79545 Zip Code Natural Disasters and Weather Extremes
Hot Rankings
The chance of earthquake damage in 79545 Zip Code is about the same as Texas average and is much lower than the national average. The risk of tornado damage in 79545 Zip Code is lower than Texas average and is higher than the national average.
Earthquake Index, #880
| 79545 Zip Code | 0.02 |
| Texas | 0.04 |
| U.S. | 1.81 |
The earthquake index value is calculated based on historical earthquake events data using USA.com algorithms. It is an indicator of the earthquake level in a region. A higher earthquake index value means a higher chance of an earthquake.
Volcano Index, #1
| 79545 Zip Code | 0.0000 |
| Texas | 0.0000 |
| U.S. | 0.0023 |
The volcano index value is calculated based on the currently known volcanoes using USA.com algorithms. It is an indicator of the possibility of a region being affected by a possible volcano eruption. A higher volcano index value means a higher chance of being affected.
Tornado Index, #1545
| 79545 Zip Code | 173.48 |
| Texas | 208.58 |
| U.S. | 136.45 |
The tornado index value is calculated based on historical tornado events data using USA.com algorithms. It is an indicator of the tornado level in a region. A higher tornado index value means a higher chance of tornado events.
Other Weather Extremes Events
A total of 2,281 other weather extremes events within 50 miles of 79545 Zip Code were recorded from 1950 to 2010. The following is a break down of these events:
| Type | Count | Type | Count | Type | Count | Type | Count | Type | Count |
| Avalanche: | 0 | Blizzard: | 0 | Cold: | 1 | Dense Fog: | 0 | Drought: | 9 |
| Dust Storm: | 1 | Flood: | 221 | Hail: | 1,408 | Heat: | 1 | Heavy Snow: | 8 |
| High Surf: | 0 | Hurricane: | 0 | Ice Storm: | 5 | Landslide: | 0 | Strong Wind: | 9 |
| Thunderstorm Winds: | 585 | Tropical Storm: | 0 | Wildfire: | 3 | Winter Storm: | 5 | Winter Weather: | 9 |
| Other: | 16 | ||||||||
Volcanos Nearby
No volcano is found in or near 79545 Zip Code.
Historical Earthquake Events
A total of 1 historical earthquake event that had a recorded magnitude of 3.5 or above found in or near 79545 Zip Code.
| Distance (miles) | Date | Magnitude | Depth (km) | Latitude | Longitude |
| 44.0 | 1978-06-16 | 5.3 | 10 | 33.03 | -100.77 |
Historical Tornado Events
A total of 46 historical tornado events that had recorded magnitude of 2 or above found in or near 79545 Zip Code.
| Distance (miles) | Date | Magnitude | Start Lat/Log | End Lat/Log | Length | Width | Fatalities | Injuries | Property Damage | Crop Damage | Affected County |
| 2.9 | 1982-05-27 | 2 | 32°26'N / 100°41'W | 32°28'N / 100°31'W | 5.00 Miles | 30 Yards | 0 | 0 | 250K | 0 | Nolan |
| 7.9 | 1982-05-27 | 2 | 32°25'N / 100°44'W | 32°26'N / 100°41'W | 3.00 Miles | 30 Yards | 0 | 0 | 250K | 0 | Mitchell |
| 11.2 | 1986-04-19 | 3 | 32°27'N / 100°26'W | 32°29'N / 100°21'W | 4.50 Miles | 600 Yards | 1 | 100 | 25.0M | 0 | Nolan |
| 12.1 | 1973-03-23 | 2 | 32°28'N / 100°24'W | 32°28'N / 100°21'W | 3.30 Miles | 300 Yards | 0 | 0 | 250K | 0 | Nolan |
| 15.5 | 1968-05-24 | 3 | 32°38'N / 100°36'W | 32°38'N / 100°40'W | 4.10 Miles | 67 Yards | 0 | 0 | 25K | 0 | Scurry |
| 15.7 | 1982-05-27 | 2 | 32°10'N / 100°52'W | 32°25'N / 100°44'W | 15.00 Miles | 30 Yards | 0 | 0 | 250K | 0 | Mitchell |
| 16.9 | 1968-05-24 | 3 | 32°38'N / 100°42'W | 32°39'N / 100°40'W | 2.70 Miles | 100 Yards | 0 | 0 | 25K | 0 | Scurry |
| 16.9 | 2004-06-11 | 2 | 32°10'N / 100°44'W | 32°12'N / 100°36'W | 10.30 Miles | 200 Yards | 0 | 3 | 250K | 0 | Mitchell |
| Brief Description: A National Weather Service damage survey team concluded that a significant tornado struck rural areas of southeastern Mitchell County during the evening of the 11th. The team examined a damage path marked by shredded vegetation (mostly mesquite trees), downed utility poles, agricultural fences, and a complex of destroyed mobile homes that extended over ten miles in a continuous horseshoe shaped path that crossed State Route 208 twenty miles south-southeast of Colorado City. The tornado developed seventeen miles south-southeast of Colorado City around 2028 CST. Damage indicates the tornado's motion was initially toward the southeast then east as it crossed the heavily traveled State Route 208. Two Texas Tech University students traveling north on 208 (south of the tornado's path) watched as a Ford Expedition drove into the tornadic circulation. The large sports utility vehicle was blown 100 yards off of the highway. Evidence supports the vehicle was rolled a considerable distance by the tornadic winds, but it is unclear whether it became airborne. Three motorists were transferred to local hospitals. One person sustained serious injuries that included a broken back. A detailed damage path analysis and corresponding radar data suggest that the tornado then tracked very slowly east a few miles before curving to the northeast. Similar curved damage paths (turning left of the tornado's original motion) are commonly observed when well-developed tornadoes enter the dissipation stage. The tornado proved to remain very dangerous, however, as eight mobile homes were destroyed by the tornado near the end of its life cycle twenty miles southeast of Colorado City. The light weight and unanchored structures were blown over and shredded by the dissipation stage tornadic winds. The trailers were arranged in a complex and were used to provide shelter for groups of hunters that frequent the ranch property. They were not occupied when the tornado struck. In summary, a significant round of severe thunderstorms affected parts of west Texas during the afternoon and evening of the 11th. At least two supercell storms produced giant hail and one strong tornado over the region. A supercell thunderstorm tracked across Terrell County in the west Texas Lower Trans Pecos region during the late afternoon hours. Multiple reports of large hail including two different instances of tennis ball sized stones were received as this storm tracked east along U.S. Highway 90 between Sanderson and Dryden. A second area of convection erupted over the eastern Permian Basin by late afternoon and continued into the evening hours. A severe storm associated with this activity produced half-dollar size hail in the Westbrook community. An isolated classic supercell evolved from this complex of storms and took on a distinctly deviant southeastward storm motion. This storm took on radar characteristics consistent with a classic tornadic supercell. Hail up to the size of golfballs was observed southeast of Colorado City as the storm evolved into its tornadic phase. A long-lived significant tornado tracked across mainly rural areas of Mitchell County just after sunset. The tornado resulted in three injuries when it crossed State Route 208 and blew a vehicle off of the highway. Severe rear flank downdraft winds also resulted in widespread wind damage south of the tornado's path. | |||||||||||
| 18.4 | 1961-03-16 | 2 | 32°24'N / 100°27'W | 32°24'N / 100°04'W | 22.40 Miles | 100 Yards | 0 | 0 | 3K | 0 | Taylor |
| 18.8 | 1968-05-24 | 3 | 32°38'N / 100°46'W | 2.00 Miles | 67 Yards | 0 | 0 | 25K | 0 | Scurry | |
| 19.4 | 1965-05-25 | 2 | 32°09'N / 100°41'W | 2.00 Miles | 200 Yards | 0 | 1 | 250K | 0 | Mitchell | |
| 21.1 | 1962-05-31 | 2 | 32°40'N / 100°22'W | 1.00 Mile | 20 Yards | 0 | 0 | 0K | 0 | Fisher | |
| 25.5 | 1994-05-12 | 2 | 32°47'N / 100°36'W | 2.00 Miles | 75 Yards | 0 | 0 | 500K | 0 | Fisher | |
| 26.1 | 1965-08-31 | 2 | 32°45'N / 100°22'W | 2.00 Miles | 20 Yards | 0 | 0 | 0K | 0 | Fisher | |
| 26.5 | 1963-04-26 | 2 | 32°44'N / 100°55'W | 32°48'N / 100°36'W | 19.00 Miles | 67 Yards | 0 | 0 | 0K | 0 | Scurry |
| 28.1 | 1967-04-12 | 2 | 32°43'N / 100°15'W | 0.20 Mile | 40 Yards | 0 | 0 | 0K | 0 | Fisher | |
| 30.0 | 1969-06-12 | 2 | 32°04'N / 100°16'W | 0.50 Mile | 50 Yards | 0 | 0 | 25K | 0 | Coke | |
| 30.7 | 1967-04-12 | 2 | 32°51'N / 100°28'W | 0.30 Mile | 200 Yards | 0 | 0 | 0K | 0 | Fisher | |
| 32.0 | 1985-04-28 | 2 | 32°08'N / 100°07'W | 32°11'N / 100°07'W | 2.50 Miles | 300 Yards | 1 | 0 | 250K | 0 | Taylor |
| 32.5 | 1962-06-07 | 2 | 32°54'N / 100°32'W | 32°52'N / 100°30'W | 3.60 Miles | 200 Yards | 0 | 0 | 0K | 0 | Fisher |
| 33.0 | 1985-04-28 | 2 | 32°07'N / 100°08'W | 32°08'N / 100°07'W | 1.50 Miles | 300 Yards | 0 | 0 | 250K | 0 | Nolan |
| 34.8 | 1985-04-28 | 2 | 32°36'N / 100°01'W | 3.50 Miles | 400 Yards | 0 | 0 | 25K | 0 | Jones | |
| 35.7 | 1953-07-15 | 2 | 31°54'N / 100°38'W | 1.00 Mile | 33 Yards | 0 | 0 | 3K | 0 | Coke | |
| 39.0 | 1989-05-13 | 2 | 32°35'N / 99°56'W | 1.50 Miles | 150 Yards | 0 | 0 | 0K | 0 | Jones | |
| 40.9 | 1990-04-05 | 2 | 32°35'N / 99°54'W | 0.20 Mile | 10 Yards | 0 | 0 | 0K | 0 | Jones | |
| 41.2 | 1991-05-02 | 2 | 32°53'N / 100°08'W | 0.20 Mile | 10 Yards | 0 | 0 | 25K | 0 | Jones | |
| 41.5 | 1978-07-03 | 2 | 32°29'N / 99°52'W | 0.10 Mile | 50 Yards | 0 | 0 | 250K | 0 | Taylor | |
| 43.0 | 1976-04-15 | 3 | 32°02'N / 100°06'W | 31°58'N / 99°57'W | 9.90 Miles | 33 Yards | 0 | 0 | 25K | 0 | Runnels |
| 43.6 | 2005-06-05 | 2 | 32°34'N / 101°18'W | 32°30'N / 101°19'W | 5.00 Miles | 1300 Yards | 0 | 0 | 80K | 0 | Borden |
| Brief Description: A significant tornado developed in southern Borden County shortly after 18:00 CST. This tornado initially formed just north of Farm to Market Road 1785 three miles west of that highway's intersection with Farm to Market Road 1205. The tornado then slowly moved southwest, and resulted in a wide swath of damage to mesquite trees, road signs, fences, and utility poles as it crossed Farm to Market Road 1785. The tornado's damaging ground circulation briefly dissipated south of Farm to Market Road 1785 in south-central Borden County. Video provided by the public and storm spotters indicated that this phase of the tornado's life cycle was characterized by a condensation funnel that reached half way to the ground with no debris visible near the ground. National Weather Service meteorologists that conducted a damage survey of the tornado's track initially concluded that the broken damage path was likely the result of two separate tornadoes. Photographic evidence, however, supports that the funnel aloft remained well-defined and that the tornado reformed about one mile north of the Borden and Howard County line. The tornado crossed a county road near the Howard County line, and left a three-quarter mile wide swath of damage to mesquite trees and fences. Large drifts of wind blown mud accumulated several feet high along barbed-wire fences on the north side of the tornadoes circulation. A tin shed also was severely damaged. The tornado then moved over plowed fields as it crossed into north-central Howard County. Damage in the Borden County segment of the tornado's path would suggest a weak category rating. This may be largely due to a lack of man made structures that were affected. More significant (F2) damage was observed along the Howard County segment of the damage path. The total path length over Borden and Howard Counties was nine miles. An outbreak of severe thunderstorms and tornadoes affected parts of west Texas during the afternoon and evening of the 5th. Thunderstorms developed along a stationary frontal boundary over the western low rolling plains and the northeastern Permian Basin during the late afternoon. These storms evolved into supercells, and one storm produced a series of tornadoes across southern Borden and northern Howard Counties. By mid evening, a small cluster of organized severe storms evolved and produced more widespread hail, damaging winds, and heavy rainfall. Damages to agricultural interests across the region were significant, and accounted for a majority of the estimated $2.2 million worth of losses reported. | |||||||||||
| 44.1 | 1990-05-14 | 2 | 32°50'N / 100°00'W | 0.20 Mile | 10 Yards | 0 | 3 | 0K | 0 | Jones | |
| 45.4 | 2004-03-04 | 2 | 32°07'N / 99°55'W | 32°14'N / 99°47'W | 10.00 Miles | 440 Yards | 0 | 2 | 800K | 0 | Taylor |
| Brief Description: A quickly moving tornado tore a 10 mile path through southern Taylor County. This tornado hit the community of Tuscola, where it damaged the Jim Ned high school injuring two people. A strong upper level disturbance combined with a strong surface low pressure system moving across West Central Texas produced a significant squall line that moved through the entire San Angelo county warning area. This squall line was accompanied by 60 to 80 MPH winds which produced widespread damage, especially across the Big Country. Embedded within the squall line, were several Supercell thunderstorms which produced nine tornadoes within the San Angelo county warning area. | |||||||||||
| 45.8 | 1982-03-14 | 2 | 32°04'N / 99°55'W | 32°05'N / 99°53'W | 2.00 Miles | 150 Yards | 0 | 0 | 250K | 0 | Runnels |
| 46.0 | 1962-05-25 | 3 | 32°50'N / 100°00'W | 32°53'N / 99°58'W | 4.10 Miles | 67 Yards | 1 | 1 | 25K | 0 | Jones |
| 46.4 | 1971-02-18 | 2 | 32°00'N / 99°57'W | 0.50 Mile | 100 Yards | 0 | 0 | 3K | 0 | Runnels | |
| 46.4 | 1990-05-14 | 2 | 32°53'N / 100°00'W | 0.20 Mile | 10 Yards | 0 | 2 | 0K | 0 | Jones | |
| 47.2 | 1979-10-30 | 2 | 32°13'N / 99°48'W | 0 | 0 | 25K | 0 | Taylor | |||
| 47.5 | 1970-04-26 | 2 | 32°12'N / 99°48'W | 0.10 Mile | 200 Yards | 0 | 0 | 3K | 0 | Taylor | |
| 47.9 | 1965-05-12 | 2 | 32°00'N / 99°57'W | 32°00'N / 99°53'W | 4.10 Miles | 440 Yards | 0 | 1 | 3K | 0 | Runnels |
| 48.2 | 1990-05-14 | 2 | 32°56'N / 100°01'W | 2.00 Miles | 100 Yards | 0 | 2 | 250K | 0 | Jones | |
| 48.4 | 1973-03-10 | 2 | 32°20'N / 99°45'W | 0 | 1 | 25K | 0 | Taylor | |||
| 48.6 | 1971-02-18 | 2 | 31°57'N / 99°57'W | 0.20 Mile | 50 Yards | 0 | 0 | 3K | 0 | Runnels | |
| 48.9 | 1982-03-14 | 3 | 31°52'N / 100°09'W | 32°04'N / 99°42'W | 30.00 Miles | 173 Yards | 0 | 4 | 2.5M | 0 | Runnels |
| 49.0 | 1990-04-05 | 2 | 32°27'N / 99°44'W | 0.20 Mile | 10 Yards | 0 | 0 | 0K | 0 | Taylor | |
| 49.3 | 1982-03-14 | 2 | 32°05'N / 99°53'W | 32°07'N / 99°45'W | 8.00 Miles | 150 Yards | 0 | 0 | 250K | 0 | Taylor |
| 49.9 | 1965-05-15 | 3 | 32°27'N / 99°44'W | 32°35'N / 99°43'W | 9.30 Miles | 100 Yards | 0 | 2 | 250K | 0 | Jones |
| 49.9 | 2005-06-05 | 2 | 32°31'N / 101°24'W | 32°29'N / 101°27'W | 4.00 Miles | 300 Yards | 0 | 0 | 25K | 300K | Howard |
| Brief Description: The long-lived tornado that developed in south-central Borden County crossed into Howard County east of County Road 41. The tornado's damage path narrowed as it moved over a hay field northeast of Luther. Three hundred round bales of hay, weighing 2,000 pounds each, were shredded by the tornadic winds. All of the hay bales were destroyed and the individual straws of hay served as small missiles, stripping mesquite trees of their bark in a thicket to the west. The tornado crossed County Road 41 about two miles south of the Howard and Borden County line. Chunks of asphalt, some up to six inches in diameter, were removed from the road's surface and deposited in an adjacent field. A 250 yard wide swath was cut through mesquite filled range land west of the road. Large mesquite trees were reduced to stumps that only stood a few feet tall, and were partially debarked. A railroad boxcar that was being used for storage was destroyed one mile west of County Road 41. The boxcar broke into three large pieces as it initially bounced along the earth, leaving large craters in the ground, and then was lofted. The three pieces were displaced a mile to the southwest from the boxcar's original location, near the end of the damage path. A National Weather Service damage survey team concluded that a significant rating (F2) was warranted based on the magnitude of tree and vegetation damage, and the lofting and displacement of the railroad boxcar. The tornadoes total path length across Borden and Howard Counties was nine miles, with a maximum path width of three quarters of a mile in south-central Borden County. An outbreak of severe thunderstorms and tornadoes affected parts of west Texas during the afternoon and evening of the 5th. Thunderstorms developed along a stationary frontal boundary over the western low rolling plains and the northeastern Permian Basin during the late afternoon. These storms evolved into supercells, and one storm produced a series of tornadoes across southern Borden and northern Howard Counties. By mid evening, a small cluster of organized severe storms evolved and produced more widespread hail, damaging winds, and heavy rainfall. Damages to agricultural interests across the region were significant, and accounted for a majority of the estimated $2.2 million worth of losses reported. | |||||||||||
* The information on this page is based on the global volcano database, the U.S. earthquake database of 1638-1985, and the U.S. Tornado and Weather Extremes database of 1950-2010.