<?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>S1026-87742023000100059</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2023.1.1709</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Hurricane-induced lahars at Volcán de Colima (México): seismic characterization and numerical modeling]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-Valdés]]></surname>
<given-names><![CDATA[J. Ivonne]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Márquez-Ramírez]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Coviello]]></surname>
<given-names><![CDATA[Velio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Capra]]></surname>
<given-names><![CDATA[Lucia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Consiglio Nazionale delle Ricerche Research Institute for Geo-Hydrological Protection ]]></institution>
<addr-line><![CDATA[Padua ]]></addr-line>
<country>Italia</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>1</numero>
<fpage>59</fpage>
<lpage>70</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742023000100059&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742023000100059&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742023000100059&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Volcán de Colima, one of the most active volcanoes in Mexico, has experienced several volcanic crises over the last century with the emplacement of voluminous block-and-ash flow deposits providing large volumes of loose material along the main ravines. During the rainy season, this material is easily eroded forming lahars. Over 40 events with variable magnitude (105-106 m3) have been detected each year. The largest events that cause damages to infrastructure are usually triggered during the hurricane season (from mid-August to October) when more than 250 mm of rain usually are accumulated over a few days. On 23 October 2015, Hurricane Patricia hit the Volcán de Colima. The hurricane was announced as having reached category 5 thereby representing the largest ever recorded hurricane event in Mexico. It rapidly weakened after landfall but followed a straight trajectory toward the volcano. Up to 400 mm of rain were recorded over 30 hours. The event was recorded at a monitoring station located in the middle reaches of the La Lumbre ravine on the SW flank of the volcano, which was equipped with a rain gauge, a geophone (10 Hz), and a video camera. A multi-pulse lahar started around 8 pm (GMT) and lasted for more than five hours. The seismic signal and the video images were analyzed to identify the timing of the main pulses, the sediment concentrations, and maximum flow peak discharge. Data show that the lahar was characterized by three main pulses, in the range of debris flows with maximum flow-depth of 8 m, interspersed by more dilute tails as hyperconcentrated flow, as also observed from the frequency contents of the seismic signal. A total volume of 2.5 × 106 m3 was estimated based on the strong correlation between the seismic amplitude and the flow discharge. The lahar destroyed one bridge and ~500 m of the interstate road leaving several villages cut off for a few days. Based on the flow magnitude, duration, and the associated damage, this event probably represents the largest one recorded over the last 20 years. The FLO-2D model was used to replicate the observed event to estimate the maximum inundation limits of lahars along the five principal ravines of the volcano, in an attempt to design a hazard map for catastrophic hurricane-induced events.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El Volcán de Colima, uno de los volcanes más activos de México, ha experimentado varias crisis volcánicas durante el último siglo con el emplazamiento de voluminosos depósitos de flujo de bloques y cenizas que ha rellenado las principales barrancas con abundante material inconsolidado. Durante la temporada de lluvias, este material se erosiona fácilmente formando lahares. Se han detectado más de 40 eventos por año, con magnitud variable (105-106 m3). Los eventos más grandes, que normalmente causan daños a la infraestructura, suelen desencadenarse durante la temporada de huracanes (desde mediados de agosto a octubre) con la acumulación de más de 250 mm de lluvia en pocos días. El 23 de octubre de 2015, el huracán Patricia impactó el Volcán de Colima. El huracán fue anunciado como categoría 5, el evento más grande jamás registrado en México; se debilitó rápidamente después de tocar tierra, pero mantuvo una trayectoria directa hacia el volcán. Se registraron hasta 400 mm de lluvia en 30 h. Una estación de monitoreo ubicada a lo largo de la barranca La Lumbre, en el flanco SO del volcán, equipada con un pluviómetro, un geófono (10 Hz) y una cámara de video, registró el evento. El evento comenzó alrededor de las 8 p.m. (GMT) y duró más de 5 horas. La señal sísmica y las imágenes de video fueron analizadas para identificar los pulsos principales y definir la concentración de sedimentos y la descarga pico del flujo. Los datos muestran que el lahar se caracterizó por tres pulsos principales, en el rango de flujos de escombros con una profundidad máxima de 8 m, intercalados por colas más diluidas en el rango de flujos hiperconcentrados, como también se observa a partir de los contenidos de frecuencia de la señal sísmica. Se estimó un volumen total de 2.5×10 6 m3 para el flujo con base en la curva de descarga calculada. El lahar destruyó un puente y ~500 m de la carretera interestatal dejando varios pueblos sin comunicación durante unos días. Con base en la magnitud del lahar, su duración y el daño asociado, este evento probablemente es el más grande registrado durante los últimos 20 años. Se utilizó el modelo FLO-2D para replicar el evento observado, y estimar los límites máximos de inundación del lahar a lo largo de las cinco barrancas principales del volcán, con la intención de elaborar un nuevo mapa de peligro por lahares para eventos asociados a huracanes.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Hurricane Patricia]]></kwd>
<kwd lng="en"><![CDATA[lahar]]></kwd>
<kwd lng="en"><![CDATA[seismic characterization]]></kwd>
<kwd lng="en"><![CDATA[numerical modeling]]></kwd>
<kwd lng="en"><![CDATA[Volcán de Colima]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="es"><![CDATA[Huracán Patricia]]></kwd>
<kwd lng="es"><![CDATA[lahar]]></kwd>
<kwd lng="es"><![CDATA[caracterización sísmica]]></kwd>
<kwd lng="es"><![CDATA[modelado numérico]]></kwd>
<kwd lng="es"><![CDATA[Volcán de Colima]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
</kwd-group>
</article-meta>
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