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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
28               GEOLOGY OF NEW YORK CITY
(Lispenard's creek) with the famous Collect (Kolck) pond, a depressed and bog-like pond on the present site of the Tombs in Centre Street. The Tombs, fifty years ago known as " The Hall of Justice," stands about at the center of this old pond, or lake, a celebrated resort for winter pastimes, and referred to by its contemporaries as " a beautiful sheet of water."
Further north, at the foot of Rivington,* Grand, Houston, 5th, 7th, 10th and 30th Streets, the edges of the island were eroded and frayed by a variable fringe of marshes. The is­land area has been almost everywhere below 14th Street added to by artificial enlargements, and these extensions of filled land have been, all along its southern limits, quite consid­erable.
The present Battery Park is made land. Greenwich Street, on the west side, was the former boundary of Manhattan Is­land, and the line of Water Street the limit on the east. The rapid currents of both the Hudsott and East Rivers probably existed to even a greater degree in "the past than they do to­day, and to their wearing and tearing down the unconsolidated strata on either side, and their convergence at the south, is due the triangular extremity of the island and its contracted area. Below Barclay Street, on the North River, the rock is met sloping toward the river, but in other places the mud, tenacious and rigid, forms an almost impenetrable layer over the bottom.
The present borders of the Harlem River illustrate the growth upward of mud flats, and it was over such surfaces that the filled-in areas about New York were made. They are lifted gradually toward the water level by slow accumulations of sediment. They are invaded by grass (Spartina patens, Ait), which, growing thicker and thicker, entraps more and more silt, and gradually creates a land surface below the water, to become a widely extended swamp-bed. Such
*Here were Marinus Willet's and Stuyvesant's Meadows, where, by common repute, at Burnt Hill Point, Manhattan Island, or Dry Dock, Kidd and Blackbear buried their treasure. The meadows were a mile along the shore.
Ch. 2: Manhattan Island Page of 281 Ch. 2: Manhattan Island
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