But if the disturbance affects a huge are nota, as a outstanding earthquake can, the resulting seismic sea waves nay beHAs as if them had be generated by oneself a line ratIT than at a point.

• 但是，假如扰动阻碍的地区很大，象强烈震地所能做到的，那末所产生的震地海浪运动好象沿直线产生而否则在一点产生。