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Linville, NC Natural Disasters and Weather Extremes

 
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The chance of earthquake damage in Linville is about the same as North Carolina average and is much lower than the national average. The risk of tornado damage in Linville is much lower than North Carolina average and is much lower than the national average.

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

Earthquake Index, #151

Linville, NC
0.20
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

Linville, 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, #891

Linville, NC
44.88
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 3,149 other weather extremes events within 50 miles of Linville, NC were recorded from 1950 to 2010. The following is a break down of these events:

TypeCountTypeCountTypeCountTypeCountTypeCount
Avalanche:0Blizzard:0Cold:4Dense Fog:0Drought:1
Dust Storm:0Flood:376Hail:968Heat:0Heavy Snow:35
High Surf:0Hurricane:8Ice Storm:5Landslide:0Strong Wind:18
Thunderstorm Winds:1,525Tropical Storm:5Wildfire:5Winter Storm:33Winter Weather:6
Other:160 

Volcanos Nearby

No volcano is found in or near Linville, NC.

Historical Earthquake Events

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

No historical earthquake events found in or near Linville, NC.

Historical Tornado Events

A total of 21 historical tornado events that had recorded magnitude of 2 or above found in or near Linville, NC.

Distance (miles)DateMagnitudeStart Lat/LogEnd Lat/LogLengthWidthFatalitiesInjuriesProperty DamageCrop DamageAffected County
8.11965-04-09236°11'N / 81°56'W0.50 Mile300 Yards0125K0Avery
18.81989-05-05235°57'N / 81°41'W36°01'N / 81°25'W15.00 Miles73 Yards00250K0Caldwell
25.31979-05-24235°45'N / 81°40'W0.30 Mile30 Yards00250K0Burke
26.61974-04-04235°49'N / 81°32'W35°52'N / 81°27'W5.70 Miles33 Yards00250K0Caldwell
32.31998-05-07435°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..
32.71998-05-07235°37'N / 81°59'W35°37'N / 81°59'W3.70 Miles880 Yards00482K0Mcdowell
 Brief Description: Another supercell which tracked across the mountains spawned a tornado that travelled through a portion of Glenwood. Several homes and mobiles 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..
37.51951-08-09235°45'N / 81°20'W0.50 Mile100 Yards0025K0Catawba
39.21989-05-05435°35'N / 81°27'W35°41'N / 81°25'W6.00 Miles800 Yards0325.0M0Catawba
40.41962-06-03236°36'N / 82°12'W0025K0Washington
41.91957-04-08236°17'N / 82°35'W36°19'N / 82°33'W3.00 Miles440 Yards003K0Washington
42.41989-05-05435°32'N / 81°29'W35°35'N / 81°27'W3.00 Miles800 Yards41925.0M0Lincoln
43.02005-07-07235°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.
43.42010-10-26235°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.
44.21989-05-05435°28'N / 81°35'W35°32'N / 81°29'W5.00 Miles800 Yards03025.0M0Cleveland
44.61998-05-07235°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..
46.41967-04-22236°12'N / 82°41'W0.20 Mile250 Yards00250K0Greene
46.71954-08-18235°40'N / 81°12'W35°44'N / 81°09'W5.40 Miles50 Yards0025K0Catawba
48.11975-05-18235°23'N / 81°50'W003K0Rutherford
48.32010-10-26235°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.
49.01975-01-25236°47'N / 81°46'W36°47'N / 81°44'W1.30 Miles30 Yards0025K0Washington
49.81975-01-25236°47'N / 81°44'W36°48'N / 81°42'W1.90 Miles30 Yards0225K0Smyth


* 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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