An earthquake occurred in Lituya Bay, Alaska, on July 9, 1958, at 22:15:58 PST (July 10 at 06:15:58 UTC) with a moment magnitude of 7.8 to 8.3 and a maximum Mercalli intensity of XI (Extreme). The strike-slip earthquake took place on the Fairweather Fault and triggered a rockslide of 30 million cubic meters (40 million cubic yards) and about 90 million tons into the narrow inlet of the bay. The impact was heard 80 kilometers (50 mi) away, and the sudden displacement of water resulted in a megatsunami that washed out trees to a maximum elevation of 524 meters (1,719 feet) at the entrance of Gilbert Inlet. This is the largest and most significant megatsunami in modern times; it forced a re-evaluation of large-wave events and the recognition of impact events, rockfalls, and landslides as causes of very large waves.
Lituya Bay is a fjord located on the Fairweather Fault in the northeastern part of the Gulf of Alaska. It is a T-shaped bay with a width of 2 miles (3 km) and a length of 7 miles (11 km). Lituya Bay is an ice-scoured tidal inlet with a maximum depth of 722 feet (220 m). The narrow entrance of the bay has a depth of only 33 feet (10 m). The two arms that create the top of the T-shape of the bay are the Gilbert and Crillon inlets and are a part of a trench on the Fairweather Fault.
In the past 172 years, Lituya Bay has had four tsunamis over 100 ft (30 m): 1854 (395 ft or 120 m), 1899 (200 ft or 60 m), 1936 (490 ft or 150 m), and 1958 (1,720 ft or 520 m).
Near the crest of the Fairweather Mountains sit the Lituya and the North Crillon glaciers. They are each about 12 miles (19 km) long and 1 mile (1.6 km) wide with an elevation of 4,000 feet (1,200 m). The retreats of these glaciers form the present "T" shape of the bay, the Gilbert and Crillon inlets.
The major earthquake that struck on the Fairweather Fault had a moment magnitude of 7.8 and a maximum perceived intensity of XI (Extreme) on the Mercalli intensity scale. The epicenter of the quake was at latitude 58.37° N, longitude 136.67° W near the Fairweather Range, 7.5 miles (12.1 km) east of the surface trace of the Fairweather fault, and 13 miles (21 km) southeast of Lituya Bay. This earthquake was the strongest in over 50 years for this region, since the Cape Yakataga earthquake on September 3, 1899, which was estimated to be magnitude 8.2 on the Richter scale. The shock was felt in southeastern Alaskan cities over an area of 400,000 square miles (1,000,000 km2), as far south as Seattle, Washington, and as far east as Whitehorse, Yukon, Canada.
The earthquake caused a subaerial rockfall in the Gilbert Inlet. Over 30 million cubic meters of rock fell from a height of several hundred meters into the bay, creating a megatsunami. The impact of the rockslide included the creation of wave run up that shaved up to 400m of ice off the front of the Lituya Glacier and eroded or completely eradicated its rocky deltas. After the earthquake it was observed that a subglacial lake, located northwest of the bend in the Lituya Glacier at the head of Lituya Bay, had dropped 100 ft (30 m). This proposed another possible cause to the production of the 100 ft (30 m) wave which caused destruction as high as 1,720 ft (520 m) above the surface of the bay as its momentum carried it upslope. The wave caused damage to the vegetation up the headlands around the area where the rockfall occurred, up to a height of 524 meters, as well as along the shoreline of the bay. It is possible that a good amount of water drained from the glacial lake through a glacial tunnel flowing directly in front of the glacier, though neither the rate of drainage nor the volume of water drained could produce a wave of such magnitude. Even if a large enough drainage were to take place in front of the Gilbert Glacier, the run-off would have been projected to be on the opposite side in Crillon Inlet. After these considerations it was determined that glacial drainage was not the mechanism that caused the giant wave.
The Lituya Bay megatsunami caused damage at higher elevations than any other tsunami, being powerful enough to push water up the tree covered slopes of the fjord with enough force to clear trees to a reported height of 524 m (1,719 ft). A 1:675 recreation of the tsunami found the wave crest was 150 m (490 ft) tall. Five people were killed, many people were injured, and many homes destroyed. Two people on a fishing boat died from a wave in the bay. Two more people, a fishing boat captain and his seven-year-old son, were struck by the wave and lifted high into the air by the swell. Remarkably, both survived with minimal injuries. In Yakutat, the only permanent settlement close to the epicenter at the time, infrastructure such as bridges, docks, and oil lines all sustained damage. A wave tower collapsed and a cabin was damaged beyond repair. Sand boils and fissures occurred near the coast southeast of there, and underwater cables that supported the Alaska Communication System were cut. Lighter damage was also reported in Pelican and Sitka. It ripped limbs off trees and swept many away, decimating the shoreline's surrounding forest and leaving the high tide line barren and with few upright surviving trees except on the northern and southern edges. The megatsunami flooded the entire bay and created a damage line up to 213 m (699 ft) around the outline of the bay, with evidence of this damage line still visible from space to this day.
At 22:15 hours PST on July 9, 1958, which was still daylight at that time of year, an earthquake with a magnitude of 7.8 struck the Lituya Bay area. The tide was ebbing at about plus 1.5 m and the weather was clear. Anchored in a cove near the west side of the entrance of the bay, Bill and Vivian Swanson were on their boat fishing when the earthquake hit:
With the first jolt, I tumbled out of the bunk and looked toward the head of the bay where all the noise was coming from. The mountains were shaking something awful, with slide of rock and snow, but what I noticed mostly was the glacier, the north glacier, the one they call Lituya Glacier. I know you can't ordinarily see that glacier from where I was anchored. People shake their heads when I tell them I saw it that night. I can't help it if they don't believe me. I know the glacier is hidden by the point when you're in Anchorage Cove, but I know what I saw that night, too. The glacier had risen in the air and moved forward so it was in sight. It must have risen several hundred feet. I don't mean it was just hanging in the air. It seems to be solid, but it was jumping and shaking like crazy. Big chunks of ice were falling off the face of it and down into the water. That was six miles away and they still looked like big chunks. They came off the glacier like a big load of rocks spilling out of a dump truck. That went on for a little while—it's hard to tell just how long—and then suddenly the glacier dropped back out of sight and there was a big wall of water going over the point. The wave started for us right after that and I was too busy to tell what else was happening up there.
When the earthquake struck, Howard G. Ulrich and his 7-year-old son were in Lituya Bay aboard their boat, the Edrie. They were anchored in a small inlet on the southern side of the bay. The two had gone out on the water at 20:00 hours PST and when the earthquake hit, the resulting rocking of his boat woke Ulrich up. He observed the wave's formation from the deck, hearing a very loud smash at the base of Lituya Bay. In his record of the wave he notes the appearance of it and how it formed:
The wave definitely started in Gilbert Inlet, just before the end of the quake. It was not a wave at first. It was like an explosion, or a glacier sluff. The wave came out of the lower part, and looked like the smallest part of the whole thing. The wave did not go up 1,800 feet, the water splashed there.
The wave made its way to his boat 2–3 minutes after he saw it and carried the Edrie down to the southern shore and then back near the center of the bay. Ulrich was able to control the boat once the main wave passed, maneuvering through subsequent waves up to 20 ft high until he could finally exit the bay.