Display listing of nearby significant earthquakes

This earthquake caused 28 fatalities and about $11 million damage to highways and timber. It is characterized by extensive fault scarps, subsidence and uplift, a massive landslide, and a seiche in Hebgen Lake. A maximum MM intensity X was assigned to the fault scarps in the epicentral area. The instrumental epicenter lies within the region of surface faulting. The most spectacular and disastrous effect of the earthquke was the huge avalanche of rock, soil, and trees that cascaded from the steep south wall of the Madison River canyon. This slide formed a barrier that blocked the gorge and stoped the flow of the Madison River and within a few weeks, created a lake almost 53 m deep. The volume of material that blocked the Madison River below Hebgen Dam has been estimated at 28-33 million m³. Most of the 28 deaths were caused by rockslides that covered the Rock Creek public campground on the Madison River, about 9.5 km below Hebgen Dam.

New fault scarps as high as 6 m formed near Hebgen Lake. The major fault scarps formed along pre-existing normal faults northeast of Hebgen Lake. Subsidence ocurred over much of an area that was about 24 km north-south and about twice as long east-west. As a result of the faulting near Hebgen Lake, the bedrock beneath the lake was permanently warped, causing the lake floor to drop and generate a seiche. Maximum subsidence was 6.7 m in Hebgen Lake Basin. About 130 km² subsided more than 3 m, and about 500 km² subsided more than 0.3 m. The earth-fill dam sustained significant cracks in its concrete core and spillway, but it continued to be an effective structure.

Many summer houses in the Hebgen Lake area were damaged: houses and cabins shifted off their foundations, chimneys fell, and pipeines broke. Most small-unit masonry structures and wooden buildings along the major fault scarps survived with little damage when subjected only to vibratory forces. Roadways were cracked and shifted extensively, and much timber was destroyed. Highway damage near Hebgen Lake was due to landslides slumping vertically and flowing laterally beneath pavements and bridges, which caused severe cracks and destruction. Three of the five reinforced bridges in the epicentral area also sustained significant damage.

High intensities were observed in the northwest section of Yellowstone National Park. Here, new geysers erupted and massive slumping caused large cracks in the ground from which steam emitted. Many hot springs became muddy.
(above from reference #542)

Reference #1250 lists $26 million dollars damage.