144 Mr. J. Lycett on the so-called Sands 
C. Micaceous, foxy-coloured or yellowish, incoherent sands, 
seldom much compacted, but locally becoming soft sandstone, 
from 20 to 40 feet, abruptly terminated upwards by 
D. Concretionary marly bed, usually darker in colour than the 
sands, but varying much in structure and aspect within short 
distances, and everywhere more or less fossiliferous ; the tests 
of Mollusca are less frequently preserved than in the lower 
zone. A constant mineral feature is the presence of small 
oval grains of hydrate of iron disseminated through the rock ; 
a structure which, however, is not peculiar, as it is present in 
the Inferior Oolite at Dundry and in the Lias of France. 
From 2 to 4 feet is the thickness of this bed in the Cotteswolds. 
Immediately overlying this upper Ammonitiferous bed are 
several others of hard brown or yellowish calcareo-siliceous 
sandstones, in which fossils are usually very sparingly distributed, 
and, from the evidence these afford, the beds have by universal 
consent been assigned to the Inferior Oolite. 
In Yorkshire, the lofty iron-bound coast at the Peak and at 
Blue Wick exhibits the same remarkable deposit in considerable 
thickness, and slightly modified’ in its mineral character from 
the Cotteswold Sands. In a visit which I recently made to this 
coast, in company with my friend Professor Morris, the identity’ 
of the lower portion of the Dogger or Inferior Oolite of Phillips 
with the Gloucestershire Sands was strongly impressed upon my 
mind. At Blue Wick the Dogger is altogether about 80 feet in 
thickness, and rises in successive beds in descending order from 
the rocky beach into the face of the lofty cliff, the lower 40 feet 
representing the sands of the Cotteswolds. Beneath these suc- 
ceed the hard beds of the Upper Lias Shale, 200 feet thick, 
followed by the Middle Lias, nearly equal in mass; ultimately, 
at the Peak, facing Robin Hood’s Bay, these great deposits are 
all exposed in one vast unbroken section, forming a lofty mural 
cliff, nearly 400 feet in height and three miles in length, in the 
course of which the Dogger attains the summit of the cliff. 
Words are scarcely adequate to express my admiration of this 
grand exposition of the lower Jurassic rocks, which for extent 
and completeness can scarcely be paralleled. Proceeding north- 
wards, the upper 40 feet of the Dogger loses more than half its 
thickness, and the lower portion, or representative of the Sands, 
thins out altogether ; a great fault then succeeds, by which the 
Middle Lias is upraised to the summit of the cliff. 
The highest bed of the Upper Lias consists of black, finely 
laminated -shale, the transition to the sandstone above being 
abrupt and very distinctly marked. The sands are here com- 
pacted into thick-bedded, dark grey micaceous sandstones in 
