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Examples

  • The mean surface-velocity between the two inner coseismals is therefore 2,882 feet per second, and between the two outer ones 3,095 feet per second.

    A Study of Recent Earthquakes Charles Davison 1899

  • The mean surface-velocity of 2,955 feet per second between the first and third coseismals is probably, however, the most accurate estimate of the surface-velocity yet made in a slight earthquake.

    A Study of Recent Earthquakes Charles Davison 1899

  • Now, the average distance between the two inner coseismals is 32-3/4 miles, between the two outer ones (so far as drawn) 35-1/6 miles, and between the first and third 67-1/6 miles.

    A Study of Recent Earthquakes Charles Davison 1899

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