. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. DEVONIAN OF NKW IIRUNSWKK. >05 les in Feet. ',) and s . 2800 paste ; red, kness . 2500 )ncrc- 400 flags, shale igula; beds, Trilo- fcct or more )cvonian arc cnt memoirs lin that the it side of St the eastern believed to r less mcta- thc section, mber of the roups to be , they may ig between the centre ' the Upper shales, and led. It is to have a iver, in
. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. DEVONIAN OF NKW IIRUNSWKK. >05 les in Feet. ',) and s . 2800 paste ; red, kness . 2500 )ncrc- 400 flags, shale igula; beds, Trilo- fcct or more )cvonian arc cnt memoirs lin that the it side of St the eastern believed to r less mcta- thc section, mber of the roups to be , they may ig between the centre ' the Upper shales, and led. It is to have a iver, in the per of Mr " West and north of Mount Prospect, where the (!ordaito shales disappear beneath the stratified gravel which covers the top of that hill, the dip of the beds at tho base of this group rapidly diminishes â¢^ â¢^ c a; c o c3 ^ bo Majrof WcBt noach. MlHpeck Rtvcr. Di'iivcr Lnkc . Mount rrosi);!i! _2 a ^ c a. J I I .2 t- ^ â 'â¢' t*. O J-. U S K -J a" W Eh O S C'dhlbrook. 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. JliiMiii. 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; Halifax [N. S. ] : A. and W. Mackinlay
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
