Publisher's Synopsis
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1890 edition. Excerpt: ... THE DAILEY CHEEK BASIN. The Dailey Creek basin is situated to the east and northeast of Blocton, to the west and northwest of Montevallo and to the southwest of Helena, Gurnee being in the north end of this basin. It is bounded on the northwest by the "Interior fault;' and the Blocton basin, also by a portion of the Gould basin; on the north and northeast by Dry Creek basin and Lolley basin, on the east side by the Montevallo basin, and on the south side by the "Overturned Measures" and the "South boundary fault." The following is a description of the boundary of the Dailey Creek basin: Commencing at the gap in the Conglomerate ridge where the Little Mayberry Creek cuts through it, at the fault where the flat measures and the "Overturned" measures come close together, thence northwestwardly along the anticlinal to the northwest corner of section 15, township 22, range 4 west, thence due north along the section lines on the west side of sections 10 and 3, to the southwest corner of section 34, township 21, range 4 west; thence northeast to the northeast corner of said section 34; thence northwestward down Jesse's Creek to the southwest corner of section 15, township 21, range 4 west; thence northwest to the southeast edge of the Interior fault vertical rocks near the northwest corner of section 16, township 21, range 4 west; thence southwestward along the southeast edge of the Interior fault leaving Boothtown to your left; thence close by Cadle Station, crossing the railroad at this point, close by the Gardner old mine; continuing close along the edge of the Interior fault to the edge of the coal field at a point about a quarter of a mile west of the southeast corner of section 17, township 24, range 10 east; thence eastward along the...
