Relict slopes and palaeovalleys at Taracena-Guadalajara (central Spain): Geomorphological and palaeogeographical interpretation

Peña-Monné, Jose Luís; Rubio-Fernández, Virginia; Sampietro-Vattuone, María Marta; Giménez, Rosario García

doi:10.1016/j.yebeh.2019.106855

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Connection Between River Terrace and Slope Deposits1

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2024

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Cited by 3 publications

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“…5c, 5d, ALBAR-5). Similar landforms have been described in the valley of the Cinca River, southern Pyrenees (Sancho et al, 1988), and in the valley of the Henares River, close to Guadalajara (Peña-Monné et al, 2020). In both cases, talus flatirons are connected with river terraces.…”

Section: Connection Between River Terrace and Slope Depositssupporting

confidence: 74%

The connections between river terraces and slope deposits as paleoclimate proxies: The Guadalaviar - Turia sequence (Eastern, Iberia Chain, Spain)

Peña-Monné

Cunha

Sampietro-Vattuone

et al. 2022

Global and Planetary Change

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Section: Connection Between River Terrace and Slope Depositssupporting

confidence: 74%

The connections between river terraces and slope deposits as paleoclimate proxies: The Guadalaviar - Turia sequence (Eastern, Iberia Chain, Spain)

Peña-Monné

Cunha

Sampietro-Vattuone

et al. 2022

Global and Planetary Change

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Late Quaternary palaeoenvironmental controls on concentric talus evolution in the Central Ebro Basin (NE Spain)

2022

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The polyphasic evolution of the testimonial buttes in the central area of the Ebro basin (Los Monegros) is analysed. This is a semiarid area that favours high erosion rates. An evolutionary model of the Jubierre hills is presented that shows the environmental cycles represented by aggradational and degradative processes on the slopes that resulted in the present arrangement of talus flatiron rings. In the four studied cases, talus relicts are composed of detritic material from a disappeared caprock pediment. Four slope stages (S4 to S1) that formed under stable climate conditions are identified. Older stages (S4 and S3) are estimated by comparison with other talus flatirons in the region. The S2 stage contains Bronze Age archaeological remains and the radiocarbon age obtained was 1608–1446 years cal BC (2σ), while S1 is younger. A palaeoenvironmental interpretation was made for these aggradational stages (S4 to S1). The active erosion of these hills led to a relief inversion, and talus flatirons remain as the only features revealing the presence of the relict hills and past human occupations.

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Block alignments/talus flatiron stages as response to lithological factors and dynamic slope changes in the Central Ebro Basin, NE Spain

Peña-Monné,

Sampietro-Vattuone,

Picazo-Millán

et al. 2024

Quaternary Science Reviews

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Relict slopes and palaeovalleys at Taracena-Guadalajara (central Spain): Geomorphological and palaeogeographical interpretation

Cited by 3 publications

References 23 publications

The connections between river terraces and slope deposits as paleoclimate proxies: The Guadalaviar - Turia sequence (Eastern, Iberia Chain, Spain)

The connections between river terraces and slope deposits as paleoclimate proxies: The Guadalaviar - Turia sequence (Eastern, Iberia Chain, Spain)

Late Quaternary palaeoenvironmental controls on concentric talus evolution in the Central Ebro Basin (NE Spain)

Block alignments/talus flatiron stages as response to lithological factors and dynamic slope changes in the Central Ebro Basin, NE Spain

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