Persona:
Jordá Pardo, Jesús Francisco

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0000-0002-3937-9199
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Jordá Pardo
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Jesús Francisco
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    Los mamíferos del Cuaternario kárstico de Guadalajara (Castilla - La Mancha, España)
    (Array, 1999-01-01) Arribas Herrera, Alfonso; Jordá Pardo, Jesús Francisco
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    Charcoal analysis at the San Chuis hill fort (Allande, Asturias, Spain).
    (Ernestina Badal, Yolanda Carrión, Miguel Macías, María Ntinou (Coords.),, 2013-03-04) Badal, Ernestina; Carrión Marco, Yolanda; Jordá Pardo, Jesús Francisco
    The archaeological site of the San Chuis hill fort (Allande, Asturias, Spain) is located in the central part of the western Cantabrian Range. The site was occupied between 920 - 480 cal BC (2870 - 2430 cal BP) and 100 cal BC - 540 cal AD (2050 - 1410 cal BP). Repeated and long-lasting occupation resulted in the overlapping of architectural structures from the first and second Iron Ages and the Roman Period. The study of the wood charcoal remains from these structures allows us to distinguish two groups of wood remains. Those timbers used in the construction of the buildings and those used as firewood.
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    Los depósitos kársticos y su contribución al conocimiento del medio Ambiente en España durante el Cuaternario
    (ITGE-ENRESA, 2009-02-17) Jordá Pardo, Jesús Francisco
    Jordá Pardo, J.F. (1993): Los depósitos kársticos y su contribución al conocimiento del medio Ambiente en España durante el Cuaternario. Síntesis del Medio Ambiente en España durante los dos últimos millones de años. Instituto Tecnológico Geominero de España y ENRESA - Contrato CEC FI2W-CT91-0075. Commission of the European Communities, Directorate General for Science, Research and Developement. Madrid: 105-128.
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    Excavaciones arqueológicas en la Cueva de La Güelga.(Cangas de Onís. Asturias).
    (2011-11-30) Carral Gonzalez, Pilar; Trancho, Gonzalo; Álvarez Alonso, David; Rojo Hernández, Julio Antonio; Wood, Rachel; Menéndez Fernández, Mario; Quesada López, José Manuel; Jordá Pardo, Jesús Francisco; Gómez García, Eduardo; https://orcid.org/0000-0002-6289-691X
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    Una aproximación geoarqueológica al hábitat humano pleistoceno del occidente cantábrico (Asturias, norte de España)
    (Universidad Nacional de Educación a Distancia (UNED). Centro Asociado de Asturias, 2014-01-01) Álvarez Alonso, David; Iriarte Chiapusso, María José; Jordá Pardo, Jesús Francisco
    El objetivo de este trabajo se centra en presentar las características geológicas y geomorfológicas del extremo occidental de la región cantábrica y los principales aspectos geomorfológicos, geoarqueológicos y paleoambientales relacionados con la actividad humana desarrollada en ese territorio durante el Pleistoceno. Todos estos aspectos han condicionado tanto las características del hábitat humano a lo largo de los tiempos paleolíticos como las distintas adaptaciones que los grupos humanos tuvieron que llevar a cabo para poder desarrollar sus modos de vida y garantizar su supervivencia.
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    El registro arqueológico del Pleistoceno superior final en el abrigo de la Peña de Estebanvela (S de la Cuenca del Duero, Segovia, España).
    (Array, 2004) Cacho Quesada, Carmen; Ripoll López, Sergio; Jordá Pardo, Jesús Francisco; Muñoz Ibáñez, Francisco Javier
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    Cova Rosa revisited. New geoarchaeological research at the Upper Pleistocene – Lower Holocene site of Cova Rosa (Sardéu, Ribadesella, Asturias, Spain)
    (2022-09-12) Jordá Pardo, Jesús Francisco; Carral Gonzalez, Pilar; Duarte, Carlos; Maestro, Adolfo; Maximiano, Alfredo; Molina, Juana; Obeso, Ramón; Colectivo Espeleológico L´Esperteyu Cavernícola Espeleo Club; Alvarez-Fernandez, Esteban; https://orcid.org/0000-0002-6289-691X
    The karstic cavity of Cova Rosa (Sardéu, Ribadesella, Asturias), developed in the La Escalada limestones (Moscovien, Carboniferous), contains an important archaeosedimentary sequence covering the Late Upper Pleistocene and the Lower Holocene. This sequence, excavated during the second half of the 20th century by Jordá Cerdá and Gómez Fuentes (1982), presents levels of Solutrense, Lower and Upper Magdalenian and Mesolithic. The sequence was studied sedimentologically by Hoyos Gómez (1979). In the last years members of a large research team are working again on this site and its materials (Álvarez-Fernández and Jordá Pardo, 2018) and in this contribution we present the new lithostratigraphic sequence that has been studied again with geoarchaeological methodology. In addition, thanks to the 22 radiocarbon dates obtained (Álvarez-Alonso et al., 2021), we can place the sequence on the Quaternary chronostratigraphic scale
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    Study of the access routes to the Castilian plateau through the Sella River valley (Asturias, Spain) during the end of the Upper Palaeolithic
    (Elsevier, 2022-12-18) Válles Fernández, Manuel Amalio; Menéndez Fernández, Mario; Jordá Pardo, Jesús Francisco; Cocero Matesanz, David
    The Sella River valley (Asturias, Spain) has been and is currently a benchmark in Palaeolithic discoveries and research. The location and the number of archaeological sites along its orography certify a significant human presence in the valley throughout all of Prehistory. The mobility that these human groups exercised and developed along the fluvial valley and its geographical location, invites the study of access routes to the exploitation of existing resources, as well as the exploration of territories, such as access to the valley of the Duero River, during the Late Glacier. The use of auxiliary tools such as Geographic Information Systems (GIS) for the study and tracing of prehistoric transit routes, have meant enormous progress in this field, although they are not the definitive solution. In this work we verify the existence of errors generated by these tools. The superimposition of the routes calculated on the real orography of the territory subject to study in this article, reflect certain paths that are impossible to carry out. A verification on the ground is necessary, which serves to elaborate the best route in this case, referring to the Azilian period