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<br />Colorado Earthquake Hazard <br /> <br />earthquakes is being compiled under the Colorado <br />Earthquake Hazard Reduction Program (CEHRP). <br /> <br />Recorded Earthquake History <br /> <br />Like many other states in the Rocky Mountain West, <br />Colorado has a relatively short history of recorded <br />earthquakes. Much of what is known about earth- <br />quakes in Colorado comes from citizens who settled <br />Colorado and from scientists who have studied <br />earthquakes. Observations of the severity of earth- <br />quake effects on people, buildings, and the physical <br />environment are categorized by the Modified Mer- <br />calli (MM) intensity scale. The table on the previous <br />page lists some of the significant earthquakes felt in <br />Colorado since 1870. The largest known earth- <br />quake, the 6.5 magnitude event on November 7, <br />1882, caused damage on the eastern and western <br />slopes of Colorado and was felt throughout the state. <br />That earthquake was also felt as far west as Salt <br />Lake City, Utah, as far east as Salina, Kansas, and <br />as far north as Ft. Washakie in north central Wyo- <br />ming. Scientists and engineers are re-investigating <br />the November 7, 1882 earthquake in order to under- <br />stand more about its size, the location of the epicen- <br />ter, and the damaging effects from the largest <br />earthquake in Colorado's recorded history. <br /> <br />Induced Seismicity <br /> <br />Colorado is one of the few places in the world where <br />earthquakes have been generated or triggered by <br />human activities. The most obvious cases of human- <br />induced earthquakes involve experimental nuclear <br />explosions to stimulate natural gas recovery. Three <br />such explosions have been detonated in or very near <br />Colorado: Projects Gasbuggy, Rulison, and Rio <br />Blanco. At the Rangely oil field, scientists were actu- <br />ally able to turn on and off earthquakes by control- <br />led fluid injection. <br /> <br />Another case of possible induced seismicity occurred <br />in the 1960s northeast of Denver. In 1961, a deep in- <br />jection well was drilled at the Rocky Mountain Arse- <br />nal. Fluid injection began in 1962 and a series of <br />earthquakes occurred shortly thereafter. The largest <br />of the earthquakes, the August 9, 1967, 5.3 magni- <br /> <br />tude and the November 27, 1967, 5.2 magnitude <br />earthquakes, occurred about 18 months after injec- <br />tions stopped. The relationship between the fluid in- <br />jections and earthquakes was never conclusively <br />solved, but the 5.3 and 5.2 magnitude events in 1967 <br />caused over one million dollars in damage in Denver <br />and its northern suburbs. For the past several dec- <br />ades, the seismicity at the Rocky Mountain Arsenal <br />has been monitored, and scientists and engineers <br />from government and the private sector are working <br />to understand earthquakes there. <br /> <br /> <br />1967. Earthquake Damage Northglenn, CO <br /> <br />Colorado Population At Risk <br /> <br />Nearly three-fourths of Colorado's 3.4 million resi- <br />dents live in the Front Range communities. In addi- <br />tion to permanent residents, Colorado is visited each <br />year by nearly five million tourists and business peo- <br />ple. Besides people, most of Colorado's infrastruc- <br /> <br />30 <br />