VOL. XIV. (1) MENDIP ARCHIPELAGO TS 
yielded derived Zaphrentis Phillipst, Spirifera striata, 
and ossicles of Poteriocrinus, well preserved in Liassic 
strata. : 
At many points round the Downside outlier, where the 
Lower Lias rests on the Carboniferous Limestone, the 
former is conglomeratic; whilst in the pre-f/anordis beds 
conglomeratic conditions are the exception rather than 
the rule. 
Other Liassic sections are at Felton Vicarage, and east 
of Goblincombe Farm. At Hanging Farm I procured, 
from normal Liassic strata, Zelleria perforata, Extra- 
crinus ossicles, etc. 
The following appears to be the sequence in this 
Misirict :— 
Pars angulatus, 
Freestone, and conglomerates wherever 
: the Liassic Sea first washed the Car- 
and planorbis zones. : = : first Ww . 
\ boniferous Limestone. 
Bone-bed. 
Limestone. 
Pre-planorbis 
j Limestone. 
