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Ch. 2: Manhattan Island

Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island Text size:minus plus Restore normal size   Mail page  Print this page
MANHATTAN ISLAND
147
to the friable dust, which was removed with pick and shovel. For 20 feet to the west the surface was covered with the green actinolite dust and fragments up to large boulders. I should say the gneiss walls were about 4 feet apart at 128th Street, 15 feet apart at 100 feet north, where the stump now appears. Above the present stump no solid rock appeared on the surface, but what appeared to be a deep, green clay. On the removal of this clay the actinolite was struck. My attention was called to this dike almost every time I asked the men operating whether they had found anything new. They all said it was the toughest rock they ever had dealings with. A similar greenish soil containing actinolite continued from the 129th Street end of the dike to the N. E. corner of 128th Street and Convent Avenue, but I did not see solid actinolite in place. It may have been that the actinolite was washed down from the dike into the depression in the gneiss rock, or it may have been that the depression was caused by the decaying of the dike in place. The gneiss to the east of the depression was 10 to 15 feet higher than the gneiss to the west of the depression."
East of the degraded dike there were broad surfaces (20 feet square), rusty brown, through iron staining, showing gneissoidal partings, which must have been more extensive, and indicated" a possibility of slipping of the steeply inclined foliae.
BIBLIOGRAPHY
In 1816, Hayden, in the Geological portion of Professor Cleve­land's Mineralogy, " describes a granite ridge crossing New York Island and appearing at Hurlgate, on Long Island,thence extend­ing into Connecticut." (Stevens.)
Wm. Maclure, in his famous Geological Map of the United States, puts down New York Island as " primitive formation."
S. Akerly, in 1820, published " An Essay on the Geology of the Hudson River and the Adjacent Regions; illustrated by a geological section of the country from the neighborhood of Sandy Hook, in N. J., northward through the Highlands, in New York, towards the Catskill Mountains." He speaks of the southern
Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island
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