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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
222
GEOLOGY OF NEW YORK CITY
bridges. It was substantially vegetable residues, generally homogeneous, and inclosing in spots flattened twigs and small branches, while, in its upper layers roots, tendrils, and in­numerable fibers appeared. It formed a brown body, deeply carbonized in black streaks, and drying to a board-like, leath­ery fabric, hard, feebly elastic, and tenacious. The accom­panying diagram shows its distribution and thickness (fur­nished by the Degnon Construction Co.). It reached a depth of over forty feet in some sections, rested on clay, was cov­ered by filling, and occupied saucers and pockets which may have been previously water-excavated gullies and basins. Mr. H. Cleary (assistant engineer) described the conditions as follows:
" The peat varies in depth (from 4 inches to 25 feet), and in composition depending upon its location in the pond. That in the Leonard Street area is deep (25 feet maximum), dense, brownish-black, fibrillous, and nearly homogeneous in texture, having a very slight odor, and appears to have been displaced by the gravel filling deposited upon it. That in the peripheral area at northerly and southerly limits of pond is shallower, fairly uniform (3 feet to 4 feet) in depth, and nearly level, is tan colored, odorless, dense, and fibrillous with horizontal lamination, containing roots, twigs, branches, leaves, and logs in a partial state of decomposition, but very compactly embedded in the peat. At northern area of pond many cedar stumps and roots in situ were found in a very slightly decomposed state, but compactly imbedded in the peat. The peat rested directly upon blue clay, into which the rootlets had freely penetrated and were visible passing into the sand below the clay in a flattened and decomposed state. The clay varies under the central and southerly areas of the pond from several feet to a few inches in depth, being uniformly about two feet thick under northerly pond area of tan colored peat.
" This pond was filled in during the years 1800 to 1834 to the level of the street surface. Mean water level stands at
Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York
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