. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. k ilir DEVONIAN OF NEW BRUNSWICK. fi05 " West and north of Mount Prospoct, where the Cordaito shales disappear beneath the stratified gravel wiiich covers tlm top of that hill, the dip of the bcdrt at the base of this group rapidly diminishes :1 ) { i f Btjr WcitlleAch. MiBpeck Benvcr Lnko . Mount *!ii'l I o > .=
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. k ilir DEVONIAN OF NEW BRUNSWICK. fi05 " West and north of Mount Prospoct, where the Cordaito shales disappear beneath the stratified gravel wiiich covers tlm top of that hill, the dip of the bcdrt at the base of this group rapidly diminishes :1 ) { i f Btjr WcitlleAch. MiBpeck Benvcr Lnko . Mount *!ii'l I o > .= <«⢠<â¢â¢ Sea â = .3-3 * § a u i- V 01 3 5 gal ij I i 5 I a. I " S £ a S3 Ui U b â 4 » u fi w h cT n a â £om a â 2-5. 3 e $ âºJ H o O. Coldbrook. from 30° to 15°, and the strike at the same horizon varies 10°. The lowest member is a coarse reddish conglomerate, having a red slaty paste filled with large subangular fragments of a gray altered rock, like the lower slate of the Coldbrook group. It also contains frag- ments of reddish sandstone, and a few pieces of impure slaty lime- stone. The conglomerate is overlaid by thick beds of purple clay !i»i. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; Montreal : Dawson
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
