Ralph Stockman Tarr

Biographical details

Portrait of Ralph Stockman Tarr Ralph Stockman Tarr,  1911 Encyclopædia Britannica, Volume 12… (1911)

“ The main river has cleft the plateau in a huge gash; innumerable side gorges have cut it to right and left; and weathering has etched out the cliffs and crags and helped to paint it in the gaudy colour bands that stretch before the eye. There is grandeur here and weirdness in abundance, but beauty is lacking. Powell puts the case graphically when he writes: “A wall of homogeneous granite like that in the Yosemite is but a naked wall, whether it be 1000 or 5000 ft. high. Hundreds and thousands of feet mean nothing to the eye when they stand in a meaningless front. ”
Source: Wikisource

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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