197,887 research outputs found
Reseña de: M. Gloria Ríos Guardiola y M. Belén Hernández González (eds.). Mujeres con luz, Murcia: Ediciones de la Universidad de Murcia (edit.um), 2017. ISBN 978-84-17157-41-8
No full textReseña de: M. Gloria Ríos Guardiola y M. Belén Hernández González (eds.). Mujeres con luz, Murcia: Ediciones de la Universidad de Murcia (edit.um), 2017. ISBN 978-84-17157-41-
Cap a Guardiola de Berguedà. Estret de Rigoréixer i Moixeró
No full textBoItinerari: Molí de Can Ferrer (960 m.) – Estret de Llúria – Basa del Coll de la Bama (1.700 m.) – Coll de la Bena (1.450 m.) – Veïnat del coll de la Bena (1.400 m.) – Gisclareny (1.339 m.) – Veïnat de Berta – Sant Miquel de Turbians (1.240 m.) – Collada de Turbians (1.460 m.) – Guardiola de Berguedà (719 m.
Baixant cap a Guardiola de Berguedà. Sta. Fe de Quer, Bagà i Puigllançada
No full textBoItinerari: Molí de Can Ferrer (960 m.) – Estret de Llúria – Basa del Coll de la Bama (1.700 m.) – Coll de la Bena (1.450 m.) – Veïnat del coll de la Bena (1.400 m.) – Gisclareny (1.339 m.) – Veïnat de Berta – Sant Miquel de Turbians (1.240 m.) – Collada de Turbians (1.460 m.) – Guardiola de Berguedà (719 m.
What comes after sovereignty?
No full textThis paper addresses the question of sovereignty from a perspective that connects the origins of public international law, with a series of onto-theological assumptions about the nature of place that were decisive in the emergence of modern colonialism. It will argue that insofar as sovereignty depends on some form of transcendence, external or internal, it is and has been ‘’impotent’’ from the very outset. However, contrary to the idea expressed in the well-known tale about the emperor’s new clothes, it is not the case that acknowledgement of this impotence would entail the end of sovereignty. Faced with the truth of its ultimate impotence, the sovereign supplements its role as decider with that of the intrigant. This new figure of sovereignty is embodied in the expert politician who announces the coming catastrophe in order to avert it, or contain it, through the use of ‘’limited’’ but ultimately borderless violence
Judit Freixa, M. Isabel Guardiola, Josep Martines & M. Amor Montané (ed.), «Dictionarization of Catalan Neologisms», Berlín, Peter Lang Verlag, 2023, 428 p.
No full textRessenya sobre el llibre de Judit Freixa, M. Isabel Guardiola, Josep Martines & M. Amor Montané (ed.), Dictionarization of Catalan Neologisms, Berlín, Peter Lang Verlag, 2023, 428 p., ISBN: 9783631880456
A Guardiola de Berga
No full textBoItinerari: Gréixer - Camp de Ventolana - Canal de la Serp - El Raset - Penyes Altes de Moixeró (2.260 m.) - Gréixer (Casa-Refugi i ermita de Sant Andreu) - Guardiola de Berga - Sant Julià de Cerdanyol
Sant Miquel de Turbians, a 1.240 m.
No full textBoItinerari: Molí de Can Ferrer (960 m.) – Estret de Llúria – Basa del Coll de la Bama (1.700 m.) – Coll de la Bena (1.450 m.) – Veïnat del coll de la Bena (1.400 m.) – Gisclareny (1.339 m.) – Veïnat de Berta – Sant Miquel de Turbians (1.240 m.) – Collada de Turbians (1.460 m.) – Guardiola de Berguedà (719 m.
Gisclareny (1.339 m.) i el Pedraforca
No full textBoItinerari: Molí de Can Ferrer (960 m.) – Estret de Llúria – Basa del Coll de la Bama (1.700 m.) – Coll de la Bena (1.450 m.) – Veïnat del coll de la Bena (1.400 m.) – Gisclareny (1.339 m.) – Veïnat de Berta – Sant Miquel de Turbians (1.240 m.) – Collada de Turbians (1.460 m.) – Guardiola de Berguedà (719 m.
Veïnat del coll de la Bena, a 1.400 m.
No full textBoItinerari: Molí de Can Ferrer (960 m.) – Estret de Llúria – Basa del Coll de la Bama (1.700 m.) – Coll de la Bena (1.450 m.) – Veïnat del coll de la Bena (1.400 m.) �� Gisclareny (1.339 m.) – Veïnat de Berta – Sant Miquel de Turbians (1.240 m.) – Collada de Turbians (1.460 m.) – Guardiola de Berguedà (719 m.
Le grotte della guardiola: preliminari osservazioni speleologiche e geologiche
No full textEnAlong the bottom of Guardiola rock cliff (south-east Salento, see Fig. 1) two caves are present. The entry of the Guardiola cave A is partially out of the sea level. This cave in particularly charming because the karstic forms and the reflection of a pale blue light of water. The strike-cave is ESE-WNW, its lenght is 65 m. A fresh-water spring is located in the middle portion of the south wall cave. Guardiola cave B is quite below the sea level. It shows a SE-NW strike and a lenght of 30 m. Also in this cave a fresh-water spring has been located.The fresh-water springs of the Guardiola caves A and B witness an important discharge zone of the "deep water-bearing stratum", the most important water resource of the Salento Peninsula. Guardiola rock cliff is formed by massive fossil-rich limestones, most probably of the Paleogene. A very extendend fault plane (strike SE-NW) constitutes the main tectonic structure of the zone. The form of the karstic structures of the Guardiola caves is strictly dependent on the tectonic setting and fracture pattern
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