Bathurst, N. B. July 13 - 1929 Coppen had the garage fix the two flats yester- day and so we did not job started from Friday 1pm until 9 p.m. It was an uninteresting drive to Newcastle where we put at 2 p.m., on sandy dusty roads. For Tuesday travel was light. Had a Palmer funnel here. Every now and then we saw the horizontal muddy gray-brown heavy bedded SS that would weather into thin flakes a few inches thick. Holes are practically absent. All are of muddy coarse and fine sandstone with irregular grains of coarse crysmic in which the layers fuses are quartz pebbles. It is all more a less cross bedded and the angle have long pieces of gravel. It in my layers an ochre. From Newcastle to Bathurst it is 45 miles through the woods. We arriving at 6 p.m., at the Gloucester Hotel. In places we saw the same Carboniferous SS and at the sea side as Newcastle. The river banks at Bathurst opposite the Paper Pulp Mills on the red Bathurst formation, the basal part of the Pennsylvanian. It is a brick red not quite so dark red as our Triassic. Anthracite coal, smother up about 1/3 of the whole with surrounded quartz pebbles up to