On March 27, 1964, the Great Alaskan earthquake off Anchorage, Alaska, set in motion local landslide tsunamis, as well as a trans-Pacific wave. The tsunami wave travel time to Crescent City was 4.1 hours after the earthquake, but it only produced localized flooding. The second and third waves to hit Crescent City were smaller, but the fourth wave struck with a height of approximately after having drawn the harbor out nearly dry. The next morning the damage was counted: 289 buildings and businesses had been destroyed; 1,000 cars and 25 large fishing vessels had been crushed; 12 people were confirmed dead, over 100 were injured, and more were missing; and 60 blocks had been inundated, with 30 city blocks destroyed. Although most of the missing were later accounted for, not all were tracked down. Insurance adjusters estimated that the city received more damage from the tsunami on a block-by-block basis than did Anchorage from the initial earthquake.
On March 27, 1964, the Great Alaskan earthquake off Anchorage, Alaska, set in motion local landslide tsunamis, as well as a trans-Pacific wave. The tsunami wave travel time to Crescent City was 4.1 hours after the earthquake, but it only produced localized flooding. The second and third waves to hit Crescent City were smaller, but the fourth wave struck with a height of approximately after having drawn the harbor out nearly dry. The next morning the damage was counted: 289 buildings and businesses had been destroyed; 1,000 cars and 25 large fishing vessels had been crushed; 12 people were confirmed dead, over 100 were injured, and more were missing; and 60 blocks had been inundated, with 30 city blocks destroyed. Although most of the missing were later accounted for, not all were tracked down. Insurance adjusters estimated that the city received more damage from the tsunami on a block-by-block basis than did Anchorage from the initial earthquake.