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dc.contributor.author
Peña Monné, José Luis  
dc.contributor.author
Sampietro Vattuone, Maria Marta  
dc.contributor.author
Picazo Millán, Jesús Vicente  
dc.contributor.author
Alcolea Gracia, Marta  
dc.date.available
2024-08-19T10:04:50Z  
dc.date.issued
2024-09  
dc.identifier.citation
Peña Monné, José Luis; Sampietro Vattuone, Maria Marta; Picazo Millán, Jesús Vicente; Alcolea Gracia, Marta; Block alignments/talus flatiron stages as response to lithological factors and dynamic slope changes in the Central Ebro Basin, NE Spain; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 340; 9-2024; 1-19  
dc.identifier.issn
0277-3791  
dc.identifier.uri
http://hdl.handle.net/11336/242696  
dc.description.abstract
The central sector of the Ebro Depression is characterized by an abundance of isolated buttes with relict talus flatiron morphologies and block slopes on the footslopes. This paper presents two unusual study cases where the block slopes are aligned in parallel with the retreating escarpment. The evolutionary process of both buttes started with the formation of talus flatirons and ended with aligned block slopes. This is because both buttes initially had a detrital caprock (Pleistocene pediment) which eroded away to expose a sandstone layer that functioned as a new caprock and so changed the slope dynamics. Seven stages were identified at La Cobeta butte and five at Puyalon butte. The relative ages obtained for stages II and IV enabled an estimation of the escarpment retreat rates. The chronologies of the other stages of block alignments were estimated using Schmidt-hammer rebound values. The estimated age of the stage II (ca. 6588-6222 cal yr BP) coincides with three radiocarbon datings obtained in the deposit. Stage III (ca. 4235-3684 cal yr BP) is contemporary with the 4.2 Bond event. Stage IV (ca. 2800-2500 cal yr BP) coincides with the 2.8 Bond event and is associated with ceramic potsherds and radiocarbon datings. Stages V and VI developed during the Warm Roman period and the Medieval Climatic Anomaly respectively. Lastly, stage VII was formed during the Little Ice Age. The information obtained regarding the morphological arrangement improves our knowledge of the regional evolutionary model where talus flat irons and block slopes develop in a semiarid environment.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Pergamon-Elsevier Science Ltd  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Holocene  
dc.subject
Rock slopes  
dc.subject
Escarpment retreat  
dc.subject
Isolated buttes  
dc.subject
Talus flatirons  
dc.subject
Paleoenvironments  
dc.subject.classification
Geociencias multidisciplinaria  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
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Otras Historia y Arqueología  
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Historia y Arqueología  
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HUMANIDADES  
dc.title
Block alignments/talus flatiron stages as response to lithological factors and dynamic slope changes in the Central Ebro Basin, NE Spain  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2024-08-15T15:30:54Z  
dc.journal.volume
340  
dc.journal.pagination
1-19  
dc.journal.pais
Estados Unidos  
dc.description.fil
Fil: Peña Monné, José Luis. Universidad de Zaragoza. Facultad de Filosofía y Letras; España  
dc.description.fil
Fil: Sampietro Vattuone, Maria Marta. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Laboratorio de Geoarqueología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina  
dc.description.fil
Fil: Picazo Millán, Jesús Vicente. Universidad de Zaragoza. Facultad de Filosofía y Letras; España  
dc.description.fil
Fil: Alcolea Gracia, Marta. Universidad de Zaragoza. Facultad de Filosofía y Letras; España  
dc.journal.title
Quaternary Science Reviews  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S0277379124003652  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.quascirev.2024.108864