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" ... north extension of Main street. It has a south face of 525 feet and has been worked about 200 feet to the north. The stone is typical limestone of this area, being coarsely crystalline and having a slightly bluish light gray color. It contains suture... "
Report of the State Geologist on the Mineral Industries and Geology of Vermont - Page 55
by Vermont. State Geologist - 1908
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Reports 2nd Series

Missouri. Division of Geological Survey and Water Resources - Geology - 1903 - 810 pages
...slightly bluish light gray color. It contains suture joints from two to fifteen inches apart and varying in size from a fraction of an inch to three inches in depth. The following is a der scription of the stone by channel cuts from the top to the bottom of...
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Reports: 2d series, Issue 2

Missouri. Division of Geological Survey and Water Resources - Geology - 1904 - 526 pages
...slightly bluish light gray color. It contains suture joints from two to fifteen inches apart and varying in size from a fraction of an inch to three inches in depth. The following is a der scription of the stone by channel cuts from the top to the bottom of...
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The Quarrying Industry of Missouri

Ernest Robertson Buckley, Henry Andrew Buehler - Quarries and quarrying - 1904 - 520 pages
...slightly bluish light gray color. lt contains suture joints from two to fifteen inches apart and varying in size from a fraction of an inch to three inches in depth. The following is a der scription of the stone by channel cuts from the top to the bottom of...
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The Mining World, Volume 27

Mineral industries - 1907 - 452 pages
..."cross fiber'' or "slip fiber." Cross fiber asbestos forms, veins in which the fiber in most cases extends directly across the vein, perpendicular to...often silky and of high grade, ranging in size from. a small fraction of I in. to 3 ins. in length. On the other hand, slip fiber occurs in slickenside fault...
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Transactions of the Geological Society of South Africa, Volumes 30-31

Geological Society of South Africa - Geology - 1928 - 520 pages
...found. These black masses were usually round or oval, but sometimes curved or flattened, and varied in size from a fraction of an inch to three inches in length. They occur in layers which conform roughly to the bedding. In thin section the black patches were seen...
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Transactions, Volumes 30-32

Geological Society of South Africa - Geology - 1928 - 804 pages
...found. These black masses were usually round or oval, but sometimes curved or flattened, and varied in size from a fraction of an inch to three inches in length. They occur in layers which conform roughly to the bedding. In thin section the black patches were seen...
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