2016-05-24T08:27:59Z
2016-05-24T08:27:59Z
1997
2016-05-24T07:54:35Z
This article aims to make the karst morphological forms to be found in conglomerate rocks, as well as the sedimentary sequence types recorded in such deposits, more widely known. Particular attention is paid to points where prehistoric occupation has been traced, sites such as: the Font Major Cave (Espluga de Francoli, Tarragona), the Hort de la Boquera, the Filador Rock-shelter and the Colls Rock-shelter (Margalef de Montsant, Tarragona), and the Parco Cave (Alôs de Balaguer, Lleida). By means of this approach the characteristics of karst deposits in conglomerate rocks are analyzed both from an archaeological and a sedimentary point of view.
Article
Published version
English
Geoarqueologia; Carst; Geologia estructural; Sedimentologia; Archaeological geology; Karst; Structural geology; Sedimentology
Association Française pour l'étude du Quaternaire
Reproducció del document publicat a: http://www.persee.fr/web/revues/home/prescript/article/quate_1142-2904_1997_num_8_2_1579
Quaternaire, 1997, vol. 8, num. 2-3, p. 267-277
cc-by-nc-nd (c) Association Française pour l'étude du Quaternaire, 1997
http://creativecommons.org/licenses/by-nc-nd/3.0/es