123 
this shell which indicates any difference in horizon, as the 
lithological characters seem similar. Therefore it is very 
probable that any distinction between the Gryphza beds and 
those below must be more or less artificial. Before proceeding 
to describe the higher beds I must introduce other sections to 
shew how we connect our series, and continue to the Fullers 
Earth Clay. 
SECTION VI. 
First Cutting West of Notgrove Station, North side. (Clypeus to Gryphea 
Grits. 
) ft. ins. 
B? 1—Fossiliferous stone, with horizontal fracture in layers... 4 0 
C 2—Stone like lower portion eae erit, but tiie Ch jane 
Plottii abundant er 3. (0 
3—Rotten stone, in fact a paste of oolitic arene, clayey, with 
crushed variety of T. globata a 2 0 
4—Yellow stone, upper part of a more Biecntes poe iisieen 
rubbly, with irregular cleavage. T. globata abundant . 31 (0 
D 5—Trigonia grit, 3 beds separated by marly partings, bidet 
lighter and much harder. Rh. hampenensis in clusters, 
Wald. Hughesi, Am. Parkinsoni, eaauenl of Tri mines 
abundant ae 4 6 
E 6—BoreD BED. Thickness aaahis ond not always separated 
from Freestone below ree P oN 0 8 
7—White Freestone, rather soft and tainly os no oh 
MOOS ee nee Me 1220 
F 8—Five or six beds of thinnish, Sa ans oe el 
white coloured, softer partings ae 4. a nck ee 0 
9—Two beds with occasional Giryphaea sublobata =e oes 2 4 
10—Bed with Gryphea sublobata abundant, visible... ae 1 6 
SECTION VII. 
Section of the Fifth Cutting West of Bourton-on-the-Water Station. 
Junction of the Inferior Oolite and Fullers Earth. 
A  1—Depth of Fuller’s Earth pe ee and blue (ave 
about five feet of rock) ~. 14 0 
B 2—Band of waterworn nodules of a pink non- ipalitie SS aviet 
when broken, Serpulae and oysters on the outside 
0 
3—Rough oolitic debris, with somewhat rubbly oolitic stone 0 
4—Reddish sandy oolitic debris ... 43 se aac der 0 4 
5—Same, but rather harder and more compacted, like stone.. 0 
6—Light brown Limestone, with darker i ili Waldheimia 
ornithocephala 2 crushed... 0 3 
7—Rubbly marl... a “ee aaa ao wie soa 0 6 
8—Light brown sandy stone... ame ae aa aes 0 10 
