The adjacent map shows expected levels of tsunami encroachment to Valdez depending on the type of tsunami.
Yellow is the current highest high tides. Scenario's 1-6 signify an underwater sluf of shelf falling into deeper waters. Scenario's 13-15 are typical fault slips occurring in Prince William Sound or the Gulf of Alaska.
september 3, 1899, 7.9 Cape Yakataga earthquake, There was also a report stating that a ship, docked near the Lowe River in 12 m (40 ft) of water, could not anchor at the same spot with 60 m (200 ft) of cable after the earthquake (Coulter and Migliaccio, 1966), which suggests there was a significant submarine landslide at this location.
february 14, 1908, round shaking in Valdez lasted two minutes from this MS6.0 earthquake Grant and Higgins, (1913, p. 12) found that several submarine cables were broken, and concluded that this was due to slumping of the delta front. The cables were broken close to the city of Valdez, inside Valdez Narrows. Locations of the breaks are shown in figure 4. In addition, the steamer Northwestern, while approaching the dock, encountered a ‘tidal wave’ large enough to make the boat rock very perceptibly
september 21, 1911 This MS6.9 earthquake had an epicenter beneath western Prince William Sound. …during this earthquake the submarine cable from Valdez to Sitka was broken This is almost exactly at one of the locations where the cable was broken during the earthquake of February 14, 1908.
january 31, 1912, The MS7.2 earthquake occurred in the middle of Prince William Sound (Doser, 2006). The submarine cables were again broken in Port Valdez.
february 23, 1925 ,A part of the dock collapsed into the bay, and an unusual wave accompanying the tremors tore up a section of the boardwalk along Water Street. The submarine cables were broken again
march 27, 1964, The Mw9.2 Alaska earthquake of 5:36 p.m. March 27, 1964, at Valdez was characterized by a strong, rapid, rolling motion lasting from three to five minutes, during which people had great difficulty standing. The ground surface was heaving and subsiding like a swell in the open ocean, except more frequent and rapid. The great disaster during the earthquake happened in the dock and harbor area, where a massive submarine landslide generated a tsunami, inundating the waterfront up to two blocks inland. The slide and slide-generated waves were responsible for the deaths of 30 people at the city dock. Two men were killed by falling cargo and another died because of a heart attack.
The second wave crossed the waterfront 10–15 minutes after the first wave, carrying a large amount of the debris.
Shortly after the first and second waves, a tectonic tsunami caused by the seafloor deformation in Prince William Sound and Gulf of Alaska started to approach Port Valdez. After the first 25 minutes, waves reaching Valdez were on the low tide and not high enough to be noticed by the Valdez residents, and could possibly fail to reach a normal hightide level (Wilson and Tørum, 1972). With the tide rising throughout the entire evening, activity of the tectonic waves became more destructive. Most notably the so-called third wave, between 10:30 p.m. and midnight on March 27, and the fourth wave, between 12:30 a.m. and 1:45 a.m. the following morning, flooded the city. Most likely the crests of the third and the fourth wave occurred around 11:45 p.m. and 1:35 a.m., respectively (Wilson and Tørum, 1972). Since the tectonic tsunami became superimposed with the high tide, the third wave reached 0.76 m (2.5 ft) above ground in the Valdez Hotel on McKinley Street and most likely reached Hobart Street at 11:45 p.m. Water from the fourth wave, nearly coincident with the predicted high tide, was 1.5–1.8 m (5–6 ft) deep in buildings along McKinley Street and 0.6 m (2 ft) deep on Hobart Street. Since the final wave left water marks on building exteriors several inches higher than the interior water marks, it was concluded that the final wave advanced and receded with considerable speed.
The highest location obliterated by waves was near the large, abandoned Cliff Mine. According to Plafker and Mayo (1965), the waves deposited driftwood at points 52 m (170 ft) above sea level and splashed silt and sand up to an elevation of 67 m (220 ft). Directly across from the Cliff Mine in Anderson Bay at the south shore of Port Valdez, the waves ran up to 24 m (78 ft) above the water level and destroyed a small fishing camp. All structures of the camp were swept away, leaving only the driven piling foundations. Its sole inhabitant, Harry Henderson, was missing and presumably drowned in the violent local waves that struck Anderson Bay.