<?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>0256-7024</journal-id>
<journal-title><![CDATA[Revista Geológica de América Central]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Geol. Amér. Central]]></abbrev-journal-title>
<issn>0256-7024</issn>
<publisher>
<publisher-name><![CDATA[Universidad de Costa Rica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0256-70242022000200052</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v67i0.51700</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Application of Scenario Earthquakes for Analysis of Seismically Triggered Landslide Hazard: A Case Study in Costa Rica]]></article-title>
<article-title xml:lang="en"><![CDATA[Aplicación de escenarios de terremotos para el análisis de la amenaza de deslizamientos disparados por sismos: un estudio de caso en Costa Rica]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Seal]]></surname>
<given-names><![CDATA[Dylan M.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jessee]]></surname>
<given-names><![CDATA[M. Anna Nowicki]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hamburger]]></surname>
<given-names><![CDATA[Michael W.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ruiz]]></surname>
<given-names><![CDATA[Paulo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Indiana University Department of Earth &amp; Atmospheric Sciences ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Indiana University - Purdue University Indianapolis Department of Earth Sciences ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Costa Rica (UCR) Escuela Centroamericana de Geología (ECG) ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2022</year>
</pub-date>
<numero>67</numero>
<fpage>52</fpage>
<lpage>75</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242022000200052&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242022000200052&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242022000200052&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se muestran las capacidades de la modelación de escenarios de terremotos hipotéticos como una herramienta para la evaluación de la amenaza de deslizamientos cosismicos. El entorno geológico - tectónico de Costa Rica y sus características orográficas resultaron ideales para probar esta técnica. El modelo trabaja con: pendiente del terreno, velocidad máxima del suelo (VMS), índice topográfico compuesto (ITC), magnitud y profundidad del sismo disparador para pronosticar la probabilidad de deslizamientos y sus efectos. Se examinaron 5 ambientes tectónicos, eventos de subducción en las penínsulas de (1) Nicoya y (2) Osa respectivamente, (3) eventos intraplaca bajo la Cordillera Volcánica Central (CVC) y el (4) Cinturón Deformado del Centro de Costa Rica y (5) eventos en el tras-arco en el Caribe. Los resultados muestran variabilidad en los valores de umbral de pendientes VMS e ITC dependiente del ambiente modelado, para producir probabilidades de disparo de deslizamientos superiores al 10 %. La magnitud del sismo es siempre el principal controlador de la probabilidad máxima de ocurrencia de deslizamientos. Se validaron las predicciones del modelo comparando los resultados con inventarios de deslizamientos observados en los terremotos de Cinchona (2009) y Limón (1991), donde más del 70% de los deslizamientos ocurrieron en zonas con una probabilidad &gt; 20%. Finalmente utilizamos un modelo global de impacto de deslizamientos para predecir los rangos de exposición y letalidad para cada escenario, revelando que los terremotos de tamaño moderado en CDCCR y CVC y los grandes terremotos de subducción representan un peligro potencial significativo para la población de Costa Rica.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract In this study, we demonstrate the capabilities of hypothetical scenario earthquakes as a new tool for assessment of hazards associated with earthquake-triggered landslides. Costa Rica offers an ideal environment for demonstrating the utility of scenario earthquakes due to its diverse tectonic environments and associated widespread seismic hazard, rugged topography, and high landslide susceptibility. We investigate the relative influence of landslide proxies such as topographic slope, peak ground velocity (PGV), and compound topographic index (CTI), and earthquake source parameters such as magnitude and depth, on predicted landslide probability and fatality. We examine five distinct tectonic environments, including subduction events beneath the (1) Nicoya and (2) Osa peninsulas respectively, (3) intraplate earthquakes beneath the Central Volcanic Range (CVR) and (4) the Central Costa Rica Deformed Belt (CCRDB), and (5) back-arc thrust events on the eastern Caribbean coast. Our results demonstrate that the slope, PGV, and CTI thresholds necessary to produce landslide probabilities greater than 10% vary by tectonic environment. In all cases, we observe magnitude to be the primary control on the predicted maximum landslide probability and overall areal landslide coverage. We validate model predictions with observed landslide inventories from the 2009 Cinchona and 1991 Limon earthquakes, demonstrating a good fit, where over 70% of landslides occurring in zones of greater than 20% probability. We also use a global model of landslide impact to predict exposure and fatality ranges for each scenario earthquake of this study, revealing that moderate-sized earthquakes in the CCRDB and CVR and large subduction megathrust earthquakes each pose a significant hazard to Costa Rica&#8217;s population.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[earthquakes]]></kwd>
<kwd lng="en"><![CDATA[coseismic-landslides]]></kwd>
<kwd lng="en"><![CDATA[scenario]]></kwd>
<kwd lng="en"><![CDATA[natural hazards]]></kwd>
<kwd lng="en"><![CDATA[Costa Rica]]></kwd>
<kwd lng="es"><![CDATA[terremotos]]></kwd>
<kwd lng="es"><![CDATA[deslizamientos-cosismicos]]></kwd>
<kwd lng="es"><![CDATA[escenarios]]></kwd>
<kwd lng="es"><![CDATA[peligros]]></kwd>
<kwd lng="es"><![CDATA[Costa Rica]]></kwd>
</kwd-group>
</article-meta>
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