Usage examples (7)

• With evidence so abundant, a new method of drawing coseismal lines becomes possible.
• The coseismal lines obtained in this manner are represented by the continuous curves in Fig. 62.
• The curves separating these zones would be coseismal lines corresponding to the times 5. 32-1/2, 5. 33-1/2, and
• In the Hereford earthquake of 1896, the centre of the innermost coseismal line (Fig. 62) is close to the region lying between the two epicentres.