The MW 6.2 Punta Santa Elena (Coahuila-Zacatecas) earthquake of 28 April 1841, the largest documented pre-instrumental event and its implications on seismic hazard in Northeastern Mexico
In this study, we compiled reports from different catalogs and newspapers about the greatest earthquake documented in Northeastern Mexico. From these descriptions, we located the 28 April 1841 earthquake using the Bakun and Wentworth ( 1997 ) attenuation model for the Basin and Range region. From 13...
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| Veröffentlicht in: | Journal of seismology 2021-04, Vol.25 (2), p.477-485 |
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| creator | Sosa-Ramírez, Rocío L. Paz-Martínez, Edgar G. Montalvo-Arrieta, Juan C. |
| description | In this study, we compiled reports from different catalogs and newspapers about the greatest earthquake documented in Northeastern Mexico. From these descriptions, we located the 28 April 1841 earthquake using the Bakun and Wentworth (
1997
) attenuation model for the Basin and Range region. From 13 observations with an intensity range of III–VII, we calculated a
M
w
6.2 and the central intensity SW from Punta Santa Elena, Coahuila (24.65° N, 101.60° W). This earthquake could represent the fourth biggest event in the Mexican Basin and Range province after the events of Bavispe, Sonora, of 1887 (
M
w
7.5), Parral, Chihuahua, of 1928 (
M
w
6.5), and Valentine, Texas in the Texas-Chihuahua border, of 1931 (
M
w
6.4). Finally, this study provides new insights on earthquake potential in the region to be considered for enhanced hazard quantification and shows that the region is seismically active and prone to events up to
M
> 6. |
| doi_str_mv | 10.1007/s10950-021-09991-2 |
| format | Article |
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1997
) attenuation model for the Basin and Range region. From 13 observations with an intensity range of III–VII, we calculated a
M
w
6.2 and the central intensity SW from Punta Santa Elena, Coahuila (24.65° N, 101.60° W). This earthquake could represent the fourth biggest event in the Mexican Basin and Range province after the events of Bavispe, Sonora, of 1887 (
M
w
7.5), Parral, Chihuahua, of 1928 (
M
w
6.5), and Valentine, Texas in the Texas-Chihuahua border, of 1931 (
M
w
6.4). Finally, this study provides new insights on earthquake potential in the region to be considered for enhanced hazard quantification and shows that the region is seismically active and prone to events up to
M
> 6.</description><identifier>ISSN: 1383-4649</identifier><identifier>EISSN: 1573-157X</identifier><identifier>DOI: 10.1007/s10950-021-09991-2</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Attenuation ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Geological hazards ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Hydrogeology ; Original Article ; Seismic activity ; Seismic hazard ; Seismology ; Structural Geology</subject><ispartof>Journal of seismology, 2021-04, Vol.25 (2), p.477-485</ispartof><rights>The Author(s), under exclusive licence to Springer Nature B.V. part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer Nature B.V. part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2342-4158f3a4156e4347d6456a1d16fe038c24db56db32eba956d279f73186b748af3</citedby><cites>FETCH-LOGICAL-c2342-4158f3a4156e4347d6456a1d16fe038c24db56db32eba956d279f73186b748af3</cites><orcidid>0000-0002-7285-107X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10950-021-09991-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10950-021-09991-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>315,782,786,27931,27932,41495,42564,51326</link.rule.ids></links><search><creatorcontrib>Sosa-Ramírez, Rocío L.</creatorcontrib><creatorcontrib>Paz-Martínez, Edgar G.</creatorcontrib><creatorcontrib>Montalvo-Arrieta, Juan C.</creatorcontrib><title>The MW 6.2 Punta Santa Elena (Coahuila-Zacatecas) earthquake of 28 April 1841, the largest documented pre-instrumental event and its implications on seismic hazard in Northeastern Mexico</title><title>Journal of seismology</title><addtitle>J Seismol</addtitle><description>In this study, we compiled reports from different catalogs and newspapers about the greatest earthquake documented in Northeastern Mexico. From these descriptions, we located the 28 April 1841 earthquake using the Bakun and Wentworth (
1997
) attenuation model for the Basin and Range region. From 13 observations with an intensity range of III–VII, we calculated a
M
w
6.2 and the central intensity SW from Punta Santa Elena, Coahuila (24.65° N, 101.60° W). This earthquake could represent the fourth biggest event in the Mexican Basin and Range province after the events of Bavispe, Sonora, of 1887 (
M
w
7.5), Parral, Chihuahua, of 1928 (
M
w
6.5), and Valentine, Texas in the Texas-Chihuahua border, of 1931 (
M
w
6.4). Finally, this study provides new insights on earthquake potential in the region to be considered for enhanced hazard quantification and shows that the region is seismically active and prone to events up to
M
> 6.</description><subject>Attenuation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Geological hazards</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrogeology</subject><subject>Original Article</subject><subject>Seismic activity</subject><subject>Seismic hazard</subject><subject>Seismology</subject><subject>Structural Geology</subject><issn>1383-4649</issn><issn>1573-157X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9UU1rFTEUHUTBWv0Dri64UTA1X5OZLMujVaFVwYriJtw3c6cvdV7ymmRK9af560z7BHdu7rmE88HNaZrngh8Jzrs3WXDbcsalYNxaK5h80ByItlOsjm8P6656xbTR9nHzJOcrzrntrTpofl9sCM6_gjmS8GkJBeEz3s2TmQLCy1XEzeJnZN9xwEID5ldAmMrmesEfBHEC2cPxLvkZRK_FayjVbsZ0SbnAGIdlS6HQCLtEzIdc0v0DzkA3FQHDCL5k8Nvd7GuAjyFDDJDJ560fYIO_MFVKgA-xhhLmQinAOd36IT5tHk04Z3r2Fw-bL6cnF6t37Ozj2_er4zM2SKUl06LtJ4UVDGmlu9Ho1qAYhZmIq36Qely3ZlwrSWu0dZOdnTolerPudI-TOmxe7H13KV4v9TB3FZcUaqSTrehMp5USlSX3rCHFnBNNrv7KFtNPJ7i768jtO3K1I3ffkZNVpPaiXMnhktI_6_-o_gAr6JTc</recordid><startdate>20210401</startdate><enddate>20210401</enddate><creator>Sosa-Ramírez, Rocío L.</creator><creator>Paz-Martínez, Edgar G.</creator><creator>Montalvo-Arrieta, Juan C.</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-7285-107X</orcidid></search><sort><creationdate>20210401</creationdate><title>The MW 6.2 Punta Santa Elena (Coahuila-Zacatecas) earthquake of 28 April 1841, the largest documented pre-instrumental event and its implications on seismic hazard in Northeastern Mexico</title><author>Sosa-Ramírez, Rocío L. ; Paz-Martínez, Edgar G. ; Montalvo-Arrieta, Juan C.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2342-4158f3a4156e4347d6456a1d16fe038c24db56db32eba956d279f73186b748af3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Attenuation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earthquakes</topic><topic>Geological hazards</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrogeology</topic><topic>Original Article</topic><topic>Seismic activity</topic><topic>Seismic hazard</topic><topic>Seismology</topic><topic>Structural Geology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sosa-Ramírez, Rocío L.</creatorcontrib><creatorcontrib>Paz-Martínez, Edgar G.</creatorcontrib><creatorcontrib>Montalvo-Arrieta, Juan C.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of seismology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sosa-Ramírez, Rocío L.</au><au>Paz-Martínez, Edgar G.</au><au>Montalvo-Arrieta, Juan C.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The MW 6.2 Punta Santa Elena (Coahuila-Zacatecas) earthquake of 28 April 1841, the largest documented pre-instrumental event and its implications on seismic hazard in Northeastern Mexico</atitle><jtitle>Journal of seismology</jtitle><stitle>J Seismol</stitle><date>2021-04-01</date><risdate>2021</risdate><volume>25</volume><issue>2</issue><spage>477</spage><epage>485</epage><pages>477-485</pages><issn>1383-4649</issn><eissn>1573-157X</eissn><abstract>In this study, we compiled reports from different catalogs and newspapers about the greatest earthquake documented in Northeastern Mexico. From these descriptions, we located the 28 April 1841 earthquake using the Bakun and Wentworth (
1997
) attenuation model for the Basin and Range region. From 13 observations with an intensity range of III–VII, we calculated a
M
w
6.2 and the central intensity SW from Punta Santa Elena, Coahuila (24.65° N, 101.60° W). This earthquake could represent the fourth biggest event in the Mexican Basin and Range province after the events of Bavispe, Sonora, of 1887 (
M
w
7.5), Parral, Chihuahua, of 1928 (
M
w
6.5), and Valentine, Texas in the Texas-Chihuahua border, of 1931 (
M
w
6.4). Finally, this study provides new insights on earthquake potential in the region to be considered for enhanced hazard quantification and shows that the region is seismically active and prone to events up to
M
> 6.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s10950-021-09991-2</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0002-7285-107X</orcidid></addata></record> |
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| source | SpringerNature Journals |
| subjects | Attenuation Earth and Environmental Science Earth Sciences Earthquakes Geological hazards Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Hydrogeology Original Article Seismic activity Seismic hazard Seismology Structural Geology |
| title | The MW 6.2 Punta Santa Elena (Coahuila-Zacatecas) earthquake of 28 April 1841, the largest documented pre-instrumental event and its implications on seismic hazard in Northeastern Mexico |
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