Fluvanna, TX Natural Disasters and Weather Extremes
Hot Rankings
The chance of earthquake damage in Fluvanna is about the same as Texas average and is much lower than the national average. The risk of tornado damage in Fluvanna is much lower than Texas average and is lower than the national average.
Earthquake Index, #256
| Fluvanna, TX | 0.04 |
| 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
| Fluvanna, TX | 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, #1544
| Fluvanna, TX | 112.27 |
| 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 2,097 other weather extremes events within 50 miles of Fluvanna, TX 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: | 0 | Dense Fog: | 0 | Drought: | 15 |
| Dust Storm: | 0 | Flood: | 230 | Hail: | 1,315 | Heat: | 0 | Heavy Snow: | 0 |
| High Surf: | 0 | Hurricane: | 0 | Ice Storm: | 0 | Landslide: | 0 | Strong Wind: | 0 |
| Thunderstorm Winds: | 520 | Tropical Storm: | 1 | Wildfire: | 0 | Winter Storm: | 3 | Winter Weather: | 0 |
| Other: | 13 | ||||||||
Volcanos Nearby
No volcano is found in or near Fluvanna, TX.
Historical Earthquake Events
A total of 1 historical earthquake event that had a recorded magnitude of 3.5 or above found in or near Fluvanna, TX.
| Distance (miles) | Date | Magnitude | Depth (km) | Latitude | Longitude |
| 30.5 | 1978-06-16 | 5.3 | 10 | 33.03 | -100.77 |
Historical Tornado Events
A total of 29 historical tornado events that had recorded magnitude of 2 or above found in or near Fluvanna, TX.
| Distance (miles) | Date | Magnitude | Start Lat/Log | End Lat/Log | Length | Width | Fatalities | Injuries | Property Damage | Crop Damage | Affected County |
| 21.2 | 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. | |||||||||||
| 24.9 | 1961-06-05 | 2 | 33°13'N / 101°22'W | 33°09'N / 101°20'W | 5.10 Miles | 200 Yards | 0 | 0 | 0K | 0 | Garza |
| 25.4 | 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. | |||||||||||
| 28.5 | 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 |
| 30.3 | 1969-05-05 | 2 | 33°09'N / 101°37'W | 33°11'N / 101°33'W | 4.70 Miles | 33 Yards | 0 | 0 | 3K | 0 | Lynn |
| 30.9 | 1968-05-24 | 3 | 32°38'N / 100°46'W | 2.00 Miles | 67 Yards | 0 | 0 | 25K | 0 | Scurry | |
| 31.1 | 1962-06-16 | 2 | 33°12'N / 101°32'W | 33°18'N / 101°22'W | 11.90 Miles | 33 Yards | 0 | 0 | 0K | 0 | Garza |
| 35.1 | 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 |
| 36.3 | 2009-04-16 | 2 | 32°18'N / 101°34'W | 32°25'N / 101°27'W | 11.00 Miles | 450 Yards | 0 | 0 | 83K | 0K | Howard |
| Brief Description: EVENT NARRATIVE: At 1953 CST, a trained weather spotter reported a tornado about 5 miles northwest of Big Spring. The NWS Storm Survey confirmed two snapped power poles, minor tree damage and an empty oil pump storage tank knocked over near this location. The tornado then tracked north northeastward and bent an 80 foot aluminum radio tower in half towards the east and snapped two additional power poles due to damaging northerly winds on its northwest flank; this occurred sometime around 2000 CST. At 2005 CST, another trained spotter reported a tornado near the town of Fairview, TX. The damage survey concluded this was a valid report, as the tornado began to turn right snapping multiple power poles and damaging a 12???X10??? storage shed anchored 2-3 feet in the ground along the way. The storage shed was tossed east northeast approximately 30 yards, indicating the tornado passed north of the residence. As the tornado continued eastward just north of Farm to Market Road 2230 east of Fairview, a significant line of power pole damage (2 miles) was observed. There were a total of 28 poles snapped towards the south around 2015 CST. Twenty of these were distribution poles and 8 of these were larger transmission poles. The tornado then possibly weakened and turned left to the northeast. On its way, it damaged another storage shed and a home's north side windows approximately 4 miles northeast of Fairview. The last approximated time for tornadic wind damage was around 2030 CST. The path recorded for this event is not the exact path the tornado actually took. Please see attached image. EPISODE NARRATIVE: A mid to upper level closed low was located over southwest Utah the day of the event. Near the surface, a quasi dryline was located from a line near the mountains of west Texas to the eastern NM/TX border. Dewpoints in the low to mid 50 F range resulted in moderate surface based instability east of the dryline during the early evening hours. The upper dynamics combined with the surface convergence along the dryline led to the development of severe weather as the deep layer shear increased with the approach of the aforementioned feature. There was also a brief window for tornadic storms as low level profiles became increasingly backed east of the dryline as height falls increased ahead of the upper trough just west of the region. A tornado watch was issued from 1642-2400 local. | |||||||||||
| 37.4 | 1994-05-12 | 2 | 32°47'N / 100°36'W | 2.00 Miles | 75 Yards | 0 | 0 | 500K | 0 | Fisher | |
| 37.9 | 1970-05-12 | 2 | 33°15'N / 101°41'W | 33°18'N / 101°35'W | 6.80 Miles | 17 Yards | 0 | 0 | 3K | 0 | Lynn |
| 38.0 | 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 |
| 40.9 | 1991-05-07 | 2 | 32°28'N / 101°51'W | 32°30'N / 101°46'W | 3.50 Miles | 120 Yards | 0 | 0 | 250K | 0 | Martin |
| 41.7 | 1957-05-24 | 3 | 33°10'N / 101°47'W | 33°24'N / 101°40'W | 17.50 Miles | 200 Yards | 0 | 1 | 250K | 0 | Lynn |
| 42.0 | 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 |
| 42.2 | 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 |
| 43.6 | 2005-06-12 | 2 | 33°15'N / 100°39'W | 33°14'N / 100°41'W | 2.00 Miles | 1200 Yards | 0 | 0 | 150K | 15K | Kent |
| Brief Description: The National Weather Service in Lubbock, TX conducted a damage survey in Kent County, approximately 8 miles to the northeast of Clairemont. In collaboration with the Center for Severe Weather Research in Boulder, CO and Texas Tech University meteorologists assessing the tornadoes across the county with Doppler-On-Wheels (DOW) data, a better understanding of the wind fields and tornado timing was achieved. The area of assessed damage was bounded by a triangle comprised of FM2320 to the south, FM1228 to the east, and CR112 to the west. There was a damage path characterized by tree damage across the zone. The path of the damage was oriented from a northeast-east to southwest-west direction. DOW data confirmed the large, wedge tornado initially propagated to the east and northeast, became nearly stationary, then rotate southward around the west side of the parent mesocyclone. The tornado moved to the southwest, then south and crossed FM1228 from the north/northeast to the south/southwest. The path of the tornado was between 0.6 to 0.7 miles wide. In assessing the damage, a circulatory patter was evident in a wheat field owned by a private farmer, with all of the wheat laying down to the south. Along this quadrant of the circulation, large farm equipment (tractors and cotton trailers) were tossed and mangled. An 80,000 lb box car was shaken by the tornado and the associated strong wind but was not moved from its location, however the contents inside were disturbed. The farm vehicles were tossed briefly a few times as there were scar marks and impact marks in the field as the equipment was blown to the south. The front-end of one tractor was snapped off after the second impact with the ground, as the vehicle was likely too heavy to remain airborne and was dragged and rolled by the tornadic wind and circulation. On the east side of the circulation, there were tree branches not grown in that immediate area that were stripped clean of bark. A cotton trailer (lighter than the other equipment) was lifted from its original location and was tossed to the north and mangled upon impact. The equipment was tossed approximately 3/10 of a mile within the circulation. It was evident from the damage pattern and debris, the circulation was multi-vortex in nature. The DOW measured wind speeds ranging from 45, 65 and 90 meters per second at various stages of the tornado life cycle at heights between 3 and 50 meters above ground level. | |||||||||||
| 44.2 | 1965-06-08 | 2 | 32°54'N / 102°10'W | 32°54'N / 101°50'W | 19.40 Miles | 17 Yards | 0 | 8 | 25K | 0 | Dawson |
| 45.0 | 1967-04-12 | 2 | 32°51'N / 100°28'W | 0.30 Mile | 200 Yards | 0 | 0 | 0K | 0 | Fisher | |
| 45.5 | 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 |
| 45.5 | 1981-05-07 | 2 | 33°29'N / 101°23'W | 1.50 Miles | 40 Yards | 0 | 0 | 250K | 0 | Crosby | |
| 45.8 | 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 |
| 46.3 | 1991-04-24 | 2 | 33°18'N / 100°45'W | 33°18'N / 100°35'W | 12.10 Miles | 350 Yards | 0 | 0 | 25K | 0 | Kent |
| 46.9 | 1970-05-31 | 2 | 32°30'N / 102°07'W | 32°40'N / 101°52'W | 18.60 Miles | 67 Yards | 0 | 0 | 0K | 0 | Martin |
| 46.9 | 1989-06-06 | 3 | 33°29'N / 101°01'W | 33°29'N / 100°59'W | 1.00 Mile | 900 Yards | 0 | 0 | 25K | 0 | Dickens |
| 47.3 | 1964-06-20 | 2 | 32°15'N / 101°40'W | 0.80 Mile | 23 Yards | 0 | 0 | 3K | 0 | Howard | |
| 47.8 | 1980-06-19 | 2 | 32°50'N / 102°04'W | 2.50 Miles | 100 Yards | 0 | 1 | 25K | 0 | Dawson | |
| 49.4 | 1989-06-06 | 3 | 33°37'N / 101°32'W | 33°29'N / 101°01'W | 29.00 Miles | 900 Yards | 0 | 0 | 25K | 0 | Crosby |
| 49.4 | 1971-05-08 | 2 | 33°24'N / 101°46'W | 2.00 Miles | 67 Yards | 0 | 0 | 25K | 0 | Lubbock | |
* 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.