San Francisco Earthquake
Massive Earthquake Results in Human Tragedy and Economic Loss"
Exploring the Impact of the 1906 San Francisco Earthquake
San Francisco CA was hit by one of the most devastating earthquakes recognized by man on April 18, 1906. The earthquake affected 430 kilometers of the famous San Andreas fault ranging from northwest of San Juan Bautista to Cape Mendocino (Ellsworth, 1990). The city that was once San Francisco was reduced by and large to a pile of rubble. The once proud citizens of San Francisco were reduced to wandering and sorrowful masses, trying to rebuild the once great city and recover from the loss and devastation experienced by the unexpected natural disaster.
Geology of the Earthquake
From a geological perspective, the earthquake was characterized by large horizontal displacements that caused much speculation from geologists (USGS, 2000). From these displacements the "elastic-rebound theory" of earthquakes which today is the primary model used to describe earthquake cycles was crafted (USGS, 2000). From a scientific perspective the great San Francisco earthquake benefited scientists tremendously because it provided insight into the cause and evolution of seismic activity along fault lines.
The first shocks were felt at 5:12 AM, with the full earthquake hitting less than a minute later centered in San Francisco (Ellsworth, 1990). The entire quake lasted for less than one minute, between 45 and 60 seconds total, though the aftershocks were felt for some time after (USGS, 2000). The earthquake was felt in states as far away as Oregon and Nevada (USGS, 2000).
The total length of the earthquake was felt for about 290 miles, the largest recorded (USGS, 2001).
The magnitude of the earthquake was estimated between 7.7 (Wald, Kanamori, Helmberger & Heaton, 1993) and 7.9 (USGS, 2000). Because seismology and the study of earthquakes were limited during the early 1900s, an accurate assessment of the magnitude is not possible. There are some accounts that suggest that the earthquake was as great as 8.3, but these are largely unproven (USGS, 2000).
Before this earthquake little scientific effort was dedicated to seismic research. After the earthquake however scientists took an active interest in the area of seismography and government issued investigations into earthquakes became quite commonplace (USGS, 2000).
Today much is understood in the realm of seismography, and researchers actually have the ability to some extent to pinpoint a frame of time an earthquake is most likely to occur in.
The Human Toll and Economy
The casualties from the earthquake were severe. Almost 500 deaths in San Francisco were reported, and 166 deaths reported in surrounding areas (Greeley, 1906; NOAA, 1972). People wandered about in a state of devastation, shock, helplessness and sorrow as a result of the earthquake of 1906.
Thousands of people were left homeless, with estimates at 225,000 people (USGS, 2000). Buildings were also destroyed, to the tune of nearly 30,000 (NOAA, 1972). The reconstruction efforts would be very slow, because so many areas needed to be rebuilt.
Economically, San Francisco and the surrounding area suffered property damages exceeding 480 million dollars from fire and the direct consequences of the earthquake (1906 dollars, which would be much more today) (USGS 2000).
The physical effects of the earthquake included the displacement of the earth's surface region, the destruction of hundreds of buildings and the rupture of many underground pipes along the fault line (America Hurrah, 2004). Fire resulting from the quake burned continuously for two days resulting in further loss of property and life (America Hurrah, 2004).
One survivor of the earthquake, Edith Weatherred, a reporter, said the following of the earthquake: "rushing to the streets, we saw flames from more than a dozen fires enveloping whole blocks... hydrants had been twisted out of shape, the water supply cut off... came the message, God save us! The city is doomed!" Clearly the impact on human life and living was severe (America Hurrah, 2004).
Communications were inhibited within the city as telephone and communications completely stopped (Hansen, n.d.)....
The quake intensity as per the Mercalli scale that was used at that time was between 8 and 9, which seismologists today equate to a value of 7.9 on the Richter scale. [Dr. Frank J. Collazo] the quake created a rupture of 296 miles, which rates it as one of the biggest quakes ever. Geologist John M. Clarke said, " the heavy waves travelled at the rate of about
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