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| | First Biennial Report, 1878, Geology of Kansas |
 | | This is, in part, owing to the fact, that the State has not been disposed to employ a geologist to examine the territory covered by the Coal Measures, as well as to the fact that the deposits near the coal beds are quite irregular. |
 | | Thus, at Pleasanton, Linn county, coal was found in one lead shaft of a workable thickness, and less than eighty feet from the surface, while in another shaft, two hundred and sixty feet deep, and only two hundred yards distant, none was found. |
 | | The width of the trackway is from eleven to twelve inches, measuring, as usual, from center to center. |
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