1987 Whittier Narrows Earthquake example essay topic
On October 1, 1987, at 7: 42 a.m. the residents of the Los Angeles basin got a jolting reminder of the perils of 'living on the fault line. ' This was due to the so-called Whittier Narrows earthquake. Hardest hit by the quake, was Whittier (pop. 72,000). Whittier is twelve miles from downtown Los Angeles and was the community closest to the epicenter. When the quake, registering 6.1 on the Richter scale, first struck, it was thought to be centered along the Old Whittier Fault.
However, after extensive study, it was determined that it was actually the result of a 'new' fault, or a fault that had not previously been discovered by scientists. What are the lessons learned from the Whittier quake? And, how does this quake compare to other more recent, higher magnitude quakes? Despite the fact that regular warnings are part of California living, repeated in schools, in earthquake exercises, by local and state governments, and even in the front of telephone books, many people were caught off-guard and panicked.
Fortunately, Californians learned a lot from the Whittier quake. The Whittier earthquake was not the 'big one' that Angeleno's perpetually wait for. This may be hard to comprehend given the extensive damage caused by the earthquake. Although classified as 'moderate,' the quake left more than 100 injured and six dead, including an electrical repairman buried in an underground tunnel, a college student struck by falling concrete in a campus garage, and three people who died of heart attacks brought on by the shock.
As a spokesman for the city of Whittier put it, the crumbled business district 'looks like downtown Beirut. ' (Kerr, 16). Twenty buildings there were condemned and over 2000 homes were damaged. According to Magnuson, 'Eight blocks in Whittier's business district were closed after bricks cascaded on cars, and at least eight buildings were too damaged to be saved' (Magnuson, p. 32). It is estimated that the Whittier Narrows earthquake caused over $358-million in damage.
The practical lessons learned from this quake seem to be the same as those learned in both previous and subsequent earthquakes. Among them is the necessity for earthquake preparedness. This was identified, and mandates were developed, before the 1987 Whittier quake. The California Earthquake Hazards Reduction Act of 1986 was enacted to direct the Seismic Safety Commission to establish a series of five-year programs to reduce state-wide earthquake hazards significantly by the year 2000.
The first program became the States' official earthquake hazard mitigation program (The Commission, p. 1). The quake was also a lesson to those who have long ignored the warnings about the hazards posed by old, unsafe, masonry buildings. In 1933, un reinforced masonry was banned in new construction, after 130 people were killed by a 6.3-magnitude earthquake. However, thousands of pre-1993 buildings had not been earthquake-proofed when the 1987 Whittier quake hit (Magnuson, p. 32). This was despite the fact that there had been a 1992 deadline in place to ensure that all buildings were earthquake-proof. Building damage by the quake confirmed the value of ongoing efforts to improve the seismic resistance of these buildings, and increased efforts were made towards enforcement of these building codes.
Since the earthquake however, buildings throughout California, and particularly Southern California have continued to be 'retrofitted' or made more earthquake-proof. However, the process is slow, 'Remedial strengthening of buildings in the City of Los Angeles is progressing, but such efforts are slow or absent elsewhere in the region' (Kerr, p. 270). Not only were practical lessons learned from this quake, but scientific ones as well. For example, after subsequent weeks of analysis of seismic data, the epicenter was pinpointed several miles northwest of the end of the Whittier fault. Additionally, the quake's motion was indicative not of a strike-slip, but of thrust faulting, meaning that slippage along a thrust fault hidden deep below the surfaced had triggered the quake. (Horgan, p. 21).
What scientists had discovered is that we are at risk from not just 'major' faults, but smaller folds near the earth's surface that seem to mark regions threatened by earthquakes. According to Dr. Lucy Jones of the U.S. Geological Survey in Pasadena, 'thrust faults underlying Los Angeles probably cannot create quakes with a magnitude greater than 6.5 or 7. But she suggests that such earthquakes originating directly under the city, could prove more devastating than an 8 magnitude quake along the San Andreas fault, which passes some 35 miles northwest of the city' (Horgan, p. 18). This information could prove vital in predicting or forecasting earthquakes. Since the 1987 Whittier Narrows earthquake there have been even larger, more devastating earthquakes, that repeated many of the same warnings. For example, Californians learned even greater lessons from the October 17, 1989, Loma Prieta earthquake, or as its commonly known, the San Francisco earthquake.
Although larger than the 1987 Whittier earthquake, the quake which measured Magnitude 7.1, is still considered of moderate size. It is believed to have re-ruptured the southernmost 25-mile segment of the 1906 San Andreas fault break. The epicenter was approximately 11.5 miles deep on the San Andreas fault. This deepness and location along one of California's largest faults, is where it differs from the 1987 Whittier quake. In addition, it caused even more damage than the Whittier quake. The Loma Prieta earthquake resulted in approximately $10-billion in direct damage and indirect losses.
There were 63 deaths and 350 hospitalized injuries (California Seismic Safety Commission, p. 1). The most devastating loss of life occurred when the I-880 Cypress Street viaduct collapsed. It took 43 lives. As in the Whittier quake, many older buildings of types known to be vulnerable suffered major structural failures. In total, over 24,000 residential structures, 3,500 commercial buildings and 140 public buildings in the ten-county area sustained earthquake damage. And, not surprisingly, according to the Seismic Safety Commission, 'the earthquake's most spectacular building damage affected un reinforced masonry structures, many of which were located in older downtown commercial areas...
Of approximately 900 un reinforced masonry (URM) buildings damaged in the earthquake, at least 50 were irreparable' (page, 1). It seems then, that the lesson to be learned from Whittier had been forgotten, or gone unheeded. As a result, new studies were conducted and books and guidelines developed. Many contained the same warnings and preparation advice that were delivered after the 1987 Whittier earthquake. Even after the Whittier earthquake, California still did not have safety codes for residential buildings. In fact, this was still the same situation when the Loma Prieta earthquake hit.
As the California State Seismic Commission states, 'although important progress is being made in confronting the URM building danger, California has not yet mustered the political resolve to require seismic bracing or anchoring of older homes or of mobile homes. Nor has California begun to deal with some other significant hazardous building types. However, several encouraging developments are being made in earthquake preparation as a result of these two earthquakes. The second program of the Earthquake Hazards Reduction Act of 1986 reflects on not only the progress made in the first five years, but builds on lessons learned from the Whittier Narrows earthquake and the Loma Prieta earthquake. According to the Commission, 'when the activities proposed in this second program are well underway, California will have a complete and comprehensive hazard reduction program. The state's ability to withstand the inevitable earthquake will be significantly improved' (The Commission, p. 8).
California is well on its way to being better prepared for the 'big one. ' This is thanks in part, to the lessons of these two earthquakes, and the risk of a larger earthquake occurring at any time. Several new goals that have been developed in the California at Risk program reflect this readiness. These initiatives include: establish seismic evaluation and retrofit building standards, improve safety of older public school buildings, improve safety of state-owned buildings, improve safety of homes, reduce workplace hazards, improve earthquake performance of transportation structures, map geologic hazards, and improve emergency communications (The Commission, p. 8).
Bibliography
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California Seismic Safety Commission. Loma Prieta's Call to Action. Sacramento, California, (1991).
Commission, The. California at Risk: Reducing Earthquake Hazards, 1992-1996.
Degenkolb, Henry. The Whittier Narrows Earthquake, October 1, 1987.
San Francisco, California: Degenkolb, (1988).
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Science 239.1409-1412, (1988, March).
Horgan, John. 'All Shook Up. ' Scientific American 257.18-19, (1987, December).
Kerr, Richard. 'What is Worse Than the 'Big One'?' Science 238.269-270, (1987, October).
Magnuson, Ed. 'A Ten-Second Wake-Up Call. ' Time 130.32, (1987, October).
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