Wea. MON. MARCH 8, 1909 Ther. that Keith says looks like Chochie = basal Lava Cambrian, it is of a trap sheet. Further down lies a jume if dolomite that looks li[e] we saw this morning. If or it maybe I am the thrust sheet. Still further down lies in a thick mass of tandul slate very much like the th[if] slate on which Keith tells may be of his time. Our arms, At Coramsville we descended into the Jo. muska Rim to see the steeply standing slate with a few jume if limestone. On the shale cliffs collected a Bzzyrnskin and to day one pit a Plectambryla, ac[illegible] and a fourth spe- cimen that we could not determine. Then went to near Fridgey Corners to see blue-black slates with many specimens of Climacograptus. I have a picture. Then autoed to Phillipotany where we put up for the night.