Early Scotia about time only occurs Pre-Cambrian schist and metamorphous diorite, then are of the Portuogrie. It was 1.30 when we left Scotia Centre. Then on tried through Milton (due along the road occurs Cheshire quartzite), Enser Junction, and then along the valley of the Kinnosaki through the Green Dits north of the Carnels it came to Mont. Pelin. All the rocks in the Green Dits are highly metamorphous Portuogrie. Then on to Barre, the town of greatest granite quarries and granite mills. Other granite make the heart or core of the Green Dits through by car crosses the Kidder Dits. The higher lie to the cross of the granite axis. Stayed one night at the good Barne Hotel at Barne,