<?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>S1026-87742020000100080</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.1.1548</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelado de volúmenes utilizando análisis geomorfológico para el estudio de sedimentos aportados por deslizamientos en el flanco sur del Volcán Pico de Orizaba, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Modeling landslide volume using geomorphologic analysis in the southern flank of Pico de Orizaba Volcano, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Legorreta-Paulín]]></surname>
<given-names><![CDATA[Gabriel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castro]]></surname>
<given-names><![CDATA[Rutilio Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arana-Salinas]]></surname>
<given-names><![CDATA[Lilia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geografía Departamento de Geografía Física]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Posgrado en Geografía ]]></institution>
<addr-line><![CDATA[Ciudad de México México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Autónoma de la Ciudad de México  ]]></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>1</numero>
<fpage>80</fpage>
<lpage>88</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000100080&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000100080&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000100080&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En la presente investigación se muestra el modelado de la relación entre el área y el volumen de deslizamientos en una cuenca de origen volcánico y sedimentario, utilizando un análisis geomorfológico de relieve para caracterizar la inestabilidad potencial de sus laderas. El uso de este método permite una mejor comprensión de la capacidad del aporte del volumen de material producido por deslizamientos, que depende de cada una de las formas del relieve y a su vez del material que lo compone. El análisis está apoyado en los Sistemas de Información Geográfica (SIG), el uso de drones y de técnicas estadísticas para crear un método integral en la estimación del volumen de deslizamientos. Este método se aplicó a la cuenca del Río Chiquito-Barranca del Muerto en el flanco sur del volcán Pico de Orizaba, México. La cuenca es propensa a los procesos gravitacionales debido a sus condiciones fisiográficas (e.g. depósitos volcánicos y sedimentarios altamente intemperizados que forman terrenos montañosos y escarpados, y que se ven afectados por precipitaciones extremas en la época de lluvias) y antropogénicas (de forestación y cambio de uso de suelo). En el área, se cartografiaron más de seiscientos deslizamientos y se agruparon en distintas formas de relieve. Utilizamos un dron para realizar mediciones a detalle de deslizamientos representativos para establecer una relación empírica entre el área del deslizamiento y su volumen. Esta relación, expresada como una ley de potencias con un exponente de escala, se usó para estimar la contribución potencial del material producido por el total de los deslizamientos en cada forma del relieve en la cuenca. El estudio muestra que el método puede ser útil en lugares remotos con difícil acceso e información topográfica escasa. También muestra que las formas del relieve sedimentarias contribuyen con más sedimentos por kilómetro cuadrado, a pesar de tener menos deslizamientos que las formas volcánicas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In this research, the relationship between surface area and volume of landslides in a volcanic watershed is presented, together with the geomorphological analysis of landforms that may lead to slope instability. The use of this method allows a better understanding of the potential landslide volume contribution along homogeneous units. The analysis is supported by Geographic Information Systems (GIS), the use of drones, and statistical techniques to create a comprehensive method for landslide volume estimation for each landform. This approach is applied to the Río Chiquito-Barranca del Muerto watershed on the south flank of Pico de Orizaba volcano, Mexico. The watershed is prone to gravitational processes because of its physical geographical conditions (highly weathered volcanic and sedimentary deposits that form hilly and steep terrains which are affected by extreme seasonal precipitation) and anthropogenic conditions (deforestation and land use change). In the area, more than six hundred landslides were mapped and grouped into different forms of relief. In the study area, representative landslides were measured in detail with the help of a drone to establish an empirical relationship between the area of the landslide and its volume. This relationship, expressed as a power law with a scale exponent, was used to estimate the potential contribution of the material produced by the landslides in each form of the relief, already pre-established in the basin. The study shows that the method can be useful in remote places with difficult access and sparse topographic information. It also shows that sedimentary landforms contribute with more sediments per square kilometer, even though, they have less landslides than the volcanic landforms.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[formas del relieve]]></kwd>
<kwd lng="es"><![CDATA[SIG]]></kwd>
<kwd lng="es"><![CDATA[volcán Pico de Orizaba]]></kwd>
<kwd lng="es"><![CDATA[volúmenes de deslizamientos]]></kwd>
<kwd lng="es"><![CDATA[vehículos aéreos no tripulados]]></kwd>
<kwd lng="es"><![CDATA[dron]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[GIS]]></kwd>
<kwd lng="en"><![CDATA[landforms]]></kwd>
<kwd lng="en"><![CDATA[landslide volumen modeling]]></kwd>
<kwd lng="en"><![CDATA[Pico de Orizaba volcano]]></kwd>
<kwd lng="en"><![CDATA[unmanned aerial vehicle]]></kwd>
<kwd lng="en"><![CDATA[drone]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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