August 26 continued should be exposed, it is plain that a major fault occurs between the two nearby places llying down the southern jar so that the Lil. Der. comes to lie against the fossil Lileuvian. As we were sorting into Les Enyl. and the Heldutug series with our prospect if it exposed anyther der, one autred to the Les enyl. locality found geo-terdes. While I looked for fossils in the enyl. Brickmay and Cion sorted around to see if they could find young or older beds. Young ones have all been recorded away while form was could not be seen. However they found a loose block with Ornograptus that had the lithology of the un-terfied der lies as found in places in the enyl., and so they tried to find graptolites in the rock in the place. And to Brickmay for some good ones. According to Les Enyl. is Lileuvian, and instead of it being one continuous bed of enyl. it is probably a series of enyl. gree, in a slaty series of sandstones having Ornograptus. There are at least 3 species of Ormo. and one dictyomena According there is no probability of finding in the area what lies on tops of this enyl. grees. Probably some-what faulting to our side Brickmay may find em-tact between the Lil. and Der. I now think that it is no Heldutug because much most of Oratapecia.