Page:Field Notes of Junius Henderson, Notebook 2.pdf/17

 is over 2 miles wide and the anticline and syncline both show beautifully the section being as follows. ((Drawing in field book. I am not sure if this is the same place but similar relations can be seen on US 287 north of Livermore)) E. cuts a trough from N 24˚ E through the N end of anticline then swings over into syncline and cuts through it to junction with W , then both swing E through anticline. The cliff on the S side seems surely Lyons formation. Section as follows,