川の波路の變遷によつて知り得たる伊賀國島ヶ原地塊の運動
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概要
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The longitudinal profile of a river has been regarded as a curve which resembles a hyperbola or exponential curve, tangent to the base level. A continuous profile of a graded river like this will break and tend to make a cusped point, if such kind of deformation as to make the gradient of the lower course from a point in it steeper than that of the iipper one, do occur. There are vertical movements as shown in Table I, 1-5, by Avhich cusped points will necessarily be formed.
- 東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,地震研究所の論文
- 1930-04-08
東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,地震研究所 | 論文
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