. Bulletin of the scientific laboratories of Denison University. 192 Bulletin of Lahoratofies of Denison University [Voi. xii The ore is usually massive and often fine-granular, admixed or otherwise closely associated with iron, and is less often of the gravel and larger concretionary nodular types so characteristic of the Cartersville district and other of the Paleozoic area-de- posits. Of the former occurrence the locality to the northeast of Cohutta Springs, in Murray county, and that of the Drake- town district, in Haralson and Paulding counties, are perhaps the most typical. Near the Tenn
. Bulletin of the scientific laboratories of Denison University. 192 Bulletin of Lahoratofies of Denison University [Voi. xii The ore is usually massive and often fine-granular, admixed or otherwise closely associated with iron, and is less often of the gravel and larger concretionary nodular types so characteristic of the Cartersville district and other of the Paleozoic area-de- posits. Of the former occurrence the locality to the northeast of Cohutta Springs, in Murray county, and that of the Drake- town district, in Haralson and Paulding counties, are perhaps the most typical. Near the Tennessee line, in the northeast part of Murray county and 5 to 6 miles northeast of Cohutta Springs, the manganese occurs as small nests or pockets in ex- tensive beds of iron-ore in the Ocoee (pre-Cambrian) quartzites and slates. The manganese is not entirely free from iron, and much of it is a manganiferous iron-ore of apparently homogene- ous composition. Fig. Scale ofMi/es. Topographical Map of the Darketovvn District, Georgia. (Tallapoosa and Mari- etta Topographic Sheets, U. S. Geol. Survey.) Contour-interval, loo ft. The ore of the Draketown district in Haralson and Pauld- ing counties is either massive or minutely-divided manganese oxide, in a finely-banded quartzite or sandstone intercalated with mica-schist. The siliceous rock is heavily charged with. 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]
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