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Isoseismal lines are then drawn to link together areas of equal shaking.
The isoseismal lines for the earthquake were poorly defined, due to variations both in topography and ground conditions.
Davison, C. (1921) On scales of seismic intensity and on the construction of isoseismal lines.
The isoseismal lines for the earthquake are elongated in a north-south direction, parallel to the strike of the Kaurik-Chango Fault Zone.
Wörterbuch der geographischen Begriffe