First
photo in a series of three sequential photos show the arrival
of a major wave at Laie Point on the Island of Oahu, Hawaii about
3,600 km from the source. Photograph Credit: Henry Helbush. Source:
National
Geophysical Data Center.
The Island of Kauai, Hawaii, was hit twice as hard by this tsunami
than by the Aleutian Islands tsunami in 1946. Houses were washed
out and destroyed at Wainiha and Kalihiwai. At Haena, the waves
reached heights of 16 m. In addition to that bridges were destroyed
and sections of highways were flooded. At Hilo, Hawaii, the run-up
was reached 3.9 m and damaged buildings. In Hilo Bay, Cocoanut
Island was covered by 1 m of water and the bridge connecting it
to shore was destroyed.
Second
photo in a series of three sequential photos show the arrival
of a major wave at Laie Point on the Island of Oahu, Hawaii. Photograph
Credit: Henry Helbush. Source: National
Geophysical Data Center.
Although the northwest side of the Hawaiian Islands received high
levels of water, the rest of the islands only received elevated
water levels on average of 2 to 3 m. Both the 1946 and 1957 tsunamis
occurred in the same general location (the Aleutian Islands).
Even though the 1957 earthquake released more energy than the
earthquake of 1946. The tsunami generated by this 1957 event caused
less damage than the tsunami of 1946. This uncertainty of the
potential destructive power of a tsunami forces Pacific
Tsunami Warning System to issue warnings even when a tsunami
may have little or no effect.
Third photo in a series of
three sequential photos show the arrival of a major wave at Laie
Point on the Island of Oahu, Hawaii. Photograph Credit: Henry
Helbush. Source: National
Geophysical Data Center.