<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742023000200114</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2023.2.1735</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Depósitos de lahar en la subcuenca del Río Cutio, volcán Pico de Tancítaro, Michoacán, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Lahar deposits in the Cutio river subcatchment; Pico de Tancítaro volcano, Michoacán, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Tenorio]]></surname>
<given-names><![CDATA[Felipe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vázquez]]></surname>
<given-names><![CDATA[Rosario]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mendiola]]></surname>
<given-names><![CDATA[Fabiola]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carlón-Allende]]></surname>
<given-names><![CDATA[Teodoro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Unidad Michoacán ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Escuela Nacional de Estudios Superiores ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>México</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>40</volume>
<numero>2</numero>
<fpage>114</fpage>
<lpage>126</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742023000200114&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742023000200114&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742023000200114&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los lahares originados en volcanes inactivos pueden causar pérdidas económicas y de vidas humanas en sus alrededores sin advertencia alguna, especialmente si no se cuenta con un registro de eventos pasados. Estos fenómenos se han estudiado en varias regiones volcánicas de México; sin embargo, en la mayoría de los casos, se carece de registros a largo plazo sobre su frecuencia y magnitud. En la presente investigación evaluamos las características de los depósitos de lahar y otros depósitos volcaniclásticos, históricos y modernos en la subcuenca del Río Cutio, ubicada al noroeste del volcán Pico de Tancítaro, cuyo drenaje natural atraviesa las localidades de Peribán de Ramos y Corona, Michoacán. En esta subcuenca se originó un lahar de tipo hiperconcentrado el día 23 de septiembre de 2018, tras 58 mm de lluvia acumulada en dos horas, que ocasionó el desbordamiento del Río Cutio. El lahar afectó la zona conurbada de Peribán y erosionó profundamente el canal del río, dejando expuestos los depósitos analizados en este trabajo. Para caracterizar dichos depósitos se llevaron a cabo análisis estratigráficos, granulométricos, datación por 14C y análisis de difracción de rayos X. Se identificaron cuatro unidades que se clasificaron, de acuerdo con su distribución granulométrica, como depósitos de flujo de escombros cohesivos. También se reconoció un horizonte interestratificado de caída de escorias y ceniza fechado por 14C en ca. 20970 años a.C. Adicionalmente, se identificaron depósitos dentro y fuera del cauce del Río Cutio, clasificados como flujos hiperconcentrados, asociados al evento de inundación súbita ocurrido en septiembre de 2018. La información obtenida aporta nuevas evidencias de registros históricos del desbordamiento recurrente del Río Cutio, con la formación de flujos hiperconcentrados y flujos de escombros, y también la ocurrencia de flujos de escombros cohesivos por el colapso gravitacional de sectores del Pico de Tancítaro, debilitados por la intensa alteración hidrotermal. En particular, los flujos de escombros cohesivos, por su capacidad de transporte, pueden tener un impacto catastrófico, ocasionando daños severos en la infraestructura civil y urbana, así como pérdida de vidas. Estas condiciones representan un peligro latente no sólo para la localidad de Peribán de Ramos, sino para otras poblaciones aledañas. Aunque el volcán Pico de Tancítaro es considerado como inactivo, los resultados del presente trabajo ponen en evidencia la necesidad de un estudio detallado para definir el peligro asociado a lahares, el cual será fundamental para la mitigación del impacto negativo en las zonas urbanas y agrícolas en áreas de posible inundación, incluyendo las localidades de Peribán de Ramos y Corona, Michoacán.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Lahars originated from inactive volcanoes can cause economic damage and loss of lives in their surroundings without any warning if a record of past events is not available. These phenomena have been studied in several volcanic regions in Mexico; however, in most of those cases, there is a lack of long-term registry of their magnitude and frequency. In this work, we evaluate the features of lahar deposits and other volcaniclastic deposits (historic and modern) found in the Cutio river subcatchment, located in the northwestern flank of Pico de Tancítaro volcano, whose natural drainage crosses the localities of Peribán de Ramos and Corona, in the state of Michoacán. Within this subcatchment, a hyperconcentrated flow took place on September 23, 2018, after 58 mm of accumulated rainfall in 2 hr, which caused the overspill of Cutio river. This event affected the urbanized zone of Peribán and deeply eroded the riverbanks and riverbed of Cutio, leaving ancient deposits exposed along the walls of the river, which were analyzed in this work. To characterize these deposits, we conducted stratigraphic and granulometric analyses, 14C dating, and X-Ray diffraction analysis. From these, we identify four units classified according to their granulometric distribution as cohesive debris flows, whose origin can be associated to discrete flank failures from the western flank of the Pico de Tancítaro volcano. We also recognized a horizon interstratified with these deposits, classified as a pyroclastic fallout of scoria and ash, dated at ca. 20970 yr B.C. by 14C. Apart from these past units, we also identified deposits inside and outside of Cutio riverbed that were classified as hyperconcentrated flows associated with the flood event of September 2018. The data here presented bring to light new evidence about the historic record of lahars at Pico de Tancítaro volcano, including hyperconcentrated and debris flows from overflowing of the Cutio River, and also cohesive debris flows derived from the collapse of hydrothermally altered portion of the edifice. In case that this type of activity occurs in the future, it might have catastrophic consequences for the surrounding areas. Although the Pico de Tancítaro volcano is considered inactive, our results indicate that a detailed lahar hazard evaluation is needed to mitigate their impact in the urban and agricultural zones susceptible to be flooded, including the localities of Peribán de Ramos and Corona, Michoacán.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[estratigrafía volcánica]]></kwd>
<kwd lng="es"><![CDATA[flujos de escombros cohesivos]]></kwd>
<kwd lng="es"><![CDATA[Pico de Tancítaro]]></kwd>
<kwd lng="es"><![CDATA[lahar]]></kwd>
<kwd lng="es"><![CDATA[peligros volcánicos]]></kwd>
<kwd lng="en"><![CDATA[volcanic stratigraphy]]></kwd>
<kwd lng="en"><![CDATA[cohesive debris flows]]></kwd>
<kwd lng="en"><![CDATA[Pico de Tancítaro]]></kwd>
<kwd lng="en"><![CDATA[lahar]]></kwd>
<kwd lng="en"><![CDATA[volcanic hazards]]></kwd>
</kwd-group>
</article-meta>
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