"One Serjio's bed B 4 is of the banded-reticulate (due to weather) character that I have often regarded as typical Reed mantown spheronin. It is a very peculiar deposit; the modules of me characters marked by anything that weathers into dolomite. Over the moraled some previous described comes a well bedded thin paired drl = One Serjio's B 3 1/2. Below is B 3 1/2. This then is an old erosion surface. For it has shallowed, followed by land and erosion and solution of holes and caves now filled with drl. of subsequent fills. The last interval is not thought to have been long. Another aerially eroded surface occurs between beds B 4 and B 5. In B 4 occurs Piloceras and we saw the old holes into which Bellings type came. Now our Piloceras in B 5. Bed B 5 has many once-eroded Cryptosorus, some in place and others fallen around smalling local empls. Another unconformity in B 5, higher up. The Phillipstony sheet is at not two miles across, fine here due to Challet interjps. The dips are much steeper in the W, as high as 70 (the stress side), but in the E flatten down to about 30. However there are also real thrusts in the sheet such since one may be seen in the road cutting about 1/2 mile E of Phill-lystony, and farther east the mantle bed is cut out in this section but present farther west and was much quarried for marble - here are the rolling marble smiles.