Hostname: page-component-78c5997874-dh8gc Total loading time: 0 Render date: 2024-11-06T09:39:15.917Z Has data issue: false hasContentIssue false

III.—On the Theory of Vorticose Earthquake-Shocks

Published online by Cambridge University Press:  01 May 2009

Charles Davison
Affiliation:
Emmanuel College, Cambridge.

Extract

Earthquake-shocks have generally been divided into three classes:

a. Undulatory shocks, by far the most commonly felt, consisting of one or several waves, the movement at any place being to and fro along a line inclined to the horizon, but in general nearly horizontal.

b. “Sussultatore” shocks, consisting of one or more up-and-down movements, in a nearly vertical direction.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1882

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 257 note 1 Perrey, M.. “Liste les tremblements de terre ressentis pendant les années 1845 et 1848”: Mém. de l'Acad. de Dijon, 18451846.Google Scholar

page 257 note 2 Perrey, M.. “Note sur les tremblements de terre en 1858, etc.”: Mém. Cour. de l'Acad. Roy. de Belgique (1861)Google Scholar, Collection in 8vo. tome xii.

page 257 note 3 Perrey, M.. “Note historique sur les tremblements de terre des Antilles”: Comptes Rendus (12 12, 1843), vol. xvi. pp. 12831303.Google Scholar

page 258 note 1 Milne, Prof. J.. Letter on “Earthquake Vibrations”: Nature (12. 8, 1881), vol. xxv. p. 126.CrossRefGoogle Scholar

page 258 note 2 The above are notes of the principal shocks taken from the account by Father Faura of his observations and seismographic records at Manila: Proc. Roy. Soc. (12. 17, 1881), vol. xxxi. pp. 462–8.Google Scholar

page 258 note 3 Perrey, M.. “Note sur les tremblements de terre en 1857, etc.”: Mém. Cour. de l'Acad. Eoy. de Belgique (1860), Collection in 8vo. vol. x.Google Scholar

page 258 note 4 Perrey, M.. “Sur les tremblements de terre ressentis dans le bassin du Rhone”: Ann. de la Soc. Roy. d'Agric. de Lyon (1845), vol. viii. pp. 265370.Google Scholar

page 259 note 1 Mallet, Mr. R.. “The Neapolitan Earthquake of 1857,” vol. i. p. 76.Google Scholar

page 259 note 2 Perrey, M.. “Note sur les tremblements de terre en 1856, etc.”: Mém. Cour. de l'Acad. Roy. de Belgique (1859), Collection in 8vo. vol. viii.Google Scholar

page 260 note 1 Journal des Mines, vol. xii. pp. 95–96. Quoted by Perrey, M.. “Mémoire sur les tremblements de terre ressentis en France, en Belgique et en Hollande, etc.”: Mém. Cour. de l'Acad. Eoy. de Bruxelles, vol. xviii. p. 103.Google Scholar

page 260 note 2 Perrey, M.. “Sur les tremblements de terre ressentis dans le bassin du Rhone”: Ann. de la Soc. Roy. d'Agric. de Lyon (1845), vol. viii. p. 341.Google Scholar

page 260 note 3 If a disturbance take place at any point of a homogeneous and isotropic solid, two spherical waves will diverge from that point with unequal velocities. In the first every particle moves approximately along a line joining it to the centre of disturbance, and the corresponding wave is said to consist of direct vibrations. In the second the particles vibrate in planes perpendicular to the lines joining them to the centre of disturbance, and are said to execute transverse vibrations.

page 261 note 1 MrMallet, R.. “Neapolitan Earthquake of 1857,” vol. i. pp. 7678.Google Scholar

page 261 note 2 If a and b be the distances of the nearest and furthest points of the seismic focus from any place, V the velocity of the direct wave, v that of the transverse wave, and λ the length of the former; the two waves will not have separated before

page 264 note 1 On the Dynamics of Earthquakes,” Trans. Roy. Irish Academy (1846), vol. xxi. pp. 51105.Google Scholar

page 264 note 2 Naturalist's Journal” (1879), p. 308.Google Scholar

page 264 note 3 Neapolitan Earthquake of 1857,” vol. i. pp. 377–8.Google Scholar