2018
DOI: 10.21701/bolgeomin.129.1.007
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Geoarchaeological analysis of Mousterian settlements in the upper part of the Eresma river valley: Abrigo del Molino (Segovia, Spain)

Abstract: Hasta 2012, la ausencia de investigaciones arqueológicas sistemáticas en el alto valle del Eresma, hacía que esta área fuera considerada como un vacío ocupacional durante el Paleolítico. En este trabajo se presentan los primeros resultados del proyecto 'Primeros Pobladores de Segovia', cuyo enfoque geoarqueológico ha permitido, no sólo el descubrimiento de yacimientos musterienses como el Abrigo del Molino, sino la contextualización de las primeras ocupaciones humanas de esta zona del valle del Eresma desde un… Show more

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Cited by 5 publications
(12 citation statements)
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“…The San Lázaro rock shelter is a small cavity originated in the cretaceous dolomites of the left bank of the Eresma river (Segovia, Central System, Central Iberia) and about 15 m above the riverbed (Figure 1). The site, discovered in 2014, takes its name from the medieval bridge that crosses the Eresma river a few meters far from the rock shelter [53]. In turn, the San Lázaro rock shelter is located about 400 m upstream of the Eresma river, and the Molino rock shelter, a Mousterian site excavated between 2013 and 2018 by the same research team [54][55][56][57].…”
Section: Geographical and Geological Contextmentioning
confidence: 99%
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“…The San Lázaro rock shelter is a small cavity originated in the cretaceous dolomites of the left bank of the Eresma river (Segovia, Central System, Central Iberia) and about 15 m above the riverbed (Figure 1). The site, discovered in 2014, takes its name from the medieval bridge that crosses the Eresma river a few meters far from the rock shelter [53]. In turn, the San Lázaro rock shelter is located about 400 m upstream of the Eresma river, and the Molino rock shelter, a Mousterian site excavated between 2013 and 2018 by the same research team [54][55][56][57].…”
Section: Geographical and Geological Contextmentioning
confidence: 99%
“…Cavities are of very limited dimensions (hectometer length and metric height and width), showing a clear rocky-structural control, concentrated in certain carbonate levels previous to karstification or in which stabilization stages were concentrated in the nesting. Many of them, due to their small size, could be classified as balms, rock shelters and flaps, rather than caves, and their genesis is related to stabilization moments of the valley nesting and lateral erosion of the slopes by the fluvial-karstic system [53]. The upper part of the Eresma river encompasses the area of its birth on the summits of the central range and its course on the northern slopes of the mountains and highland foothills [58,59].…”
Section: Geographical and Geological Contextmentioning
confidence: 99%
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“…Álvarez-Alonso et al, 2016). Recent radiocarbon and luminescence dating at Jarama VI (Kehl et al, 2013; Wood et al, 2013, Jordá-Pardo et al, 2014), as well as luminescence ages for Hotel California (Arnold et al, 2013), Hundidero (Carbonell et al, 2014), Pinilla del Valle (Márquez et al, 2008; Arsuaga et al, 2012), Galería de las Estatuas (Arsuaga el al., 2017), and Abrigo del Molino (Álvarez-Alonso et al, 2013, 2016b) place the LMP in Central Iberia before 45 ka. Afterwards, the dispersion of AMH into Central Iberia was apparently delayed for a long period of time.…”
Section: Introductionmentioning
confidence: 95%