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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                        43
such swamps as Collect Pond developed. This pond had ap­parently itself undergone oscillations in its level, as Cozzens speaks of the soft mud from its bottom being charged with salt, as if the channel waters had entered it. The depression of land allowed the rapid currents of the two encircling rivers to attack the drift debris, loading the inland portions of the island, and in conjunction with its own drainage form these beds of sand, gravel and clay which, again upon re-elevation, were again disturbed and submerged, to be covered by later beds, until the island assumed its present status. What strik­ing changes may have been produced by still greater elevations will be described in the resume of this article. The nature of the boulders found in this portion of the " drift" is men­tioned in the accompanying paper on the " Evidences of Gla­cial Action," etc.
The increasing number of very high buildings (" sky­scrapers ") in the lower districts of Manhattan Island has re­sulted in enlarged and more detailed acquaintance with the surface conditions above the floor rock, though the general expression and succession is identical, or but slightly varied throughout, at all the new basements. Some of these extend downward to considerable depths. In the Commercial Cable building (Broad and New Streets) the cellar floor is sixteen feet below the water-level, in the Mutual Life extension (Cedar Street) the cellar is thirty-two feet below the water-level. Messrs. Weiskopf & Stern, engineers of the City Investing building, furnished the following interesting statement:
"The soil under this building is a very fine sand mixed with very soft loam, and is almost of a uniform character from the top to hard pan. We encountered hard pan at a depth of about 65 feet below what we term 'curb A,' which is the curb level on Church Street, at the south side of the lot, and which curb is about 9 feet lower than the Broadway curb in front of this building. The mean low-water level is about —17 feet with reference to curb A, and the level of the boiler-room floor is 21 to 21 1-2 feet below curb A. The building is founded
Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island
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