. Geology of the Narragansett basin. Geology. STEDCTUEB OF THE BASIK 123 strata, of which there can not be less than 12,000 feet now remaining. East of this Hne the upper strata are apparently denuded and the structure y/'^o' '7/VS* -Jl^O' ^S'Oii JfPfS 4i'^. i?2«00' -^/•.*^ ^/'aa ' 7/W* Fig 9 —Outline map and general cross section of the basin is less well shown (see fig. 8)^ largely owing to the coveiing of glacial drift. In the southern arm, as is shown in Dr. Foerste's report, like. Please note that these images are extracted from scanned page images that may have been digitally enhanced fo
. Geology of the Narragansett basin. Geology. STEDCTUEB OF THE BASIK 123 strata, of which there can not be less than 12,000 feet now remaining. East of this Hne the upper strata are apparently denuded and the structure y/'^o' '7/VS* -Jl^O' ^S'Oii JfPfS 4i'^. i?2«00' -^/•.*^ ^/'aa ' 7/W* Fig 9 —Outline map and general cross section of the basin is less well shown (see fig. 8)^ largely owing to the coveiing of glacial drift. In the southern arm, as is shown in Dr. Foerste's report, like. 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 Shaler, Nathaniel Southgate, 1841-1906; Woodworth, Jay Backus, 1865-1925; Foerste, Aug. F. (Aug. Frederic), 1862-1936. Washington, Govt. Print. Off.
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Keywords: ., bookcentury1800, bookdecade1890, bookpublishe, booksubjectgeology
