1906 San Francisco earthquake

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"San Francisco earthquake" redirects here. For the 1989 earthquake, see 1989 Loma Prieta earthquake. For the 2014 earthquake, see 2014 South Napa earthquake.

1906 San Francisco earthquake
1906 San Francisco earthquake is located in California
Eureka
Eureka
Dunsmuir
Dunsmuir
Chico
Chico
Truckee
Truckee
Santa Rosa
Santa Rosa
Salinas
Salinas
Bakersfield
Bakersfield
Fresno
Fresno
Paso Robles
Paso Robles
Santa Monica
Santa Monica
Indio
Indio
1906 San Francisco earthquake
UTC time1906-04-18 13:12:27
ISC event16957905
USGS-ANSSComCat
Local dateApril 18, 1906 (1906-04-18)
Local time05:12 a.m. local time
Magnitude7.9 Mw[1]
Depth5 mi (8.0 km)[2]
Epicenter37°45′N 122°33′W / 37.75°N 122.55°W / 37.75; -122.55Coordinates: 37°45′N 122°33′W / 37.75°N 122.55°W / 37.75; -122.55[2]
TypeStrike-slip[3]
Areas affectedNorth Coast
San Francisco Bay Area
Central Coast
United States
Max. intensityXI (Extreme)[4]
TsunamiYes[5]
Casualties700–3,000+[6]

The 1906 San Francisco earthquake struck the coast of Northern California at 5:12 a.m. on Wednesday, April 18 with an estimated moment magnitude of 7.9 and a maximum Mercalli intensity of XI (Extreme). High intensity shaking was felt from Eureka on the North Coast to the Salinas Valley, an agricultural region to the south of the San Francisco Bay Area. Devastating fires soon broke out in the city and lasted for several days. Thousands of homes were dismantled. As a result, up to 3,000 people died and over 80% of the city of San Francisco was destroyed. The events are remembered as one of the worst and deadliest earthquakes in the history of the United States. The death toll remains the greatest loss of life from a natural disaster in California's history and high in the lists of American disasters.

Tectonic setting[edit]

The San Andreas Fault is a continental transform fault that forms part of the tectonic boundary between the Pacific Plate and the North American Plate.[3] The strike-slip fault is characterized by mainly lateral motion in a dextral sense, where the western (Pacific) plate moves northward relative to the eastern (North American) plate. This fault runs the length of California from the Salton Sea in the south to Cape Mendocino in the north, a distance of about 810 miles (1,300 km). The maximum observed surface displacement was about 20 feet (6 m); geodetic measurements show displacements of up to 28 feet (8.5 m).[7]

Earthquake[edit]

USGS ShakeMap showing the earthquake's intensity.

The 1906 earthquake preceded the development of the Richter magnitude scale by three decades. The most widely accepted estimate for the magnitude of the quake on the modern moment magnitude scale is 7.9;[1] values from 7.7 to as high as 8.3 have been proposed.[8] According to findings published in the Journal of Geophysical Research, severe deformations in the earth's crust took place both before and after the earthquake's impact. Accumulated strain on the faults in the system was relieved during the earthquake, which is the supposed cause of the damage along the 450-kilometer-long segment of the San Andreas plate boundary.[8] The 1906 rupture propagated both northward and southward for a total of 296 miles (476 km).[9] Shaking was felt from Oregon to Los Angeles, and inland as far as central Nevada.[10]

A strong foreshock preceded the main shock by about 20 to 25 seconds. The strong shaking of the main shock lasted about 42 seconds. There were decades of minor earthquakes – more than at any other time in the historical record for northern California – before the 1906 quake. Widely interpreted previously as precursory activity to the 1906 earthquake, they have been found to have a strong seasonal pattern and have been postulated to be due to large seasonal sediment loads in coastal bays that overlie faults as a result of the erosion caused by hydraulic mining in the later years of the California Gold Rush.[11]

For years, the epicenter of the quake was assumed to be near the town of Olema, in the Point Reyes area of Marin County, because of evidence of the degree of local earth displacement. In the 1960s, a seismologist at UC Berkeley proposed that the epicenter was more likely offshore of San Francisco, to the northwest of the Golden Gate. The most recent analyses support an offshore location for the epicenter, although significant uncertainty remains.[2] An offshore epicenter is supported by the occurrence of a local tsunami recorded by a tide gauge at the San Francisco Presidio; the wave had an amplitude of approximately 3 in (8 cm) and an approximate period of 40–45 minutes.[12]

Analysis of triangulation data before and after the earthquake strongly suggest that the rupture along the San Andreas Fault was about 500 km in length, in agreement with observed intensity data. The available seismological data support a significantly shorter rupture length, but these observations can be reconciled by allowing propagation at speeds above the S-wave velocity (supershear). Supershear propagation has now been recognized for many earthquakes associated with strike-slip faulting.[13]

Impact[edit]

Damaged houses on Howard Street (left), and ruins in the vicinity of Post and Grant Avenue

At the time, 375 deaths were reported;[14] however, hundreds of fatalities in Chinatown went ignored and unrecorded. The total number of deaths is still uncertain, but various reports presented a range of 700–3,000+.[15] Most of the deaths occurred in San Francisco itself, but 189 were reported elsewhere in the Bay Area; nearby cities, such as Santa Rosa and San Jose, also suffered severe damage. In Monterey County, the earthquake permanently shifted the course of the Salinas River near its mouth. Where previously the river emptied into Monterey Bay between Moss Landing and Watsonville, it was diverted 6 miles south to a new channel just north of Marina.

Between 227,000 and 300,000 people were left homeless out of a population of about 410,000; half of those who evacuated fled across the bay to Oakland and Berkeley. Newspapers described Golden Gate Park, the Presidio, the Panhandle and the beaches between Ingleside and North Beach as covered with makeshift tents. More than two years later, many of these refugee camps were still in operation.[16]

Selected Mercalli intensities
MMI Locations
XI (Extreme) San Francisco, Santa Rosa
X (Extreme) Sebastopol, San Bruno
IX (Violent) San Jose, Point Arena
VIII (Severe) Eureka, Salinas
VII (Very strong) Truckee, Parkfield
VI (Strong) Willows, Fresno
V (Moderate) Chico, Paso Robles
IV (Light) Dunsmuir, Bakersfield
III (Weak) Santa Monica, Indio
U.S. Earthquake Intensity Database, NGDC

The earthquake and fire left long-standing and significant pressures on the development of California. At the time of the disaster, San Francisco had been the ninth-largest city in the United States and the largest on the West Coast, with a population of about 410,000. Over a period of 60 years, the city had become the financial, trade and cultural center of the West; operated the busiest port on the West Coast; and was the "gateway to the Pacific", through which growing U.S. economic and military power was projected into the Pacific and Asia. Over 80% of the city was destroyed by the earthquake and fire. Though San Francisco rebuilt quickly, the disaster diverted trade, industry and population growth south to Los Angeles, which during the 20th century became the largest and most important urban area in the West. Many of the city's leading poets and writers retreated to Carmel-by-the-Sea where, as "The Barness", they established the arts colony reputation that continues today.

The 1908 Lawson Report, a study of the 1906 quake led and edited by Professor Andrew Lawson of the University of California, showed that the same San Andreas Fault which had caused the disaster in San Francisco ran close to Los Angeles as well. The earthquake was the first natural disaster of its magnitude to be documented by photography and motion picture footage and occurred at a time when the science of seismology was blossoming.

Intensity[edit]

The most important characteristic of the shaking intensity noted in Andrew Lawson's (1908) report was the clear correlation of intensity with underlying geologic conditions. Areas situated in sediment-filled valleys sustained stronger shaking than nearby bedrock sites, and the strongest shaking occurred in areas of former bay where soil liquefaction had occurred. Modern seismic-zonation practice accounts for the differences in seismic hazard posed by varying geologic conditions.[17] The shaking intensity as described on the Modified Mercalli intensity scale reached XI (Extreme) in San Francisco and areas to the north like Santa Rosa where destruction was devastating.

Damage[edit]

Although the impact of the earthquake on San Francisco was the most famous, the earthquake also inflicted considerable damage on several other cities. These include San Jose and Santa Rosa, the entire downtown of which was essentially destroyed.[18][19][20]

Fires[edit]

Arnold Genthe's photograph, looking toward the fire on Sacramento Street

As damaging as the earthquake and its aftershocks were, the fires that burned out of control afterward were even more destructive.[21] It has been estimated that up to 90% of the total destruction was the result of the subsequent fires.[22] Within three days,[23] over 30 fires, caused by ruptured gas mains, destroyed approximately 25,000 buildings on 490 city blocks. One of the largest of these fires was accidentally started in a house on Hayes Street by a woman making breakfast for her family. This came to be known as the "Ham and Eggs Fire". Some were started when firefighters, untrained in the use of dynamite, attempted to demolish buildings to create firebreaks. The dynamited buildings themselves often caught fire. The city's fire chief, Dennis T. Sullivan, who would have been responsible, had died from injuries sustained in the initial quake.[24] In all, the fires burned for four days and nights.

Due to a widespread practice by insurers to indemnify San Francisco properties from fire, but not earthquake damage, most of the destruction in the city was blamed on the fires. Some property owners deliberately set fire to damaged properties, in order to claim them on their insurance. Capt. Leonard D. Wildman of the U.S. Army Signal Corps[25] reported that he "was stopped by a fireman who told me that people in that neighborhood were firing their houses...they were told that they would not get their insurance on buildings damaged by the earthquake unless they were damaged by fire".[26]

Burning of the Mission District (left) and a map showing the extent of the fire

One landmark building lost in the fire was the Palace Hotel, subsequently rebuilt, which had many famous visitors, including royalty and celebrated performers. It was constructed in 1875 primarily financed by Bank of California co-founder William Ralston, the "man who built San Francisco". In April 1906, the tenor Enrico Caruso and members of the Metropolitan Opera Company came to San Francisco to give a series of performances at the Grand Opera House. The night after Caruso's performance in Carmen, the tenor was awakened in the early morning in his Palace Hotel suite by a strong jolt. Clutching an autographed photo of President Theodore Roosevelt, Caruso made an effort to get out of the city, first by boat and then by train, and vowed never to return to San Francisco. Caruso died in 1921, having remained true to his word. The Metropolitan Opera Company lost all of its traveling sets and costumes in the earthquake and ensuing fires.[27]

Some of the greatest losses from fire were in scientific laboratories. Alice Eastwood, the curator of botany at the California Academy of Sciences in San Francisco, is credited with saving nearly 1,500 specimens, including the entire type specimen collection for a newly discovered and extremely rare species, before the remainder of the largest botanical collection in the western United States was destroyed in the fire.[28][29] The entire laboratory and all the records of Benjamin R. Jacobs, a biochemist who was researching the nutrition of everyday foods, were destroyed.[30] The original California flag used in the 1846 Bear Flag Revolt at Sonoma, which at the time was being stored in a state building in San Francisco, was also destroyed in the fire.[31]

The fire following the earthquake in San Francisco, cost an estimated $350 million at the time, equivalent to $8.97 billion. The devastating quake levelled about 80% of the city.[32]

Response[edit]

The city's fire chief, Dennis T. Sullivan, was gravely injured when the earthquake first struck and later died from his injuries. The interim fire chief sent an urgent request to the Presidio, an army post on the edge of the stricken city, for dynamite. General Frederick Funston had already decided that the situation required the use of troops. Telephoning a policeman, he sent word to Mayor Eugene Schmitz of his decision to assist, and then ordered army troops from nearby Angel Island to mobilize and come into the city. Explosives were ferried across the bay from the California Powder Works in what is now Hercules.

Soldiers looting during the fire

During the first few days, soldiers provided valuable services like patrolling streets to discourage looting and guarding buildings such as the U.S. Mint, post office, and county jail. They aided the fire department in dynamiting to demolish buildings in the path of the fires. The army also became responsible for feeding, sheltering, and clothing the tens of thousands of displaced residents of the city. Under the command of Funston's superior, Major General Adolphus Greely, Commanding Officer, Pacific Division, over 4,000 troops saw service during the emergency. On July 1, 1906, civil authorities assumed responsibility for relief efforts, and the army withdrew from the city.

On April 18, in response to riots among evacuees and looting, Mayor Schmitz issued and ordered posted a proclamation that "The Federal Troops, the members of the Regular Police Force and all Special Police Officers have been authorized by me to kill any and all persons found engaged in Looting or in the Commission of Any Other Crime".[33] In addition, accusations of soldiers themselves engaging in looting also surfaced.[34]

Early on April 18, 1906, recently retired Captain Edward Ord of the 22nd Infantry Regiment was appointed a Special Police Officer by Mayor Eugene Schmitz and liasioned with Major General Adolphus Greely for relief work with the 22nd Infantry and other military units involved in the emergency. Ord later wrote a long letter[35] to his mother on the April 20 regarding Schmitz' "Shoot-to-Kill" Order and some "despicable" behavior of certain soldiers of the 22nd Infantry who were looting. He also made it clear that the majority of soldiers served the community well.[34]

Aftermath[edit]

Refugees leaving the city

Property losses from the disaster have been estimated to be more than $400 million in 1906 dollars.[6] This is equivalent to $11.2 billion in 2018 dollars. An insurance industry source tallies insured losses at $235 million, the equivalent to $6.55 billion in 2018 dollars.[36][37]

Political and business leaders strongly downplayed the effects of the earthquake, fearing loss of outside investment in the city which was badly needed to rebuild.[38] In his first public statement, California governor George Pardee emphasized the need to rebuild quickly: "This is not the first time that San Francisco has been destroyed by fire, I have not the slightest doubt that the City by the Golden Gate will be speedily rebuilt, and will, almost before we know it, resume her former great activity".[39] The earthquake itself is not even mentioned in the statement. Fatality and monetary damage estimates were manipulated.[40]

Almost immediately after the quake (and even during the disaster), planning and reconstruction plans were hatched to quickly rebuild the city. Rebuilding funds were immediately tied up by the fact that virtually all the major banks had been sites of the conflagration, requiring a lengthy wait of seven-to-ten days before their fire-proof vaults could cool sufficiently to be safely opened. The Bank of Italy had evacuated its funds and was able to provide liquidity in the immediate aftermath. Its president also immediately chartered and financed the sending of two ships to return with shiploads of lumber from Washington and Oregon mills which provided the initial reconstruction materials and surge. In 1929, Bank of Italy was renamed and is now known as Bank of America.

William James, the pioneering American psychologist, was teaching at Stanford at the time of the earthquake and traveled into San Francisco to observe first-hand its aftermath. He was most impressed by the positive attitude of the survivors and the speed with which they improvised services and created order out of chaos.[41] This formed the basis of the chapter "On some Mental Effects of the Earthquake" in his book Memories and Studies.[42]

H. G. Wells had just arrived in New York on his first visit to America when he learned, at lunch, of the San Francisco earthquake. What struck him about the reaction of those around him was that "it does not seem to have affected any one with a sense of final destruction, with any foreboding of irreparable disaster. Every one is talking of it this afternoon, and no one is in the least degree dismayed. I have talked and listened in two clubs, watched people in cars and in the street, and one man is glad that Chinatown will be cleared out for good; another's chief solicitude is for Millet's 'Man with the Hoe.' 'They'll cut it out of the frame,' he says, a little anxiously. 'Sure.' But there is no doubt anywhere that San Francisco can be rebuilt, larger, better, and soon. Just as there would be none at all if all this New York that has so obsessed me with its limitless bigness was itself a blazing ruin. I believe these people would more than half like the situation."[43]

View from the Ferry Building tower, southwest down on Market Street
The Agassiz statue in front of the Zoology building (now building 420), Stanford University.

The earthquake was crucial in the development of the University of California, San Francisco and its medical facilities. Until 1906, the school faculty had provided care at the City-County Hospital (San Francisco General Hospital, 1915–2016, but Zuckerberg San Francisco General Hospital and Trauma Center (SFGH) since 2016), but did not have a hospital of its own. Following the 1906 San Francisco earthquake, more than 40,000 people were relocated to a makeshift tent city in Golden Gate Park and were treated by the faculty of the Affiliated Colleges. This brought the school, which until then was located on the western outskirts of the city, in contact with significant population and fueled the commitment of the school towards civic responsibility and health care, increasing the momentum towards the construction of its own health facilities. Finally, in April 1907, one of the buildings was renovated for outpatient care with 75 beds. This created the need to train nursing students, and, in 1907, the UC Training School for Nurses was established, adding a fourth professional school to the Affiliated Colleges.

The grandeur of citywide reconstruction schemes required investment from Eastern monetary sources, hence the spin and de-emphasis of the earthquake, the promulgation of the tough new building codes, and subsequent reputation sensitive actions such as the official low death toll. One of the more famous and ambitious plans came from famed urban planner Daniel Burnham. His bold plan called for, among other proposals, Haussmann-style avenues, boulevards, arterial thoroughfares that radiated across the city, a massive civic center complex with classical structures, and what would have been the largest urban park in the world, stretching from Twin Peaks to Lake Merced with a large atheneum at its peak. But this plan was dismissed during the aftermath of the earthquake.

For example, real estate investors and other land owners were against the idea due to the large amount of land the city would have to purchase to realize such proposals.[44] City fathers likewise attempted at the time to eliminate the Chinese population and export Chinatown (and other poor populations) to the edge of the county where the Chinese could still contribute to the local taxbase.[45] The Chinese occupants had other ideas and prevailed instead. Chinatown was rebuilt in the newer, modern, Western form that exists today. The destruction of City Hall and the Hall of Records enabled thousands of Chinese immigrants to claim residency and citizenship, creating a backdoor to the Chinese Exclusion Act, and bring in their relatives from China.[46][47][48]

While the original street grid was restored, many of Burnham's proposals inadvertently saw the light of day, such as a neoclassical civic center complex, wider streets, a preference of arterial thoroughfares, a subway under Market Street, a more people-friendly Fisherman's Wharf, and a monument to the city on Telegraph Hill, Coit Tower.

The earthquake was also responsible for the development of the Pacific Heights neighborhood. The immense power of the earthquake had destroyed almost all of the mansions on Nob Hill except for the James C. Flood Mansion. Others that hadn't been destroyed were dynamited by the Army forces aiding the firefighting efforts in attempts to create firebreaks. As one indirect result, the wealthy looked westward where the land was cheap and relatively undeveloped, and where there were better views and a consistently warmer climate. Constructing new mansions without reclaiming and clearing old rubble simply sped attaining new homes in the tent city during the reconstruction.[citation needed]

Reconstruction was swift, and largely completed by 1915, in time for the 1915 Panama–Pacific International Exposition which celebrated the reconstruction of the city and its "rise from the ashes".

Since 1915, the city has officially commemorated the disaster each year by gathering the remaining survivors at Lotta's Fountain, a fountain in the city's financial district that served as a meeting point during the disaster for people to look for loved ones and exchange information.

Housing[edit]

One of the eleven housing camps

The army built 5,610 redwood and fir "relief houses" to accommodate 20,000 displaced people. The houses were designed by John McLaren, and were grouped in eleven camps, packed close to each other and rented to people for two dollars per month until rebuilding was completed. They were painted navy blue, partly to blend in with the site, and partly because the military had large quantities of navy blue paint on hand. The camps had a peak population of 16,448 people, but by 1907 most people had moved out. The camps were then re-used as garages, storage spaces or shops. The cottages cost on average $100 to put up. The $2 monthly rents went towards the full purchase price of $50. Most of the shacks have been destroyed, but a small number survived. One of the modest 720 sq ft (67 m2) homes was purchased in 2006 for more than $600,000.[49] The last official refugee camp was closed on June 30, 1908.[50]

A 2017 study found that the fire had the effect of increasing the share of land used for nonresidential purposes: "Overall, relative to unburned blocks, residential land shares on burned blocks fell while nonresidential land shares rose by 1931. The study also provides insight into what held the city back from making these changes before 1906: the presence of old residential buildings. In reconstruction, developers built relatively fewer of these buildings, and the majority of the reduction came through single-family houses. Also, aside from merely expanding nonresidential uses in many neighborhoods, the fire created economic opportunities in new areas, resulting in clusters of business activity that emerged only in the wake of the disaster. These effects of the fire still remain today, and thus large shocks can be sufficient catalysts for permanently reshaping urban settings."[51]

Relief[edit]

During the first few days after news of the disaster reached the rest of the world, relief efforts reached over $5,000,000.[52] London raised hundreds of thousands of dollars. Individual citizens and businesses donated large sums of money for the relief effort: Standard Oil gave $100,000; Andrew Carnegie gave $100,000; the Dominion of Canada made a special appropriation of $100,000 and even the Bank of Canada in Ottawa gave $25,000.[52] The U.S. government quickly voted for one million dollars in relief supplies which were immediately rushed to the area, including supplies for food kitchens and many thousands of tents that city dwellers would occupy the next several years.[53] These relief efforts were not enough to get families on their feet again, and consequently the burden was placed on wealthier members of the city, who were reluctant to assist in the rebuilding of homes they were not responsible for. All residents were eligible for daily meals served from a number of communal soup kitchens and citizens as far away as Idaho and Utah were known to send daily loaves of bread to San Francisco as relief supplies were coordinated by the railroads.[54]

Insurance payments[edit]

Insurance companies, faced with staggering claims of $250 million,[55] paid out between $235 million and $265 million on policyholders' claims, often for fire damage only, since shake damage from earthquakes was excluded from coverage under most policies.[56][57] At least 137 insurance companies were directly involved and another 17 as reinsurers.[58] Twenty companies went bankrupt, and most excluded shake damage claims.[57] Lloyd's of London reports having paid all claims in full, more than $50 million[59] and the insurance companies in Hartford, Connecticut report also paying every claim in full, with the Hartford Fire Insurance Company paying over $11 million and Aetna Insurance Company almost $3 million.[57]

After the 1906 earthquake, global discussion arose concerning a legally flawless exclusion of the earthquake hazard from fire insurance contracts. It was pressed ahead mainly by re-insurers. Their aim; a uniform solution to insurance payouts resulting from fires caused by earthquakes. Until 1910, a few countries, especially in Europe, followed the call for an exclusion of the earthquake hazard from all fire insurance contracts. In the U.S., the question was discussed differently. But the traumatized public reacted with fierce opposition. On August 1, 1909, the California Senate enacted the California Standard Form of Fire Insurance Policy, which did not contain any earthquake clause. Thus the state decided that insurers would have to pay again if another earthquake was followed by fires. Other earthquake-endangered countries followed the California example.[60] The insurance payments heavily affected the international financial system. Gold transfers from European insurance companies to policyholders in San Francisco led to a rise in interest rates, subsequently to a lack of available loans and finally to the Knickerbocker Trust Company crisis of October 1907 which led to the Panic of 1907.[61]

Centennial commemorations[edit]

The 1906 Centennial Alliance[62] was set up as a clearing-house for various centennial events commemorating the earthquake. Award presentations, religious services, a National Geographic TV movie,[63] a projection of fire onto the Coit Tower,[64] memorials, and lectures were part of the commemorations. The USGS Earthquake Hazards Program issued a series of Internet documents,[65] and the tourism industry promoted the 100th anniversary as well.[66]

Eleven survivors of the 1906 earthquake attended the centennial commemorations in 2006, including Irma Mae Weule (May 11, 1899 – August 8, 2008),[67] who was the oldest survivor of the quake at the time of her death in August 2008, aged 109.[68] Vivian Illing (December 25, 1900 – January 22, 2009) was believed to be the second-oldest survivor at the time of her death, aged 108, leaving Herbert Hamrol (January 10, 1903 – February 4, 2009) as the last known remaining survivor at the time of his death, aged 106. Another survivor, Libera Armstrong (September 28, 1902 – November 27, 2007), attended the 2006 anniversary, but died in 2007, aged 105.[69]

Shortly after Hamrol's death, two additional survivors were discovered. William Del Monte, then 103, and Jeanette Scola Trapani (April 21, 1902 – December 28, 2009),[70] 106, stated that they stopped attending events commemorating the earthquake when it became too much trouble for them.[71] Del Monte and another survivor, Rose Cliver, then 106, attended the earthquake reunion celebration on April 18, 2009, the 103rd anniversary of the earthquake.[72] Cliver (October 9, 1902 – February 18, 2012)[73] died in February 2012, aged 109. Nancy Stoner Sage (February 19, 1905 – April 15, 2010) died, aged 105, in Colorado just three days short of the 104th anniversary of the earthquake on April 18, 2010. Del Monte attended the event at Lotta's Fountain on April 18, 2010 and the dinner at John's Restaurant the night before.[74] 107-year-old George Quilici (April 26, 1905 – May 31, 2012) died in May 2012,[75] and 113-year-old Ruth Newman (September 23, 1901 – July 29, 2015) in July 2015.[76] William Del Monte (January 22, 1906 – January 11, 2016), who died 11 days shy of his 110th birthday, was thought to be the last survivor.[77]

In 2005 the National Film Registry added San Francisco Earthquake and Fire, April 18, 1906, a newsreel documentary made soon after the earthquake, to its list of American films worthy of preservation.[78]

Panoramas[edit]

San Francisco burning in 1906.
San Francisco fire 1906
A 360 degree panoramic view of damage across the city after the disaster in 1906. In the distance large buildings remain but local structures are reduced to piles of rubble, with some chimney stacks remaining.
San Francisco 360° panorama showing damage, 1906
Panoramic view of earthquake and fire damage from Stanford Mansion site, April 18–21, 1906. Note the ruins of the original City Hall building at far right.[79]
"San Francisco in ruins from Lawrence Captive Airship – 2000 feet [660 m] above San Francisco Bay – Overlooking waterfront. – Sunset over Golden Gate." Market Street leads directly away from Ferry Building tower, center foreground.

In popular culture[edit]

  • The movie Frisco Jenny depicts the earthquake.
  • The 1936 movie San Francisco is based on the event.
  • Rebuilding San Francisco following the 1906 earthquake destruction is a scenario in the Sim City videogame.[80]
  • In Part 2 of the episode "Time's Arrow" of Star Trek: The Next Generation, the crew of the U.S.S. Enterprise time-travels back to 1893, where Captain Jean-Luc Picard places a monitoring device in a hospital ward, claiming to a curious doctor that he's helping to make the building safer from earthquakes. The doctor scoffs that "there hasn't been an earthquake here in thirty years," referencing the "great" earthquake of October 21, 1868, and unaware that the much more devastating 1906 earthquake is only 13 years in the future.
  • In the Walt Disney animated film, Big Hero 6, the fictional setting of "San Fransokyo" is intended to be San Francisco in an alternate timeline in which the city was rebuilt by Japanese immigrants following the earthquake, though the premise is never mentioned in the film.[81] In Big Hero 6: The Series it was revealed that a character named Lenore Shimamoto caused the earthquake when her experiment with energy amplifier caused a "Great Catastrophy".
  • In the William Carter puzzles of the Don't Starve videogame, it is suggested that the earthquake was triggered by the dark powers of Codex Umbra, a mysterious book.[82]
  • Beth Cato's Breath of Earth, an alternate-history fantasy novel, takes place in the lead-up to and aftermath of the earthquake.[83]

See also[edit]

Notes[edit]

  1. ^ a b "Where Can I Learn More About the 1906 Earthquake?". Berkeley Seismological Laboratory. 2008-01-28. Archived from the original on 2008-03-27.
  2. ^ a b c Location of the Focal Region and Hypocenter of the California Earthquake of April 18, 1906
  3. ^ a b Segall, P.; Lisowski, M. (1990), "Surface Displacements in the 1906 San Francisco and 1989 Loma Prieta Earthquakes", Science, American Association for the Advancement of Science, 250 (4985): 1241–4, Bibcode:1990Sci...250.1241S, doi:10.1126/science.250.4985.1241, PMID 17829210
  4. ^ Stover, C.W.; Coffman, J.L. (1993), Seismicity of the United States, 1568–1989 (Revised), U.S. Geological Survey professional paper 1527, United States Government Printing Office, p. 75
  5. ^ Geist, E.L.; Zoback, M.L. (1999), "Analysis of the tsunami generated by the Mw 7.8 1906 San Francisco earthquake", Geology, Geological Society of America, 27 (1): 15–18, Bibcode:1999Geo....27...15G, doi:10.1130/0091-7613(1999)027<0015:aottgb>2.3.co;2
  6. ^ a b USGS, Casualties and damage after the 1906 Earthquake, United States Geological Survey
  7. ^ 1906 San Francisco Quake: How large was the offset? USGS Earthquake Hazards Program — Northern California. Accessed September 3, 2006
  8. ^ a b Thatcher, Wayne (10 December 1975). "Strain accumulation and release mechanism of the 1906 San Francisco Earthquake". Journal of Geophysical Research. 80 (35): 4862–4872. Bibcode:1975JGR....80.4862T. doi:10.1029/JB080i035p04862. Retrieved February 1, 2016.
  9. ^ 1906 Earthquake: How long was the 1906 Crack? USGS Earthquake Hazards Program – Northern California, Accessed September 3, 2006
  10. ^ Christine Gibson Archived December 5, 2010, at the Wayback Machine. "Our 10 Greatest Natural Disasters," American Heritage, Aug./Sept. 2006.
  11. ^ Seasonal Seismicity of Northern California Before the Great 1906 Earthquake, (Journal) Pure and Applied Geophysics, ISSN 0033-4553 (Print) 1420-9136 (Online), volume 159, Numbers 1–3 / January, 2002, Pages 7–62.
  12. ^ Tsunami Record from the Great 1906 San Francisco Earthquake, United States Geological Survey, 2008
  13. ^ Song S.G,; Beroza G.C.; Segall P. (2008). "A Unified Source Model for the 1906 San Francisco Earthquake" (PDF). Bulletin of the Seismological Society of America. 98 (2): 823–831. doi:10.1785/0120060402.
  14. ^ William Bronson, The Earth Shook, The Sky Burned (San Francisco: Chronicle Books, 1996)
  15. ^ Casualties and Damage after the 1906 earthquake USGS Earthquake Hazards Program – Northern California, Accessed September 4, 2006
  16. ^ Displays at the U.S. Army Corps of Engineers Museum in Sausalito, California
  17. ^ California Geological Survey – Seismic Hazards Zonation Program – Seismic Hazards Mapping regulations
  18. ^ "A Dreadful Catastrophe Visits Santa Rosa" Press Democrat, Santa Rosa, California, 19 April 1906, accessed 23 Feb. 2015.
  19. ^ Sta. Rosa [i.e. Santa Rosa] Courthouse
  20. ^ The 1906 San Francisco Earthquake and Fire
  21. ^ "Over 500 Dead, $200,000,000 Lost in San Francisco Earthquake". The New York Times. April 18, 1906. Retrieved April 19, 2008. Earthquake and fire today have put nearly half of San Francisco in ruins. About 500 persons have been killed, a thousand injured, and the property loss will exceed $200,000,000.
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References[edit]

Contemporary disaster accounts

External links[edit]

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