<?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>S1026-87742020000200109</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.2.1556</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis de flujos de escombros desde un enfoque dendrocronológico en Ixtacamaxtitlán, Sierra Norte de Puebla, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Debris flows analysis based on dendrochronological approach at Ixtacamaxtitlán, Sierra Norte de Puebla, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pablo-Pablo]]></surname>
<given-names><![CDATA[Marco Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Franco-Ramos]]></surname>
<given-names><![CDATA[Osvaldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alcántara-Ayala]]></surname>
<given-names><![CDATA[Irasema]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></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 Geografía ]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>37</volume>
<numero>2</numero>
<fpage>109</fpage>
<lpage>120</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000200109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000200109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000200109&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Los procesos de remoción en masa son una de las amenazas geomorfológicas más importantes en México, debido a sus potenciales consecuencias como el desastre ocurrido en octubre de 1999 en las montañas de la Sierra Norte de Puebla, donde cientos de procesos de remoción ocasionaron graves daños a la población. El propósito de este estudio fue la reconstrucción de flujos de escombros en dos valles localizados en el Cerro Tenextepecuaco, dentro de la Sierra Norte de Puebla, con base en métodos geomorfológicos y dendrocronológicos. Se estudiaron 37 árboles de Juniperus deppeana, para elaborar una cronología de referencia local, así como para fechar y mapear los flujos de escombros y determinar la estabilidad del relieve con base en la edad de los árboles. El análisis comparativo de las curvas de lluvia máxima en 24 hrs, para el periodo de mayo a octubre de 1992 a 2013, y el Índice de Ancho de Anillo (IAA) revelaron que en agosto de 2007 y agosto de 2010 se reactivaron dos canales del valle poniente como consecuencia de las intensas lluvias de 93 y 56 mm respectivamente, las cuales generaron supresión de los anillos de crecimiento de algunos árboles. También, en esos años, se observó una mayor dinámica geomorfológica con importantes cambios en la cubierta vegetal, observados en las imágenes de satélite de Google EarthTM. En el 2013 los árboles registraron ligeras supresiones y los canales permanecieron activos. A partir del 2014 la especie mostró realces y, en las imágenes, se observó una recolonización de árboles, lo que sugiere una aparente estabilización geomorfológica. Los resultados expuestos demuestran el potencial de Juniperus deppeana en México para estudios dendrogeomorfológicos, mismos que se pueden utilizar para enriquecer los planes de prevención y mitigación de peligros naturales en la zona de estudio.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Owing to their potential consequences, such as the disaster triggered by hundreds of landslides in October 1999 in the mountain range Sierra Norte de Puebla, mass movement processes are among the most significant geomorphological hazards in Mexico. In this paper, we presented the reconstruction and analysis of debris flows at two valleys located on the Tenextepecuaco mountain in the Sierra Norte de Puebla, based on geomorphologic and dendrogeomorphic methods. From 37 Juniperus deppeana trees we made a Local Reference Chronology, also to dating and mapping the debris flow events and finally for determine the stability/instability of the landforms using the age of the trees. The comparative analysis of the maximum rainfall series in 24 hours, for the period from May to October from 1992 to 2013, and the tree-ring width index suggested that in August 2007 and August 2010 two channels of the western valley were reactivated triggered by heavy rainfall amounting 93 and 56 mm, respectively. As a result of such event, some tree-rings series recorded a growth suppression, and that was also observed in satellite images by Google EarthTM through changes in the vegetation cover. Other trees showed a less growth suppressions in 2013 and the channels were kept active. Since 2014, some trees showed a growth release, and recolonization of trees was also identified in the satellite imagery by Google EarthTM, suggesting an apparent geomorphological stability. The applied methodology showed the potential of Juniperus deppeana to be used for dendrogeomorphic studies in México, also in others geomorphic context. Additionally, particular results of the study can contribute to the existing efforts on prevention and mitigation of natural hazards within the regional context.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[flujos de escombros]]></kwd>
<kwd lng="es"><![CDATA[dendrogeomorfología]]></kwd>
<kwd lng="es"><![CDATA[Juniperus deppeana]]></kwd>
<kwd lng="es"><![CDATA[Ixtacamaxtitlán]]></kwd>
<kwd lng="es"><![CDATA[Puebla]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[debris Flow]]></kwd>
<kwd lng="en"><![CDATA[dendrogeomorphology]]></kwd>
<kwd lng="en"><![CDATA[Juniperus deppeana]]></kwd>
<kwd lng="en"><![CDATA[Ixtacamaxtitlán]]></kwd>
<kwd lng="en"><![CDATA[Puebla]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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