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Evolución postglaciar de la laguna de Villaseca (NW de la Península Ibérica) a partir del análisis de diatomeas
(Universidade da Coruña, 1997)
[Abstract] The lake of Villaseca is located in the foothills of the southern Cantabrian Mountains, nearby Villaseca de Laciana (León,NWIberian Peninsula). This lake has a glacier origin and has been formed due to the ...
Contribución al conocimiento de la vegetación holocena en el NO de la Península Ibérica (Galicia, España)
(Universidade da Coruña, 1997)
[Abstract] A paleobocanic scudy ofcwo Galician sierras, Coure! siecra and Queixa-Invernadoiro sierra is presenced here. A palynological scudy ofche Laguna Lucenza was carried ouC in che Coure! sierra. Eighc radiocarbon ...
The glaciation of Serra de Queixa-Invernadoiro and Serra do Gerês-Xurés, NW Iberia. A critical review and a cosmogenic nuclide (10Be and 21 Ne) chronology.
(Universidade da Coruña, 2015)
[Abstract]The Serras of Queixa-Invernadoiro and Gerês-Xurés in the NW of the Iberian Peninsula are two
small mountain massifs located at low altitude that were glaciated in the Pleistocene. The prevailing
granitic lithology ...
Nuevos datos para la cronología glaciar pleistocena en el NW de la Península Ibérica
(Universidade da Coruña, 1999)
[Abstract] The age of glacial features subaerial exposition: polished surfaces and morainic blocks using cosmogenic isotopes in granite substrate areas of the NW Iberian Peninsula have permitted to distinguish several ...