Orcheston The cyl. dips about 20 degres to the east and is layers made up of a white limestone more or less hols- get that we have it called the Hellburne. It may just as create the lense whitle li. of the Celechester. Pors may laye blocks of it 2 to 6 for across, and are 10' long. There are also pieces of the Mallett sandy dol. but apparently more of the Highgate li. than houlded limestone. This appears to me to be Celechester shale lath-holes and especially about the lower ends, [illegible] Dorrell's, nice guard gates with small heels, are waiting for the sand filling between the li. boulders of the cyl. They are therefore of the age of the deposit and are not for blocks in the cyl. as Reid thinks. In one place above through, in the Celechester I get what appears The Lattrellia? May may not the Lower Cambrian here fan into the Ordovician fauna and then into my cap Ordovician Cambrian. No Millin was seen, nor is the shale