A Look at Iowa Most Significant Earthquakes

Iowa, despite not being renowned for seismic activity, is not immune to earthquakes. Over its history, the state has encountered notable quakes that have caused damage and unsettled residents. Let’s delve into some of these significant earthquakes and what they reveal about the geological landscape and potential hazards of the region.

The 1867 Waverly Earthquake

The most destructive earthquake in Iowa’s history, the 1867 Waverly earthquake, struck on April 24, 1867, around 9:30 a.m. With an estimated magnitude of 5.5, its epicenter was near Waverly, Bremer County, in northeastern Iowa. The quake’s effects rippled across Iowa and neighboring states, including Minnesota, Wisconsin, Illinois, Missouri, and Nebraska. It resulted in cracked walls, chimneys, and windows, along with toppling furniture and dishes. Notably, it also created a 12-mile-long and 4-foot-wide fissure near the Cedar River, accompanied by rumbling noises and flashes of light.

This earthquake likely stemmed from the reactivation of an ancient fault in the Precambrian basement rocks beneath Iowa’s sedimentary layers. The fault might have been stressed by glacial loading during the Ice Age or regional tectonic forces linked to Missouri’s New Madrid seismic zone. The event underscored Iowa’s seismic vulnerability, hinting at potential future earthquakes.

The 1909 Colfax Earthquake

On September 3, 1909, at approximately 5:40 a.m., the 1909 Colfax earthquake rattled central Iowa. With a magnitude of 5.1, its epicenter was near Colfax, Jasper County. Its tremors extended over 200,000 square miles, affecting states like Iowa, Minnesota, Wisconsin, Illinois, Missouri, Kansas, Nebraska, and South Dakota. Though it caused minor damage, including plaster and brick cracks, and rattling windows and dishes, it also triggered landslides and sand boils along the Des Moines River.

This earthquake likely resulted from fault movement in the Paleozoic sedimentary rocks overlying Iowa’s Precambrian basement. Influences could range from regional tectonic stresses to local factors like groundwater withdrawal or coal mining. The event highlighted Iowa’s susceptibility to moderate earthquakes and suggested the existence of hidden faults underground.

The 1984 Perry Earthquake

The most recent widely felt earthquake in Iowa occurred on October 7, 1984, around 7:46 a.m., near Perry, Dallas County, with a magnitude of 4.5. Its tremors stretched across approximately 400,000 square miles, affecting multiple states. Although it caused no significant damage, it startled many and caused swaying or falling objects. Seismometers across the nation recorded its seismic waves.

Similar to the 1867 Waverly earthquake, the 1984 Perry earthquake likely resulted from fault movement in the Precambrian basement rocks. Regional tectonic stresses or local effects such as groundwater withdrawal or oil and gas production might have triggered the fault. This event emphasized Iowa’s ongoing seismic activity and the potential for larger earthquakes in the future.


These earthquakes demonstrate that Iowa, despite its low seismic reputation, faces notable earthquake risks. Movements in the Precambrian basement or Paleozoic sedimentary rocks, influenced by various natural or human-induced factors, underscore the state’s seismic instability. It’s imperative for residents to acknowledge and prepare for potential seismic hazards. The next significant quake could strike at any time.

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