FAQs about US Seismic Zones

Seismic zones are geographic regions classified according to their likelihood of experiencing earthquakes and the expected level of ground shaking. These zones help engineers, planners, and government agencies design buildings, infrastructure, and emergency preparedness strategies that can withstand seismic activity. Areas with higher seismic risk require stricter building codes and earthquake-resistant construction standards.
The highest earthquake risk in the United States is found along the West Coast, particularly in California, Alaska, Washington, Oregon, and Hawaii. California is especially vulnerable due to the San Andreas Fault and numerous other active fault systems. Alaska experiences more earthquakes than any other U.S. state because of its location along the Pacific Ring of Fire.
The New Madrid Seismic Zone is a major earthquake-prone region located in the central United States, primarily affecting parts of Missouri, Arkansas, Tennessee, Kentucky, and Illinois. It is best known for the powerful series of earthquakes that occurred between 1811 and 1812. Scientists continue to monitor the area because it remains one of the most active seismic regions east of the Rocky Mountains.
Yes, earthquakes can occur throughout much of the United States. While California experiences the most well-known earthquakes, significant seismic activity also occurs in Alaska, Washington, Oregon, Hawaii, Nevada, Utah, Idaho, Oklahoma, South Carolina, and the New Madrid Seismic Zone in the central United States. Even regions with lower seismic risk can experience occasional earthquakes.
U.S. seismic hazard zones are determined using geological studies, historical earthquake records, fault mapping, ground motion models, and scientific assessments conducted by organizations such as the U.S. Geological Survey (USGS). These analyses estimate the probability and intensity of future earthquakes and help guide building codes and land-use planning.
Seismic zones are important because they help ensure that buildings, bridges, dams, and other structures are designed to withstand expected earthquake forces. Construction requirements vary depending on the level of seismic risk in a particular area. Following seismic design standards helps reduce property damage, prevent structural failures, and save lives during earthquakes.