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Appendix I: Glaciation in Great New York

Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York Text size:minus plus Restore normal size   Mail page  Print this page
214             GEOLOGY OF NEW YORK CITY
faces are as universal as the boulders so frequently found near them. In Dr. Gale's examination the record of grooved sur­faces challenges our admiration from the persistency of their occurrence, for whenever the rock was uncovered, exposed, in all probability, for centuries to rain and frost and heat, these extraordinary rulings remain, altered, of course, partially erased, but never obliterated. A few examples of these early notes are of instructive interest. It may be premised that the gneissoid rocks of New York are not the best arranged or composed mineral aggregate for the preservation of these grooves. The decomposable character of the mica and feld­spar, their considerable permeability to water, and the vary­ing hardness and denseness of the rock furnish a poorer sur­face than more homogeneous rocks, as sandstones, limestones, and fine-grained granites, so that the grooves, scratches, and striae over the gneisses and mica-schists oi Manhattan Island undergo a gradual blurring, and are best preserved where the rock is more siliceous and more dense.
At 70th Street and 10th Avenue Dr. Gale records abun­dant drift grooves and scratches, in direction N. 35° W.; again, at 77th Street (same avenue), " numerous, and extend­ing almost everywhere in favorable situations into the river even below the lowest tide-water marks, and again to the highest elevations on the island." Again, on the Blooming-dale Road, between Bloomingdale village and Manhattan-ville, where the rock rose seventy feet above the Hudson, the whole surface, over four thousand square feet, was scored with grooves from half an inch to an inch in depth, from one to six inches in width, and from forty to sixty feet in length. North of this were many more, some reaching three inches in depth, so that, in fact, for thousands of feet over the rock at the water's edge and on the highest points he records the omnipresent grooves.
Grooves are yet traceable on the rock shoulders above Mofningside Park, south of 118th and 120th Streets, but strong channelings are reported from 163d Street and St. Nicholas Avenue.
Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York
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