. Bulletin of the scientific laboratories of Denison University. Art. IX,] Watson, Manganese Ore-Deposits of Georgia. 179 Cambrian to Carboniferous. Several faults of the minor-thrust type cut the rocks at close intervals. The ores are limited to the residual decay derived from an underlying long, narrow belt of Knox dolomite, marking the position of a dissected chain of ridges trending northeast-southwest. This belt of the Knox formation is included between two faults, and is in contact on the east and west sides with the Rome shales and sandstones. In 1890, the Catoosa Mining Company made ex
. Bulletin of the scientific laboratories of Denison University. Art. IX,] Watson, Manganese Ore-Deposits of Georgia. 179 Cambrian to Carboniferous. Several faults of the minor-thrust type cut the rocks at close intervals. The ores are limited to the residual decay derived from an underlying long, narrow belt of Knox dolomite, marking the position of a dissected chain of ridges trending northeast-southwest. This belt of the Knox formation is included between two faults, and is in contact on the east and west sides with the Rome shales and sandstones. In 1890, the Catoosa Mining Company made extensive preparations for mining manganese on its property, located Fig, 15,. 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 Denison University; Denison Scientific Association. Granville, Ohio : [The University]
Size: 1666px × 1499px
Photo credit: © Book Worm / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., boo, bookauthordenisonuniversity, bookcentury1900, bookdecade1900
