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the wasatch fault zone stretches through the wasatch mountains and into the great salt lake. the wasatch fault zone was originally formed during the mesozoic and cenozoic eras of geologic time. the fault zone has been characterized by multiple earthquake events throughout the ages, creating the scariest part of utah.


the national geospatial-intelligence agency (nga) and the usgs have published a gis and geologic hazard model of the wasatch fault zone. this model includes data from the ugs and from the usgs to address the needs of hazard mitigation planners and scientists. the model provides a state-of-the-art view of the wasatch fault zone. it includes the locations and depths of seismically active zones, the locations of major faults, and the locations of mapped and inferred tectonic features such as thrust and fracture zones and other features that affect the potential for seismic activity. the model also includes known, mapped, or inferred active or extinct faults and other faults that could affect future seismic activity. the model is included on the web as an arcgis map service at or a kml file at .


the wasatch fault zone was formed from the combination of the wasatch mountain thrust and the sevier river thrust. the sevier river thrust is the main thrust that defines the wasatch mountain thrust. the wasatch mountain thrust and the sevier river thrust are composed of thrust faults, normal faults, and transform faults. the wasatch mountain thrust is a north-directed thrust that forms the northwest-southeast trending wasatch range in northwestern utah. the sevier river thrust (also known as the great salt lake thrust) is a south-directed thrust that was responsible for the formation of the sevier valley. the wasatch mountain thrust displaces the sevier valley and the sevier river thrust at a rate of up to 80 mm/yr. 84d34552a1