<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-27T12:51:29Z</responseDate><request verb="GetRecord" identifier="oai:uvadoc.uva.es:10324/52606" metadataPrefix="dim">https://uvadoc.uva.es/oai/request</request><GetRecord><record><header><identifier>oai:uvadoc.uva.es:10324/52606</identifier><datestamp>2022-03-23T21:52:55Z</datestamp><setSpec>com_10324_1161</setSpec><setSpec>com_10324_931</setSpec><setSpec>com_10324_894</setSpec><setSpec>col_10324_1318</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:doc="http://www.lyncode.com/xoai" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="cef666fa559dbbb7" confidence="600" orcid_id="0000-0001-9760-3876">Serrano Cañadas, Enrique</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="419fbd9b-98ac-47b9-82ed-b2c0590256ae" confidence="600" orcid_id="">Giner Robles, Jorge Luis</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="dacc4942-11f6-43e7-9cae-5b786477c625" confidence="600" orcid_id="">Gumiel Martínez, Pablo</dim:field>
<dim:field mdschema="dc" element="contributor" qualifier="author" authority="8e55b658-a997-4971-b322-2c219f8ee07c" confidence="600" orcid_id="">López Martínez, Jerónimo</dim:field>
<dim:field mdschema="dc" element="date" qualifier="accessioned">2022-03-23T12:49:56Z</dim:field>
<dim:field mdschema="dc" element="date" qualifier="available">2022-03-23T12:49:56Z</dim:field>
<dim:field mdschema="dc" element="date" qualifier="issued">2004</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="citation" lang="es">Cuaternario y geomorfología: Revista de la Sociedad Española de Geomorfología y Asociación Española para el Estudio del Cuaternario, Vol. 18, Nº. 1-2, 2004, págs. 13-24</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="issn" lang="es">0214-1744</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="uri">https://uvadoc.uva.es/handle/10324/52606</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationfirstpage" lang="es">13</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationissue" lang="es">1-2</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationlastpage" lang="es">24</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationtitle" lang="es">Cuaternario y geomorfología</dim:field>
<dim:field mdschema="dc" element="identifier" qualifier="publicationvolume" lang="es">18</dim:field>
<dim:field mdschema="dc" element="description" lang="es">Producción Científica</dim:field>
<dim:field mdschema="dc" element="description" qualifier="abstract" lang="es">El glaciar rocoso de Hurd constituye un buen ejemplo del ambiente periglaciar en la Antártida marítima.&#xd;
La realización de seis sondeos eléctricos verticales en el mismo y su entorno inmediato ha permitido caracterizar su estructura interna y la presencia de permafrost a una profundidad de aproximadamente dos metros. El glaciar rocoso forma parte del sistema de derrubios del ámbito de transición entre un medio glaciar y otro periglaciar con permafrost continuo. El estudio detallado del glaciar rocoso y su entorno mediante la cartografía geomorfológica y los sondeos eléctricos ha permitido aproximarnos al conocimiento del sistema de transferencia de derrubios asociado a glaciares rocosos en la Antártida marítima.</dim:field>
<dim:field mdschema="dc" element="description" qualifier="abstract" lang="es">The Hurd rock glacier is a good example of the periglacial environment in maritime Antarctica. By means&#xd;
of six vertical electric sounding in the rock glacier and sourounding, its internal structure and the presence of permafrost at about 2 m depth have been pointed out. The rock glacier is an element of the debris morphodynamic system in the transition from a glacial environment to the periglacial one with continuous permafrost. The detailled study of the rock glacier and his sourounding from geomorphological map and electric sounding has let to know the debris transfer system linked to the rock glacier on maritime Antarctica.</dim:field>
<dim:field mdschema="dc" element="description" qualifier="project" lang="es">Plan Nacional de I+D (proyecto ANT98-0225)</dim:field>
<dim:field mdschema="dc" element="description" qualifier="project" lang="es">Plan Nacional de I+D (proyecto REN2001-0643)</dim:field>
<dim:field mdschema="dc" element="format" qualifier="mimetype" lang="es">application/pdf</dim:field>
<dim:field mdschema="dc" element="language" qualifier="iso" lang="es">spa</dim:field>
<dim:field mdschema="dc" element="publisher" lang="es">Asociación Española para el Estudio del Cuaternario</dim:field>
<dim:field mdschema="dc" element="publisher" lang="es">Sociedad Española de Geomorfología</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="accessRights" lang="es">info:eu-repo/semantics/openAccess</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="uri" lang="*">http://creativecommons.org/licenses/by-nc-nd/4.0/</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="holder" lang="es">© Asociación Española para el Estudio del Cuaternario</dim:field>
<dim:field mdschema="dc" element="rights" qualifier="holder" lang="es">© Sociedad Española de Geomorfología</dim:field>
<dim:field mdschema="dc" element="rights" lang="*">Attribution-NonCommercial-NoDerivatives 4.0 Internacional</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Glaciares</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Geomorfología - Regiones polares</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Regiones antárticas - Geografía</dim:field>
<dim:field mdschema="dc" element="subject" lang="es">Antártida</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="unesco" lang="es">54 Geografía</dim:field>
<dim:field mdschema="dc" element="subject" qualifier="unesco" lang="es">2506.07 Geomorfología</dim:field>
<dim:field mdschema="dc" element="title" lang="es">El glaciar rocoso de Hurd: estructura e inserción en el sistema de transferencia de derrubios antártico marítimo (isla Livingston, islas Shetland del sur, Antártida)</dim:field>
<dim:field mdschema="dc" element="title" qualifier="alternative">The Hurd rock glacier: structure and insertion in the debris transfer system of Maritime Antarctica (Livingston Island, South Shetland Islands, Antarctica)</dim:field>
<dim:field mdschema="dc" element="type" lang="es">info:eu-repo/semantics/article</dim:field>
<dim:field mdschema="dc" element="type" qualifier="hasVersion" lang="es">info:eu-repo/semantics/publishedVersion</dim:field>
<dim:field mdschema="dc" element="relation" qualifier="publisherversion" lang="es">https://recyt.fecyt.es/index.php/CUGEO/article/view/17024</dim:field>
<dim:field mdschema="dc" element="peerreviewed" lang="es">SI</dim:field>
</dim:dim></metadata></record></GetRecord></OAI-PMH>