..Report on the building and ornamental stones of Canada, volI-V . widens out and nooutcrops of rock are encountered until the vicinity of the forks is reached. Summary—Credit Valley Area. The outcrops of the Medina sandstone within this area occur as an almostcontinuous line from the vicinity of Limehouse to Cataract on the northbranch of the Credit river and to near Belfontain on the south branch. Theextent of the exposures is never great as the stone constitutes a lineal bandalong the face of the Niagara cuesta. The actual exposures may be consideredas i^resenting three types, first, a regi
..Report on the building and ornamental stones of Canada, volI-V . widens out and nooutcrops of rock are encountered until the vicinity of the forks is reached. Summary—Credit Valley Area. The outcrops of the Medina sandstone within this area occur as an almostcontinuous line from the vicinity of Limehouse to Cataract on the northbranch of the Credit river and to near Belfontain on the south branch. Theextent of the exposures is never great as the stone constitutes a lineal bandalong the face of the Niagara cuesta. The actual exposures may be consideredas i^resenting three types, first, a region in which the sandstone is exposed. y.
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectbuildin, bookyear1912
