consists of Lorraine Shales will occur in less emphatic feds of angular limestone of a light grey and while the Richmond is dominant, a thent-raddul limestone, with genes of shale that become less and less upward in the section. It may be that the red beds of the Collingwood-Orin round area are part of the Manitoulin Islands, if deposited they were worked out before the "Clinton" was apparent. Parks said when he saw these iron clogs near Clay Cliff that it was the Wolverine River from Toronto run again. Manitouaning August 15-1912 Thursday. Got up at 6 A.M. and loaded 4 boxes oforris and shipped them to Redland State Hotel, Collingwood, Left on personano at 10 A.M. with Parks and Walter. DRT to Orin round at 11.30, stopping at Leldon Hotel.