Smithsonian miscellaneous collections . Unconformdlile i t lictween the Cambrian (7 = Tapeats sandstone) and the tines; exprsure of ?)exposed between the \ich(_an as seen m plate 42 and the highest beds of the Algonkian shown on the nibeneath the clitts of Lanil)rian (/=lapeats) sandstone as the outcrop of the latter winds m and out aroithe Chuar series (C/i) aie beautitulh exposed on the west side of the Grand Canyon in the Canyon \ alle> gressing MidiThe lineThe local ,..„ seas covered them with its beach sands^ t(irmit> (.^() at the base of the Cambrian (r=Tapeats sandstone) cuts

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Smithsonian miscellaneous collections . Unconformdlile i t lictween the Cambrian (7 = Tapeats sandstone) and the tines; exprsure of ?)exposed between the \ich(_an as seen m plate 42 and the highest beds of the Algonkian shown on the nibeneath the clitts of Lanil)rian (/=lapeats) sandstone as the outcrop of the latter winds m and out aroithe Chuar series (C/i) aie beautitulh exposed on the west side of the Grand Canyon in the Canyon \ alle> gressing MidiThe lineThe local ,..„ seas covered them with its beach sands^ t(irmit> (.^() at the base of the Cambrian (r=Tapeats sandstone) cuts across the north and west sides of the Grand Canyon of the Colorado River, Arizona, op[ VOL. 6-1, NO. 4, PU. 43

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Keywords: ., bookcentury1800, bookdecade1860, bookidsmiths, booksubjectscience