Results 21 to 30 of about 86 (73)

Análisis espacio-temporal de los eventos de nevadas en el Pirineo español y su relación con la circulación atmosférica

open access: yesCuadernos de Investigación Geográfica, 2017
Este estudio analiza la variabilidad interanual y estacional de los eventos de acumulación de nieve en los Pirineos Españoles, así como la relación entre diferentes tipos de tiempo y los episodios de nevadas normales (P30 x P80) e intensas (x P80 ...
F.M. Navarro-Serrano, J.I. López-Moreno
doaj   +1 more source

Mountain ungulates and the conservation of scarce plant species: the cases of Delphinium montanum and Xatardia scabra

open access: yesPirineos: Revista de Ecología de Montaña, 2002
[fr] Une étude de suivi a été développée dans le Parc naturel et Réserve de Chasse du Cadí-Moixeró (Catalogne, Espagne). Le but était de tester la possible influence négative de la haute densité de population des isards (Rupicapra pyrenaica) sur la ...
P. Aymerich   +2 more
doaj   +1 more source

Death in the high mountains: Evidence of interpersonal violence during Late Chalcolithic and Early Bronze Age at Roc de les Orenetes (Eastern Pyrenees, Spain)

open access: yesAmerican Journal of Biological Anthropology, Volume 184, Issue 1, May 2024.
Abstract Objectives To test a hypothesis on interpersonal violence events during the transition between Chalcolithic and Bronze Age in the Eastern Pyrenees, to contextualize it in Western Europe during that period, and to assess if these marks can be differentiated from secondary funerary treatment.
Miguel Ángel Moreno‐Ibáñez   +7 more
wiley   +1 more source

Diversidad y continuidad de los sistemas técnicos del Paleolítico Medio en los Pirineos sur-orientales

open access: yesTreballs d'Arqueologia, 2008
[FR] Dans cet article, on présente une synthèse méthodologique sur la technologie employée dans l’élaboration de produits taillés pendant le Paléolithique moyen et, en même temps, on réalise une analyse comparative des méthodes de taille documentés dans les niveaux N10 de la Roca dels Bous et les unités UA3, S5, S6 et S7 d’Estret de Tragó.
Casanova, Joel   +3 more
openaire   +4 more sources

Ava de Fenollet. Estudio de una vizcondesa occitana de mediados del siglo XIII

open access: yesEn la España Medieval
Este artículo se centra en Ava, hija de Pere V de Fenollet, vizcondado que actualmente se encuentra en el departamento de los Pirineos Orientales (Francia) pero que históricamente formó parte del Languedoc.
Núria Pacheco Catalán
doaj   +1 more source

Estructura de Ios mantos superior e inferior del Pedraforca (Pirineos orientales)

open access: yes, 2001
The Pedraforca nappe is one of the allochtonous structural units in which the Cover Upper thrust sheets of the southern Pyrenees are organised. Its is internally constituted by two thrust sheets, namely Upper Pedraforca thrust sheet and Lower Pedraforca thrust sheet. As a whole, they were emplaced in a piggyback thrusting sequence. But in the detail, a
Martinez, A.   +3 more
openaire   +1 more source

Condiciones metamórficas de las metabasitas del Roc de Frausa (Pirineos Orientales)

open access: yes, 1996
An approach to the metamorphic conditions based in mineral paragenesis of metabasites from different areas of Roc de Frausa Massif has been made. Regional peak metamorphism is showed by the metamorphic paragenesis in granulites conditions from Les Hies sector (Clpx + PI + Amph + llm); P-T conditions during Hercynian metamorphism are 750 ± 20 °C and 4.5
Navidad, M.   +2 more
openaire   +1 more source

Inclusiones fluidas en material filoniano del Valle de Ribes, Pirineos Orientales, España

open access: yesActa geológica hispánica, 1978
Fluid inclusions in quartz and scheelite from two localities of a vein field have been studied. The veins are related to a latehercynian granitic intrusion. The ore minerals from the veins are arsenopyrite, pyrite, pyrrhotite, chalcopyrite, gold and sulphosalts of the PbS-Bi z-S,-Sb2S 3 system.
openaire   +3 more sources

Génesis y evolución de la fosa de la Cerdanya (Pirineos Orientales)

open access: yes, 1986
The Cerdanya basin is located at the SW end of the Tet fault, in its NW block. Its formation, during the Upper Miocene, was conditioned by dextral slip of this fault anf the normal slip of E-W trending faults that absorbed the movement of the ...
Roca, E., Santanach, P.
openaire   +1 more source

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