Ralph Stockman Tarr

Ralph Stockman Tarr

Summary

Portrait of Ralph Stockman Tarr Ralph Stockman Tarr 1911 Encyclopædia Britannica (1911)

Although the river freezes in the winter, so that ice-boating is a favourite winter sport, the summer climate is warm enough for the cultivation of grapes and other fruits, which is aided to a considerable extent by the influence of the large body of water enclosed between the valley walls, which tends to retard both early and late frosts, and thus to extend the growing season. In addition to smaller towns and villages, there are a number of larger towns and cities, including Hudson and Catskill, nearly opposite each other, and farther down Kingston and the thriving city of Poughkeepsie.
Source: Wikisource

Portrait of Ralph Stockman Tarr Ralph Stockman Tarr 1911 Encyclopædia Britannica (1911)

The third and lowest section of the tidal part of the Hudson extends from the lower end of the Highlands to New York Bay. This is a region of ancient and metamorphic Paleozoic rocks on the eastern side, and mainly Triassic rocks on the west. Because of their less resistance to denudation, these rocks have permitted a broadening of the valley in this part of the course. Just below Peekskill the river broadens out to form Haverstraw Bay, at the extremity of which is the headland of Croton Point.
Source: Wikisource

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