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Jorge Sanjurjo Sánchez
Instituto Universitario de Geología “Isidro Parga Pondal”Universidade da CoruñaCampus de Elviña, 15071 A Coruña (Spain)
Juan Ramón Vidal Romaní
Instituto Universitario de Geología “Isidro Parga Pondal”Universidade da CoruñaCampus de Elviña, 15071 A Coruña
Marcos Vaqueiro Rodríguez
Clube Espeleolóxico A Trapa, c/Manuel de Castro 8-3D. 36210 Vigo
Reimundo Costas Vázquez
Clube Espeleolóxico Trapa c/Manuel de Castro 8-3D. 36210 Vigo
Aurora Grandal d'Anglade
Instituto Universitario de Geología “Isidro Parga Pondal”Universidade da CoruñaCampus de Elviña, 15071 A Coruña
Vol. 37 (2013), Articles, pages 73-87
Submitted: Jul 10, 2018 Accepted: Jul 10, 2018 Published: Dec 9, 2013
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Granite caves and cavities are geomorphological environments associated with underground water flows with a strong turbulent regime linked to seasonality. Though not much studied, they have a great sedimentary and geomorphological interest but sometimes also archaeological because remains of human activity (mainly lithic industry and pottery). Pottery remains appear either exposed or buried and may be characterised mineralogically and dated by thermoluminescence (TL). Water dynamics justifies erosion and fragmentation of ceramic remains which appear broken and spread inside the cavities. This fact hinders their dating due to the small size of the fragments and the disappearance of the original sedimentary context, which does not allow the calculation of part of the received annual radiation dose. In this work, the results from the dating and the estimation of ages of different ceramic fragments of several granite caves of Galicia are presented. The obtained ages go from Medieval (1 ka BP) to Roman or pre-Roman (2 ka BP), Chalcolithic (6 ka BP) and even the beginning of the Neolithic (7 ka BP).


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