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" ... concretions in the upper part. The Codell sandstone member occurs as a lentil above the Blue Hill shale member and immediately below the base of the Niobrara formation. The Codell sandstone member ranges in thickness from a few inches to as much as... "
Muscovite in the Spruce Pine District, North Carolina - Page 154
by Thomas Lingle Kesler, Jerry Chipman Olson - 1942 - 38 pages
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Census Reports Tenth Census. June 1, 1880: Cotton production in the United ...

United States. Census Office. 10th Census, 1880, United States. Census Office - United States - 1884 - 966 pages
...stated : Those of the better class of uplands are formed by a yellow or brownish loam, varying greatly in thickness from a few inches to as much as 20 feet, but averaging •¿a Soluble silica Fotaâh Soda No. 180. ¡ No. 290. Ï5!*» LA FATKTTE соиктт (R....
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The Geology of Parts of North Lincolnshire and South Yorkshire: (Expanation ...

William Augustus Edmond Ussher, Charles Fox-Strangways, Alan Charles Grant Cameron, Clement Reid, Alfred John Jukes-Browne - Geology - 1890 - 256 pages
...there are 18 feet of this clay. Intimately associated with these deposit is a bed of peat, which varies in thickness from a few inches to as much as 20 feet. It is well exposed in the Humber at Melton below high-water mark, and has been met with in several...
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Bulletin, Issue 707

Geology - 1922 - 424 pages
...mainly sandstones, but there are also many beds of shale, and in places there are coal beds, which range in thickness from a few inches to as much as 20 feet. An old prospect in one of the thick beds is shown in Plate LXXX, B (p. 195). The coal beds, however...
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Information Circular, Issues 8458-8466

Mineral industries - 1970 - 822 pages
...in the Iowa Gulch area, occurs as dikes intruded into nearly all the faults. The fault traces vary in thickness from a few inches to as much as 20 feet, averaging approximately 2 feet. Generally, abundant gouge is presen; in the faults, indicating considerable...
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Uranium in Coal in the Western United States

Geological Survey (U.S.), Norman MacLaren Denson - Coal - 1959 - 390 pages
...bentonite is a dense homogeneous clay in which individual grains cannot be distinguished. The bentonite beds range in thickness from a few inches to as much as 20 feet. The base of the Salt Lake formation in the vicinity of Trapper Creek is a thick sequence of friable...
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The Spotted Horse Coalfield, Sheridan and Campbell Counties, Wyoming

Wilds Williamson Olive - Coal - 1957 - 192 pages
...part of the township, where the coal is commonly split into two benches, separated by rock ranging in thickness from a few inches to as much as 20 feet. The lower bench reaches a maximum observed thickness of 6 feet 2 inches at locality 706, and the upper...
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Geological Survey Bulletin, Issue 1200

Geology - 1966 - 1468 pages
...feet thick and locally contain thin siliceous layers parallel with bedding; quartzite and shale layers range in thickness from a few inches to as much as 20 feet and are most abundant in upper 200 feet of formation. Thickness about 1,300 feet. Overlies Crystal...
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Geological Survey Bulletin, Issues 1286-1289

Geology - 1969 - 278 pages
...principally of quartz and plagioclase feldspar and contains lesser amounts of muscovite and biotite. Beds range in thickness from a few inches to as much as 3 feet ; many are finely laminated, and a few have graded bedding. The schist and graywacke have been...
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Geological Survey Professional Paper, Issues 219-220

Geological Survey (U.S.) - 1949 - 430 pages
...sequence varies much from place to place. It includes both marine and terrestrial sediments. The limestone beds range in thickness from a few inches to as much as 20 feet. Those from 3 to 6 feet thick are most common and retain their individuality for considerable distances...
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U.S. Geological Survey Professional Paper

Geology - 1950 - 222 pages
...sequence varies much from place to place. It includes both marine and terrestrial sediments. The limestone beds range in thickness from a few inches to as much as 20 feet. Those from 3 to 6 feet thick are most common and retain their individuality for considerable distances...
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