27 feet;β€”
Ash-coloured Sand100
Clayey Sand40
Dark Grey Clayey Sand110
Angular Green-coated Flints20
Chalk, with Flints (? Upper Chalk), 2441⁄2 feet;β€”
Chalk, with flints1196
Hard Chalk, without flints80
Chalk, softer, with a few flints316
Nodular Chalk, with three beds of tabular flints136
Chalk, with layers of flint326
Chalk, with a few flints and patches of sand96
Very Light-grey Chalk, with a few flints300
Chalk, without Flints (Lower Chalk), 341 feet;β€”
Light Grey Chalk, and a few thin beds of marl1330
Grey Chalk Marl, with compact and marly beds
and occasional pyrites
1610
Grey Marl200
Harder Grey Marl, rather sandy and with
occasional pyrites
270
Chalk Marl, 591⁄4 feet;β€”
Hard Rocky Marl (? Tottenhoe Stone)06
Bluish Grey Marl, rather sandy, lower part more clayey589
Upper Greensand;β€”
Dark Green Sand, mixed with grey clay139
Gault, 1301⁄2 feet;β€”
Bluish Grey Micaceous Clay, slightly sandy390
The same, with two layers of clayey greensand67
Micaceous Blue Clay; at base a layer full of
phosphatic nodules
8411
Lower Greensand (?), 1881⁄2 feet;β€”
Red and Yellow Clayey Sand and Sandstone10
Compact Red Clay, with patches of variegated sandstone40
Dark Red Clay47
Red Clay, Whitish Sand, and Mottled Sandstone30
Hard Red Conglomerate, with pebbles from the
size of a marble to that of a cannon-ball
20
Micaceous Red Clay, mottled in places260
Layers of White Sandstone and Red Sand38
Mottled Sandstone04
Red Sand and Sandstone, with pebbles (a spring)20
Layers of Red Sandstone and White Sand40
Pebbly Red Sand and Sandstone10
White and Red Sandstone50
Fine Light Red Sand29
Hard Sandstone03
Very Fine Light Red Sand40
Red Clay20
Clayey Sand13
Red Sandy Micaceous Clay, with sandstone25
Compact Hard Greenish Sandstone100
Very Micaceous Red Clay10
Grey and Red Clayey Sand11
Light-coloured Soft Sandstone21
Red Sand and Sandstone62
Greenish Sandstone40
White and Grey Clayey Sand, with iron pyrites20
Reddish Clayey Sand, with layers of sandstone38
Micaceous Red Clay184
Greenish Sandstone05
Red Mottled Micaceous Clay, with patches of sand346
Red Quartzose Micaceous Sandstone20
Brownish-red Clayey Sand and Sandstone40
Very Hard Micaceous Sandstone, with pebbles of
white quartz
40
Light Red Clayey Sand100
Red Micaceous Quartzose Sandstone80
Light Red Clayey Sand, small fragments of chalk20
Whitish and Greenish Hard Micaceous Sandstone60
Total13020

The engravings, Figs. 246 to 249, which are on the authority of G. R. Burnell, do not exactly agree with Prestwich’s section, but in the main they are both alike. The following summary may be found of service;β€”

Feet.In.
London Clay2360
Lower London Tertiaries886
Chalk6449
Upper Greensand139
Gault1306
Lower Greensand (?)1886

Michelmersh, Hants.β€”Fig. 250 shows a section of a well in this village, comprised within the writer’s practice. The shaft is 4 ft. 6 in. in diameter and 400 feet deep, steined both above and below the chalk with 9-inch work, the upper course having rings of cement at every 12 inches.

The strata pierced were;β€”

Feet.In.
Surface Soil40
Dark Clay270
Chalk2500
Band of Calcareous Sand26
Upper Greensand170
Total3006

The water rises some 19 feet in the shaft, and is abundant, although up to the present its quantity has not been tested.

Mile End, Middlesex.β€”Well at Charrington, Head, and Co.’s brewery. Figs. 251 to 253. The surface is 331⁄2 feet above Trinity high-water mark.

In the upper part there are three iron cylinders built upon 9-inch brickwork, which is carried down into the mottled clay. A 9-inch iron cylinder, partially supported by rods from the surface, rises some 28 feet into the brick shaft into which it is built by means of rings. Another iron cylinder is carried down into the chalk, the space between the cylinders being filled in with concrete.

The strata passed were;β€”

Feet.In.
Made Earth70
Valley Drift, 6 feet;β€”
Sand30
Gravel30
London Clay, 86 feet;β€”
Blue Clay70
Hard Brown Clay, with claystones680
Brown Sandy Clay20
Hard Brown Sandy Clay, rotten at bottom90
Woolwich and Reading Beds630
Thanet Sand, 40 feet;β€”
Green Sand20
Brownish-green Quicksand and Pebbles20
Brown Sand20
Grey and Brownish-green Sand20
Green Sand and Pebbles20
Brown Sand20
Green Sand and Pebbles150
Grey Sand and small Pebbles20
Dark Grey and Green Sand106
Green Sand and Green-coated Flints06
To Chalk2020
Chalk Flints06
Hard Chalk and Water20
Total2046

The water-level is some 103 feet from surface, and the yield 60,000 to 70,000 gallons a day.

Norwich.β€”Well at Coleman’s works. After a few feet of alluvium the borer passed through hard chalk with flints at distances of about 6 or 7 feet apart, for 700 feet, with the exception of 10 feet at the depth of 500 feet where the rock was soft and of a rusty colour, thence the flints were thicker, namely, about 4 feet apart to the depth of 1050 feet. After this 102 feet were pierced of chalk, free from flints, to the upper greensand, a stratum of about 6 feet, and then gault for 36 feet. The whole boring being full of water to within 16 feet of the surface.

Section of strata;β€”

Feet.
Alluvium12
Hard Chalk, with flints483
Soft Chalk10
Hard Chalk190
Hard Chalk, flints closer350
Chalk without flints102
Upper Greensand6
Gault36
Total1189

Paris.β€”The wells sunk in the Paris basin, of which Fig. 254 is a section, are very numerous, and many of them of great depth. Fig. 255 is a plan indicating the position of the principal wells, and Figs. 256 to 258 sections giving each a summary of the nature and thickness of the formations passed through.

For boring these wells special tools had to be used, which have already been described at length in Chap. VI.

A large Artesian well was, in 1867, being constructed by Dru at Butte-aux-Cailles, Fig. 255, for the supply of the city of Paris, which is intended to be carried down through the greensand to a depth of 2600 or 2900 feet to reach the Portland limestone. The boring in 1867 was 490 feet deep, and its diameter 47 inches.

During the previous 21⁄2 years, M. Dru was engaged in sinking a similar well of 19 inches diameter for supplying the Sugar Refinery of M. Say, in Paris, Fig. 255; 1570 feet deep of this well had been bored in 1867, see Fig. 258.

The well at Grenelle was sunk by Mulot in 1832, and after more than eight years’ incessant labour, water rose on the 26th of February, 1842, from the total depth of 1806 feet 9 inches. The diameter of the bore-hole is 8 inches, ending, as is seen in the detail sections, Figs. 259 to 262, in the lower greensand.

The well of Passy was intended to be executed in the Paris basin which it was to traverse with a diameter, hitherto unattempted, of 1 mètre (3·2809 feet); that of the Grenelle well being only 20 centimètres (8 inches). It was calculated that it would reach the water-bearing stratum at nearly the same depth as the latter, and would yield 8000 mètres or 10,000 cubic mètres in twenty-four hours, or about 1,786,240 gallons to 2,232,800 gallons a day.

Figs. 263 to 266 show a detail section of the strata passed.

The operations were undertaken by Kind under a contract with the Municipality of Paris, by which he bound himself to complete the works within the space of twelve months from the date of their commencement, and to deliver the above quantity of water for the sum of 300,000 francs, 12,000l. On the 31st of May, 1857—after the workmen had been engaged nearly the time stipulated for the completion of the work, and when the boring had been advanced to the depth of 1732 feet from the surface—the excavation suddenly collapsed in the upper strata, at about 100 feet from the ground, and filled up the bore. Kind would have been ruined had the engineers of the town held him to the strict letter of his contract; but it was decided to behave in a liberal manner, and to release him from it, the town retaining his services for the completion of the well, as also the right to use his patent machinery. The difficulties encountered in carrying the excavation through the clays of the upper strata were found to be so serious that, under the new arrangement, it required six years and nine months of continuous efforts to reach the water-bearing stratum, of which time the far larger portion was employed in traversing the clay beds. The upper part of this well was finally lined with solid masonry, to the depth of 150 feet from the surface; and beyond that depth tubing of wood and iron was introduced. This tubing was continued to the depth of 1804 feet from the surface, and had at the bottom a length of copper pipe pierced with holes to allow the water to enter. At this depth the compound tubing could not be made to descend any lower; but the engineers employed by the city of Paris were convinced that they could obtain the water by means of a preliminary boring; and therefore they proceeded to sink in the interior of the above tube of 3.2809 feet diameter, an inner tube 2 feet 4 inches diameter, formed of wrought-iron plates 2 inches thick, so as to enable them to traverse the clays encountered at this zone. At last, the water-bearing strata were met with on the 24th of September, 1861, at the depth of 1913 feet 10 inches from the ground-line; the yield of the well being, at the first stroke of the tool that pierced the crust, 15,000 cubic mètres in 24 hours, or 3,349,200 gallons a day; it quickly rose to 25,000 cubic mètres, or 5,582,000 gallons a day; and as long as the column of water rose without any sensible diminution, it continued to deliver a uniform quantity of 17,000 mètres, or 3,795,000 gallons a day. The total cost of this well was more than 40,000l., instead of 12,000l., at which Kind had originally estimated it.

It may be questioned whether the engineers of the town were justified in passing the contract with Kind to finish the work within the time, and for the sum at which he undertook it; but they certainly treated him with kindness and consideration, in allowing him to conduct the work at the expense of the city of Paris, for so long a period after the expiration of his contract. It seems, however, that the French well-borers could not at the time have attempted to continue the well upon any other system than that introduced by Kind; that is to say, upon the supposition that it should be completed of the dimensions originally undertaken. Experience has shown that both steining and tubing were badly executed at the well of Passy. The masonry lining was introduced after Kind’s contract had expired, and when he had ceased to have the control of the works; the wrought-iron tubing at the lower part of the excavation being a subsequent idea. It has followed from this defective system of tubingβ€”the wood necessarily yielding in the vertical jointsβ€”that the water in its upward passage escaped through the joints, and went to supply the basement beds of the Paris basin, which are as much resorted to as the London sand-beds for an Artesian supply; and, in fact, the level of the water has been raised in the neighbouring wells by the quantity let in from below, and the yield of the well itself has been proportionally diminished, until it has fallen to 450,000 gallons a day. That the increased yield of the neighbouring wells is to be accounted for by the escape of the water from the Artesian boring is additionally proved by the temperature of the water in them; it is found to be nearly 82Β° Fah., or nearly that observed in the water of Passy. This was an unfortunate complication of the bargain made between Kind and the Municipal Council; but it in no respect affects the choice of the boring machinery, which seems to have complied with all the conditions it was designed to meet. The descent of the tubes and their nature ought to have been the subject of special study by the engineers of the town, who should have known the nature of the strata to be traversed better than Kind could be supposed to do, and should have insisted upon the tubing being executed of cast or wrought-iron, so as effectually to resist the passage of the water. At any rate, this precaution ought to have been taken in the portions of the well carried through the basement beds of the Paris basin, or through the lower members of the chalk and the upper greensand.

Ponders End, Middlesex.β€”At the works of the London Jute Company. It will be seen from the Figs. 267, 268, that this well is bored all but the top 4 feet, which is 5 feet across and steined with 9-inch work. The uppermost tube is 12 inches in diameter, decreased to 9 inches, and then to 8 inches, and ending with a 6-inch bore, unlined, in the chalk.

The strata passed were;β€”

Alluvium, 6 feet;β€”Feet.In.
Clay and Mud36
Peat26
Sand and Shingle (Gravel).70
London Clay, 15 feet;β€”
Blue Clay80
Sandy Clay (basement bed?)70
Reading Beds, 491⁄2 feet;β€”
Dead Sand100
Mottled Clays220
Sand and Metal (pyrites?)10
Sandy Clay30
Sand and Pebbles40
Dead Sand16
Dead Sand and Pebbles10
Sand and Pebbles70
Thanet Sand (?), 35 feet;β€”
Green Sand270
Dead Sand80
To Chalk1126
In Chalk2906
Total4030

The water at this well overflows.

Freshwater, Isle of Wight.β€”Well, Figs. 269, 270, sunk at Golden Hill for H.M. Government. The diameter of the shaft is 4 feet 6 inches, brickwork 9 inches thick, there are 3 feet in cement at the top of the well, and 3 feet 9 inches at the bottom. There are four courses in cement every 5 feet, internal work four courses in cement every 10 feet. The bore-hole is lined throughout with pipes of 6 inches, 5 inches, and 4 inches diameter respectively.

Winchfield, Hants.β€”Well, Figs. 271 to 273, at the brewery of Messrs. W. Cave and Son. The shaft above the steining is lined with iron cylinders into which the bore-pipe is carried up.

The strata passed were;β€”

Feet.
Made Earth, Soil, Gravel, Blue Clay
and Dead Sand
350
Dark Sandy Clay3
Black Pebbles2
Coloured Clay5
Stone (septaria?)2
Coloured Clay22
Coarse Shifting Sands7
Total391

The following Table, compiled from the Government Memoirs and other reliable sources, furnishes in a condensed form the most important particulars relating to wells, and trial bore-holes comprised within the geographical area known as the London Basin.

The first column gives the name of the place where the well is situated, the second column that of the county, and the third column the precise locality. The following abbreviations have been employed: B. for Bedfordshire; Berks, Berkshire; Bucks, Buckinghamshire; E., Essex; H., Hampshire; Herts, Hertfordshire; K., Kent; M., Middlesex; S., Surrey.

O.D. stands for, above Ordnance Datum; T., above Trinity high-water mark.

PARTICULARS OF WELLS.
Name of Place.County.Locality.Depth.
of
Shaft.
of
Bore.
in
Tertiary
Strata.
in
Chalk.
to Water
from
Surface.
feet.feet.feet.feet.feet
Remarks.
AbridgeE.Brewery100190290β€”30
London Clay, 280 feet.
ActonM.Mr Engleheart’sβ€”β€”28411912
Dittoβ€žMr. Wood’sβ€”β€”31513540
Ditto, Eastβ€žMr. Davis’sβ€”β€”26768
Albany Streetβ€žLondonβ€”β€”182125β€”
100 feet O.D.
Aldershot PlaceH.β€” β€”β€”β€”194β€”β€”
260 feet O.D.
Dittoβ€žβ€” β€”β€”β€”148691⁄2β€”
245 feet O.D.
Amwell EndHerts.New River Company723473⁄4363833⁄4β€”
Yield about 2,500,000 gallons a day.
ArleseyB.Asylum1003657120β€”
233 feet O.D.; water rises into shaft; yield 2640 gallons an hour.
AshS.S.W. Railway Stationβ€”600370230β€”
290 feet O.D.
Bank of EnglandM.London1371971⁄22341⁄210088
About 27 feet T.; yield, 35 gallons a minute.
BagshotS.Orphan Asylum123523646β€”β€”
Last 192 feet London Clay.
Balham Hillβ€žNear Clapham Commonβ€”β€”347β€”β€”
Last 40 feet Thanet sands.
BarkingE.Byfron’s140β€”140β€”30
Bottom in hard pebbles.
Barnet, EastHerts.Lion’s Down122270162230130
Shaft half steined, half iron cylinders.
Ditto, Newβ€žNear Railway Station137302159280130
BatterseaS.Jones’s Works249β€”249
Dittoβ€žBeaufoy’s Works240β€”240β€”β€”
Yield said to equal 15,000 gallons a day.
BearwoodBerks.Mr. Walters’sβ€”β€”35015
Beaumont GreenHerts.Near Cheshunt1831⁄2β€”1261⁄257
BelleisleM.Pashes and Co.’sβ€”β€”185118118
Berkeley Squareβ€žLondon1601562249280
BermondseyS.Crimscott Streetβ€”β€”120β€”β€”
9 feet O.D.; yield plentiful.
Dittoβ€žDonkin’s Worksβ€”232911⁄21401⁄216
Yield 30 gallons a minute.
Berry GreenHerts.Hadham402060β€”8
BexleyK.Brickfield651101291⁄4453⁄460
Bishop StortfordHerts.Waterworks1601401161⁄21831⁄2140
Supply 10,000 gallons a minute.
Dittoβ€žHockerill851259012078
Good supply.
Dittoβ€žNew Road77β€”5621
BlackfriarsM.Apothecaries’ Hallβ€”β€”21876
BlackheathK.Near Enfield Terraceβ€”β€”10930
Boston Heathβ€žNear Woolwichβ€”β€”13070
BowM.Starch Works176148174150
Boxley WoodK.Near Maidstone3861⁄22131⁄23600β€”
382 feet T.; last 781⁄2 feet in chalk, marl, and gault.
BraintreeE.Near Pod’s Brook551902287216
Yield, 11,500 gallons an hour.
BrentfordM.Brewery30338315535
BromleyK.Gas Works5012015020β€”
Supply abundant.
Dittoβ€žWidmore Kiln529814010
Dittoβ€žDitto55851201061
Dittoβ€žTylney Road778513725
Dittoβ€žWaterworksβ€”β€”70180β€”
Yield, 500 to 600 gallons a minute.
BroxbourneHerts.β€” β€”84β€”846
Water overflowed.
Busheyβ€žNear Watford1422414521
CamberwellS.The Groveβ€”β€”2083001⁄290
Camden StationM.L. and N.W. Railway180220234166150
100 foot O.D.
Camden TownM.Pickford’sβ€”β€”21582120
Good supply.
Dittoβ€žWhitaker’s Brewery2357521090190
CanterburyK.Orphan Asylumβ€”β€”145β€”120
CaterhamS.Waterworksβ€”β€”89349β€”
709 feet T.; through chalk, and 39 feet into upper greensand.
ChelmsfordE.Moulsham20036836620276
Water overflowed at first.
CheshuntHerts.New River Company144271071⁄2631⁄2120
Yield, 702,000 gallons a day.
Dittoβ€žTheobald’s Park711311⁄21211⁄28165
Chiswell StreetM.Whitbread’s Brewery183150183150132
Chiswickβ€žGriffin Brewery204200297107β€”
Yield, 14 gallons a minute.
Dittoβ€žLamb Brewery203194293104
Dittoβ€žDitto833929750
Clewer GreenBerks.Capt. Winterbottom’s4229427066
Dittoβ€žWycombe Cottage2024616997
ColnbrookM.Paper Millsβ€”β€”207175β€”
Water found at 203 feet down.
Colney Hatchβ€žAsylum137193189141
Covent Gardenβ€žMarket14021826098120
70 feet O.D.
Cricklewoodβ€žNear Hampstead2258529119110
157 feet T.
CroydonS.Well for Local Board77β€”1162β€”
Yield 1,500,000 gallons a day.
Dittoβ€žNew Wellβ€”β€”15137111⁄2
Dartford CreekK.Paper Mills34493350β€”
Supply good.
Dittoβ€žDitto102401⁄2302201⁄22
DenhamBucks.Tile House110856712885
DeptfordK.Waterworks27β€”1413β€”
20 feet O.D.
DulwichS.Champion Hillβ€”β€”210298
East Ham LevelE.Beckton Gas Works25175117832
EdgwareM.Mr. Day’sβ€”β€”2904540
Edgware Roadβ€žThe Hydeβ€”β€”10137
EdlesboroughBucks.Well, near Millβ€”301β€”β€”70
6-inch bore; through 50 feet of chalk marl to lower greensand.
ElthamK.Dr. King’s46β€”46β€”17
Dittoβ€žThe Moat110β€”10010
Dittoβ€žMr. Tuck’s441231221⁄2441⁄225
Dittoβ€žWell Hallβ€”1071043
Ditto Parkβ€žβ€” β€”β€”β€”12294170
Enfield LockE.Small Arms Factory452391⁄21521⁄21324
Eppingβ€žWaterworks2751294004260
Slow spring.
ErithK.Mineral Oil Company166β€”14620
FarnhamS.Near Hale Farm176β€”8096
Fleet StreetM.London, Shoe Lane100225100225
FulmerBucks.J. Kay’s85β€”473⁄4371⁄4β€”
Through gravel and Reading beds.
Golden LaneM.Baths and Washhouses158β€”1511⁄261⁄2β€”
65 feet O.D.
GravesendK.Church Street102341201248
Supply good and abundant.
Greenwichβ€žBrewery221588010011
Dittoβ€žEast Street189β€”15930
Dittoβ€žHospital Brewery1551501241⁄21801⁄219
7 feet T.; supply 120 gallons a minute.
Hackney RoadM.Wiltshire Brewery963153⁄41523⁄425980
Haggerstoneβ€žImperial Gas Works1181⁄23021641⁄2256
Hainault ForestE.β€” β€”165β€”11055
Halsteadβ€žThe White Hartβ€”β€”17030
HammersmithM.Average of four wellsβ€”β€”24568β€”
Yield, 16 gallons a minute.
Hampsteadβ€žLower Heath32013037872β€”
Now not used.
Hampstead Roadβ€žEagle Brewery1389414686147
Dittoβ€žReservoir244β€”15292106
77 feet T.
Hanwellβ€žAsylum2309029030β€”
Water to surface.
Harrowβ€žWaterworks1931⁄22191581⁄2254125
226 feet O.D.
Haverstock Hillβ€žOrphan School23016031278196
176 feet O.D.
Hayesβ€žDawley Court193002318827
Hendonβ€žMr. Booth’sβ€”β€”24413276
Highburyβ€žBrewery10421018013495
Yield, 1000 gallons an hour.
Dittoβ€žNew Park13611319950
HoddesdonHerts.New River Company52234241⁄22611⁄22
HollowayM.β€” β€”140200240100
Dittoβ€žCity Prisonβ€”β€”217102
Dittoβ€žHanley Roadβ€”β€”6713
Dittoβ€žRedcap Laneβ€”β€”21090
Dittoβ€žIslington Workhouse234306299250
Hornseyβ€žNear Churchβ€”β€”20248
Dittoβ€žThe Prioryβ€”β€”225β€”β€”
HorselydownS.Anchor Brewery10016215810450
HoxtonM.β€” β€”1521015111
Hyde Park Cornerβ€žSt. George’s Hospital2001371⁄43191⁄418100
50 foot O.D.; yield, 3300 gallons an hour.
Ickenhamβ€žPublic Well64806480
Isle of Dogsβ€žOil Mills273371241⁄22391⁄210
Isle of GrainK.Fort180140320β€”20
21 feet O.D.
IsleworthM.Sion Houseβ€”β€”420115β€”
Water overflowed at the rate of 5 gallons a minute.
Dittoβ€žMr. Wilmot’sβ€”327327β€”β€”
Water rose above surface.
Islington Greenβ€žWebb’s Mineral Water Worksβ€”320176144200
Kensingtonβ€žBreweryβ€”β€”197β€”β€”
16 feet T.
Dittoβ€žBritannia Brewery100170270β€”88
Dittoβ€žHorticultural Society20020131784100
60 feet O.D.
Dittoβ€žWorkhouseβ€”β€”270100
Ditto Gardensβ€žSerpentine263582631⁄4573⁄4105
60 feet O.D.; yield, 250 gallons a minute.
Kentish Townβ€žWaterworks5397633241⁄26443⁄4β€”
Through London clay, 236 feet; London tertiaries, 881⁄2 feet; chalk, 6443⁄4 feet; upper greensand, 133⁄4 feet; gault, 1301⁄2 feet; and into lower greensand (?), 1881⁄2 feet.
Kilburnβ€žBrewery2503023545150
Kingsburyβ€žBrent Reservoir101139132108
Kingston-on-ThamesS.Brook Street9038037199β€”
25 feet O.D.; yield, about 44,000 gallons a day.
KnightsbridgeM.β€” β€”240β€”240β€”50
LambethS.Beaufoy’s Vinegar Works100275201174β€”
Yield, 92 gallons a minute.
Dittoβ€žSouth Lambeth Road251661874
Dittoβ€žBethlehem Hospital301611912015
Dittoβ€žLion Brewery, Belvedere Roadβ€”β€”24517340
Dittoβ€žDuke Street, Street, Clowes & Sons’26184210
Lea BridgeM.Waterworks118β€”10018
Leicester Squareβ€žAlhambra150195244101
Limehouseβ€žJohnson’s, Commercial Road9011019010
Dittoβ€žBrewery, Fore Streetβ€”β€”1391⁄2
Liquorpond Streetβ€žReid’s Brewery2221⁄2401361261⁄2121
70 feet O.D.; yield, 277,200 gallons in 24 hours.
Long Acreβ€žCombe & Co.’s Brewery263228223268β€”
70 feet O.D.; yield, 90 gallons a minute
LoughtonE.β€” β€”β€”53532421190
No water from chalk.
Lower MordenS.On the Green2036534045β€”
Water to surface.
LutonB.Waterworks50272β€”322
MaldonE.Waterworks234β€”234β€”β€”
Entirely through London clay.
MargateK.Cobb’s Brewery31243β€”374
Marylebone RoadM.London; a Brewery18610123255156
Mile Endβ€žMann’s Brewery195β€”18510
Dittoβ€žCharrington’s Brewery204β€”2022103
331⁄2 feet T.; yield, 60,000 to 70,000 gallons a day.
Ditto Roadβ€žCity of London Unionβ€”β€”17510
Millbankβ€žDistillery11519020510070
Level of T.
Dittoβ€žWestminster Breweryβ€”β€”22570β€”
51⁄2 feet T.
MitchamS.Nightingale’s Factoryβ€”21118922
Monkham ParkE.Near Waltham Abbey2251253047650
MortlakeS.Mortlake Brewery302882873150
Yield, 14,000 gallons a day.
Dittoβ€žMr. Randell’sβ€”36531550
New CrossK.Naval School501301255560
NortholtM.Near Harrow12228180604
Notting Daleβ€žNear Notting Hillβ€”β€”24412
Notting Hillβ€žMr. Knight’sβ€”β€”230200
Old Kent RoadS.Welsh Ale Breweryβ€”β€”30170β€”
10 feet O.D.
Old WindsorBerks.Pelham Placeβ€”β€”2229
Dittoβ€žThe Union6018024047
Orange StreetM.Back of National Gallery17412625050115
42 feet T.
Oxford Streetβ€žStar Brewery166170158178
PeckhamS.Marlborough Houseβ€”β€”100123
Pengeβ€žPalace Grounds25031035820290
PentonvilleM.Brewery, Caledonian Road2191⁄2β€”2191⁄245180
To chalk.
Dittoβ€žPrison1702001⁄22191⁄2151
Pimlicoβ€žCubitt’s Works188β€”188β€”β€”
2 feet T.
Dittoβ€žBrewer Street30368271127
Dittoβ€žSimpson’s Factoryβ€”β€”23110036
1 foot T.
Pinnerβ€žHatch End140β€”6080
PlaistowE.Odam’s Manure Worksβ€”β€”1701⁄2128
Ponders EndM.London Jute Company43991121⁄22901⁄2β€”
Water overflows.
Dittoβ€žCrape Works204262
Dittoβ€žLocal Board (Speller)β€”β€”106961⁄2
Dittoβ€žWaterworks2318197107β€”
43 feet T.
Pudsey HallE.Near Canewdon297β€”297β€”β€”
Water abundant and good.
RatcliffeM.Queen’s Head Breweryβ€”β€”160200
Dittoβ€žMarine Brewery16236150102
Dittoβ€žRavenhill’sβ€”137
Regent’s Parkβ€žColosseum15010017179
Dittoβ€žMr. Day’sβ€”β€”18421680
Dittoβ€žZoological Gardens1839122450120
Yield, 90,000 gallons a day.
RichmondS.Old Waterworksβ€”β€”276103
Dittoβ€žStar and Garterβ€”β€”41676
RomfordE.Ind, Coope, & Co.155β€”14510
RotherhitheS.Brandram’s Works3022210714527
Yield, 100,000 gallons in 12 hours.
Dittoβ€žTunnel Flour Millsβ€”β€”125135β€”
15 feet O.D.; yield, 80 gallons a minute.
RuislipM.Near β€œThe George”15903⁄4753⁄430β€”
Water to surface.
Saffron WaldenE.β€” β€”β€”β€”β€”1000
SandhurstBerks.Well at Collegeβ€”603β€”β€”β€”
Trial boring; chalk reached.
SandwichK.The Bank70β€”62820
Sheernessβ€žWaterworks30084384β€”β€”
51⁄2 feet O.D.; yield, 10,000 gallons an hour.
Dittoβ€žDockyard330125455β€”53
Yield, 675 gallons an hour.
ShoreditchM.Truman’s Brewery300230199331120
Yield, 71⁄2 gallons a minute.
Shorne Meade FortK.Near Gravesend112β€”771⁄2341⁄2
Shortlandsβ€žNear Bromley5915010910061
Yield, 1000 gallons an hour.
SloughBucks.Eton Union2810310724
Dittoβ€žRoyal Nurseryβ€”β€”94171⁄2
Dittoβ€žUpton Parkβ€”β€”1021⁄41701⁄4
Dittoβ€žWaterworks117β€”90277
Heading into chalk.
SmithfieldM.Booth’s Distilleryβ€”β€”2307070
SouthendE.Waterworks417β€”417β€”100
Old well.
SouthwarkS.Barclay’s Brewery115288212211β€”
Level of T.; yield, 300 gallons a minute.
Dittoβ€žGuy’s Hospital13217319610984
2 feet T.; yield, 33 gallons a minute.
StainesM.Ashby’s Breweryβ€”β€”369154β€”
Water to surface.
StiffordE.S.E. of Church63β€”3330
Stockwell GreenS.Waltham’s Brewery10021021010046
Yield, 33 gallons a minute.
Dittoβ€žHammerton’s Brewery25186211154β€”
Yield, 46 gallons a minute.
StratfordE.Great Eastern Works56344106294
Dittoβ€žSavill Bros.’ Brewery1121⁄2β€”1091⁄23
Dittoβ€žLangthorn Chemical Works60395132323β€”
Supply abundant.
StreathamS.The Common100185285
SudburyM.London and North-Western Rail. Station200β€”12080
Tottenhamβ€žWarne’s Worksβ€”β€”147104
Dittoβ€žLong Waterβ€”β€”1491⁄21011⁄2
Dittoβ€žTottenham Hallβ€”253153100
Tottenham Court Roadβ€žMeux’s Brewery188622156654β€”
85 feet O.D.; yield, 121⁄2 gallons a minute.
Tower Hillβ€žRoyal Mint1951⁄22021951⁄220280
Trafalgar Squareβ€žLondon168228248148β€”
Yield, 450 gallons a minute.
UpchurchK.Burntwick Islandβ€”236236
Dittoβ€žMilford Hope Marshesβ€”30421094β€”
Good supply at bottom.
Upper Thames StreetM.City of London Brewery9041521029510
Uxbridgeβ€žThe Dolphin121β€”811⁄2391⁄23
Dittoβ€žNear Market Placeβ€”β€”10428151⁄2
Dittoβ€žPage’s Lane98β€”98
Dittoβ€žTown Wellβ€”β€”1093019
Dittoβ€žNear β€œKing’s Arms”2484108β€”19
To chalk.
Dittoβ€žNew Year’s Green Farm63β€”63β€”51
Dittoβ€žHurdle Yard78391⁄278391⁄2
Dittoβ€žNear Meeting House411⁄21091⁄21153639
Dittoβ€žThe Union511621753829
VauxhallS.Burnett’s Distillery14018622410255
Yield, 80 gallons a minute.
Waltham AbbeyE.Brewery164β€”1604β€”
Water supply from bed of sand.
Walthamstow Marshβ€žEast London Waterworksβ€”β€”152140β€”
15 feet T.
WandworthS.Young & Bainbridge’s1701642746045
Yield, 10 gallons a minute.
Dittoβ€žPrisonβ€”β€”3571261⁄280
Yield, 27 gallons a minute.
Dittoβ€žCounty Asylumβ€”β€”331630
Westbourne GroveM.Hippodrome240673007
West Draytonβ€žVictoria Oil Mills12274186100β€”
Water overflowed.
Dittoβ€žVitriol Worksβ€”β€”1331⁄2451⁄2
Dittoβ€žDrayton Mills3146149β€”β€”
To chalk.
West HamE.Mr. Tucker’sβ€”β€”132306
Dittoβ€žUnionβ€”β€”11055
West India DockM.South of Export Dockβ€”β€”120240
Westminsterβ€žArtillery Breweryβ€”β€”230
Dittoβ€žChartered Gas Worksβ€”β€”225
Dittoβ€žVickers’ Distillery1161842495170
Yield, 94 gallons a minute.
Dittoβ€žSwallow Streetβ€”β€”210β€”60
Whitechapelβ€žFurze’s Brewery130218248100
Dittoβ€žSmith’s Distillery10626421016036
36 feet T.
Dittoβ€žSmith, Druce, & Co.’s1411⁄2β€”1411⁄2β€”85
39 feet T.
Willesdenβ€žMr. Kilsby’sβ€”β€”2739730
WimbledonS.Convalescent Hospital2003675373050
Ditto, Newβ€žOpposite β€œWhite Hart”——19375
WindsorBerksClower Lodge4017517540
Dittoβ€žRoyal Brewery72β€”72β€”β€”
Through clay and running sand to chalk.
Dittoβ€žJennings’ Breweryβ€”β€”3050012
Winkfield Plainβ€žCaptain Forbes’——30412670
WithamE.β€” β€”β€”β€”306β€”5
Woodley LodgeBerks.3 miles east of Reading9535130
WoolwichK.Well of Arsenalβ€”β€”541⁄23111⁄237
Dittoβ€žPaper Factoryβ€”55051⁄25441⁄2β€”
Yield, 650 gallons a minute.
Dittoβ€žDockyardβ€”6082058870
Yield good.
WormleyHerts.Nunsbury26761⁄2801⁄222β€”
Water overflows.
Dittoβ€žWest End851501⁄272631⁄262
Wormwood ScrubbsM.β€” β€”β€”β€”2501165

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