Rate of Recession of Niagara Falls
Rate of Recession of Niagara Falls
复制标题
尼亚加拉大瀑布的衰退速度
DOI:
10.1086/278833
复制
发表时间:
1907
期刊:
影响因子:
--
通讯作者:
D. W. Johnson
中科院分区:
文献类型:
--
作者:
D. W. Johnson
542 THE AMERICAN NATURALIST[VoL. XLI receding upstream, that the gorge below the falls is the result of this recession, and that it would be possible, by sufficiently accurate observations, to determine the rate of recession. He then discusses the data upon which computations of the rate of recession must be based, consisting of surveys of the crest-line of the falls made in 1842, 1875, 1886, 1890, and in 1905; and camera-lucida sketches made in 1827. After considering the relative accuracy of the different surveys and sketches, and platting the results together, the author concludes that a gradual recession of the Horseshoe Falls is demonstrated, while a much slower rate of recession is indicated for the American Falls. These changes are strikingly represented by contrasted photographs and sketches made from the same view-point, but many years apart. Concerning quantitative results of the study, the author points out that the available data may be treated in a variety of ways, and made to yield widely divergent results. The lack of harmony is due iin part to inaccuracies in the surveys, some of which are unavoidable; and in part to the fact that the rate at which the limestone crest breaks away is necessarily irregular. Too much confidence should not, therefore, be placed in exact mathematical expressions of the rate of recession. In general, however, the evidence proves a recession of about 5 feet a year with a possible error of not more than 1 foot, for the Horseshoe Falls, in the sixty-three years from 1842 to 1905; and a recession of less than 3 inches a year for the American Falls, in the seventy-eight years from 1827 to 1905. The time consulme (1 in the total recession of the falls from their former position near Lewiston is not considered in this report, except that the author briefly notes some of the many variable factors which must be taken into account in estimating such time. A short report by W. Carvel Hall on the latest survey of the crest line of the falls is appended to the paper.