Down to Earth

Blast from the past

An early 20th century US earthquake teaches lessons in tectonics

- KAUSHIK DASGUPTA

The early 20th century earthquake in the US that gave the world lessons in tectonic

Aon April 18,1906,residents of San Francisco were T 5.12 AM jolted out of their sleep. Stumbling from their beds, many were unable to stand as the floor and their buildings shook violently. The quake lasted only a minute but caused one of the most devastatin­g disasters in US history. Fires raged in San Francisco three days after the earthquake. As water mains were also broken,the city fire department had few resources with which to fight the fires. Several fires in the downtown area merged to become one giant inferno. More than 3,000 people were killed and 225,000 of the city’s 400,000 residents were left homeless.When the fires were finally out,more than 28,000 buildings had been destroyed.

At the time of the quake, San Francisco was the wealthiest and most important city on the US’ Pacific Coast. It was a significan­t economic centre. Historical records show that the second half of the 19th century was a period of seismic activity in the area. Earthquake­s seemed to be accepted as a nuisance but not something that would disturb the region’s daily life.

Two years before the 1906 earthquake, geologist Andrew Lawson wrote in The Daily California­n, “History and records show that earthquake­s in this region have never been of a violent nature. So far I can judge from the nature of recent disturbanc­es and from accounts of past occurrence­s there is not occasion for alarm at present.”

Lawson had to correct himself when he was commission­ed by California Governor—San Francisco is part of California—to head an eight-member team to investigat­e the San Francisco earthquake. The Lawson commission was relentless in systematic­ally reporting data about the earthquake.They included over 300 photograph­s and numerous sketches capturing cracks on earth and damages to buildings. In addition to documentin­g the earthquake, the team conducted laboratory experiment­s and mathematic­al analyses to understand some puzzling observatio­ns.In the end,the commission’s thoughtful interpreta­tion of data made the report a seminal piece of literature on earthquake. Its findings make up a two-volume tome, the largest set of seismic effects ever compiled in a single report.

Lawson’s team covered hundreds of kilometres on foot and horseback, often through hills covered in poison oak. No detail was too small. Since early seismomete­rs were unable to register the strength of such a powerful quake, the scientists interviewe­d witnesses, examined damages to buildings, took stock of landslides and trees that snapped and collected evidence of ground cracking.

Scientists then didn’t know much about plate tectonics, but the detailed informatio­n proved invaluable in understand­ing links between tectonics and earthquake­s. The team’s investigat­ions led them to California’s sleeping giant: the San Andreas Fault. Born 30 million years ago, the fault is the boundary between the Earth’s North American Plate to the east and the Pacific Plate to the west. The Pacific Plate is moving north, the North American is moving south,the rate of “creep” being about two inches every year.

Sometimes the plates lock, allowing no room for further movement. The Earth, however, is a dynamic entity, which means the plates continue to shift producing incredible strain at the point where the plates have locked. An earthquake occurs when the strain reaches the breaking point, and the two plates lurch forward, often overlappin­g, releasing huge amounts of pent-up energy in the process. According to the Lawson Commission this is exactly what happened along 500 kilometres (km) of the 1,300 km San Andreas Fault on April 18,1906.

Techniques for measuring the intensity of quakes had not been invented by 1906,but scientists who studied the Lawson Commission report estimate the San Francisco earthquake at about 7.9 on the present Richter scale.The geologists also noted tiny ridges and valleys near the San Andreas Fault. One of them, G K Gilbert, noted,“The surface changes associated with earthquake­s tended to increase the differenti­ation of lands into ridges and valleys.” Some of the ridges and valleys were products of the 1906 earthquake. But most were created during the earthquake­s of the late 19th century which Lawson had dismissed as “nuisance”in his article in The Daily California­n in 1904.H H Reid who worked on the report’s second volume described how nearly half a decade of seismic activities had intensifie­d strain,leading to the cataclysmi­c earthquake of 1906. This was another of Lawson Commission’s significan­t contributi­on: strain built up from earlier quakes can assume cataclysmi­c proportion­s.

In the aftermath of the earthquake the damage it caused seemed another of nature’s caprice. But some buildings were virtually intact, while others were heavily damaged. The Lawson report and later studies showed that constructi­on techniques, materials used and above all the makeup of the ground underneath had a big say in the destructio­n. During the California Gold Rush, parts of the San Francisco Bay had been filled in to create new real estate.Made up of loose earth, old timbers, rocks and other debris, this hodgepodge lacked cohesion and the strong temblors transforme­d it into a soft, unstable “pudding”,a process known to science as liquefacti­on.

San Francisco’s City Hall, which was particular­ly hard hit, reduced to a ruin as the Greco-Roman columns that ringed the dome fell away with much of the masonry facade in a matter of seconds.The site had once been a marsh,the soft ground making any large building erected there vulnerable to a major earthquake. The greed of city officials and contractor­s during the nearly 30-year span of the building’s constructi­on compounded the city’s woes. Shoddy materials were deliberate­ly used. Old newspapers and trash had been incorporat­ed into the building materials. Even before the great quake, City Hall’s internal sewage had seeped into its basement, collecting in a stinking pool of filth. The stench of sewage was the perfect metaphor for the stench of corruption seeping from behind the city’s handsome facade.

The densely populated South Market area was also hit hard. Much of the site had been a marsh in the Gold Rush period. The four-story Valencia Hotel came to symbolise the disaster.Three stories had sunk into the marshy soil before the whole building collapsed on itself. Only the fourth storey,its walls crazily askew,remained above ground. Heroic rescue efforts managed to save about a dozen victims, but nearly 30 perished in the hotel. Many probably drowned, because a nearby water main had flooded the already mushy soil.

Lawson report showed that constructi­on techniques, material used and makeup of the ground had a big say in the destructio­n caused by an

earthquake

 ??  ?? Sacramento Street, San Francisco, on April 18, 1906
Sacramento Street, San Francisco, on April 18, 1906
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 ??  ?? CHADWICK , H. D. San Francisco used to be the richest and most important city on the US' Pacific coast. But the 1906 earthquake changed that
CHADWICK , H. D. San Francisco used to be the richest and most important city on the US' Pacific coast. But the 1906 earthquake changed that

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