<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692025000101455</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2025.64.1.1810</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The Chuquibamba Landslide Western Cordillera, Peru revisited: New evidence of a dry debris avalanche]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Núñez]]></surname>
<given-names><![CDATA[J.M.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Macias]]></surname>
<given-names><![CDATA[J.L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arce]]></surname>
<given-names><![CDATA[J.L.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gómez]]></surname>
<given-names><![CDATA[J.C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Instituto Politécnico Nacional Centro Interdisciplinario de Investigaciones y Estudios sobre Medio Ambiente y Desarrollo ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[Cd. De México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[Cd. De México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Instituto Geofísico del Perú  ]]></institution>
<addr-line><![CDATA[Lima ]]></addr-line>
<country>Perú</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2025</year>
</pub-date>
<volume>64</volume>
<numero>1</numero>
<fpage>1455</fpage>
<lpage>1477</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692025000101455&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692025000101455&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692025000101455&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Landslides represent a serious mountain hazard to lives and infrastructure, especially when geological factors such as highly fractured rocks, faulting, steep topography, and weathering combine with seismic triggering factors. Considering the potential of producing outcomes, we study the Chuquibamba rotational landslide that runs along the NW-SE Incapuquio-Challaviento fault system in southernmost Peru. Its elongated U-shaped and polylobate crown scarp is typical of fault-related landslides, and it is carved into the ignimbrites of the Chuquibamba Formation. The geomorphology of the failure and its associated deposit define seventeen coalescing rotational slides and a widespread debris avalanche. This deposit, the main topic of this study, dated at ca. 102 ± 5 ka using 10Be (from previous works), is confined to the lower parts of the Grande River valley. It is exposed for about 22.5 km from 3,900 to 1,167 masl with its main front located at ~ 10 km upstream of the Majes River. It covers an area of 33.64 km2 with a minimum volume of 0.72 km3. The resulting deposit has an H/L = 0.12, which is typical of dry debris avalanches elsewhere. It consists of block and matrix facies that have different textural and granulometric features. At the time of its emplacement, the moving avalanche overpassed 20 and 12 m-high obstacles, attaining minimum speeds of 20 and 15 m/s at distances of 15 and 20 km from the source, respectively. After the landslide emplacement, the debris avalanche was re-mobilized by intense rains that produced debris flows, as attested by outcrops along the extension of the debris avalanche and beyond its front. All the features of the Chuquibamba dry avalanche, along with modern seismicity and the intersection of active faults in the region, suggest that the failure had a tectonic origin (uplift and movement along faults) instead of deglaciation, extraordinary rain, or extreme rock weathering. Therefore, landslide generation is a potential hazard in this area of Peru.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Los deslizamientos en zonas montañosas representan un serio peligro para la vida e infraestuctura, en particular cuando se combinan factores geológicos con factores sísmicos que los pueden detonar. Considerando la posibilidad de generación de estos procesos, estudiamos el caso del deslizamiento rotacional de Chuqibamba, que se alinea a lo largo del sistema de fallas NW-SE Incapuquio-Challaviento en el extremo sur del Perú. La forma elongada en "U" del deslizamiento y su corona de escarpe poli-lobulada, son rasgos típicos de deslizamientos relacionados con fallas que afectaron hasta las ignimbritas de la Formación Chuquibamba. La geomorfología del colapso y depósitos asociados, definen diecisiete bloques rotacionales coaslescentes y un depósito extenso de avalancha de escombros. Este depósito, objeto de este estudio, fechado en aproximadamente 102 ± 5 ka por 10Be (tomado de trabajos previos), está confinado en el valle del Río Grande. Aflora a lo largo de 22.5 km, desde los 3,900 hasta 1,167 msnm con el frente principal ubicado a ~10 km río arriba del Río Majes. El depósito cubre un área de 33.64 km2, un volumen mínimo de 0.72 km3 con un H/L = 0.12, típico de flujos de escombros secos. La avalancha superó obstáculos de 20 y 12 m de altura, con velocidades mínimas de 20 y 15 m/s a distancias de 15 y 20 km desde la fuente respectivamente. Después del emplazamiento del colapso, la avalancha de escombros fue removilizada por lluvias intensas produciendo flujos de escombros, tal como quedó registrado en los afloramientos en todo el depósito y más allá de éste. Todas las características de la avalancha seca de Chuquibamba, junto con la sismicidad moderna de la región, sugieren que el colapso tuvo un origen tectónico (levantamiento y movimiento a lo largo de fallas), más que deglaciación, lluvias extraordinarias o intemperismo severo de las rocas. Por lo tanto, la generación de deslizamientos es un peligro potencial en esta zona del Perú.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Rotational landslide]]></kwd>
<kwd lng="en"><![CDATA[debris avalanche]]></kwd>
<kwd lng="en"><![CDATA[facies]]></kwd>
<kwd lng="en"><![CDATA[Chuquibamba]]></kwd>
<kwd lng="en"><![CDATA[Peru]]></kwd>
<kwd lng="es"><![CDATA[Deslizamiento rotacional]]></kwd>
<kwd lng="es"><![CDATA[avalancha de escombros]]></kwd>
<kwd lng="es"><![CDATA[facies]]></kwd>
<kwd lng="es"><![CDATA[Chuquibamba]]></kwd>
<kwd lng="es"><![CDATA[Perú]]></kwd>
</kwd-group>
</article-meta>
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