The dip of the Marlins is apparently to the south. About half way down in the 30- fat ocean my large Alot- cenia (similar or identical one from the Bearpaw section). Along the railroad track the lowest beds are shown here H. ranunculi, Phtherodonta, ostracods, Byrgson, ?Spirorbis. These are thin bedded dark colored brittle beds and more shaly than ?gives large small fossils. Practically the Tectoculites beds. This is made up of 2 layers; at the top of the lower one in a half mile gone L. altus arounds, Rather large specimens.