3. 重力異常と地下構造との關係(VII) : 山の高さと地殼均衡
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概要
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Using the gravimetric data obtained in Japan, the East Indies and in U.S.A., it was found that whether a mountain is in an isostatic equilibrium or not depends not only on the horizontal span of that mountain, but also on its height above the sea level. Most mountains that are higher than a. few hundred meters are, at least in the three regions studied, in isostatic equilibrium irrespective of the magnitudes of their horizontal spans. Various estimates of the lowest height of a mountain that cannot be supported by the elasticity of the earth's crust agree in giving a value of a few hundred meters.
- 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
- 1942-03-30
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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