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Brazos Country, TX Natural Disasters and Weather Extremes

 
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The chance of earthquake damage in Brazos Country is about the same as Texas average and is much lower than the national average. The risk of tornado damage in Brazos Country is lower than Texas average and is higher than the national average.

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

Earthquake Index, #1515

Brazos Country, TX
0.00
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

Brazos Country, 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, #971

Brazos Country, TX
189.71
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 2,312 other weather extremes events within 50 miles of Brazos Country, TX were recorded from 1950 to 2010. The following is a break down of these events:

TypeCountTypeCountTypeCountTypeCountTypeCount
Avalanche:0Blizzard:0Cold:0Dense Fog:0Drought:40
Dust Storm:4Flood:299Hail:802Heat:11Heavy Snow:10
High Surf:0Hurricane:2Ice Storm:12Landslide:0Strong Wind:27
Thunderstorm Winds:891Tropical Storm:4Wildfire:6Winter Storm:8Winter Weather:14
Other:182 

Volcanos Nearby

No volcano is found in or near Brazos Country, TX.

Historical Earthquake Events

No historical earthquake events that had recorded magnitudes of 3.5 or above found in or near Brazos Country, TX.

No historical earthquake events found in or near Brazos Country, TX.

Historical Tornado Events

A total of 65 historical tornado events that had recorded magnitude of 2 or above found in or near Brazos Country, TX.

Distance (miles)DateMagnitudeStart Lat/LogEnd Lat/LogLengthWidthFatalitiesInjuriesProperty DamageCrop DamageAffected County
6.91983-01-31229°47'N / 96°08'W29°50'N / 96°08'W3.00 Miles60 Yards042.5M0Austin
7.61998-10-18229°49'N / 95°56'W29°49'N / 95°56'W1.00 Mile50 Yards1175K0Waller
 Brief Description: Tornado destroyed mobile home. One person killed and another injured in the home. Nine other homes damaged and 2 barns destroyed. M47MH
13.41986-02-05229°50'N / 95°51'W29°50'N / 95°49'W4.00 Miles170 Yards05250K0Waller
15.31992-11-21229°41'N / 95°48'W29°47'N / 95°46'W4.00 Miles200 Yards0625.0M0Harris
16.21986-02-05229°50'N / 95°49'W29°52'N / 95°46'W4.00 Miles170 Yards00250K0Harris
16.41960-02-17229°46'N / 95°48'W29°48'N / 95°44'W4.90 Miles100 Yards0325K0Harris
19.11964-02-04229°36'N / 96°20'W29°37'N / 96°17'W3.80 Miles880 Yards01250K0Colorado
19.31961-03-16229°57'N / 96°16'W0.10 Mile80 Yards003K0Austin
21.11965-04-19329°27'N / 96°00'W0.20 Mile150 Yards1325K0Fort Bend
21.11974-09-13329°35'N / 95°45'W29°37'N / 95°43'W3.60 Miles73 Yards020K0Fort Bend
21.71957-10-14230°03'N / 95°55'W0.50 Mile17 Yards0025K0Waller
22.51962-06-18230°04'N / 95°56'W000K0Waller
22.81992-11-21229°47'N / 95°46'W29°58'N / 95°36'W21.00 Miles200 Yards0525.0M0Harris
23.51981-05-09229°30'N / 95°49'W29°28'N / 95°47'W3.30 Miles40 Yards0025K0Fort Bend
24.21957-10-14230°06'N / 96°06'W1.00 Mile33 Yards0025K0Waller
24.61961-11-22329°24'N / 96°05'W2.00 Miles200 Yards010K0Wharton
25.21957-10-14330°07'N / 96°00'W1.00 Mile33 Yards0025K0Waller
25.81973-02-13229°58'N / 95°43'W29°59'N / 95°40'W3.30 Miles30 Yards0125K0Harris
26.02003-11-17229°37'N / 95°38'W29°37'N / 95°38'W1.50 Miles200 Yards060500K0Fort Bend
 Brief Description: Tornado touched down on west Airport Drive near Industrial in Sugar Land. 60 injuries with 7 people sent to hospital for further treatment. Damage to several office building roofs in Industrial Park. Additional damage to a Daycare facility at West Airport Drive and Dairy Ashford Road. Roof damage to several residential homes in the Meadows subdivision. Reports of several cars overturned or blown off of road along Airport Drive. A total of 24 tornadoes touched down during this 15 hour period of severe weather in southeastern Texas on November 17, 2003. In addition to these tornadoes, a major flood developed over Harris and surrounding counties during the middle of this tornadic outbreak. Over 300 homes, along with hundreds of vehicles, were flooded. These tornadic storms developed over parts of Wharton and Matagorda counties shortly after sunrise with the first confirmed tornado occurring just east of El Campo around 9:00 am. Strong 500mb upper level troughing over the western U.S. moved from west to east across the Southern Plains. The polar jet stream associated with this 500 millibar trough surged into west Texas and then curved sharply northeastward into the Central Plains. The sub-tropical jet stream was oriented west to east across deep southern Texas. This jet stream pattern was the impetus to strong lower level convergence due to the enhanced upper level divergence. Low level moisture had substantially increased and was about 200 percent of normal by 6 AM. Vertical wind profiles also showed a great deal of low level wind shear with the greatest shear occurring in the lowest 2000 feet. In addition, these veering wind speeds rapidly increased with height. A focus for the thunderstorm development was provided by a weak low level boundary which was aligned southwest to northeast, or generally along the U.S. Highway 59 corridor. This feature was nearly-stationary and thunderstorms repeatedly developed and moved along this boundary. The axis of heaviest rain was coincident with this boundary.
26.41950-06-05330°11'N / 96°24'W30°01'N / 96°03'W23.90 Miles67 Yards06250K0Washington
27.01966-03-28329°27'N / 96°20'W29°23'N / 96°12'W9.30 Miles1760 Yards0025K0Colorado
27.51993-04-07229°25'N / 96°17'W0.50 Mile400 Yards0050K0Wharton
 Brief Description: The Wharton Newspaper reported large trees blown down, metal roofs blown off barns and water pump housings blown over on Farm-to-Market Road 2614 northwest of Egypt near the community of Bonus. There were numerous reports of street flooding in the Wharton vicinity.
28.31974-07-14229°47'N / 95°34'W0.80 Mile880 Yards002.5M0Harris
29.11972-03-20229°20'N / 96°05'W0.50 Mile50 Yards0025K0Wharton
29.92003-11-17229°38'N / 95°34'W29°38'N / 95°33'W0.50 Mile50 Yards00300K0Fort Bend
 Brief Description: Tornado touched down in the Meadows subdivision in Fort Bend County and traveled into Harris County. One home lost roof with several other homes damaged. A total of 24 tornadoes touched down during this 15 hour period of severe weather in southeastern Texas on November 17, 2003. In addition to these tornadoes, a major flood developed over Harris and surrounding counties during the middle of this tornadic outbreak. Over 300 homes, along with hundreds of vehicles, were flooded. These tornadic storms developed over parts of Wharton and Matagorda counties shortly after sunrise with the first confirmed tornado occurring just east of El Campo around 9:00 am. Strong 500mb upper level troughing over the western U.S. moved from west to east across the Southern Plains. The polar jet stream associated with this 500 millibar trough surged into west Texas and then curved sharply northeastward into the Central Plains. The sub-tropical jet stream was oriented west to east across deep southern Texas. This jet stream pattern was the impetus to strong lower level convergence due to the enhanced upper level divergence. Low level moisture had substantially increased and was about 200 percent of normal by 6 AM. Vertical wind profiles also showed a great deal of low level wind shear with the greatest shear occurring in the lowest 2000 feet. In addition, these veering wind speeds rapidly increased with height. A focus for the thunderstorm development was provided by a weak low level boundary which was aligned southwest to northeast, or generally along the U.S. Highway 59 corridor. This feature was nearly-stationary and thunderstorms repeatedly developed and moved along this boundary. The axis of heaviest rain was coincident with this boundary.
30.31955-05-23229°19'N / 96°05'W0.50 Mile33 Yards000K0Wharton
30.31974-08-29229°47'N / 95°32'W1.00 Mile67 Yards00250K0Harris
30.82003-11-17229°37'N / 95°33'W29°37'N / 95°33'W0.50 Mile50 Yards00500K0Harris
 Brief Description: Tornado touched down in the Meadows subdivision in Fort Bend County and traveled into Harris County. Tornado moved over the intersection of West Bellfort and Kirkwood. Numerous apartments lost roofs in the extensive SW Village Apartment Complex damage. A total of 24 tornadoes touched down during this 15 hour period of severe weather in southeastern Texas on November 17, 2003. In addition to these tornadoes, a major flood developed over Harris and surrounding counties during the middle of this tornadic outbreak. Over 300 homes, along with hundreds of vehicles, were flooded. These tornadic storms developed over parts of Wharton and Matagorda counties shortly after sunrise with the first confirmed tornado occurring just east of El Campo around 9:00 am. Strong 500mb upper level troughing over the western U.S. moved from west to east across the Southern Plains. The polar jet stream associated with this 500 millibar trough surged into west Texas and then curved sharply northeastward into the Central Plains. The sub-tropical jet stream was oriented west to east across deep southern Texas. This jet stream pattern was the impetus to strong lower level convergence due to the enhanced upper level divergence. Low level moisture had substantially increased and was about 200 percent of normal by 6 AM. Vertical wind profiles also showed a great deal of low level wind shear with the greatest shear occurring in the lowest 2000 feet. In addition, these veering wind speeds rapidly increased with height. A focus for the thunderstorm development was provided by a weak low level boundary which was aligned southwest to northeast, or generally along the U.S. Highway 59 corridor. This feature was nearly-stationary and thunderstorms repeatedly developed and moved along this boundary. The axis of heaviest rain was coincident with this boundary.
31.11986-02-05230°01'N / 95°37'W2.50 Miles70 Yards002.5M0Harris
31.11983-05-20229°54'N / 96°06'W29°55'N / 95°00'W4.00 Miles333 Yards12250K0Harris
31.41970-10-23229°18'N / 96°00'W1.20 Miles33 Yards0025K0Wharton
31.51964-06-15229°18'N / 96°06'W1.50 Miles20 Yards003K0Wharton
31.51966-04-14229°18'N / 96°06'W1.00 Mile33 Yards000K0Wharton
32.41970-10-23229°18'N / 95°54'W1.50 Miles27 Yards0025K0Wharton
35.21971-02-25230°10'N / 96°23'W0.30 Mile33 Yards003K0Washington
35.21971-02-25230°10'N / 96°23'W0.30 Mile33 Yards000K0Washington
35.81986-02-05330°02'N / 95°33'W29°59'N / 95°29'W5.00 Miles70 Yards2025.0M0Harris
36.01983-02-09229°39'N / 95°27'W1.50 Miles50 Yards03250K0Harris
36.31983-05-20229°50'N / 95°32'W29°56'N / 95°22'W12.00 Miles333 Yards172.5M0Harris
36.81965-09-22330°13'N / 95°44'W0.80 Mile33 Yards000K0Montgomery
37.31979-09-18229°44'N / 95°25'W1.00 Mile350 Yards012.5M0Harris
38.21953-12-02229°12'N / 96°02'W1.50 Miles200 Yards003K0Wharton
38.41983-05-20230°04'N / 95°34'W30°04'N / 95°27'W7.00 Miles333 Yards152.5M0Harris
39.51964-05-01230°18'N / 96°12'W30°20'N / 96°07'W5.60 Miles880 Yards0025K0Washington
40.01966-06-18229°48'N / 95°24'W29°51'N / 95°21'W4.90 Miles27 Yards000K0Harris
42.11967-09-21229°56'N / 95°22'W2.00 Miles50 Yards033K0Harris
43.11970-10-27229°53'N / 95°20'W2.00 Miles40 Yards000K0Harris
43.21953-12-02230°22'N / 96°11'W250K0Washington
43.21992-11-21229°42'N / 95°23'W29°47'N / 95°15'W12.00 Miles200 Yards0625.0M0Harris
43.71967-09-21229°34'N / 96°44'W1.00 Mile33 Yards003K0Colorado
44.71971-02-25229°44'N / 96°47'W0.50 Mile50 Yards0025K0Colorado
44.81955-06-05229°42'N / 96°47'W000K0Colorado
45.81971-02-25229°48'N / 96°48'W0.50 Mile50 Yards000K0Fayette
46.11983-02-09229°29'N / 95°21'W29°34'N / 95°17'W8.00 Miles50 Yards0025K0Brazoria
46.11983-11-19230°24'N / 96°14'W1.10 Miles100 Yards002.5M0Brazos
46.31978-05-29229°48'N / 95°16'W0.20 Mile20 Yards00250K0Harris
47.41964-04-17229°55'N / 95°23'W29°42'N / 95°07'W21.90 Miles27 Yards123K0Harris
47.61981-05-03229°26'N / 95°19'W29°32'N / 95°18'W7.20 Miles73 Yards010250K0Brazoria
47.81971-02-25229°48'N / 96°50'W0.50 Mile50 Yards000K0Fayette
48.61976-03-08329°22'N / 95°26'W29°27'N / 95°14'W13.40 Miles200 Yards0182.5M0Brazoria
48.62003-11-17229°40'N / 95°14'W29°40'N / 95°14'W0.70 Mile100 Yards00550K0Harris
 Brief Description: Tornado touched down just east of Highway 288 in the Third Ward. One church completely destroyed, 50 homes damaged, and extensive tree damage. Wind damage to several downtown buildings in SE Houston near Minute Maid ballpark. A total of 24 tornadoes touched down during this 15 hour period of severe weather in southeastern Texas on November 17, 2003. In addition to these tornadoes, a major flood developed over Harris and surrounding counties during the middle of this tornadic outbreak. Over 300 homes, along with hundreds of vehicles, were flooded. These tornadic storms developed over parts of Wharton and Matagorda counties shortly after sunrise with the first confirmed tornado occurring just east of El Campo around 9:00 am. Strong 500mb upper level troughing over the western U.S. moved from west to east across the Southern Plains. The polar jet stream associated with this 500 millibar trough surged into west Texas and then curved sharply northeastward into the Central Plains. The sub-tropical jet stream was oriented west to east across deep southern Texas. This jet stream pattern was the impetus to strong lower level convergence due to the enhanced upper level divergence. Low level moisture had substantially increased and was about 200 percent of normal by 6 AM. Vertical wind profiles also showed a great deal of low level wind shear with the greatest shear occurring in the lowest 2000 feet. In addition, these veering wind speeds rapidly increased with height. A focus for the thunderstorm development was provided by a weak low level boundary which was aligned southwest to northeast, or generally along the U.S. Highway 59 corridor. This feature was nearly-stationary and thunderstorms repeatedly developed and moved along this boundary. The axis of heaviest rain was coincident with this boundary.
48.71971-03-09229°35'N / 95°15'W1.00 Mile440 Yards0425K0Harris
49.31981-05-09230°27'N / 95°45'W30°23'N / 95°43'W5.10 Miles40 Yards0225K0Montgomery
49.41969-09-08329°42'N / 95°13'W0.80 Mile50 Yards0025K0Harris
49.61954-04-30230°08'N / 96°49'W30°12'N / 96°37'W12.80 Miles880 Yards0025K0Fayette


* 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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