PAGER - M 3.0 - EASTERN TENNESSEE
Population exposure estimates are NOT a direct estimate of earthquake damage; comparable shaking will result in significantly lower losses in regions with well built structures than in regions with vulnerable structures. Overall, the population in this region resides in structures that are a mix of vulnerable and earthquake resistant construction.
Exposure Summary
Estimated Population Exposed to Earthquake Shaking
| Est. Modified Mercalli Intensity | Est. Population Exposure | Perceived Shaking | Potential Structure Damage | |
|---|---|---|---|---|
| Resistant | Vulnerable | |||
| X | 0 | Extreme | V. Heavy | V. Heavy |
| IX | 0 | Violent | Heavy | V. Heavy |
| VIII | 0 | Severe | Moderate/Heavy | Heavy |
| VII | 0 | Very Strong | Moderate | Moderate/Heavy |
| VI | 0 | Strong | Light | Moderate |
| V | 0 | Moderate | V. Light | Light |
| IV | 0 | Light | none | none |
| II-III | 460k* | Weak | none | none |
| I | 1,997k* | Not Felt | none | none |
Full City Exposure List
| MMI | City | Population |
|---|---|---|
| II | Cleveland | 37k |
| II | East Cleveland | 2k |
| II | South Cleveland | 6k |
| II | Wildwood Lake | 3k |
| II | Hopewell | 2k |
| II | Benton | 1k |
| II | Tunnel Hill | 1k |
| II | Varnell | 2k |
| I | Harrison | 8k |
| I | Red Bank | 12k |
| I | Collegedale | 8k |
| I | Middle Valley | 11k |
| I | Ooltewah | 6k |
| I | Soddy-Daisy | 12k |
| I | Indian Springs | 2k |
| I | East Brainerd | 15k |
| I | Lakesite | 2k |
| I | Ringgold | 3k |
| I | East Chattanooga | 154k |
| I | East Ridge | 20k |
| I | Dayton | 6k |
| I | Chattanooga | 156k |
| I | Chatsworth | 4k |
| I | Fairmount | 3k |
| I | Fairview | 7k |
| I | Fort Oglethorpe | 8k |
| I | Lakeview | 5k |
| I | Rossville | 3k |
| I | Etowah | 4k |
| I | Athens | 14k |
| I | Signal Mountain | 7k |
| I | Walden | 2k |
| I | Dalton | 32k |
| I | Chickamauga | 2k |
| I | Decatur | 1k |
| I | Graysville | 1k |
| I | Vonore | 1k |
| I | Bridgeport | 3k |
| I | Cedar Bluff | 2k |
| I | Centre | 3k |
| I | Collinsville | 2k |
| I | Crossville | 1k |
| I | Fort Payne | 14k |
| I | Fyffe | 1k |
| I | Henagar | 3k |
| I | Rainsville | 5k |
| I | Stevenson | 2k |
| I | Sylvania | 1k |
| I | Adairsville | 3k |
| I | Blue Ridge | 1k |
| I | Calhoun | 14k |
| I | Canton | 18k |
| I | Cartersville | 18k |
| I | Chattanooga Valley | 4k |
| I | Cleveland | 2k |
| I | Cumming | 6k |
| I | Dahlonega | 4k |
| I | Ellijay | 2k |
| I | Euharlee | 4k |
| I | Flowery Branch | 2k |
| I | Gainesville | 33k |
| I | Holly Springs | 3k |
| I | Jasper | 3k |
| I | LaFayette | 7k |
| I | Lindale | 4k |
| I | Lookout Mountain | 2k |
| I | Lula | 2k |
| I | McCaysville | 1k |
| I | Oakwood | 3k |
| I | Raoul | 2k |
| I | Rome | 35k |
| I | Shannon | 2k |
| I | Summerville | 5k |
| I | Trenton | 2k |
| I | Trion | 2k |
| I | Andrews | 2k |
| I | Murphy | 2k |
| I | Alcoa | 8k |
| I | Altamont | 1k |
| I | Clinton | 9k |
| I | Crossville | 10k |
| I | Dunlap | 5k |
| I | Eagleton Village | 5k |
| I | Englewood | 2k |
| I | Fairfield Glade | 7k |
| I | Farragut | 19k |
| I | Greenback | 1k |
| I | Gruetli-Laager | 2k |
| I | Harriman | 7k |
| I | Jasper | 3k |
| I | Kimball | 1k |
| I | Kingston | 5k |
| I | Knoxville | 172k |
| I | Lake Tansi | 3k |
| I | Lenoir City | 8k |
| I | Lookout Mountain | 2k |
| I | Loudon | 5k |
| I | Louisville | 2k |
| I | Madisonville | 4k |
| I | Maryville | 27k |
| I | Mascot | 2k |
| I | McMinnville | 13k |
| I | Midtown | 1k |
| I | Monteagle | 1k |
| I | New Hope | 1k |
| I | Oak Ridge | 27k |
| I | Oliver Springs | 3k |
| I | Pikeville | 2k |
| I | Powells Crossroads | 1k |
| I | Rockwood | 5k |
| I | Sewanee | 2k |
| I | Seymour | 10k |
| I | Smithville | 4k |
| I | South Pittsburg | 3k |
| I | Sparta | 5k |
| I | Spencer | 2k |
| I | Spring City | 2k |
| I | Sweetwater | 6k |
| I | Tracy City | 2k |
| I | Whitwell | 2k |
PAGER results are generally available on the Internet within 30 minutes of the earthquake’s occurrence. However, information on the extent of shaking will be uncertain in the minutes and hours following and earthquake and typically improves as additional sensor data and reported intensities are acquired and incorporated into models of the earthquake's source. Users of PAGER estimates should account for uncertainty and always seek the most current PAGER release for any earthquake.

