| 30 Mr. Farey’s Notes on Mr. Bakewell’ s Geology. 
“.{P.162] fact, mentioned by me, Rep.i. 181 and sh. that 
theses lines very generally, if not invariably ?, range 
about ESE and WNW, through extensive districts, 
where the dips vary much, both ‘locally and generally ! _ 
1. 14, the complete consolidation f. — ¢ See my 
Note on page 19. 
166, |. 92 and 23, nearly horizontal *, —*Ina north and 
south direction, but having a very perceptible dip to 
the Eastward, Rep. i. 156, 168. 
1675: \0 14 singularly déitorted 128 * Mr. B. seems here 
to allude to the Wild- Park, Breedon and Clouds-bill, 
magnesian and contorted Taenectoue Rocks, as being 
identical with the yellow Lime Rock, which overlies 
the Notts, Derby, York and Durham Coal-field (see 
my Note on p. 176); notwithstanding, that they are 
herein, at pages 284, 275, &c., represented to be iden- 
tical with, and a continuation of, the Peak Limestones, 
and also with the shale Limestone near Ashburne, 
page 286, which last, as clearly wderlie this vast series 
of Coal strata, as mentioned in my secondiLetter, p. 106. 
1. 12, quantity of common lime ¢.—f Rep. il. 107, 
409 and 412. 
]. 23, edifices in the metropolis t.—f The fine Oa- 
lite stone, of the vicinity of Bath, is now coming into 
ase in London, brought by the Kennet and AvonCanal ; 
the stone using in restoringHenry VII’s Chapel atWest- 
minster, is from thence; and in an adjoining Field, 
my friend Mr. Wm. Smith has extensive quarries, and 
a rail-way thence to the Canal, where he has a Saw- 
mill at work, preparing it fer all the different purposes 
of the London Mason... 
168, I. 9, as has been traced *.—* See the articles Coal 
and Colliery, in Dr. Rees’s Cyclopedia, and Rep. i. 109. 
1, 12 and 13, occur in the South ¢.—t Phil. Mag. 
XXXIX. p. 94. 
1. 23, south of Europe t.—f{ The Rev. J. Townsend, 
who was so well acquainted with our Chalk strata, 
before he travelled in Spain, and on his return, was 
not likely to mistake Mr. B’s (‘* imaginary”) earthy 
lime-stone, for chalk (see p. 185), nor is it probable, 
that the Island of Crete or Candia, and others in the 
south of Europe, are without Chalk, as Mr. B. has 
here insinuated ; perhaps this doubt was expressed, in 
order to invalidate the suggestion alluded to at the 
canclusion of my Note on page 138. 
P. 169, 
