162 
THE LOWER OOLITES HEAR BRISTOL 
dence of this denudation, in the planed-off top of the 
Sauzei strata in the middle, in the Sonninise beds at the 
west of the hill, and in the presence of a conglomeratic bed 
of Garantianse hemera, containing fossils of Dumortieria3 
age, at the eastern end of the hill. 
Stahtonbury Hill 
Four miles east of Dundry, at Stantonbury Hill, the 
sands (and here they are true sands as at Midford) are 
capped by about 7 to 8 feet of Oolitic limestone of the Par- 
kinsoni zone. These beds are very fossiliferous, but, as 
there is no section, we have to depend for specimens on tlie 
weathered escarpment and the runnels formed by innu- 
merable rabbits which burrow in the sands beneath. Not- 
withstanding this difficulty, on a recent occasion the follow- 
ing fossils were collected in about half an hour. 
Ammonitd of the Garmitianus group. 
Rhynchonella spinosa. 
,, hamponensis, 
Terebratula spJmroidalis. 
Aidacothyris carinata. 
Lima pectiniformis. 
Pecten, sp. 
Avicula costata. 
Isastrma limitata. 
Montlivaltia, abundant in a bed considerably 
bored by Lithodomi. 
11 olectypus hemisph ericus . 
PeMacrifiMS Milleri. 
Serpula socialis. 
Cylindrites, sp. 
I have also obtained from these beds Lissocems psilo- 
discum. In reference to this Ammonite Mr. Buckman 
remarks, “ It has not been previously recorded north of the 
