336 Mr. Parey’s Notes on Mr. Bakewell’s Geology. 
[P.300] Red Marl, something harder than usual perhaps, and tilted, 
has been so denominated ; for, near to Taunton, on the SE, 
the Lias occurs again, as I have been informed. 
302, 1. 11, and worn down *,—* See Mr. John Hutchinson’s 
Works xii. p. 261 and 338. Prior: 
303, 1.3 and 4, as a field bean*.—* Some of the pieces of 
Gold from the Wicklow Mountains are much larger, ap- _ 
pearing as if kneaded into their present form, by violent 
pressure (if not aggregated by this means), and containing 
some fragments of quartz, which appear forced i the 
old. ane 
301, 1. 2, and warm springs *.—* Should not cold or ordinary 
Springs also have been noticed in Mr. B’s work?, and 
their undoubted sources from the infiltration of rain waters 
heen particularly mentioned: few of the Geological phe- 
nomena are of more general interest, or have been more su- 
perficially, or erroneously treated by Writers; see Rep. i. 500. 
1. 10, under the whole district -.—+ This is unsupported 
by any facts or observations in the Mines, &c. Rep. i. 487. 
‘1. 16 and 17, the Cromford Canal t.—t The cause of the 
temperature of the western end of this Canal being often 
higher than usual, is perfectly apparent: it is fed by .the 
large stream of very warm water issuing from Cromford 
Sough, (Rep. i. 329, and vol. iii. chap. xvi. sect, 3), on Sun- 
days and often in the night, when Mr. Arkwright’s Cotton 
Mill is not at work. 
1. 19, be frequently seen rising **.—** Since Mr. B. told 
mein May 1812, ofthis supposed prevalence of warm springs 
and general heat in the strata, through which the Cromford 
Canal is cut, from Cromford to near Crich, I have made 
very particular inquiries, while in the neighbourhood, and 
concerning the Person, formerly of Crich, whom he mentioned 
as his informant. The hot spring which rose at Middleton- 
Wood Bath, (Rep. i. 505), in Bonsal Dale, close by the 
side of the great Limestone Fault, (Rep. i. bottom of p. 281 
and in p. 282), until that by the driving of the Cromford 
Sough, a porous stratum of Limestone, or a line of fissures 
therein, connected with it, let off its hot water, at a much 
lower level, and mixed it with a great deal of cold water, 
which the sough still collects, on h sides of that which 
enters it hot; this mixed wate most d: ily let into the 
Canal at its upper end, will perfec f 
canic wonders, which are her 
see my Note on p. 226. 
305, 1. 1, principally confined to 
3 So ‘ 
Basaltic 
ihe 
