Lomes. Pumphelly has a home due. Between Dalepole and Bellor Falls are less many ruin tenaces and specially on the north side of the Corn. Rion. Ludlow is on the eastern side of the Green Onts, and here towards Bellow Falls the clay Palaeo- grie slate's are altered to garnet ifrom schist. The intended grains that caused this alteration are alsof adjacent. Mr proof are known here but in some of the Huel slates such might be found. These slats are not regionally metamorphic. The Green Onts proper are made of a dome- Hende schists of Alfordian age. A short distance beyond Bellon Falls we left the Corn. Valley and went up the Blackell Rion. Here also are seen ruin tenaces. Ludlow is in the Mack Rion valley. Travelled yesterday about 50 miles.