Cretaceous Strata.

Bishop Stortford.—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;—

Feet.
Boulder Clay 17
London Clay, 54 feet;—
Brown Clay 14
Black Clay 2
Black Sandy Loam, with iron pyrites 12
Black Clay, with lignite 11
Dark Grey Sand, with large pieces of sandstone and shells 15
Reading Beds, 4512 feet;—
Black Clay 2
Brown Clay 20
Light Brown Sand 012
Variegated Sand 18
Brown Clay 4
Flints and Pebbles 1
To Chalk 11612
Chalk 18312
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.—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;—

Drift, 14 feet;—Feet.
Sandy Gravel 5
Drift Clay 9
London Clay, 136 feet;—
Clay, with sand, shells, and septaria, the bottom part more sandy126
Dark Sand, with a few shells, yielding much water 10
Reading Beds, 45 feet;—
Mottled Plastic Clays, getting more sandy lower down, and with specks of chalk 44
Coarse Black Sandy Clay 1
Thanet Sand (?), 33 feet;—
Light-coloured Sands, firm and hard, getting darker and more friable lower down 20
Light-coloured Sands, firm, changing to coarse and dark 13
To Chalk228
Chalk, with much water, rising to about 12 feet from the surface 17
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.—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.—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;—

Feet. In.
Black Soil (Mould) 3 0
Drift, 6312 feet;—
Yellow Clay 2 6
Gravel 12 6
Quicksand 44 6
Sand, with stones 4 0
London Clay, 18612 feet;—
Clay104 0
Clay, with sand 50 0
Dark Sand 12 6
Clay Slate (? septaria) 0 9
Clay and Shells 4 0
Clay Slate (? septaria) 0 3
Dark Sand and Clay 9 6
Sand and Shells 4 0
Pebbles 1 6
Woolwich Beds;—
Sand 7 0
Red Clay 12 0
Clay and Sand 64 0
Dark Thanet Sand 30 0
To Chalk366 0
Chalk, 202 feet;—
Chalk 88 0
Rubble 1 0
Chalk113 0
Total568 0

Cheshunt, New River Company.—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 Earth 1 6
Gravel 8 0
London Clay, 47 feet;—
Blue Clay 45 0
Yellow Clay 2 0
Reading Beds, 51 feet;—
White Sand 12 0
Dark Sand 39 0
To Chalk107 6
Chalk 63 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.—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 19312 feet; the rest is a bore. In a bed of dark red sand 144 feet down, the water was very foul. Strata;—

Feet. In.
Light Blue Clay, with light-coloured stone 19 11
Brown Clay, with white stone 54 11
Dark Mottled Clay 15 0
Similar Clay, with dark and green sand 4 0
The same, very hard 3 0
The same, very hard, and dark sand 2 0
Lighter-coloured Hard Clay 5 0
The same, and dark sand 6 0
Large Pebbles 0 6
Clay and Sand 5 0
Light Blue Clay 0 4
Light-coloured Stone, with red and blue spots 1 3
Mottled Clays 7 11
Yellow, Light Blue, and Green Clay 1 0
Dark Green Clay, with black veins and spots 5 0
Blue Clay 1 6
Very Hard Brown, Yellow, and Blue Clay 4 0
Light Brown Running Sand, with water 2 6
Hard Mottled Clays 6 6
Light Brown Dead Sand 8 8
Black Peat, with dark pebbles 0 6
Brown and Green Gravel, with flints 3 2
Green Clay 0 4
To Chalk158 6
Chalk, with beds of flint 4 to 15 inches in thickness, 15 to 24 inches apart; 39512 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.

Figs. 243-245.
Well at Highbury.

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Highbury, Middlesex.—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;—

Gravel 3feet.
London Clay, 111 feet;—
Blue Clay110
Claystone 1
Reading and Thanet Sand, 85 feet;—
Mottled Clay 25
Coloured Sand 60
To Chalk199
Chalk 50
Total249

Kentish Town.—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.

Figs. 246, 247.
Boring at Kentish Town, London.

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.

Figs. 248, 249.
Boring at Kentish Town, London—continued.

London Clay, 236 feet;—Feet.In.
Yellow Clay306
Blue Clay, with septaria2056
Reading Beds, 6112 feet:—
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;—
Ash-coloured Sand100
Clayey Sand40
Dark Grey Clayey Sand110
Angular Green-coated Flints20
Chalk, with Flints (? Upper Chalk), 24412 feet;—
Chalk, with flints1196
Hard Chalk, without flints8 0
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;—
Light Grey Chalk, and a few thin beds of marl1330
Grey Chalk Marl, with compact and marly beds
and occasional pyrites

161

0
Grey Marl200
Harder Grey Marl, rather sandy and with
occasional pyrites

27

0
Chalk Marl, 5914 feet;—
Hard Rocky Marl (? Tottenhoe Stone)06
Bluish Grey Marl, rather sandy, lower part more clayey589
Upper Greensand;—
Dark Green Sand, mixed with grey clay139
Gault, 13012 feet;—
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

84

11
Lower Greensand (?), 18812 feet;—
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

2

0
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

4

0
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;—

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

Fig. 250.
Well at Michelmersh.

Michelmersh, Hants.—[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;—

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.—Well at Charrington, Head, and Co.’s brewery. [Figs. 251 to 253]. The surface is 3312 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;—

Feet.In.
Made Earth70
Valley Drift, 6 feet;—
Sand30
Gravel30
London Clay, 86 feet;—
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;—
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.

Figs. 251-253.
Well at Charrington’s, Mile End.

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Norwich.—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;—

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

Paris.—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.

Fig. 254.
Geological Section from Niort to Verdun, through the Paris Basin.
Horizontal scale, 90 miles the inch.
Vertical scale, 1500 feet the inch.

[Larger image] (201 kB)

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 212 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.

Figs. 255-258.
Reference.—P. Passy. G. Grenelle. B. Butte-aux-Cailles.
R. Sugar Refinery.

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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.

Figs. 259, 260.
Boring at Grenelle, Paris.

Figs. 261, 262.
Boring at Grenelle, Paris—continued.

Figs. 263, 264.
Boring at Passy, Paris.

Figs. 265, 266.
Boring at Passy, Paris—continued.

Figs. 267, 268.
Well at Ponders End.

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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 tubing—the wood necessarily yielding in the vertical joints—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 82° 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.—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;—

Alluvium, 6 feet;—Feet.In.
Clay and Mud36
Peat26
Sand and Shingle (Gravel).70
London Clay, 15 feet;—
Blue Clay80
Sandy Clay (basement bed?)70
Reading Beds, 4912 feet;—
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;—
Green Sand270
Dead Sand80
To Chalk1126
In Chalk2906
Total4030

The water at this well overflows.

Freshwater, Isle of Wight.—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.

Figs. 269, 270.
Well at Freshwater, Isle of Wight.

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Winchfield, Hants.—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.

Figs. 271-273.
Well at Winchfield, Hants.

[Larger image] (137 kB)

The strata passed were;—

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.Brewery100190290 30
London Clay, 280 feet.
ActonM.Mr Engleheart’s284119 12
DittoMr. Wood’s315135 40
Ditto, EastMr. Davis’s267 68
Albany StreetLondon182125
100 feet O.D.
Aldershot PlaceH.— —194
260 feet O.D.
Ditto— —148 6912
245 feet O.D.
Amwell EndHerts.New River Company 72 34734 36 38334
Yield about 2,500,000 gallons a day.
ArleseyB.Asylum100365 7120
233 feet O.D.; water rises into shaft; yield 2640 gallons an hour.
AshS.S.W. Railway Station600370230
290 feet O.D.
Bank of EnglandM.London137 19712 23412100 88
About 27 feet T.; yield, 35 gallons a minute.
BagshotS.Orphan Asylum123523646
Last 192 feet London Clay.
Balham HillNear Clapham Common347
Last 40 feet Thanet sands.
BarkingE.Byfron’s140140 30
Bottom in hard pebbles.
Barnet, EastHerts.Lion’s Down122270162230130
Shaft half steined, half iron cylinders.
Ditto, NewNear Railway Station137302159280130
BatterseaS.Jones’s Works249249
DittoBeaufoy’s Works240240
Yield said to equal 15,000 gallons a day.
BearwoodBerks.Mr. Walters’s350 15
Beaumont GreenHerts.Near Cheshunt 18312 12612 57
BelleisleM.Pashes and Co.’s185118118
Berkeley SquareLondon160156224 92 80
BermondseyS.Crimscott Street120
9 feet O.D.; yield plentiful.
DittoDonkin’s Works232 9112 14012 16
Yield 30 gallons a minute.
Berry GreenHerts.Hadham 40 20 60 8
BexleyK.Brickfield65110 12914 4534 60
Bishop StortfordHerts.Waterworks160140 11612 18312140
Supply 10,000 gallons a minute.
DittoHockerill 85125 90120 78
Good supply.
DittoNew Road 77 56 21
BlackfriarsM.Apothecaries’ Hall218 76
BlackheathK.Near Enfield Terrace109 30
Boston HeathNear Woolwich130 70
BowM.Starch Works176148174150
Boxley WoodK.Near Maidstone 38612 21312 3600
382 feet T.; last 7812 feet in chalk, marl, and gault.
BraintreeE.Near Pod’s Brook 55190228 7216
Yield, 11,500 gallons an hour.
BrentfordM.Brewery 30338315 53 5
BromleyK.Gas Works 50120150 20
Supply abundant.
DittoWidmore Kiln 52 98140 10
DittoDitto 55 85120 10 61
DittoTylney Road 77 85137 25
DittoWaterworks 70180
Yield, 500 to 600 gallons a minute.
BroxbourneHerts.— — 84 84 6
Water overflowed.
BusheyNear Watford142 24145 21
CamberwellS.The Grove208 3001290
Camden StationM.L. and N.W. Railway180220234166150
100 foot O.D.
Camden TownM.Pickford’s215 82120
Good supply.
DittoWhitaker’s Brewery235 75210 90190
CanterburyK.Orphan Asylum145120
CaterhamS.Waterworks 89349
709 feet T.; through chalk, and 39 feet into upper greensand.
ChelmsfordE.Moulsham200368366202 76
Water overflowed at first.
CheshuntHerts.New River Company144 27 10712 6312120
Yield, 702,000 gallons a day.
DittoTheobald’s Park 71 13112 12112 81 65
Chiswell StreetM.Whitbread’s Brewery183150183150132
ChiswickGriffin Brewery204200297107
Yield, 14 gallons a minute.
DittoLamb Brewery203194293104
DittoDitto 8339297 50
Clewer GreenBerks.Capt. Winterbottom’s 42294270 66
DittoWycombe Cottage 20246169 97
ColnbrookM.Paper Mills207175
Water found at 203 feet down.
Colney HatchAsylum137193189141
Covent GardenMarket140218260 98120
70 feet O.D.
CricklewoodNear Hampstead225 85291 19110
157 feet T.
CroydonS.Well for Local Board 77 11 62
Yield 1,500,000 gallons a day.
DittoNew Well 15137 1112
Dartford CreekK.Paper Mills 34 49 33 50
Supply good.
DittoDitto 10 24012 30 22012 2
DenhamBucks.Tile House110 85 67128 85
DeptfordK.Waterworks 27 14 13
20 feet O.D.
DulwichS.Champion Hill210298
East Ham LevelE.Beckton Gas Works 25175117 83 2
EdgwareM.Mr. Day’s290 45 40
Edgware RoadThe Hyde101 37
EdlesboroughBucks.Well, near Mill301 70
6-inch bore; through 50 feet of chalk marl to lower greensand.
ElthamK.Dr. King’s 46 46 17
DittoThe Moat110100 10
DittoMr. Tuck’s 44123 12212 4412 25
DittoWell Hall107104 3
Ditto Park— —122 94170
Enfield LockE.Small Arms Factory 45 23912 15212132 4
EppingWaterworks275129400 4260
Slow spring.
ErithK.Mineral Oil Company166146 20
FarnhamS.Near Hale Farm176 80 96
Fleet StreetM.London, Shoe Lane100225100225
FulmerBucks.J. Kay’s 85 4734 3714
Through gravel and Reading beds.
Golden LaneM.Baths and Washhouses158 15112 612
65 feet O.D.
GravesendK.Church Street 10234120124 8
Supply good and abundant.
GreenwichBrewery 22158 80100 11
DittoEast Street189159 30
DittoHospital Brewery155150 12412 18012 19
7 feet T.; supply 120 gallons a minute.
Hackney RoadM.Wiltshire Brewery 96 31534 15234259 80
HaggerstoneImperial Gas Works 11812302 16412256
Hainault ForestE.— —165110 55
HalsteadThe White Hart170 30
HammersmithM.Average of four wells245 68
Yield, 16 gallons a minute.
HampsteadLower Heath320130378 72
Now not used.
Hampstead RoadEagle Brewery138 94146 86147
DittoReservoir244152 92106
77 feet T.
HanwellAsylum230 90290 30
Water to surface.
HarrowWaterworks 19312219 15812254125
226 feet O.D.
Haverstock HillOrphan School230160312 78196
176 feet O.D.
HayesDawley Court 19300231 88 27
HendonMr. Booth’s244132 76
HighburyBrewery104210180134 95
Yield, 1000 gallons an hour.
DittoNew Park136113199 50
HoddesdonHerts.New River Company 52234 2412 26112 2
HollowayM.— —140200240100
DittoCity Prison217102
DittoHanley Road 67 13
DittoRedcap Lane210 90
DittoIslington Workhouse234306299250
HornseyNear Church202 48
DittoThe Priory225
HorselydownS.Anchor Brewery100162158104 50
HoxtonM.— —152 10151 11
Hyde Park CornerSt. George’s Hospital200 13714 31914 18100
50 foot O.D.; yield, 3300 gallons an hour.
IckenhamPublic Well 64 80 64 80
Isle of DogsOil Mills 273371241223912 10
Isle of GrainK.Fort180140320 20
21 feet O.D.
IsleworthM.Sion House420115
Water overflowed at the rate of 5 gallons a minute.
DittoMr. Wilmot’s327327
Water rose above surface.
Islington GreenWebb’s Mineral Water Works320176144200
KensingtonBrewery197
16 feet T.
DittoBritannia Brewery100170270 88
DittoHorticultural Society200201317 84100
60 feet O.D.
DittoWorkhouse270100
Ditto GardensSerpentine263 58 26314 5734105
60 feet O.D.; yield, 250 gallons a minute.
Kentish TownWaterworks539763 32412 64434
Through London clay, 236 feet; London tertiaries, 8812 feet; chalk, 64434 feet; upper greensand, 1334 feet; gault, 13012 feet; and into lower greensand (?), 18812 feet.
KilburnBrewery250 30235 45150
KingsburyBrent Reservoir101139132108
Kingston-on-ThamesS.Brook Street 90380371 99
25 feet O.D.; yield, about 44,000 gallons a day.
KnightsbridgeM.— —240240 50
LambethS.Beaufoy’s Vinegar Works100275201174
Yield, 92 gallons a minute.
DittoSouth Lambeth Road 25166187 4
DittoBethlehem Hospital 30161191 20 15
DittoLion Brewery, Belvedere Road245173 40
DittoDuke Street, Street, Clowes & Sons’ 26184210
Lea BridgeM.Waterworks118100 18
Leicester SquareAlhambra150195244101
LimehouseJohnson’s, Commercial Road 90110190 10
DittoBrewery, Fore Street 13912
Liquorpond StreetReid’s Brewery 22212 40136 12612121
70 feet O.D.; yield, 277,200 gallons in 24 hours.
Long AcreCombe & Co.’s Brewery263228223268
70 feet O.D.; yield, 90 gallons a minute
LoughtonE.— —535324211 90
No water from chalk.
Lower MordenS.On the Green 20365340 45
Water to surface.
LutonB.Waterworks 50272322
MaldonE.Waterworks234234
Entirely through London clay.
MargateK.Cobb’s Brewery 31243374
Marylebone RoadM.London; a Brewery186101232 55156
Mile EndMann’s Brewery195185 10
DittoCharrington’s Brewery204202 2103
3312 feet T.; yield, 60,000 to 70,000 gallons a day.
Ditto RoadCity of London Union175 10
MillbankDistillery115190205100 70
Level of T.
DittoWestminster Brewery225 70
512 feet T.
MitchamS.Nightingale’s Factory211189 22
Monkham ParkE.Near Waltham Abbey225125304 76 50
MortlakeS.Mortlake Brewery 30288287 31 50
Yield, 14,000 gallons a day.
DittoMr. Randell’s365315 50
New CrossK.Naval School 50130125 55 60
NortholtM.Near Harrow 12228180 60 4
Notting DaleNear Notting Hill244 12
Notting HillMr. Knight’s230200
Old Kent RoadS.Welsh Ale Brewery 30170
10 feet O.D.
Old WindsorBerks.Pelham Place222 9
DittoThe Union 60180240 47
Orange StreetM.Back of National Gallery174126250 50115
42 feet T.
Oxford StreetStar Brewery166170158178
PeckhamS.Marlborough House100123
PengePalace Grounds25031035820290
PentonvilleM.Brewery, Caledonian Road 21912 21912 45180
To chalk.
DittoPrison170 20012 21912151
PimlicoCubitt’s Works188188
2 feet T.
DittoBrewer Street 30368271127
DittoSimpson’s Factory231100 36
1 foot T.
PinnerHatch End140 60 80
PlaistowE.Odam’s Manure Works 17012128
Ponders EndM.London Jute Company 4399 11212 29012
Water overflows.
DittoCrape Works 20 42 62
DittoLocal Board (Speller)106 9612
DittoWaterworks 23181 97107
43 feet T.
Pudsey HallE.Near Canewdon297297
Water abundant and good.
RatcliffeM.Queen’s Head Brewery160200
DittoMarine Brewery 16236150102
DittoRavenhill’s137
Regent’s ParkColosseum150100171 79
DittoMr. Day’s18421680
DittoZoological Gardens1839122450120
Yield, 90,000 gallons a day.
RichmondS.Old Waterworks276103
DittoStar and Garter416 76
RomfordE.Ind, Coope, & Co.155145 10
RotherhitheS.Brandram’s Works 30222107145 27
Yield, 100,000 gallons in 12 hours.
DittoTunnel Flour Mills125135
15 feet O.D.; yield, 80 gallons a minute.
RuislipM.Near “The George” 15 9034 7534 30
Water to surface.
Saffron WaldenE.— —1000
SandhurstBerks.Well at College603
Trial boring; chalk reached.
SandwichK.The Bank 70 62 8 20
SheernessWaterworks300 84384
512 feet O.D.; yield, 10,000 gallons an hour.
DittoDockyard330125455 53
Yield, 675 gallons an hour.
ShoreditchM.Truman’s Brewery300230199331120
Yield, 712 gallons a minute.
Shorne Meade FortK.Near Gravesend112 7712 3412
ShortlandsNear Bromley 59150109100 61
Yield, 1000 gallons an hour.
SloughBucks.Eton Union 28103107 24
DittoRoyal Nursery 94 1712
DittoUpton Park 10214 17014
DittoWaterworks117 90 27 7
Heading into chalk.
SmithfieldM.Booth’s Distillery230 70 70
SouthendE.Waterworks417417100
Old well.
SouthwarkS.Barclay’s Brewery115288212211
Level of T.; yield, 300 gallons a minute.
DittoGuy’s Hospital132173196109 84
2 feet T.; yield, 33 gallons a minute.
StainesM.Ashby’s Brewery369154
Water to surface.
StiffordE.S.E. of Church 63 33 30
Stockwell GreenS.Waltham’s Brewery100210210100 46
Yield, 33 gallons a minute.
DittoHammerton’s Brewery 25186211154
Yield, 46 gallons a minute.
StratfordE.Great Eastern Works 56344106294
DittoSavill Bros.’ Brewery1121210912 3
DittoLangthorn Chemical Works 60395132323
Supply abundant.
StreathamS.The Common100185285
SudburyM.London and North-Western Rail. Station200120 80
TottenhamWarne’s Works147104
DittoLong Water 14912 10112
DittoTottenham Hall253153100
Tottenham Court RoadMeux’s Brewery188622156654
85 feet O.D.; yield, 1212 gallons a minute.
Tower HillRoyal Mint 19512202 19512202 80
Trafalgar SquareLondon168228248148
Yield, 450 gallons a minute.
UpchurchK.Burntwick Island236236
DittoMilford Hope Marshes304210 94
Good supply at bottom.
Upper Thames StreetM.City of London Brewery 90415210295 10
UxbridgeThe Dolphin121 8112 3912 3
DittoNear Market Place104 28 1512
DittoPage’s Lane 98 98
DittoTown Well109 30 19
DittoNear “King’s Arms” 24 84108 19
To chalk.
DittoNew Year’s Green Farm 63 63 51
DittoHurdle Yard 78 3912 78 3912
DittoNear Meeting House 4112 10912115 36 39
DittoThe Union 51162175 38 29
VauxhallS.Burnett’s Distillery140186224102 55
Yield, 80 gallons a minute.
Waltham AbbeyE.Brewery164160 4
Water supply from bed of sand.
Walthamstow MarshEast London Waterworks152140
15 feet T.
WandworthS.Young & Bainbridge’s170164274 60 45
Yield, 10 gallons a minute.
DittoPrison357 12612 80
Yield, 27 gallons a minute.
DittoCounty Asylum331 6 30
Westbourne GroveM.Hippodrome240 67300 7
West DraytonVictoria Oil Mills 12274186100
Water overflowed.
DittoVitriol Works 13312 4512
DittoDrayton Mills 3146149
To chalk.
West HamE.Mr. Tucker’s132306
DittoUnion110 55
West India DockM.South of Export Dock120240
WestminsterArtillery Brewery230
DittoChartered Gas Works225
DittoVickers’ Distillery116184249 51 70
Yield, 94 gallons a minute.
DittoSwallow Street210 60
WhitechapelFurze’s Brewery130218248100
DittoSmith’s Distillery106264210160 36
36 feet T.
DittoSmith, Druce, & Co.’s 14112 14112 85
39 feet T.
WillesdenMr. Kilsby’s273 97 30
WimbledonS.Convalescent Hospital200367537 30 50
Ditto, NewOpposite “White Hart”193 75
WindsorBerksClower Lodge 40175175 40
DittoRoyal Brewery 72 72
Through clay and running sand to chalk.
DittoJennings’ Brewery 30500 12
Winkfield PlainCaptain Forbes’304126 70
WithamE.— —306 5
Woodley LodgeBerks.3 miles east of Reading 95 35130
WoolwichK.Well of Arsenal 5412 31112 37
DittoPaper Factory550 512 54412
Yield, 650 gallons a minute.
DittoDockyard608 20588 70
Yield good.
WormleyHerts.Nunsbury 26 7612 8012 22
Water overflows.
DittoWest End 85 15012 72 6312 62
Wormwood ScrubbsM.— —250116 5


[CHAPTER VIII.]
TABLES AND MISCELLANEOUS INFORMATION.

The following tabulated form shows the order of succession of the various stratified rocks with their usual thicknesses.

Groups.Strata.Thickness
in Feet.
RECENT 1Modern Deposits.
PLEISTOCENE 2Drift and Gravel Beds 20 to 100
3Mammaliferous Crag 10 to 40
PLIOCENE 4Red Crag 30
CAINOZOIC, OR 5Suffolk (Coralline) Crag 30
TERTIARY. MIOCENE 6Faluns (Touraine) Molasse Sandstones 6000
7Hempstead Series 170
Upper 8Bembridge Series 110
9Headon Series 200
EOCENE Middle 10Barton Beds 300
11Bagshot and Bracklesham Series 1200
Lower 12London Clay and Bognor Beds 200 to 520
13Woolwich Beds & Thanet Sands 100
14Maestricht Beds 110
15Upper Chalk 300
16Lower Chalk and Chalk Marl 400
CRETACEOUS 17Upper Greensand 130
18Gault 100
19Speeton Clay 130
20Lower Greensand 250
WEALDEN 21Weald Clay 150
22Hastings Sands 600
PURBECK 23Purbeck Beds 150
UPPER 24Portland Rock and Sand 150
OOLITE 25Kimmeridge Clay 400
26Upper Calcareous Grit 40
MESOZOIC, OR MIDDLE 27Coralline Oolite 30
SECONDARY. OOLITE 28Lower Calcareous Grit 40
29Oxford Clay 400
30Kellaways Rock 30
31Cornbrash 10
32Forest Marble and Bradford Clay 50
LOWER 33Great Oolite 120
OOLITE 34Stonesfield Slate 9
35Fullers’ Earth 50 to 150
36Inferior Oolite 80 to 250
37Upper Lias Shale 50 to 300
LIAS 38Marlstone and Shale 30 to 200
39Lower Lias and Bone Beds 100 to 300
TRIASSIC, or 40Variegated Marls or Keuper 800
NEW RED 41Muschelkalk
SANDSTONE 42Red Sandstone or Bunter 600
PERMIAN or 43Red Sand and Marl 50
MAGNESIAN 44Magnesian Limestone 300
LIMESTONE 45Marl Slate 60
46Lower Red Sandstone 200
47Coal Measures 3000 to 12,000
CARBONIFEROUS 48Millstone Grit 600
49Mountain Limestone 500 to 1400
50Limestone Shales 1000
PALÆOZOIC, OR DEVONIAN or 51Upper Devonian
PRIMARY. OLD RED 52Middle Devonian 3000 to 8000
SANDSTONE 53Lower Devonian and Tilestones
54Ludlow Rocks 2000
Upper 55Wenlock Beds 1800
56Woolhope Series 3050
SILURIAN Middle 57Llandovery Rocks 2000
58Caradoc and Bala Rocks 5000
Lower 59Llandeilo Rocks 4000
60Lingula Flags 8000
CAMBRIAN 61Longmynd and Cambrian Rocks 20,000
METAMORPHIC Clay Slate, Mica-Schist.
AZOIC. Gneiss, Quartz Rocks.
IGNEOUS Granite.

The Quantity of Excavation in Wells
for each Foot in Depth.
(Hurst.)
Diameter of
Excavation.
Quantity.
ft.in.cubic yards.
30 ·2618
33 ·3072
36 ·3563
39 ·4091
40 ·4654
43 ·5254
46 ·5890
49 ·6563
50 ·7272
53 ·8018
56 ·8799
59 ·9617
601·0472
631·1363
661·2290
691·3254
701·4254
731·5290
761·6362
791·7472
801·8617
862·1017
902·3562
962·6253
1002·9089
1063·2070
1103·5198
1204·1888
The Measure in Gallons, and the Weight in Pounds,
of Watercontained in Wells, for each Foot in Depth.
Diameter.No. of Galls.Weight.
ft.in.
2019·61196·1
2630·56305·6
3043·97439·7
3660·00600·0
4078·19781·9
4698·87988·7
50122·231222·3
56147·961479·6
60175·991759·9
66206·592065·9
70239·052395·0
76275·492754·9
80313·433134·3
86353·033533·0
90395·423954·2
96441·714417·1
100489·934899·3

Brickwork.
The Number of Bricks and Quantity of Brickwork in Wells
for each Foot in Depth.
(Hurst.)
Half-Brick Thick.One Brick Thick.
Number of Bricks. Number of Bricks.
Laid
Dry.
Laid in
Mortar.
Cubic Feet of
Brickwork.
Laid
Dry.
Laid in
Mortar.
Cubic Feet of
Brickwork.
1·0 28 23 1·6198 70 58 4·1233
1·3 33 27 1·8145 80 66 4·7124
1·6 38 31 2·2089 90 74 5·3015
1·9 43 35 2·7979 112 92 6·4795
2·3 53 44 3·0926 122 100 7·0686
2·6 58 48 3·3870 132 108 7·6577
3·0 68 57 3·9760 154 126 8·8357
3·6 79 65 4·5651 174 142 10·0139
4·0 89 73 5·1541 194 159 11·1919
4·6 100 82 5·7432 214 176 12·3701
5·0 110 90 6·3322 234 192 13·5481
5·6 120 98 6·9213 254 209 14·7263
6·0 130 107 7·5103 276 226 15·9043
6·6 140 115 8·0994 296 242 17·0825
7·0 150 123 8·6884 316 260 18·2605
7·6 160 131 9·2775 336 276 19·4387
8·0 170 140 9·8665 358 292 20·6167
8·6 180 148 10·4556 378 308 21·7949
9·0 191 156 11·0446 398 326 22·9729
10·0 212 174 12·2227 438 360 25·3291

Good bricks are characterized as being regular in shape, with plane parallel surfaces, and sharp right-angles; clear ringing sound when struck, a compact uniform structure when broken, and freedom from air-bubbles and cracks. They should not absorb more than one-fifteenth of their weight in water.

After making liberal allowance for waste, 9 bricks will build a square foot 9 inches thick, or 900, 100 square feet, or say 2880 to the rood of 9-inch work, which gives the simple rule of 80 bricks = a square yard of 9-inch work.

The resistance to crushing is from 1200 to 4500 lb. a square inch; the resistance to fracture, from 600 to 2500 lb. a square inch; tensile strength, 275 lb. a square inch; weight, in mortar, 175 lb. a cubic foot; in cement, 125 lb. a cubic foot.

Compressed bricks are much heavier, and consequently proportionately stronger, than those of ordinary make.