<?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>1794-9165</journal-id>
<journal-title><![CDATA[Ingeniería y Ciencia]]></journal-title>
<abbrev-journal-title><![CDATA[ing.cienc.]]></abbrev-journal-title>
<issn>1794-9165</issn>
<publisher>
<publisher-name><![CDATA[Escuela de Ciencias y Humanidades y Escuela de Ingeniería de la Universidad EAFIT]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1794-91652019000200033</article-id>
<article-id pub-id-type="doi">10.17230/ingciencia.15.30.2</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelo geométrico tridimensional para macizos rocosos a partir de fotografías y el programa Octave: Cantera Santa Rita, Medellín, Colombia]]></article-title>
<article-title xml:lang="en"><![CDATA[Three-Dimensional Geometric Model for Rock Masses from Photographs and the Octave Program: Cantera Santa Rita, Medellín, Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Suarez-Burgoa]]></surname>
<given-names><![CDATA[Ludger O.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Castro-Caicedo]]></surname>
<given-names><![CDATA[Alvaro J.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional de Colombia  ]]></institution>
<addr-line><![CDATA[Medellín ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional de Colombia  ]]></institution>
<addr-line><![CDATA[Medellín ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>15</volume>
<numero>30</numero>
<fpage>33</fpage>
<lpage>56</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S1794-91652019000200033&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S1794-91652019000200033&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S1794-91652019000200033&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El presente artículo expone el procedimiento para lograr el modelo geométrico tridimensional de un macizo rocoso a partir de un par de tomas fotográficas hechas con una cámara corriente, uso de software libre/abierto como Octave y otras librerías libres, construcción de equipos y herramientas sencillos y la apropiación de conocimientos importantes en visión artificial. Se describe tomando como ejemplo el modelo tridimensional de un corte de voladura del macizo rocoso de la Cantera Santa Rita, localizada al sudoeste de la ciudad de Medellín (Colombia). Finalmente, se muestra mediante una validación, a partir de medidas de campo in situ, que el procedimiento descrito aquí es promisorio para que pueda instaurarse como una herramienta para la caracterización geométrica de discontinuidades de los macizos rocosos.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The present article exposes the procedure to achieve the three-dimensional geometric model of a rock mass from a pair of photographic shots made with a current camera, use of free/open software such as Octave and other free libraries, construction of equipment and simple tools and the appropriation of important knowledge in artificial vision. It is described taking as an example the three-dimensional model of a blast cut of the rock mass of the Santa Rita Quarry, located southwest of the city of Medellín (Colombia). Finally, it is shown by a validation, based on field measurements, that the procedure described here is promising so that it can be established as a tool for the geometric characterization of discontinuities of rock mass.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Visión artificial]]></kwd>
<kwd lng="es"><![CDATA[geometría epipolar]]></kwd>
<kwd lng="es"><![CDATA[orientación de discontinuidades]]></kwd>
<kwd lng="es"><![CDATA[macizos rocosos]]></kwd>
<kwd lng="en"><![CDATA[Computer vision]]></kwd>
<kwd lng="en"><![CDATA[epipolar geometry]]></kwd>
<kwd lng="en"><![CDATA[discontinuity orientation]]></kwd>
<kwd lng="en"><![CDATA[rock mass]]></kwd>
</kwd-group>
</article-meta>
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