July 6 Friday. Kindson Collected during the morning at Millers quarry. The fossils here are much like those of the Maxneso joint although a lower band of limestone. Bryony and her attendant essentially Fernstall and Churhfora are of which we only about at Maxmes Point. Picked two trees and shipped this afternoon. To me has are the material from Maxmes Point, the other has smelted jackjags and some material from Millen quarry left in the evening for Halifax. In looking over the above section it seems to be certain that taking the Railroad bridge as a center the strata dip or recede right fit in opposite directions. There is a fault or line but apparently only a slight dislocation. The beds to the south are also slightly twisted out of the strike of those to the north of the body. The second fault cuts out zones 1 and 2 and the sandy limestone appears next in quite another way ! So therefore impossible to say withy the Windsor limestone is higher or lower than the Arm bridge limestone. According to the records the Windsor limestones are higher than the Arm Bridge limestone.