252 Mr. Farey’s Notes on Mr. Bakewell’s Geology. 
P.19. spreading reports, without contradiction, of tke 
skeleton being imbedded in undisturbed coal. 
After Mr. B’s just remark on this head in p. 18, I 
lament that in page 162, this supposed complete 
consolidation of loosened Coal, by “ pressure and 
time alone,” should, as I suppose, be alluded to, 
for supporting a Theery, to which this case ap- 
pears to have no just relation. 
26, }. 18, denominated a Jed *.—* An Anglo-Wernerian 
term this (used also at page 52), used in just the re- 
verse of its meaning among the practical English 
Quarrymen and others ; who describe the subdivi- 
sions of their Rocks or thick strata, by the term 
beds, Rep. i. 222, 271, &c. 
1. 25, right angles to this t.— ¢ And level or nearly, 
Rep. i. 120 Note. 
27,1.17, the motion of water *,—* It is probably only 
the Huttonians, who at this day, consider the 
motion of water, as concerned in the formation 
of strata, but such opinion seems devoid of pro- 
bability. 
28, ]. 14, different direction *—* Denominated Stratula, 
Rep. 1. 155, see my Note on page 317. 
]. 21 and 22, remove many difficultiest.—+ See P. M. 
XXXvill. p. 357, and Mont. Mag, xxxili. p. 517. 
29, 1. 1, with stratification *.—* By Mr, Edward Martin, 
at Cribbath, in Phil. Trans. 1806, and in Williams’s 
Min. Kin. 2d Ed. ii. p. 296: and by others. 
}, 10, mountain masses .—t Rep. i. 153, Phil. Trans. 
181}, and P.M. xxxvil. p. 441, and vol. xxxix. 
p- 29 and 426. 
30, 1. 8, clay*.—* Alumina ought now always to be 
used, in naming the simple Earth ; Clay being a 
useful name, in very common use, for yarious 
mixtures of Alumma, Silex, Magnesia, &c, &c. 
40,1. 22, of the science *,— * Read—of Geological 
Science. 
43, 1.12, generally lie below *,—* Are not the bare or 
denudated tops of large modular, or imbedded 
masses, often described as foundation rocks ? P.M. 
x1. \:p.'53. 
44,1. 13, contain pebbles *.—* I believe Mr. W. Smith, 
as a Man practically acquainted with Coal-mines 
and other deep excavations in the Strata, as well 
as with the upartieial Grayel and alluvial soils, 
was, 
i ti il tl i ees 
