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" ... 60 2. Massive dull bluish-white siliceous chalk. Slightly harder than the pure chalk of 1, practically without indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky beds below. Analysis No. 6 shows... "
Annual Report of the United States Geological Survey to the Secretary of the ... - Seite 704
von Geological Survey (U.S.) - 1902
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Congressional Serial Set, Ausgabe 4690

1904 - 1040 Seiten
...indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky beds below. Analysis No. 6 shows that this chalk contains nearly twice as much silica as the chalk above. This bed occurs in the bench beneath the quarry and passes to the...
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Bulletin, Ausgaben 241-244

1904 - 768 Seiten
...indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky beds below. Analysis No. 6 shows that this chalk contains nearly twice as much silica as the chalk above. This l>ed occurs in, the bench beneath the quarry and passes to...
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Experiments on Schistosity and Slaty Cleavage

George Ferdinand Becker - 1904 - 732 Seiten
...indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky beds below. Analysis No. 6 shows that this chalk contains nearly twice as much silica as the chalk above. This bed occurs in the bench beneath the quarry and passes to the...
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Bulletin of the United States Geological Survey

Geological Survey (U.S.) - 1905 - 462 Seiten
...indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky beds below. Analysis No. 6 shows that this chalk contains nearly twice as much silica as the chalk above. This bed occurs in the tench beneath the quarry and passes to the...
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Bulletin, Ausgabe 395

1910 - 178 Seiten
...Survey 22d Ann Rent., lit. ."., 1902, pp. 687-742. 1Taff, JH, Work cited. 2. Massive, dull bluish white, siliceous chalk, slightly harder than the pure chalk...indication of bedding and because of its hardness projects in a steep bench overhanging the less chalky and friable beds below 35 feet 3. Massive, very...
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Outlines of Arkansas' Mineral Resources

Arkansas. Bureau of Mines, Manufactures, and Agriculture, George Casper Branner, Arkansas Geological Survey - 1927 - 358 Seiten
...separated by thin partitions of very slightly laminated chalk * * * 60 feet 2. "Massive, dull bluish, white siliceous chalk, slightly harder than the pure chalk...indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky and friable beds below * * * 35 feet 3. "Massive,...
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Outlines of Arkansas' Mineral Resources

Arkansas. Bureau of Mines, Manufactures, and Agriculture, George Casper Branner, Arkansas Geological Survey - 1927 - 356 Seiten
...separated by thin partitions of very slightly laminated chalk * * * 60 feet 2. "Massive, dull bluish, white siliceous chalk, slightly harder than the pure chalk...1. This chalk is practically without indication of bed ding, and because of its hardness projects in a steep bench overhanging the less chalky and friable...
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Outlines of Arkansas' Mineral Resources

Arkansas. Bureau of Mines, Manufactures, and Agriculture, George Casper Branner, Arkansas Geological Survey - 1927 - 364 Seiten
...pure chalk of 1. This chalk is practically without indication of bedding, and because of its hardness projects in a steep bench overhanging the less chalky and friable beds below * * * 35 feet 3. "Massive, very siliceous, dull blue argillaceous chalk marl * * * 8 feet 4. "Bluish...
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