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" ... deposition was long continued, forming thick beds, when they in turn were covered by other sediments. Thus the accumulation went on as the older strata gradually and slowly subsided until the thickness amounted to thousands of feet. The time was long,... "
Final Report - Seite 169
von New Jersey Geological Survey, New Jersey. State Geologist - 1910
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Annual Report of the State Geologist for ...

New Jersey Geological Survey, 1863-1915 - 1883
...these fragmental sedi* The horizontal lines in the figure have no structural significance. 72 merits and fine deposits were altered into crystalline masses....more or less gentle inclination, and dip began as an element of stratification. Upheaving and compressing forces at length began their mighty work and the...
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Annual Report of the State Geologist of New Jersey for ...

Geological Survey of New Jersey - 1883
...wherein these fragmental sedi* The horizontal lines in the figure have no structural significance. ments and fine deposits were altered into crystalline masses....more or less gentle inclination, and dip began as an element of stratification. Upheaving and compressing forces at length began their mighty work and the...
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Final Report, Band 7

New Jersey Geological Survey, New Jersey. State Geologist - 1910
...sand, clay, marl and iron ores in recent times. And there must have been sandy, clayey, caleareous and ferruginous beds like these modern deposits in...more or less gentle inclination, and dip began as an element of stratification. Upheaving and compressing forces at length began their mighty work and the...
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Iron Mines and Mining in New Jersey

William Shirley Bayley - 1910 - 512 Seiten
...amounted to thousands of feet. The time was long, perhaps as great in length as the combined age's of all the later formations. With the subsidence of...were altered into crystalline masses. This change or mctamorphism of the strata was probably slow and in progress throughout a long period of time. The...
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