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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                       41
to much disturbance or a long transportation by water. The quantity was so considerable as to defray by sale the actual expense of the contractor. Again, on Broadway, at the corner of Ann Street, the beds of sand excavated for the foundations, first, of the Herald building (1870), and later of the St. Paul (1896), were of remarkable depth.
Accumulations of sand in heavy and extended beds were' encountered in Elm Street during the construction of the Rapid Transit Subway, beds which were continued northward through Lafayette Place, at Astor Place, through lower 4th Avenue, and up to Union Square. Rock ledges were pene­trated beyond this point, revealing on the line, as at 23d Street, subsidences filled with sand, clay, and surficial fillings.
Again, on the track of the Subway beyond or north of 134th" Street very deep hills of sand were entered, themselves par­tially separable by a color line.
Seldom in excavations of the size of that made for the new Wanamaker store has the nature of the soil proved so advan­tageous to the contractors. In the plot excavated, extending along the entire front on 4th Avenue and back on 8th and 9th Streets about 200 feet, not one stone has been encountered which was large enough to require a drill to dislodge it.
That the soil generally was of clay and sand was known before actual operations were begun, borings to a depth of 25 feet having been made over almost the whole area. Another feature, which has greatly facilitated the work, is the fact that at a depth of about 35 feet below the street level there is an almost solid layer of rock. As the depth of the foundation is to be 25 feet, it has been an easy matter to sink the 161 caissons necessary to support the fourteen-story building the remaining 10 feet to this solid rock.
It has been usual to regard this assortment of beds of sand, clay and gravel as entirely quaternary, or derived from drift. The actual confusion of material originating in the sub-aerial erosion and weathering of the rocks of the island, with the glacial material pushed down over these rocks, and partially
Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island
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