Yellowstone National Park is home to one of the largest volcanic systems on Earth. Evidence of volcanic eruptions associated with the Yellowstone volcano, and the eastward track of the hot spot that created it, stretch from Idaho into northwest Wyoming. However, the eruption history of the volcano is only part of the geologic story. The park also contains evidence of faults and other geologic processes that can form faults at the Earth’s surface.
The faults in Yellowstone vary greatly in age and how they formed and they can be divided into two groups: relatively young faults that have been active in the last 1.6 million years of Earth’s history and older faults that are no longer active. Earthquakes are often associated with many of the younger faults in the park. Young faults in Yellowstone are generally related to one of three geologic origins.
The first is caldera formation and associated volcanism during one of Yellowstone’s three large eruptions.
The second is ground deformation from the ongoing movement of magma beneath Yellowstone.
And the third is tectonic extension of the Basin and Range Province.
Faults related to the Yellowstone volcanic system are found primarily in the center of the park. Caldera boundary faults, such as those at the margin of the Henry’s Fork and Yellowstone calderas, were created as their respective calderas collapsed after an eruption. As lava withdrew from beneath the caldera, the regional surface level dropped and an extensional environment was created, which caused other faults to form outside the caldera margins. The Mirror Lake Plateau is a good example of these types of faults.
Faults also form as a result of the ongoing and episodic rise and fall of the ground in Yellowstone as magma moves through the subsurface. For example, the Mallard Lake and Sour Creek resurgent dome faults, near Old Faithful and Fishing Bridge, respectively, are related to post-eruption deformation inside the Yellowstone caldera. Though largely imperceptible to park visitors, scientists can monitor inflation and deflation of the resurgent domes at the millimeter scale using high-precision GPS.
Other faults in Yellowstone are related to the Basin and Range Province, a region in the western United States characterized by alternating valleys and fault-bounded mountain ranges. The Basin and Range Province began forming at this latitude about 15 million years ago as the earth’s crust was stretched in an east-west direction. The easternmost boundary of the Basin and Range Province reaches western Wyoming, including Yellowstone and the Teton mountain range, and contains faults that are still active and capable of large earthquakes. Whereas other faults in the park are considered to be capable of medium-sized earthquakes, Basin and Range faults could produce larger events.
An example of a large Basin and Range Province earthquake is the 1959 Hebgen Lake earthquake, which registered a magnitude of 7.3 and had an epicenter about 15 miles northwest of West Yellowstone. This event caused the Red Canyon and Hebgen faults to rupture and produced damage across a large area. A landslide triggered by the earthquake dammed the Madison River and formed Earthquake Lake.
Other Basin and Range faults within the borders of Yellowstone include the East Mount Sheridan, Eagle Bay and Upper Yellowstone faults. Scientists consider these faults to be capable of producing large earthquakes, potentially similar to the Hebgen Lake earthquake. Park visitors can see the scarp (surface expression) of the East Mount Sheridan fault by hiking about one mile up the Mount Sheridan trail from Heart Lake.
With so many active processes occurring it’s no wonder that Yellowstone is one of the most seismically active areas in the United States. This is why seismic hazards are such an important issue, not just in Yellowstone, but throughout the western United States.