Thursday, Sep. 4, 1930, continued with the corners rounded off a little. It is natural that they did not come far. Volcanic rocks are fairly common but do not make up more than 20% of the coryl. The next field of boulders and pebbles appear to be the slabby baspe ss. Folded fin-de-dred sand, sometimes are often seen and partly are white Ordovician. In all of these rocks I did not see a simple joint or even a corind or steurral. Of granite boulders more, and of gneiss boulder size make seem. On the basis of the coryl data, as yet, no clear clue to distinguish the Bonaventure from the Point St. Peter series or even through in the lower baspe ss that down on the Corner of the Beach. It will be the position mainly that will distinguish the various Bonaventure-like coryls.