The geology of Hardin County, and the adjoining part of Pope County . Map Soale In Feetinyo 3000 Fredonla. Renault and Shetlervllle Lower Ohara ??:? Rosiqlare;. • Fredonla andSt. Louis Oi 100- 200 300 400 500 Fig. 29.—Map and idealized geologic section to show the vein relationshipsand stratigraphy at the Blue Diggings shaft. The zone of extensive fracturing isonly very diagrammatically shown. 300 GEOLOGY OF HARDIN COUNTY en I Pell mine.—The Pell mine is located about one mile west of the Premine, in NE. % NW. % sec. 24. The mine was abandoned for several yearsuntil the spring of 1919, when a
The geology of Hardin County, and the adjoining part of Pope County . Map Soale In Feetinyo 3000 Fredonla. Renault and Shetlervllle Lower Ohara ??:? Rosiqlare;. • Fredonla andSt. Louis Oi 100- 200 300 400 500 Fig. 29.—Map and idealized geologic section to show the vein relationshipsand stratigraphy at the Blue Diggings shaft. The zone of extensive fracturing isonly very diagrammatically shown. 300 GEOLOGY OF HARDIN COUNTY en I Pell mine.—The Pell mine is located about one mile west of the Premine, in NE. % NW. % sec. 24. The mine was abandoned for several yearsuntil the spring of 1919, when a lessee started to sink a new shaft. The oldshaft was 95 feet deep and the dump pile showed that vein materials arecoarse calcite, fluorspar, galena, and blende. Pits along the outcrop of thevein show that it is located in a fault with limestone and sandstone as thewall rocks. The fluorspar seen in the dump, and that removed from a veryshallow depth by the present lessee appeared to be of good grade. Stewart mine.—This mine is located about one mile northwest of thePell mine near the cent
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Keywords: ., bookcentury1900, bookdecade1920, booksubjectgeology, bookyear1920
