Viewing page 231 of 473

This transcription has been completed. Contact us with corrections.

[[stamped]] 0650 [[/stamped]] 
[[left margin]] 29 [[/left margin]]

The vanghanite is followed by dolomite and magnesian limestone. The upper part of the section is much sheared bright blue gray ls. This was called Lincolnshire by Cooper but he is not sure of it. The Mosheim may be 5 - Oaks. The lower beds from the Gastropod (Maclurites) zone down to the Beekmantown seems definitely to be Lenoir. The upper limestone contained no chert.

Here the vanghanite seems to belong rather to the lower than to the 5 - Oaks beds & may be Lenoir.

The Sowerbyella (small) seems to link the Lenoir at Porterfield to the Lincolnshire. It certainly would make it postchazy.