Colorado Earthquake Information
Geologic studies indicate there are about 100 potentially active faults Colorado and more than 400 earthquake tremors of magnitude 2.5 or higher have occurred in Colorado since 1870. Movement on active faults is responsible for large earthquakes. Colorado experienced a magnitude 6.5 earthquake on November 7, 1882. The location of this earthquake appears to be in the northern Front Range west of |
![]() Loma Prieta Earthquake in California, Photo by Michael Nevins |
Damages included the power plant in Denver and cracked buildings in Boulder.
For comparison, the magnitude 6.9 1989 San Francisco, California earthquake resulted in the deaths of 62 people, 3000 injured and $7 billion in property damage.
The US Geological Survey has undertaking more intensive study of earthquake activity in the Trinidad area. Within an approximate two-week period of time, eleven quakes measuring greater than 3.0 on the Richter Scale, the largest being measured at 4.5, occurred in an area about ten miles southwest of Trinidad in the fall of 2001. Additionally, dozens of smaller magnitude quakes have also been detected.
Because the occurrence of earthquakes is relatively infrequent in Colorado and the historical earthquake record is short (only about 130 years), it is not possible to accurately estimate the timing or location of future dangerous earthquakes in Colorado.
Seismologists predict that Colorado will again experience a magnitude 6.5 earthquake at some unknown point in the future.
Sudden movement on faults is responsible for large earthquakes. By studying the geologic characteristics of faults, geoscientists can often determine when the fault last moved and estimate the magnitude of the earthquake that produced the last movement.
The Sangre de Cristo Fault, which lies at the base of the Sangre de Cristo Mountains along the eastern edge of the San Luis Valley, and the Sawatch Fault, which runs along the eastern margin of the Sawatch Range, are two of the most prominent potentially active faults in Colorado.
Not all of Colorado’s potentially active faults are in the mountains and some can not be seen at the earth’s surface. For example, the Cheraw Fault, which is in the Great Plains in southeast Colorado, appears to have had movement during the recent geologic past.
Relative to other western states, Colorado’s earthquake hazard is higher than Kansas or Oklahoma, but lower than Utah, and certainly much lower than Nevada and California.
Link to Colorado earthquake information from the USGS
Link to fault maps from the USGS
COLORADO’S LARGEST HISTORIC EARTHQUAKES
(Records date back to 1867)
| DATE | LOCATION | MAGNITUDE | INTENSITY |
| 1870, Dec. 4 | Pueblo-Ft. Reynolds | -- | VI |
| 1871, Oct | Lily Park, Moffat Co. | -- | VI |
| 1880, Sep. 17 | Aspen | -- | VI |
| 1882, Nov. 7 | North-Central CO | 6.5* | VII |
| 1891, Dec. | Maybell | -- | VI |
| 1901, Nov. 15 | Buena Vista | -- | VI |
| 1913, Nov. 11 | Ridgway area | -- | VI |
| 1944, Sep. 9 | Montrose/Basalt | -- | VI |
| 1955, Aug. 3 | Lake City | -- | VI |
| 1960, Oct. 11 | Montrose/Ridgway | 5.5 | V |
| 1966, Jan. 4 | N.E. of Denver | 5.0 | V |
| 1966, Jan. 23 | CO-NM border near Dulce, NM | 5.5 | VII |
| 1967, Aug. 9 | N.E. of Denver | 5.3 | VII |
| 1967, Nov. 27 | N.E. of Denver | 5.2 | VI |
| Prepared by the Earthquake Subcommittee - Colorado Natural Hazards Mitigation Council * = magnitude estimated for older earthquake; based on historical felt reports |
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Although many of Colorado’s earthquakes occurred in mountainous regions of the state, some have been located in the western valley and plateau region or east of the mountains. The most economically damaging earthquake in Colorado’s history occurred on August 9, 1967 in the northeast Denver metropolitan area. This magnitude 5.3 earthquake, which was centered near Commerce City, caused more than a million dollars damage in Denver and the northern suburbs.
This earthquake is believed to have been induced by the deep injection of liquid waste into a borehole at Rocky Mountain Arsenal. It was followed by an earthquake of magnitude 5.2 three months later in November 1967. Although these events cannot be classified as major earthquakes, they should not be discounted as insignificant. They occurred within Colorado’s Front Range Urban Corridor, an area where nearly 75% of Colorado residents and many critical facilities are located. Since March 1971, well after the initial flurry of seismic activity, 15 earthquakes of approximate magnitude 2½ or larger have occurred in the vicinity of the northern Denver suburbs.
Summary & Conclusions: Earthquake Subcommittee -
Colorado Natural Hazards Mitigation Council
Based on the historical earthquake record and geologic studies in Colorado, an event of magnitude 6½ to 7¼ could occur somewhere in the state. Scientists are unable to accurately predict when the next major earthquake will occur in Colorado, only that one will occur. The major factor preventing the precise identification of the time or location of the next damaging earthquake is the limited knowledge of potentially active faults. Given Colorado’s continuing active economic growth and the accompanying expansion of population and infrastructure, it is prudent to continue the study and analysis of earthquake hazards. Existing knowledge should be used to incorporate appropriate levels of seismic safety in building codes and practices. The continued and expanded use of seismic safety provisions in critical and vulnerable structures and in emergency planning statewide is also recommended. Concurrently, we should expand earthquake monitoring, geological and geophysical research, and mitigation planning.
The Colorado Geological Survey has several publications on Colorado earthquakes and potentially active faults, and maintains a reference collection on Colorado seismicity that includes reports by consultants or agencies. A listing of the reports can be viewed at the CGS web site, http://geosurvey.state.co.us/Default.aspx?tabid=29
Be Prepared....
Earthquakes strike suddenly, violently and without warning. Identifying potential hazards ahead of time and advance planning can reduce the dangers of serious injury or loss of life from an earthquake.
BEFORE Check for hazards in the home.
DURING If indoors:
If outdoors:
If in a moving vehicle:
Pets after an Earthquake
The behavior of pets may change dramatically after an earthquake. Normally quiet and friendly cats and dogs may become aggressive or defensive. Watch animals closely. Leash dogs and place them in a fenced yard.
Pets may not be allowed into shelters for health and space reasons.
Prepare an emergency pen for pets in the home that includes a 3-day supply of dry food and a large container of water.
AFTER Be prepared for aftershocks.
Although smaller than the main shock, aftershocks cause additional damage and may bring weakened structures down. Aftershocks can occur in the first hours, days, weeks, or even months after the quake.
Earthquake preparedness information provided by FEMA.