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Ch. 2: Manhattan Island

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84               GEOLOGY OF NEW YORK CITY
slowly achieved, but marked by intermittent periods of extreme dynamical intensity. Such folds are seen in the Transverse Road at 79th Street and Central Park, formerly at the east fend of Washington Bridge, while they are shown in the most wonderful confusion at 15 2d Street and 7th Avenue. For a block on either side the eye traverses a face of distorted gneiss, with contracted bands of alternating feldspathic, micaceous, hornblendic rock. The strata, as a whole, lifted up in a line of double curvature, are standing almost " on end," slightly inclined eastward, while subordinate wrinklings, twistings, kinks in endless profusion, convert the surface into a " living picture " of primary forces crumpling the earth's crust, as the hands might flex and crush a bundle of paper cards. It seems probable that the minor small waves of plication were pro­duced before the final uplift came which crowded these into up-and-down shortened bends. (Figs. 14, 15, 16.)
These facts and suggestions bring before us the problem of the origin of this whole group of rocks. They sharply inter­rogate our explanation of their occurrence. Without starting out with the most simple assumptions of geology, or involving this sketch in a rudimentary classification of rocks, it is usually agreed to regard the crystalline schists to which these gneisses of Manhattan Island belong as originally sediments, or the accumulation of ancient muds, mingled, doubtless, with detri-tal matter that was not mud, but sand, both of quartz and other silicates; the whole was derived from the wear and tear, the attrition and slow degradation of still older rocks, perhaps, in the case of this island, those granulites and highly siliceous and ferruginous rocks which form the Highlands.
However accumulated, these beds of sediments represented a heavy deposit of which silica, alumina, iron oxides, lime, magnesia,- potash, and soda, and more rare elements were parts; and it was a change of hardening, solidification and chemical combination which slowly ensued, and under the auspices of certain physical conditions created these beds of
Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island
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