The earthquake of 97/02/10 04:26 UTC was recorded on a strong motion instrument located at the University of Washington. The recording station was approximately 10.8 km from the earthquake epicenter and at an azimuth of 356 degrees. Shown below are the east-west, north-south, and vertical component time histories of ground acceleration. Peak values are also listed at the right side of each seismogram. The north component recorded a peak ground acceleration of 4.42e-4 g (442 micro-g).