Minisquoi One of the li. of this Dravant emyl is made up of the then redded Mf. Milton. Probably 3/4 of it, and co- mented by a sandy dolomite. Some of the emyl has foreign rocks, all are from the Orellett up to the Up. Millin. The large blocks of "Shelburne" are metamorphosed into mattic but show no flow structure. Or Shelburne is known north of the Skinoeli over, and yet it is common in all of the Dravant emylments. It must have been place here at the time of the Dravant deposition. But are those Shelburne li., which we also meets in the emyl, at the base of the Bridgegate.