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" The country rock is jasper, thin layered and separated by seams of shale. The jasper layers differ in thickness from a fraction of an inch to several feet. The same layer varies in thickness, pinching out locally In many places. Most of the shale seams... "
Bulletin of the United States Geological Survey - Page 161
by Geological Survey (U.S.) - 1910
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Bulletin, Issue 76

Chromium - 1918 - 260 pages
...in recent years and no ore shipped since 1896. This deposit is described by EC Harder* as follows: "The country rock is jasper, thin layered and separated...thickness from a fraction of an inch to several feet thick. The same layer varies in thickness, pinching out locally in many places. Most of the shale seams...
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Report of the State Mineralogist, Issue 17

California State Mining Bureau - Gold mines and mining - 1921 - 586 pages
...first opened in 1885 and some small shipments made. This deposit is described by EC Harder as follows: "The country rock is jasper, thin layered and separated...places. Most of the shale seams are thin. Both shale and jasper are greenish gray, except where stained red or black V1v iron or manganese. "The ore occurs...
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Manganese Deposits of the United States with Sections on Foreign Deposits ...

Edmund Cecil Harder - Manganese - 1910 - 346 pages
...frequently in kidneys or wormlike aggregates. It is generally soft and is mixed with considerable clay. (6) The main mass of ore occurring along the fissure is...layer varies in thickness, pinching out locally In manyplaces. Mostof the shale seams are thin. Both shale and jasper are greenish gray except where stained...
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Manganese Deposits of the United States with Sections on Foreign Deposits ...

Edmund Cecil Harder - Manganese - 1910 - 916 pages
...jasper wall is very hard, with either amorphous or finely crystalline structure. The forrnergenerally has a steel-gray luster, and the latter is bluish....places. Most of the shale seams are thin. Both shale and jasper are greenish gray except where stained red or black by iron or manganese. The dip of the layers...
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The Cosna-Nowitna Region, Alaska, Issues 664-667

Henry Miner Eakin - Geology - 1918 - 556 pages
...dirtygray sandstone containing thin calcareous beds and numerous lenses and layers of sandy shale ranging in thickness from a fraction of an inch to several feet. The distribution of the oil in the sand is probably dependent to a considerable degree on differences in...
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The Relation of the Titaniferous Magnetite Deposits of Northeastern ...

Thomas Monteith Broderick - Iron ores - 1918 - 66 pages
...cases are rounded, giving the granulitic textures. In most cases they are arranged in bands which vary in thickness from a fraction of an inch to several feet. The rocks are commonly greenish black in color. Mode of Occurrence. — Most of the inclusions occur well...
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Geology of Petroleum

William Harvey Emmons - Geology, Economic - 1921 - 668 pages
...dirty-gray sandstone containing thin calcareous beds and numerous lenses and layers of sandy shale ranging in thickness from a fraction of an inch to several feet. The distribution of the oil in the sand is dependent on System Series Group Formation Character Thickness...
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Summary Report of the Department of Mines, Geological Survey for the ...

Geological Survey of Canada - Geology - 1924 - 526 pages
...altered to quartz-sericite schists, sericite schists, and graphitic schiste. The individual beds vary in thickness from a fraction of an inch to several feet. The quartz-sericite schists contain much quartz and sericite. Some have much biotite, some contain actinolite,...
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The American Journal of Science, Volume 11; Volume 211

Earth sciences - 1926 - 566 pages
...Fully half of the volume of rock is of thin injection sills of quartz- feldspar pegmatite that range in thickness from a fraction of an inch to several feet. The abundant injection of this zone is governed by two factors: I The sedimentary rock of this area was...
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The Vermilion Iron-bearing District of Minnesota: With an Atlas

Julius Morgan Clements - Geology - 1903 - 510 pages
...constituting the slates, and by a slight difference in size of grain. These bands within the slates vary in thickness from a fraction of an inch to several feet. The bands of slate themselves, where interlaminated with grits and near the conglomerates, also vary in...
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