Wea. FRI. OCT. 29, 1909 Ther. It is in this zone on S. bank that in seen the largest of bithersm at out 10' dry and at this. Below it is another one 41 dry to 41 this. Around and over it are squeezed the thin redded hended blue ls = sea bottom sliding. It lies in the upper of these 15th bed with 2' of thin redded material on top. On the south bank there cirl. over out W to 12' On the north bank between (1) and (2) occurs thin redded cir., situated about 10' thick. There then two are two separate cryl. beds. An upper intraformational cryl. and beneath the 10' is the great breccia layer. On the south side there is but breccia bed, to E. more nearly an intraformational thin redded edgeless cryl. that joins W into the 26' great breccia.