"Learning Tarrin Lalle and Irminutim are started most and in Jamin, Huttartom are jarred through the same Cambrian suc- cession. Reiff says the terrains have the same exact succession. At four miles south of Ludbury are come upon great fields of limestone, said to be of Trenton age. These limestone are wonderfully drawn out and kept of like angry state. The hills seem more a fur segment rather opened for the Granod Eleemos. Have two samples of these drawn out limestone. Reiff collected at another place some hack shits that which announces Middle Trenton. From here north are remain in the Ordovician, and it is but at an infolded one which was thrust to the Lower Cambrian seen to the south during the last three days. Ruffland is another fault of these younger strata but have their position in due to normal faulting. At Ludbury can be seen a complete section out of of the Trenton, but finer