10 
1.—Lower Trigonia grit. 
2.—Terebratula Phillipsii zone. 
8.—Chemnitzia zone. 
4,—Roadstone bed. 
5.—Ostrea zone. 
6.—Freestone. 
7.—Oolite Marl. 
8.—Thick bastard freestone. 
9.—Shelly freestone. 
10.—Pea grit. 
11.—Sands junction, passage beds. 
12.—Lias. 
Total height of Cleeve Cloud above the level of the sea 11,000 
feet. 
If Nos. 2, 3, 4 & 5 in the above section oceur at Leckhamp- 
ton they are not exposed. 
Numerous characteristic fossil of the Pisolite and roadstone were 
obtained, among which may be mentioned—Ostrea flabellu- 
loides, Terebratula Phillipsii, Trichites, Rhynchonella oolitica, 
Pleurotomaria (cast), Belemnites brevis, Chemnitzia, Hinnites 
tuberculosus, Modiola explanata, Pholadomya fidicula and a large 
new species, Modiola, Gresslya, Pecten lens, Lima and Echinus, 
germinaus, but the most interesting specimen was a fine beak of 
a Cephalopod, discovered in the Pea grit by the Rev. Mr. Hort. 
This is the first one of the kind found near Cheltenham ; the 
first and only one previously procured was detected by the late 
Hugh Strickland in the Inferior Oolite at Bredon. At the base 
of the escarpment, the basement beds of the Oolite appear 
similar to those at Leckhampton and. Crickley immediately over- 
lying the upper lias, and these probably form passage beds 
between the two formations, though assigned to the Lias by Dr. 
Wright, while Messrs Lycett and Brodie and other Cotswold 
Geologists incline to the former opinion. At this spot Mr. Brodie 
discovered a similar Bone Bed to the one he had previously 
