Mr. Farey’s Notes on Mr. Bakewell’s Geology. 335 
[P.294] most distant allusion was made, to my Derbyshire Mineral 
Survey, or, as to the Board having contracted for the Manu- 
script of the first Mineral Report on the English Counties 
(which series had been promised ever since 1793, Rep. i. 
pref. vi. and P. M. xxxvii. p. 8) in this Speech, or in any 
other announcement from the Officers of the Board to its 
Members or to the Public, as far as | have heard :—I forbear 
further comments. 
295, 1. 22, similar to, the limestone*.—* And supposed to be 
ihe same, in pages 220 and 274, see my Note on the latter 
age. 
s P 24, eastern side of North Wales+ .—t It is not on the 
eastern side only, of the northern Cambrian Mountains, that 
Limestone Rocks underlay Coal-measures, but on the NE 
and NW sides also; the latter calcareous Rocks, stretching 
across Anglesea, see my Note on page 275. 
296, 1. 18, said to occur in Anglesea *,—* During my stay in 
this Island, I saw, or could hear accounts from the inhabitants 
of no Rocks of Granite: the Mile-stones on the Post Road, 
seemed formed of reddish Granite, and occasional loose 
blocks of it were met with on the surface: but Mr. Wilson 
Lowry has since informed me, that in travelling across from 
the Post Road at Gwndy to the Paris Mountain, he saw low 
Rocks of Granite, not far from the former place. 
1. 22, from its hardness, beauty +.—+ See my Note on 
p- 92. Very considerable Rocks of Serpentine are found in 
the coarse Slate of the NW and W parts of Anglesea. 
297, 1. 9 and 10, sulphurous limestone*.—* See my Note on 
98. 
299, 1, 20, boundary of the coal strata *.—* See p. 268. A 
. similar « concavity” or frough of the same Limestone, seems 
to underlie the estuary of the Dee, and the Coal-measures 
therein, seem to extend from Flint to Park-Gate: how far 
this Coal-basin extends westward, under the Sea, towards 
the north Coast of Anglesea, &c. we have yet in part to 
‘learn, see my Notes on p.°108, 275, and 285. 
300, 1. 10, part of Somersetshire *.—* But a very small part 
of this County, the Quantook Hills at its western extremity ‘ 
can I think be either “ primary” or “ transition ;” unless 
that Lias, Red Marl, and Coal-measures under these, are 
so? see my Note on pages 12 and 283. Mr. Thomas Allan 
says in the Edin. Trans., that in his way to Exeter, he first 
saw ‘‘ transition strata between Bridgewater and Taunton :’ 
but on reference to the Appendix to his paper, No. | and 2, | 
it appears, 1 think, that the imbedded Grit-stone in the 
Red 
