1931 Valentine earthquake
 USGS ShakeMap | |
  Valentine  | |
| UTC time | 1931-08-16 11:40:25 |
|---|---|
| ISC event | 906944 |
| USGS-ANSS | ComCat |
| Local date | August 16, 1931 |
| Local time | 05:40 CST (UTC−06:00) |
| Magnitude | mb5.8 – 6.4[1] |
| Depth | 10 km (6.2 mi)[2] |
| Epicenter | 30°30′07″N 104°34′30″W / 30.502°N 104.575°W (USGS)[3] 30°40′N 104°22′W / 30.66°N 104.37°W (ISC–GEM)[2] |
| Type | Oblique-slip[4] |
| Areas affected | Southwestern U.S., Northern Mexico |
| Total damage | $50,000–$75,000 (1931 USD) |
| Max. intensity | MMI VIII (Severe)[5] |
| Casualties | No fatalities |
In the early morning hours of August 16, 1931, a powerful earthquake occurred in West Texas with a maximum Mercalli intensity of VIII (Severe). Estimates of its magnitude range between 5.8 and 6.4 mb, making it the most powerful earthquake ever recorded in Texas history. Its epicenter was near the town of Valentine, Texas; there, the earthquake caused damage to many homes and buildings.[6] The earthquake may have been caused by movement along oblique-slip faulting in West Texas, the most seismically active region in the state. Shaking from the earthquake was perceptible within a 400 mi (640 km) radius of the epicenter, affecting four U.S. states and northern Mexico. Several foreshocks and aftershocks accompanied the primary temblor, with the aftershocks continuing until at least November 3, 1931. The main earthquake caused no fatalities, though several people sustained minor injuries; the damage in Valentine amounted to $50,000–$75,000 ($962,195–$1,443,293 today).[7]
Geology
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The largest earthquakes in Texas history have occurred in West Texas, which is the state's most seismically active region. Earthquakes have been reported in El Paso – near the state's westernmost extent – since as early as 1887. There are several faults in the region, including the Mayfield Fault, Rim Rock Fault, and Valentine Fault, in addition to other major geologic features such as the Central Basin Platform, the Ouachita Tectonic Front, and the Rio Grande rift. The 1931 Valentine earthquake may have been generated by movement along either the Mayfield or Rim Rock Faults, though no investigation of fault displacement was performed in the area after the earthquake.[1]: 18–21 One 1987 study published in the Bulletin of the Seismological Society of America suggested that the earthquake was caused by either normal or strike-slip faulting at a depth of 6 mi (10 km), with a dip of 54° to the east, a strike of 10–20° and a rake of –150°.[4] The tremor may have resulted in broad subsidence of 4 in (11 mm) over a 10–20 mi (20–30 km) long stretch near Valentine.[1]: 21 Though no surface rupture was reported in connection with the earthquake along a fault,[8] cracks in the alluvium within the nearby Quitman Canyon developed during the earthquake, retaining depths of 7 ft (2.1 m) and widths as wide as 3 ft (0.91 m) at least 17 years after the earthquake.[9]
Earthquake
[edit]The main Valentine earthquake occurred at 5:40 a.m. Central Standard Time (11:40 UTC) on August 16, 1931, with an epicenter near 30°30′07″N 104°34′30″W / 30.502°N 104.575°W, roughly 7 mi (12 km) southwest of Valentine, Texas, and towards the southeastern end of the Rio Grande rift.[3][10] The earthquake was felt across most of Texas and in portions of Kansas, New Mexico, Oklahoma, and northern Mexico, producing perceptible shaking as far as 400 mi (640 km) away from the epicenter.[1]: 147 [11] Its hypocenter was beneath the Lobo Valley, a northwest-trending alluvial plain.[12] Estimates for its magnitude range between mb 5.6–6.4, making it the strongest earthquake in Texas on record.[13]: 1171 The United States Geological Survey (USGS) lists the earthquake as having a magnitude of mbLg 5.8 based on the amplitude of short-period surface Lg waves.[3] The ISC–GEM catalogue lists the earthquake as having a magnitude of Mw 6.3.[3] Seismographs as far as St. Louis, Missouri, recorded both foreshocks and aftershocks beginning on August 16 and continuing well after the main earthquake. The foreshocks drove many people to sleep outdoors, possibly mitigating human casualties caused by the main shock. Numerous aftershocks occurred after the main tremor, particularly in the ensuing eight hours. The strongest aftershock occurred at 1:37 p.m. CST (19:37 UTC) on August 18, cracking walls in Valentine and stopping clocks in El Paso.[1]: 153 The aftershock had a magnitude of approximately 4.2 and produced a maximum intensity of V (Moderate).[1]: 152 [14][15] A magnitude 3.0 or 3.2 aftershock occurred near Valentine at 9:50 a.m. CST (15:50 UTC) on November 3 and was detected by a seismometer in Tucson, Arizona.[1]: 153
Damage
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Shaking from the earthquake was most intense in the Valentine, Texas, area. At Valentine, the shaking intensity reached level VIII (Damaging tremor) on the Rossi–Forel scale and level VIII (Severe) on the Modified Mercalli scale.[16][14] Every building in the town excluding those made from wood frames sustained damage. Many chimneys toppled or cracked following the quake. The local school facility was damaged beyond repair, and its yard sustained minor cracks. Buildings built with adobe had walls collapse, while wooden structures displayed cracked ceilings. Other walls consisting of concrete, brick, and similar materials had large cracks. Damage also occurred in the counties of Brewster, Culberson, Jeff Davis, and Presidio.[5] While there were no fatalities, some minor injuries resulted from falling adobe.[1]: 149 The cost of damage in Valentine amounted to $50,000–$75,000.[17]
Shaking from the earthquake was noticed in the Texas Panhandle, rocking buildings and awakening many people. The Mercalli intensity in Houston was estimated to be as high as III (Weak). The intensity was mild in Ciudad Jiménez, 250 mi (410 km) to the south in Mexico. Although the Houston Post-Dispatch attributed the collapse of homes in Oaxaca City to the Valentine earthquake despite being over 1,080 mi (1,750 km) away from the epicenter, the considerable distance suggested that such effects were caused by a more local earthquake.[1]: 151 Several landslides resulted from the tremor. Such incidents took place in the Van Horn Mountains, the Chisos Mountains, southwest of Lobo, near the Big Bend, and to the northwest near Pilares and Porvenir. In New Mexico, the Guadalupe Mountains also hosted landslides; in Picacho, rock- and mudslides were reported. Hydrologic issues occurred in several artificial water bodies, leading to muddied water.[5]
See also
[edit]References
[edit]- ^ a b c d e f g h i Frohlich, Cliff; Davis, Scott D. (2002). Texas earthquakes. Austin, Texas: University of Texas Press. ISBN 9780292725508. OCLC 614456184.
- ^ a b ISC (2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 2.0, International Seismological Centre
- ^ a b c d "M 5.8 - 12 km SW of Valentine, Texas". Earthquake Hazards Program. United States Geological Survey. Retrieved December 19, 2022.
- ^ a b Doser, Diane I. (December 1987). "The 16 August 1931 Valentine, Texas, earthquake: Evidence for normal faulting in west Texas". Bulletin of the Seismological Society of America. 77 (6). Seismological Society of America: 2005–2017. doi:10.1785/BSSA0770062005 (inactive November 1, 2024).
{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link) - ^ a b c Stover, C. W.; Coffman, J. L. (1993). Seismicity of the United States, 1568–1989 (Revised). United States Geological Survey professional paper 1527. United States Government Printing Office. pp. 362, 364.
- ^ "Quake Stricken in Texas". Retrieved February 7, 2023.
- ^ "Inflation Calculator | Federal Reserve Bank of Minneapolis". minneapolisfed.org. Retrieved February 7, 2023.
- ^ Collins, E. W.; Raney, R. A. (May 19–21, 1993). Quaternary faults of west Texas. 89th Annual Meeting of the Cordilleran Section and the 46th Annual Meeting of the Rock Mountain Section of the Geological Society of America. Reno, Nevada. OSTI 5342399. S2CID 128513416.
- ^ Albritron, Claude C. Jr.; Fred Smith, J. Jr. (1965). "Structure". Geology of the Sierra Blanca Area, Hudspeth County, Texas (Report). United States Geological Survey Professional Paper. United States Government Printing Office. p. 111.
- ^ Doser, Diane I.; Galvan, Paulo (May 2015). "Determining Location and Magnitude of Historical (Pre-1963) Events in the Rio Grande Rift Region Using Intensity Information". Bulletin of the Seismological Society of America. 105 (3): 1562–1575. Bibcode:2015BuSSA.105.1562D. doi:10.1785/0120140264. S2CID 131422395.
- ^ Bodle, R. R., ed. (December 1931). "Preliminary report on the southwest Texas earthquake of August 16, 1931". Seismological Research Letters. 3 (3): 1–3. Bibcode:1931SeiRL...3c...1.. doi:10.1785/gssrl.3.3.1.
- ^ Gordon, David W. (1988). Revised Instrumental Hypocenters and Correlation of Earthquake Locations and Tectonics in the Central United States (Report). United States Geological Survey Professional Paper. United States Government Printing Office.
- ^ Dumas, David B.; Dorman, H. James; Latham, Gary V. (August 1980). "A reevaluation of the August 16, 1931 Texas earthquake". Bulletin of the Seismological Society of America. 70 (4): 1171–1180. doi:10.1785/BSSA0700041171 (inactive November 1, 2024).
{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link) - ^ a b von Hake, C. A. (1977). Earthquake history of Texas (Report). Earthquake Information Bulletin. Vol. 9. United States Geological Survey. pp. 30–32.
- ^ "Earthquakes in Texas". Texas Almanac. Texas State Historical Association. 2022. Retrieved January 20, 2022.
- ^ Byerly, Perry (April 1934). "The Texas earthquake of August 16, 1931". Bulletin of the Seismological Society of America. 24 (2): 81–99. Bibcode:1934BuSSA..24...81B. doi:10.1785/BSSA0240020081.
- ^ "Valentine Is Hard Hit". El Paso Times. No. 227. El Paso, Texas. August 17, 1931. p. 7. Retrieved December 21, 2022 – via Newspapers.com.
External links
[edit]- The International Seismological Centre has a bibliography and/or authoritative data for this event.