quartz pebbles in the shale. It is the regulation red sun-baked sandy shales with a very slight tending to ligny gneiss. About 25 and certainly not more 30 feet to the slip fault. In all about 37 feet. Havarangunde conglomerate bearing Shicim- sided at the top showing that movement has been marked from the top. It is a most decided conglomerate of fine quartz pebbles in clean sand, but the pebbles are not well rounded. This about 10 feet thick and to the north then the ground is covered. Beyond is more red shale. So it Havarangunde thrusts into the red shale. I am not interpreting it. High Falls along the railway long north we see much once of those shales and then the Bimnerate followed by the cement beds. Then the Lepes- dicta beds with Spirifer renuxensis. Above are thin hard limestone near the top which seem the Hypidula ercegmanensis bed. In a chart give of about 10 feet