| 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... | |
| 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... | |
| 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... | |
| 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... | |
| 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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