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Love Valley, NC Natural Disasters and Weather Extremes

 
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The chance of earthquake damage in Love Valley is higher than North Carolina average and is lower than the national average. The risk of tornado damage in Love Valley is lower than North Carolina average and is lower than the national average.

Topics:Earthquake IndexVolcano IndexTornado IndexOther Weather Extremes EventsVolcanos NearbyHistorical Earthquake EventsHistorical Tornado Events

Earthquake Index, #34

Love Valley, NC
1.09
North Carolina
0.18
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

Love Valley, NC
0.0000
North Carolina
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, #570

Love Valley, NC
98.56
North Carolina
115.21
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 4,362 other weather extremes events within 50 miles of Love Valley, NC were recorded from 1950 to 2010. The following is a break down of these events:

TypeCountTypeCountTypeCountTypeCountTypeCount
Avalanche:0Blizzard:0Cold:9Dense Fog:4Drought:35
Dust Storm:0Flood:432Hail:1,334Heat:1Heavy Snow:42
High Surf:0Hurricane:12Ice Storm:18Landslide:0Strong Wind:36
Thunderstorm Winds:2,091Tropical Storm:5Wildfire:0Winter Storm:47Winter Weather:54
Other:242 

Volcanos Nearby

No volcano is found in or near Love Valley, NC.

Historical Earthquake Events

No historical earthquake events that had recorded magnitudes of 3.5 or above found in or near Love Valley, NC.

No historical earthquake events found in or near Love Valley, NC.

Historical Tornado Events

A total of 27 historical tornado events that had recorded magnitude of 2 or above found in or near Love Valley, NC.

Distance (miles)DateMagnitudeStart Lat/LogEnd Lat/LogLengthWidthFatalitiesInjuriesProperty DamageCrop DamageAffected County
13.02005-07-07235°50'N / 81°10'W35°52'N / 81°08'W4.00 Miles100 Yards00150K0Alexander
 Brief Description: This tornado touched down near highway 16 just north of the Catawba County line. Two brick homes and a business received severe roof damage in this area, while a mobile home was completely destroyed. The tornado tracked northeast, damaging the roofs of several homes at a mobile home park along Friendship Church Rd before lifting near the intersection of Millersville Rd and Dairy Rd. Numerous trees were also blown down along the tornado path.
14.52005-07-07236°00'N / 80°45'W36°03'N / 80°43'W3.50 Miles200 Yards002.0M400KIredell
 Brief Description: This tornado touched down in the Houstonville Rd area and tracked almost due north. Extensive damage was done to a dairy farm in the Houstonville community, with damage to several other agricultural buildings in the area. In the Misty Rd, Anthony Rd area, the roof was torn off a mobile home as well as another home. The tornado continued to track north, crossing into Yadkin County around Tobacco Rd. At least 13 structures were damaged or destroyed in the county. In addition to the structural damage, damage to tobacco and corn crops was extensive. In addition, numerous trees were blown down along highway 21 and Hunting Creek Rd west of the tornado track. It is unclear whether this was a secondary spin-up or straight-line wind.
20.82010-10-26235°42'N / 81°09'W35°43'N / 81°07'W3.00 Miles100 Yards006.6M0KCatawba
 Brief Description: EVENT NARRATIVE: The tornado touched down initially in an industrial park near Penny Rd, where two large buildings sustained significant roof damage. Part of the exterior wall of one of the buildings collapsed. The tornado moved northeast, causing damage to shingles and siding at several homes on St Vincent Dr. Two outbuildings were thrown 30 to 40 feet and numerous trees were snapped off or uprooted in this area as well. The tornado continued to cause severe damage to trees and generally minor structural damage to homes and a church as it moved northeast toward Catawba St. The damage path continued in a east northeast direction from there, roughly paralleling highway 70. Major roof damage occurred to a food processing plant on highway 70 and several outbuildings were destroyed. Numerous headstones were blown down in a cemetery adjacent to the plant. Numerous trailers were then overturned and part of a building destroyed at a truck depot near Liberty Hill Church Rd. The tornado continued east northeast for about another half mile before lifting. EPISODE NARRATIVE: Scattered supercell thunderstorms developed over the western Carolinas and northeast Georgia as strong wind shear and moderate instability overspread the region ahead of a strong cold front. A number of tornadoes were spawned by the storms. Two strong tornadoes affected the western piedmont and foothills of North Carolina.
21.81998-05-07435°52'N / 81°23'W35°52'N / 81°19'W4.00 Miles1320 Yards021.1M0Caldwell
 Brief Description: A violent, F4 tornado touched down near Dudley Shoals then moved east-southeast cutting a winding path through valleys, to the Alexander county border. The damage path was 100 yards wide on average, but reached a width of 3/4 of a mile at times. One well-constructed home was totally destroyed, other homes were damaged, and many mobile homes sustained damage or were destroyed. Supercell thunderstorms developed in a highly sheared atmosphere in eastern Tennessee then moved east across the mountains, foothills and western piedmont of North Carolina. These long-lived, cyclic supercells produced a considerable amount of large hail and some damaging winds in the mountains. The first tornado of the day in western North Carolina occurred in Madison county. Numerous reports of hail as large as golf balls were reported from the mountains. In Madison and Yancey counties, hail covered roads. More supercell thunderstorms developed behind the previous ones and followed similar tracks. In northern Buncombe county, the town of Barnardsville had three separate severe storms cross overhead and drop hail on the ground to a depth of 3 inches. Yancey county also had 3 separate storms move across the county that accumulated hail to 6 inches in depth. The hail was still on the ground the next morning. As the supercells moved into the foothills, they began to curve a little to the right, indicative of strong mesocyclonic circulations present. One supercell produced several tornadoes from Alexander county to Davie county. Another storm produced a tornado that tracked from western Caldwell county into south-central Alexander county. A third supercell that emerged out of the mountains in McDowell county produced several tornadoes from the southern part of that county to northern Mecklenburg county. Damage was fairly significant across western North Carolina with numerous homes either damaged or destroyed. Fortunately, no one was killed. However, 2 people were injured as a result of the violent F4 tornado in eastern Caldwell county. One person received minor injuries from a lightning strike in Yancey county later in the evening. The storms continued to reform in eastern Tennessee until very late in the evening and still produced large hail as they crossed the border into the mountain counties of North Carolina, before weakening shortly after midnight..
22.41954-08-18235°40'N / 81°12'W35°44'N / 81°09'W5.40 Miles50 Yards0025K0Catawba
25.31951-08-09235°45'N / 81°20'W0.50 Mile100 Yards0025K0Catawba
29.81974-04-04235°49'N / 81°32'W35°52'N / 81°27'W5.70 Miles33 Yards00250K0Caldwell
31.31989-05-05235°57'N / 81°41'W36°01'N / 81°25'W15.00 Miles73 Yards00250K0Caldwell
33.32006-11-15235°31'N / 81°04'W35°30'N / 81°04'W1.00 Mile30 Yards000K0KLincoln
 Brief Description: EVENT NARRATIVE: NWS survey found tornado damage path on the western shores of Lake Norman near Denver. Most of the damage was concentrated in the Lake Shore Rd and Blade Trail areas. Hundreds of trees were downed, many blocking roads, with some down on homes. EPISODE NARRATIVE: A narrow line of showers and thunderstorms developed ahead of a strong cold front during the evening hours of November 15th. As the line moved into North Carolina a series of tornadoes formed along a break in the line. In all, four tornadoes touched down from the east side of Gastonia to a few miles east of Statesville. The strongest tornado produced a small area of F2 damage. One person later died from injuries suffered in the last tornado in Iredell County. Areas of damaging straight line winds also occurred in other parts of the line.
33.42008-05-08235°58'N / 80°24'W35°58'N / 80°23'W000K0KForsyth
 Brief Description: EVENT NARRATIVE: An EF-2 tornado tracked northeast out of Davie County and crossed the Yadkin River into Forsyth County. After crossing the Yadkin River, the tornado touched down near the Old Clemmons Water Treatment Plant along Idols Dam Road. The tornado tracked northeast through a heavily wooded area for just over one quarter of a mile and then lifted off the ground. The parent supercell thunderstorm went on to produce another tornado approximately one mile northeast of the first tornado's ending point. This second tornado went on to produce significant damage to the Clemmons community in Forsyth County. EPISODE NARRATIVE: A strong upper level low moving east-northeast across Kentucky and Tennessee, triggered several instances of severe damaging winds and two tornadoes across the Triad region in the northwest piedmont of North Carolina.
33.91989-05-05236°01'N / 80°23'W0.50 Mile100 Yards082.5M0Forsyth
33.91998-05-07336°01'N / 80°23'W36°01'N / 80°23'W2.00 Miles1 Yards0550.0M0Forsyth
 Brief Description: A large tornado tore through the Waterford Subdivision of Clemmons in southwest Forsyth county. The initial touchdown was at 630 pm local time. Several homes were completely destroyed, several hundred sustained major roof, wall, and window damage. Tree damage was extensive with debris scattered for miles.
34.81989-05-05435°35'N / 81°27'W35°41'N / 81°25'W6.00 Miles800 Yards0325.0M0Catawba
36.22008-05-08335°58'N / 80°22'W36°00'N / 80°19'W3.00 Miles300 Yards022.5M0KForsyth
 Brief Description: EVENT NARRATIVE: This tornado originated from the same parent supercell that produced the tornado in Davie County which lifted in Forsyth County just across the Yadkin River. This second tornado touched down just southwest of Hampton Road. Three metal barns sustained major damage around the 4800 block of Hampton Road with minor damage to two homes. The tornado continued northeast through wooded farmland before hitting the Bridgepoint Subdivision where the tornado strengthened to EF-3 intensity. Three homes were destroyed and approximately thirty homes sustained moderate damage. There were only two minor injuries in the subdivision. The tornado continued to track to the northeast across Frye Bridge Road and through a heavily wooded area. It then dissipated near the intersection of Cooper Road and Fraternity Church Road. A few homes suffered damage, primarily due to fallen trees. Hardwood tree damage in the area was consistent with EF-2 intensity as tree trunks were snapped in a 200 to 300 yard path. The overall path length of the tornado was around 3 miles with a maximum width of 300 yards. EPISODE NARRATIVE: A strong upper level low moving east-northeast across Kentucky and Tennessee, triggered several instances of severe damaging winds and two tornadoes across the Triad region in the northwest piedmont of North Carolina.
38.21998-05-07235°33'N / 81°25'W35°33'N / 81°24'W2.00 Miles440 Yards00212K0Lincoln
 Brief Description: The same supercell that produced the tornado in McDowell county spawned a strong tornado in the Vale and Cat Square area. Four homes were destroyed, 50 homes were damaged, a church roof was partially blown off and numerous trees were downed. Supercell thunderstorms developed in a highly sheared atmosphere in eastern Tennessee then moved east across the mountains, foothills and western piedmont of North Carolina. These long-lived, cyclic supercells produced a considerable amount of large hail and some damaging winds in the mountains. The first tornado of the day in western North Carolina occurred in Madison county. Numerous reports of hail as large as golf balls were reported from the mountains. In Madison and Yancey counties, hail covered roads. More supercell thunderstorms developed behind the previous ones and followed similar tracks. In northern Buncombe county, the town of Barnardsville had three separate severe storms cross overhead and drop hail on the ground to a depth of 3 inches. Yancey county also had 3 separate storms move across the county that accumulated hail to 6 inches in depth. The hail was still on the ground the next morning. As the supercells moved into the foothills, they began to curve a little to the right, indicative of strong mesocyclonic circulations present. One supercell produced several tornadoes from Alexander county to Davie county. Another storm produced a tornado that tracked from western Caldwell county into south-central Alexander county. A third supercell that emerged out of the mountains in McDowell county produced several tornadoes from the southern part of that county to northern Mecklenburg county. Damage was fairly significant across western North Carolina with numerous homes either damaged or destroyed. Fortunately, no one was killed. However, 2 people were injured as a result of the violent F4 tornado in eastern Caldwell county. One person received minor injuries from a lightning strike in Yancey county later in the evening. The storms continued to reform in eastern Tennessee until very late in the evening and still produced large hail as they crossed the border into the mountain counties of North Carolina, before weakening shortly after midnight..
38.32009-05-08236°33'N / 81°02'W36°32'N / 80°57'W5.00 Miles200 Yards06200K0KAlleghany
 Brief Description: EVENT NARRATIVE: A low end EF-2 tornado touched down on Osee Road and was intermittently on the ground approximately 5 miles moving east-southeast, finally lifting between Old Barrett Road and Glade Valley Road. A single wide mobile home was destroyed on Osee Road, causing four injuries. Along the track, cement silos were collapsed, 5 other homes were damaged, and several other structures were heavily damaged. Two people received minor injuries when struck by debris after winds blew out windows in their home. Monetary damages are estimates. EPISODE NARRATIVE: A thunderstorm complex over Kentucky and Tennessee moved east into the area during the evening of May 8th. The storm environment was such that storms would have rotation due to strong wind shear, and a low level boundary in place. Supercells developed over southeast Kentucky and moved southeast into far southwest Virginia and into northwest North Carolina during the late evening of May 8th. One storm produced an EF-2 tornado in Northern Alleghany County, with another brief EF-1 tornado touching down just south of the EF-2 track.
39.72010-03-28235°43'N / 80°22'W35°44'N / 80°21'W1.00 Mile50 Yards051.3M0KDavidson
 Brief Description: EVENT NARRATIVE: An EF1 tornado exited Rowan County, crossing the Yadkin River and entered into Davidson County. Numerous hardwood trees were either sheared off or uprooted in a wooded area south of Seven Oaks Drive. A carport was ripped from a brick home on Seven Oaks Drive. Two out buildings were also destroyed. The tornado tracked northeast across an open field before it damaged a vacant steel framed flea market building. The tornado glanced the southeastern corner of the main flea market building, tearing it away from the remainder of the building. Debris from the metal building was found approximately one mile downstream from the site. Sections of sheet metal from the building were found twisted around several tree and high tension power lines. In the adjacent Chestnut Grove Mobile Home Park, located at the intersection of Clark Road and Wind Hill Drive, three mobile homes were completely destroyed with three other mobile homes sustaining significant damage. The tornado reached EF2 intensity here with wind of 110 to 120 mph. The tornado dissipated in a wooded area northeast of Clark Road. EPISODE NARRATIVE: Convection developed ahead of an amplified upper trough across the Tennessee Valley while a strong southerly mid and upper level jet provided strong shear across the region. Tornadoes formed and track ahead of a developing surface low across Georgia and along a wedge front located across the western Piedmont of NC.
39.72010-10-26235°32'N / 81°28'W35°34'N / 81°26'W3.00 Miles200 Yards0111.2M0KLincoln
 Brief Description: EVENT NARRATIVE: This strong tornado touched down near the intersection of Locust Trail and Tola Houser Lane. Several homes at the beginning of the track received major damage to the roof and exterior wall. One home was shifted off its foundation by nearly 20 feet, with an upstairs room removed. Two vehicles at this location were rolled several yards. The tornado moved northeast across Northbrook III School Rd. Several homes were damaged or destroyed and numerous trees snapped off or uprooted just north of the Reeps Grove Church Rd intersection. The damage path at this point was nearly 200 yards wide. The tornado continued northeast, crossing Macedonia Church Rd, Peeler Rd and Patriot Way, with additional homes as well as barns and a chicken house damaged or destroyed. Numerous trees were uprooted or snapped off in this area as well. As the tornado continued east northeast, damage became more intermittent in the area around Palm Tree Church Rd, where only the tops of trees were snapped. The tornado entered into Catawba County in the vicinity of Dansbury Lane. Eleven people were injured, two seriously. EPISODE NARRATIVE: Scattered supercell thunderstorms developed over the western Carolinas and northeast Georgia as strong wind shear and moderate instability overspread the region ahead of a strong cold front. A number of tornadoes were spawned by the storms. Two strong tornadoes affected the western piedmont and foothills of North Carolina.
39.91989-05-05435°32'N / 81°29'W35°35'N / 81°27'W3.00 Miles800 Yards41925.0M0Lincoln
41.31979-05-24235°45'N / 81°40'W0.30 Mile30 Yards00250K0Burke
42.31985-05-22336°06'N / 80°16'W36°04'N / 80°13'W3.50 Miles200 Yards002.5M0Forsyth
44.62005-01-14235°34'N / 80°23'W35°34'N / 80°23'W0.30 Mile100 Yards00500K0Rowan
 Brief Description: Two metal industrial buildings sustained major damage and a barn was flattened. A home next to the barn also received minor roof damage. Several trees were snapped or uprooted.
45.41989-05-05435°28'N / 81°35'W35°32'N / 81°29'W5.00 Miles800 Yards03025.0M0Cleveland
46.31981-06-06236°04'N / 80°14'W36°10'N / 80°07'W9.40 Miles17 Yards01250K0Forsyth
47.01989-05-05336°06'N / 80°15'W36°13'N / 80°06'W10.50 Miles200 Yards03025.0M0Forsyth
47.11989-05-05236°08'N / 80°13'W36°12'N / 80°08'W5.50 Miles100 Yards0102.5M0Forsyth
48.61965-09-12235°18'N / 80°48'W0.30 Mile70 Yards0025K0Mecklenburg


* 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.


 
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