. Annual report of the Regents. New York State Museum; Science. 70 . NEW YORK STATE MUSEUM has been uninfluenced by preexisting relief features. (Fig. iC) Another feature of importance is the varying width of different parts of the gorge, and the corresponding increase in velocity of current in the narrower parts. The depth of the channel also varies in different portions of the gorge, being in general greater in the wider and less in the narrower parts. (Fig. i8). Fig. 16 Blrdseye view of Niagara gorge showing the course of the river; the falls, the railroad bridges, whirlpool, location of Fo
. Annual report of the Regents. New York State Museum; Science. 70 . NEW YORK STATE MUSEUM has been uninfluenced by preexisting relief features. (Fig. iC) Another feature of importance is the varying width of different parts of the gorge, and the corresponding increase in velocity of current in the narrower parts. The depth of the channel also varies in different portions of the gorge, being in general greater in the wider and less in the narrower parts. (Fig. i8). Fig. 16 Blrdseye view of Niagara gorge showing the course of the river; the falls, the railroad bridges, whirlpool, location of Fosters flats, escarpment at Queenston and flaring mouth of old St Davids gorge, (After Gilbert) The first mile and three fourths of the gorge, or that portion marking the retreat from the escarpment to the Devil's hole, extends nearly due south, and is fairly uniform in width, comparatively nar- row, and with a current of great velocity. The narrowness of this stretch, when compared with the channel made by the present cataract from the railroad bridges southward, seems to indicate a smaller volume of water during its formation than that now passing over the falls. An alternative hypothesis accounts for the narrow- ness of this section of the gorge by assuming it to be a preglacial drift-filled channel, made by an obsequent stream flowing north- ward to the Ontario lowland, similar to that which made the old St Davids channel, but reexcavated by the Niagara. It is highly probable that there was at least a shallow channel which served as. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original New York State Museum; University of the State of New York. Board of Regents. Albany : J. B. Lyon, State Printer
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Keywords: ., bookauthorne, bookcentury1800, bookdecade1880, booksubjectscience
