The geometrical form of volcanic cones and the elastic limit of lava
The geometrical form of volcanic cones and the elastic limit of lava
复制标题
火山锥的几何形态与熔岩的弹性极限
DOI:
10.2475/ajs.s3-30.178.283
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发表时间:
1885
影响因子:
2.9
通讯作者:
G. Becker
中科院分区:
文献类型:
--
作者:
G. Becker
General character of a volcanic cone.-If a fluid or partially fluid substance, such as lava, issues from an orifice in a plain and congeals about the mouth, the accumulation will form,an elevated mass more or less nearly reselllbling a cone. If the resistance of this solid at the base is greater than the load, matter will or may continue to accumulate on the upper pore tion, while if the resistance towards the base is smaller than the load, a readjustment of material will necessarily take place. It is to be inferred, therefore, that under favorable circumstances volcanic cones will approximate to some definite form, and this inference is strengthened by the well known fact that the form of craters has been closely imitated by experiments on plastic material. Observation, too, shows that volcanic cones are char· acterized by a remarkable regularity of outline and that the outlines of the more regular cones of volcanoes wherever observed are strikingly similar. Milne's results.-Professor John Milne has discussed the form of volcanic cones,* but his papers have not received the attention they deserve, containing, so far as I know, the first attempt to assign a definite geometrical form to a natural surface.t Though his papers are cited in some recent works on geology, I have seen no reference to this fact and it had entirely escaped my own attention until the material for a paper on the subject was completed. My results are closely