Relleno morfosedimentario y poblamiento humano del estuario de los ríos Tinto y Odiel (Huelva) durante la segunda mitad del Holoceno

• Autores: Joaquín Rodríguez Vidal, Manuel Abad de los Santos, Luis Miguel Cáceres Puro, María Luz González-Regalado Montero, María J. Clemente, Francisco Ruiz Muñoz, Tatiana Izquierdo, Antonio Toscano Grande, P. Gómez, J. Campos, Javier Bermejo Meléndez, Aránzazu Martínez Aguirre
• Localización: Avances de la Geomorfología en España 2012-2014 / coord. por Susanne Cecilia Schnabel, Álvaro Gómez Gutiérrez, 2014, ISBN 978-84-617-1123-9, págs. 604-607
• Idioma: español
• Títulos paralelos:
  • Morphosedimentary infilling and human settlement of the Tinto-Odiel Estuary (Huelva) during the Mid-Late Holocene
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• Resumen

  • The first human settlements (6000−4000 BP) in the early estuary of the Tinto and Odiel rivers were located in the ancient coastal banks or in the nearby hills. From 4000 years BP onwards, the estuarine sediments started to emerge as sand barriers and chenier plains, prograding towards the mouth. As the littoral strands stabilized morphologically, they are colonized by human settlements in successive periods, the oldest inland (Almendral) and more recent outward (Cascajera). These emerged morphologies were surrounded by muddy tidal flats in the estuary and only the high-energy marine events such as a tsunami or extraordinary storms were able to modify both the landscape and human settlements installed on them. This work also describes the morphodynamic model that built the chenier plain of La Cascajera