"[illegible] the ridge across as far across the next stratum to the first and higher ridge about goo fath [fathoms?] Just what is in this ridge I do not know, but as it is a line with the central of the Bay may it is in one probably the same explorator, see if from this the structure the indubitable thick men can be marked out. If next day I notice that there are no getting to the W. and a my half mile to the N. of it. All of these things are not to see. It rained most of the afternoon and I finally had to quit though I could not have gone much farther in account of the tide coming in. After seeing these various quartzites this afternoon, and noticing that the limestone conglomerate are always connected with them, I am ready to give up the idea of the great quartzite hills in the cross conglomerate. They are more in fact if it the infilling material between the limestone truckles and boulders. These quartzites are as a rule fine grained but very near and then quartz boulder streams in and sometimes in such quantity as to sign up to 1/2 ind and vary up to 1 inch. In one case -- in the red gneis -- half of the material is granular red feldspar, showing that the sources of these quartzites was being derived from a