2015
DOI: 10.15366/cupauam2015.41.013
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Aprendiendo a Excavar: El Yacimiento Paleolítico De Los Ahijones-Sector G Como Modelo De Investigación Y Formación. Learning to Dig: The Paleolithic Site of Los Ahijones-Sectore G as Sample of Investigations and Education.

Abstract: ResumenDurante los últimos años y gracias a la estrecha colaboración del Departamento de Prehistoria y Arqueología, la empresa Argea S.L y la Dirección General de Patrimonio de la Comunidad de Madrid, se viene desarrollando un modelo mixto de formación e investigación en el yacimiento paleolítico de Los Ahijones (Vicávaro-Madrid) en el que los alumnos de prácticas de campo del Máster de Arqueología y Patrimonio de nuestra Universidad participan activamente. En este trabajo presentamos tanto las metodologías do… Show more

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“…Ongoing work (Baena et al 2015b) indicates that use of flint hammerstones in the Madrid basin seemed to be a common feature during the Palaeolithic. Although it has been suggested elsewhere that flint hammerstones might present a higher technical efficiency without increasing the frequency of accidents , the experimental program developed here shows that knapping mistakes increase with the use of flint hammerstones.…”
Section: Discussionmentioning
confidence: 98%
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“…Ongoing work (Baena et al 2015b) indicates that use of flint hammerstones in the Madrid basin seemed to be a common feature during the Palaeolithic. Although it has been suggested elsewhere that flint hammerstones might present a higher technical efficiency without increasing the frequency of accidents , the experimental program developed here shows that knapping mistakes increase with the use of flint hammerstones.…”
Section: Discussionmentioning
confidence: 98%
“…The northern and southern margins of the Madrid Basin consist of granitic igneous rocks that contrast with the basin units formed by lacustrine and alluvial materials (arkoses with carbonates, clays and gypsum) (López-Camacho et al 1986). During the period of the Neogene there were three large sedimentary stages that are associated with three large stratigraphic units in relation to flint formations: Lower Unit (Middle RablienseAragoniense), Middle Unit (Middle Aragoniense-Lower Vallesiense) and Upper Unit (Upper Vallesiense-Turoliense) (Baena et al 2015b;Calvo et al 1996). The Lower Unit is formed by massive gypsums and clayey sequences (silt and clay formations) intercalated with conglomerates, sandstones and limestones.…”
Section: Introductionmentioning
confidence: 99%