Besides what collected saw many Byssmochia (two species, the com. one has crasse plicatines), Ordov. lophosia, C. senaria, Qd. medi, O. sinuata ? (all in small packets, maybe returned), E. modesta (like three below) There is no evidence of open-cracking nor any evidence of sub-aerial kinds. The nature of sedimentation is the same throughout. the Orpordillian and Richmon- dian. At different levels saw indistinct large ripples and in the lowest layers the small ripples 3/8 inch apart.