They bear little relation to the isoseismal lines. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The only complete map of the isoseismal lines is that drawn by. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Outside the isoseismal 4, the earthquake was observed at several places. From Wordnik.com. [A Study of Recent Earthquakes] Reference
It will be noticed that large portions of them, and especially of the isoseismal. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Fig. 19 shows the principal isoseismal lines as drawn by the Italian commissioners. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The curves in Fig. 16 represent the isoseismal lines as drawn by Dr. Johnston-Lavis. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Except towards the west, however, the course laid down for the isoseismal 7 may be trusted. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The curve for the first degree (A) coincides of course with the isoseismal line of intensity. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The isoseismal lines as drawn by Dr. Johnston-Lavis are represented by the curves in Fig. 15. From Wordnik.com. [A Study of Recent Earthquakes] Reference
It is similar in form to the second isoseismal, reaching as far as Estepone to the south-west. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The land area disturbed by the earthquake and the different isoseismal lines are shown in Fig. 41. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Secondly, it will be noticed (Fig. 60) that the isoseismal lines are not equidistant from one another. From Wordnik.com. [A Study of Recent Earthquakes] Reference
It will be seen that there is a certain rough correspondence between these curves and the isoseismal lines. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The error, however, is probably small, and we may therefore regard the isoseismal 6 as another ellipse, 141 miles long. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The region in which the slip took place may be determined roughly from the position and form of the innermost isoseismal. From Wordnik.com. [A Study of Recent Earthquakes] Reference
On the map in Fig. 60, the continuous curves represent isoseismal lines corresponding to the degrees 8, 7, 6, 5, and 4 of the. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The next isoseismal (2) marks the area of partial, but still serious, destruction; this is nearly 2 miles long from east to west. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Wherever the necessary conditions prevailed, they were found to be numerous over a district bounded approximately by the isoseismal 1. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Making use of these observations, Professor Omori has drawn two isoseismal lines within the central district, which are shown in Fig. 44. From Wordnik.com. [A Study of Recent Earthquakes] Reference
For instance, the scale of intensity used in drawing the isoseismal lines was not adopted until after the first letters of inquiry were issued. From Wordnik.com. [A Study of Recent Earthquakes] Reference
It is but rarely that the absolute intensity at any point of an isoseismal line can be ascertained, and only one example is given in this volume. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The next isoseismal (2) includes the places in which some buildings were ruined, but not as a rule completely, and in which there was no loss of life. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Mercalli is probably more trustworthy, it is interesting to compare his isoseismal lines with those obtained by his French colleagues, which are reproduced in Fig. 20. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The members of both the French and the Italian Commissions agree in ascribing the peculiar form and relative positions of the isoseismal lines to geological conditions. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Outside the isoseismal 5, there are but few records of the earthquake-sound; but it was heard faintly at Skelmorlie (in. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The land-area disturbed by the earthquake and the isoseismal lines are shown in Fig. 25, the small black oval area (which Includes. From Wordnik.com. [A Study of Recent Earthquakes] Reference
The curve D and the isoseismal. From Wordnik.com. [A Study of Recent Earthquakes] Reference
On the whole, the curve B and the isoseismal. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Within the isoseismal. From Wordnik.com. [A Study of Recent Earthquakes] Reference
Epicentral isoseismal lines of. From Wordnik.com. [A Study of Recent Earthquakes] Reference
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