Significant earthquakes of 1964

March 28, 1964 Earthquake: Alaska, United States

March 28, 1964 · M9.2 · 139 deaths · $400 million

A magnitude 9.2 earthquake struck Alaska, United States on March 28, 1964 at 03:36:16 UTC, 25 km below the surface. It killed 139 people, counting the tsunami it caused.

Map

Where it struck, with the other significant earthquakes within 200 km. Circles are sized and colored by magnitude; select one for its page.

The earthquake

Date
March 28, 1964
Time
03:36:16 UTC
Place
Alaska, United States
Magnitude
9.2 (Mw)
Focal depth
25 km (16 mi)
Intensity
10 on the Modified Mercalli scale
Epicenter
60.908° N, 147.339° W

The toll

Deaths
15; 139 with its tsunami and other effects
Damage
$284 million; $400 million with its tsunami and other effects
Houses destroyed
Many (101 to 1,000)

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

1964, March 28. This magnitude 9.2 Mw earthquake and ensuing tsunami caused 139 deaths and $400 million in property loss. The earthquake caused 15 deaths and the tsunami caused 124 deaths (106 in Alaska, 13 in California and 5 in Oregon).

Ref #542:

1964, March 28, 1964, 03:36:14 UTC. 61.04 N, 147.73 W, depth 33 km, magnitude 8.4 MS, intensity X. Prince William Sound, Alaska. This great earthquake and ensuing tsunami took 125 lives (tsunami 110, earthquake 15), and caused about $311 million in property loss. Earthquake effects were heavy in many towns, including Anchorage, Chitina, Glennallen, Homer, Hope, Kasilof, Kenai, Kodiak, Moose Pass, Portage, Seldovia, Seward, Sterling, Valdez, Wasilla, and Whittier.

Anchorage, about 120 km northwest of the epicenter, sustained the most severe damage to property. About 30 blocks of dwellings and commercial buildings were damaged or destroyed in the downtown area. The J.C. Penney Company building was damaged beyond repair; the Four Seasons apartment building, a new six-story structure, collapsed; and many other multistory buildings were damaged heavily. The schools in Anchorage were almost devastated. The Government Hill Grade School, sitting astride a huge landslide, was almost a total loss. Anchorage High School and Denali Grade School were damaged severely. Duration of the shock was estimated at 3 minutes.

Landslides in Anchorage caused heavy damage. Huge slides occurred in the downtown business section, at Government Hill, and at Turnagain Heights. The largest and most devastating landslide occurred at Turnagain Heights. An area of about 130 acres was devastated by displacements that broke the ground into many deranged blocks that were collapsed and tilted at all angles. This slide destroyed about 75 private houses. Water mains and gas, sewer, telephone, and electrical systems were disrupted throughout the area.

The earthquake was accompanied by vertical displacement over an area of about 520,000 km2. The major area of uplift trended northeast from southern Kodiak Island to Prince William Sound and trended east-west to the east of the sound. Vertical displacements ranged from about 11.5 m of uplift to 2.3 m of subsidence relative to sea level. Off the southwest end of Montague Island, there was absolute vertical displacement of about 13-15 m. Uplift also occurred along the extreme southeast coast of Kodiak Island, Sitkalidak Island, and over part or all of Sitkinak Island. This zone of subsidence covered about 285,000 km2, including the north and west parts of Prince William Sound, the west part of the Chugach Mountains and a part of the lowlands north of the mountains, most of Kenai Peninsula, and almost all the Kodiak Island group.

This great earthquake was felt over a large area of Alaska and in parts of western Yukon Territory and British Columbia, Canada.

Ref #10476, v.10:

1964 March 28 03:36:16 UTC, 60.908 N 147.339 W, 25 km depth, 9.3 Mw

Ref #13456 (access date 2023):

1964 March 28 03:36:16 UTC, 60.908 N 147.339 W, 25 km depth, 9.2 Mw

Ref #1314:

1964, March 28. 8.4 MS, 9.2 Mw.

Ref #88:

1964, March 28, 03:36:13 UTC. 61.1 N, 147.6 W, depth 20 km, magnitude 8.5 MS.

Reference #1250:

1964, March 28. 131 killed, $1020 million damage.

Ref #45:

1964, March 27 17:36:14.2. Maximum intensity IX-X. Civil defense estimates included 122 deaths from the tsunami and 9 from the earthquake. Total damage from the earthquake and tsunami was between $400-$500 million.

Ref #3381:

Public and private property damage exceeded 300 million dollars, but there were only 114 casualties.

Ref #2102:

The tsunami generated by the Prince William Sound Earthquake of March 28, 1964, was the largest since the 1960 Chilean tsunami.. 122 fatalities and over $104 million in damage resulted...

Photos

From the NCEI/WDS Natural Hazards Image Database (doi:10.7289/V5154F01). Only photos by the USGS and NOAA, which are public domain, are shown.

Uplifted dock, Prince William Sound, Alaska
Uplifted dock, Prince William Sound, Alaska The uplifted dock on Hinchinbrook Island, Prince William Sound, shows uplift. Land in this area rose about 8 feet (2.4 m) during the earthquake, and the dock could then be used only at extremely high tides. Tsunami damage also occurred in this area. Photo: U.S. Geological Survey.
Subsidence at Portage, Alaska
Subsidence at Portage, Alaska The village of Portage, at the head of Turnagain Arm of Cook Inlet, is flooded at high tide as a result of 6 feet (1.8 m) of tectonic subsidence during the earthquake. After the quake, the shoreline was as much as 2 miles (3.4 km) inland from the pre-earthquake mean shore line. The town of Portage was inundated and covered with a blanket of silt. Much of… Photo: U.S. Geological Survey.
Hanning Bay Fault Scarp, Alaska
Hanning Bay Fault Scarp, Alaska This view is looking southwest along the Hanning Bay fault scarp on southwest Montague Island in Prince William Sound. The Hanning Bay fault was reactivated during the earthquake. Its trace is marked by a 10- to 15-foot high (3.0 m to 4.5 m) bedrock scarp which trends obliquely across the field of view from the right foreground to the left background. The… Photo: U.S. Geological Survey.
Underwater Landslides at Seward, Alaska
Underwater Landslides at Seward, Alaska This view, taken a few months after the earthquake, is looking north along the waterfront at Seward. Note the 'scalloped' shoreline left by the underwater landslides, the severed tracks in the railroad yard which dangle over the landslide scarp and the heaps of railroad cars and other debris thrown up by the tsunami waves. This massive submarine landslide… Photo: U.S. Geological Survey.
Government Hill Landslide, Anchorage, Alaska
Government Hill Landslide, Anchorage, Alaska The Government Hill Elementary school in Anchorage was torn apart by subsidence of the graben at the head of the Government Hill landslide. The south wing of the school dropped about 30 feet (9 m); the east wind split lengthwise and collapsed. The playground became a chaotic mass of blocks and fissures. Part of this slide became an earthflow that spread… Photo: U.S. Geological Survey.
"L" Street Landslide, Anchorage, Alaska
"L" Street Landslide, Anchorage, Alaska A subsidence trough (or graben) formed at the head of the "L" Street landslide in Anchorage during the earthquake. The graben extends from the lower right corner of the picture to the upper left and passes beneath several houses. The slide block, which is the virtually unbroken ground to the left of the graben, moved to the left. The subsidence trough sank… Photo: U.S. Geological Survey.
Damaged Four Seasons Apartments Anchorage, Alaska
Damaged Four Seasons Apartments Anchorage, Alaska The Four Seasons Apartments in Anchorage was a six-story lift-slab reinforced concrete building which crashed to the ground during the earthquake. The building was structurally complete but unoccupied at the time of the earthquake. The main shear-resistant structural elements of the building, a poured-in-place reinforced-concrete stairwell and a combined… Photo: U.S. Geological Survey.
Scarp in "L" Street Slide, Anchorage, Alaska
Scarp in "L" Street Slide, Anchorage, Alaska A close-up of one of the scarps bounding the graben on the "L" Street landslide showing a house which was undercut by subsidence of the graben. The "L" Street slide began to move near the end of the tremor. It was a horizontal translatory slide and probably failed in sand layers or in soft sensitive clay in the area from Anchorage's Fifth Avenue South. Photo: U.S. Geological Survey.
Damage to Fourth Avenue, Anchorage, Alaska
Damage to Fourth Avenue, Anchorage, Alaska This view of damage to Fourth Avenue buildings in downtown Anchorage shows the damage resulting from the slide in this area. Before the earthquake, the sidewalk in front of the stores on the left, which are in the graben, was at the level of the street on the right, which was not involved in the subsidence. The graben subsided 11 feet (3.3 m) in response… Photo: NOAA National Geophysical Data Center.
Fourth Avenue Landslide Scarp, Anchorage, Alaska
Fourth Avenue Landslide Scarp, Anchorage, Alaska The scarp of the Fourth Avenue landslide in downtown Anchorage where two and one half blocks of shops, bars, and stores slowly settled until their entrances were below street level. The Fourth Avenue area showed evidence of earthquake-induced sliding before the 1964 earthquake. About 30 blocks of dwellings and commercial buildings were destroyed or… Photo: U.S. Geological Survey.
Turnagain Heights Landslide, Anchorage, Alaska
Turnagain Heights Landslide, Anchorage, Alaska This shows the Turnagain Heights landslide in Anchorage. Seventy-five homes twisted, slumped, or collapsed when liquefaction of subsoils caused parts of the suburban bluff to move as much as 2,000 feet (606 m) downward toward the bay, forming a complex system of ridges and depressions. The slide developed because of a loss in strength of the soils,… Photo: NOAA National Geophysical Data Center.
Fissured Highway Embankment, Alaska
Fissured Highway Embankment, Alaska This highway embankment fissured, spread and slumped on underlying alluvium. The road was built on thick deposits of alluvium and tidal estuary mud along Turnagain Arm of Cook Inlet near Portage, Alaska. These weakened deposits spread laterally away from the road center toward the edge of the embankment. This is the east approach to Twentymile River… Photo: U.S. Geological Survey.

Other significant earthquakes nearby

Within 200 km, the deadliest first.

More

Significant earthquakes of 1964The 1900sEvery quake the USGS located in 1964Recent earthquakes near hereThis day in weather history

Sources

Significant earthquakes from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI earthquake 4311.