The Friday morning earthquake was caused by a slip on the preexisting Lost River Fault.[9] The event is the largest and most significant to strike in the state of Idaho. As a result of extreme surface faulting, a maximum Mercalli intensity of IX (Violent) was decided upon, while vibrational damage was at a Mercalli intensity of VI (Strong) to VII (Very strong).[4] Three weeks later on November 18, PresidentRonald Reagan declared the earthquake a major disaster.[10][11]
Aftershocks were felt for a year afterwards;[12] nearly ten months later, a 5.4 aftershock was recorded on August 22, 1984.[11][13][14]
Surface faulting
The rupture caused clear surface faulting; a 21-mile (34 km) long northwest-trending zone of fresh scarps and ground ruptures was present on a slope of the Lost River Range. Extensive breakage occurred along a five-mile (8 km) zone between West Spring and Cedar Creek; ground surface was literally "shattered" into tilted blocks, each several meters in width. These scarps were as broad as 330 feet (100 m).[4]
A segment of the Borah Peak earthquake fault scarp near Willow Creek
The ground breakage was sixty miles (100 km), and the throw on the faulting ranged from −1.6 to 8.9 feet (−0.5 to 2.7 m).[15]
Damage
The Challis-Mackay region experienced rather thorough damage, with eleven commercial buildings and 39 homes sustaining major damage while another 200 houses suffered minor to moderate damage. Mackay in particular, about fifty miles (80 km) southeast of Challis, experienced the most severe damage. Most of the city's large buildings on its Main Street were damaged, to some extent;[16] eight of these buildings were deemed condemned and closed down. Most of these buildings were built from materials such as brick, concrete block, and stone, each varying.[4]
An estimated $12.5 million in property damage was recorded. In some places, the water grounds shifted.[11]
Fatalities and injuries
In Challis, two children were killed when a stone storefront collapsed on them while walking to school; two others suffered minor injuries. In Mackay, a woman was hospitalized due to her injuries.[17]
Old Faithful
After the earthquake and aftershocks, the eruption intervals of Old Faithful geyser in Yellowstone National Park, about 150 miles (240 km) east, were noticeably lengthened.[18]
Near Chilly Buttes of Thousand Springs Valley, a series of artesian fountains/sand blows erupted immediately after the main shock. Groundwater gushed from these fountains forming small craters and depositing aprons of light-colored sandy sediment around each crater. The blows were noted largely along waterways, especially where draws, or small streams, enter into larger ones. Observers noted that some blows had black, sediment-laden water while others ran mostly clear. Some blows continued for several minutes after the shaking stopped. The Big Lost River rose several inches as a result of this water being expelled from the ground. The eruptions were likely a response to liquefaction of a water-laden underground sediment layer.[19]
Fault scarps that outline the graben produced near Willow Creek
Payne, S. J. (2004), "Stress Triggering of Conjugate Normal Faulting: Late Aftershocks of the 1983 Ms 7.3 Borah Peak, Idaho, Earthquake", Bulletin of the Seismological Society of America, 94 (3): 828–844, Bibcode:2004BuSSA..94..828P, doi:10.1785/0120030122
Reagor, Glen; Baldwin, F.W. (1984), "Intensity survey of the Borah Peak, Idaho, earthquake of October 28, 1983", Open-File Report, doi:10.3133/ofr84166
Stover, C.W. (1984), "Preliminary isoseismal map and intensity distribution for the Borah Peak, Idaho, earthquake of October 28, 1983", Open-File Report, doi:10.3133/ofr84297
Suzette M. Jackson, John Boatwright; Strong ground motion in the 1983 Borah Peak, Idaho, earthquake and its aftershocks. Bulletin of the Seismological Society of America ; 77 (3): 724–738.
