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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
EVIDENCES OF GLACIATION                209
laden and boulder-invested mass can be easily studied. Such an exposure of the moraine is well shown to-day in an inter­section of it by Underhill Avenue, north of the water-tower, at the west entrance to Prospect Park (Fig. 49). Let the observant teacher take the class to the Grassmere station on the Staten Island Railroad, and, walking south and east, surmount one of the many intermingling hills which cover this region and which, almost treeless, reproduce a moor-like expanse, over which the eye or the feet can wander with tire­less interest.
The visitor to this peculiar region not devoid, even in its barrenness, of a certain scenic charm, must not draw the inference that the rising and falling land, spread before him in hill and valley, represents the appearance which it bore when the ice, finally retreating, left it a heavy and high ridge of débris. It was then far higher, more dike-like, and with a more approximately regular surface. Rains have torn down this rampart, and drainage lines becoming established, the whole original wall has been divided up into low, pyramidal hills. The morainal matter has here undergone some réas­sortiment by water washing, and clay and sand-layers indicate a partial re-sifting and re-sedimentation. There are few large boulders, and the coarse, gravelly, and stony soil supports a meager vegetation.
There is much in this Fox Hill region, on Staten Island, which partakes of a kettle morainic physiognomy, that is, there may have been dislodged or separated fields or pinnacles of ice here, which melted away, and heaped up circumvallating walls of rubble around their vanishing sides.
This terminal moraine touches the shore of Staten Island at Princess Bay, where about one-half a mile from the Den­tal Works the exposed face of the morainal hill is well shown under the lighthouse, broached by storms and exposing its stony contents. It is a hill of gravel, sand, and earth, with but few large boulders which, occasionally released, lie scattered over the beach. The highest point is at the lighthouse, where
Appendix I: Glaciation in Great New York Page of 281 Appendix I: Glaciation in Great New York
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