"In other words we have here a series of interbedded submarine lavas, tuffs and marine deposits all of Stedderbyan time. Volcanoes therefore when active in Lower Oronian time and in straty with Middle Oronian time. The Maguasha ark beds to the right of the Landing is said can apparently conformably by red conglomerate beds. These Clark calls Bonaventine and tuffs there as Orono-Carthian forms. To me this seems incorrect and that they belong in the Baske series. The Bonav- ventine bas flatter and envelops are formation of the Bay of Chaleum region. It occurs on both sides of the bay but especially on the north shore. Anthony & Blomide, Maguasha P.Q. Mining will collect at 60¢ per specimen. I told them to send me 25 specimens.