these banks occurs E5 and extending at least 1/2 miles farther north before we come to where we had collected so many Strick- landinia in zone E7 and the base of E6. E5 is a hard cmctoridally fracturing limestone, A light grey clays with almost no slate parting. The commonest fossil is again the Oncocerous, in fact zones E3 to E5 should be called the Oncerces beds, The next most abundant fossils is a Johnckertella or surfaces with Tentaculites and Ostracoda. Also secured thin cuteri Acostus cretice and Bogrus picked up a very large and fine Calymena rosuta. Here we also rarely meets with a Farrsite. Richardson constantly mentions fossils that I do not find in the reign, some of which I am certain are loose and from the moronic nature covering this part of Anticosti. I saw no Stricklandinia in any of threes of zone 3-5.