Wea. WED. FEB. 3, 1909 Ther. Then without head and without positive evi- dence error in a lay sequence of Pennsyl- tania - at least 2 miles far up str. The nf recognizable fossils are Calamites. It is old md sh. and 10. with gms of infraformational conformants. These are the Collete conformants. Belle says that between the Windsor and the Pennsylvania there elsewhere a still older Penn, series. However on the whole conclusions are not altogether certain; but Bell is doing the best he can on all the evidence available. All the strata seen today appear to be connected with desert condition - most decided with the Horton. The marine hori- gon in them seems more better above the one above mentioned above this regular Windsor one (the one near Petelbostien) Our expedition stopped at the mouth of Croydon Brook, and Croydend Point. Down take the same angular conformity today. All is conformable sequence.