no macula here then New Zealand fish. These chalk beds then come far away to bear hidden claw crystalline and crinoid limestone of the Cre- crows. Balance of section measured by Reeds but I did not take them down because the detail is not not so readily determinable as some places ap- pear I did the work for the entire quarry. At Twenty Pink Bridge the lower limestone has of the macula gone as in the Keizer quarries does not have this form. In both places the shale immediately above belongs to the New Zealand. The Lower Lias clay that comes in sharply and distinctly there is no transition gone.