ISBN: 1231141697

[EAN: 9781231141694], Neubuch, GEOLOGICAL SURVEY,SUBJECTS, This item is printed on demand. Paperback. This historic book may have numerous typos and missing text. Purchasers can download … More...

[EAN: 9781231141694], Neubuch, GEOLOGICAL SURVEY,SUBJECTS, This item is printed on demand. Paperback. This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1907 Excerpt: . . . and shale (see below) Shale Coal with some shale (see below) Shale and sandstone (horse) Coal with some shale (see below) Shale and sandstone L Coal, impure and somewhat coked Shale and sandstone Diabase sill with local occurrence of natural coke on top Coal and coke with impurities in an irregular distorted mass Concealed not over-Shale Coal with some shale Shale Coal with some shale Shale and sandstone Coal with bone and shaleShale Coal (varies from 1 ft. 8 in. to 3 ft. 7 in. ) Shale with some sandstone, iron ore, and volcanic beds, and a few thin beds of coal and coke Section at bend of Chickaloon Creek, one-half mile above Watsons camp, show ing details of beds 2 to 6 in condensed section. Ft. in. Black shale Coal Coal, bony Shale Coal Shale, black Coal Concealed Shale Coal Shale. -Coal Shale Coal Shale and sandstone (horse). . Coal. . . , Shale, with coal stringers Coal Shale Coal Shale Coal Shale Coal Shale In addition to the sections measured by Martin on Chickaloon Creek the following measurements were made in the tunnels opened at Watsons camp (fig. 2). The sections are from the face outward; the thicknesses are recalculated for dip. The change in direction of dip which is evident between tunnel D and those farther east (C, 3, 2; B, and A) may possibly be explained by the presence of an anticlinal axis that passes westward from the anticlinal fold at tunnel No. 1, or possibly by irregularities in beds representing the south side of such an anticline. It has been difficult to correlate the several beds within these tunnels because of striking irregularities in their thickness. The bed 16 feet 7 inches thick in tunnel A is undoubtedly the same as the bed 17 feet 3 inches thick in tunnel B. A drift from tunnel B has been run to tunnel 2, which correlate. . . This item ships from La Vergne,TN.<

2012, ISBN: 1231141697

[EAN: 9781231141694], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers c… More...

[EAN: 9781231141694], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1907 Excerpt: .and shale (see below) Shale Coal with some shale (see below) Shale and sandstone (horse) Coal with some shale (see below) Shale and sandstone L Coal, impure and somewhat coked Shale and sandstone _ Diabase sill with local occurrence of natural coke on top Coal and coke with impurities in an irregular distorted mass Concealed not over-Shale Coal with some shale Shale Coal with some shale Shale and sandstone Coal with bone and shaleShale Coal (varies from 1 ft. 8 in. to 3 ft. 7 in.) Shale with some sandstone, iron ore, and volcanic beds, and a few thin beds of coal and coke Section at bend of Chickaloon Creek, one-half mile above Watson's camp, show ing details of beds 2 to 6 in condensed section. Ft. in. Black shale Coal Coal, bony Shale Coal Shale, black Coal Concealed Shale Coal Shale.-Coal Shale Coal Shale and sandstone (horse). Coal., Shale, with coal stringers Coal Shale Coal Shale Coal Shale Coal Shale In addition to the sections measured by Martin on Chickaloon Creek the following measurements were made in the tunnels opened at Watson's camp (fig. 2). The sections are from the face outward; the thicknesses are recalculated for dip. The change in direction of dip which is evident between tunnel D and those farther east (C, 3, 2; B, and A) may possibly be explained by the presence of an anticlinal axis that passes westward from the anticlinal fold at tunnel No. 1, or possibly by irregularities in beds representing the south side of such an anticline. It has been difficult to correlate the several beds within these tunnels because of striking irregularities in their thickness. The bed 16 feet 7 inches thick in tunnel A is undoubtedly the same as the bed 17 feet 3 inches thick in tunnel B. A drift from tunnel B has been run to tunnel 2, which correlate.<