322 LIAS OF ENGLAND AND WALES: 
Sandhurst, N. of Gloucester. 
Bayshill, Cheltenham, and south of Fidler's Green. 
Cheltenham : Montpellier Wells (Sulphate of soda, sulphate of magnesia. 
chloride of sodium, &c.) ; Pittville Sffti (Sulphate of soda, chloride of 
sodium, &c.). (See p. 323.) 
Prestbury and Bishops Cleeve. 
Child's Wickham. 
Walton Cardiff, Tewkesbury : Walton Spa. 
Hampton Spa, Evesham. Wells 11 to 22 feet. (Sulphates of lime, soda, and 
magnesia, carbonates of magnesia and lime, &c. ; 50 grains per gallon). 
Evesham. (Saline wells.) 
Long Marston (Brine spring.) 
Fenny Compton. (Spring, 103 grains per gallon. Sulphate of soda, chloride 
of sodium, &c.) 
Southam Holt, abut 2 miles S.E. of Sontham. (Salt spring.) 
Willoughby Spa, S.E. of Rugby. (Well sunk 104 feet. Brine spring.) 
Shearsby, N.E. of Lutterworth. (Spring, containing chloride of sodium 
sulphate of soda, &c. 39(5 grains per gallon). (See p. 325.) 
Belvoir Spa, near Belvoir Castle. 
Burton Lazars (Chi. sodium.) 
Brentingby-cum-WyEordby, east of Melton Mowbray. 
Bracebridge, Lincoln. (Boring 320 feet.) Water containing 593 grains per 
gallon: 549 chloride of sodium; 11 bromide of sodium; 15 carbonate 
of soda; 12 carbonate of lime ; &c.* 
Middle Lias. 
Dillington, N.E. of Ilminster. 
Churchill Mill, between Kingham and Churchill, near Chipping Norton. 
Clifton, east of Deddington. 
Deddington. (Sulphur saline.) 
Sutton Bog, N.E. of railway- station, King's Sutton. (Spring containing 
sulphate of soda, chloride of sodium, &c. 199 grains per gallon.) 
Old Stratford, near Stony Stratford. Well, 110 feet in Marlstone ? (Sul- 
phate of lime, carbonate and chloride of sodium, &c. 77 grains per 
gallon.) 
<Jumley, N.W. of Market Harborough. (Saline chalybeate.) 
Grantham : Spittlegate. (50 grains of mineral matter per gallon.) 
Concerning the Bath Waters, the Rev. J. Townsend mentioned 
that "By Hetlin Court, when the hot springs had failed to supply 
the usual qunntity of water in a given time, the Corporation em- 
ployed Mr. William Smith to remedy the evil. He laid open the 
ground, detected the cause of failure, and restored the springs. At 
that time I took notice of his operations, and at a great depth saw 
the springs issuing through the blue marl." 
" When the new building was constructed over the springs of 
the Cross Bath, I particularly noticed hot and cold springs issuing 
within the space of two or three lug of ground, in such a manner 
that the cold springs were obliged to be separated from the hot 
ones, and, not being suffered to issue on the spot, were separately 
conveyed into the river Avon." t 
The hot springs rose to the surface not more than 15 or 20 feet 
above the level of the river. William Smith considered it possible 
{< that the Bath waters may be a compound from the lias, red 
* De Ranee, Rep. Brit. Assoc. for 1891, p. 802 ; aud Proc. Yorksb. Geol. and 
Polyt. Soc., vol. xii. p. 49. 
f Character of Moses, pp. 197, 313. 
