Compendio historial o relacion breve y veridica del portentoso santuario y camara angelical de Nuestra Señora de Monserrate : dirigido a los piadosos devotos..

Fecha de 1758 tomada del permiso de impresión en el v. de la port

Antidotarium clarificatum

Biblioteca de la Abadía de Montserrat

Introducció a "Lo Crestià"

Descripción basada en: D'Eiximenis a Sor Isabel de Villena. Aportació a l'estudi de la nostra cultura medieval, Barcelona, Abadía de Montserrat-Institut de Filología Valenciana, 1990, pp. 59-123

Lo regiment de la cosa pública : Eiximenis, Joan de Salisbury y Fra Joan de Gal-les, O.F.M.

Descripción basada en: D'Eiximenis a Sor Isabel de Villena. Aportació a l'estudi de la nostra cultura medieval, Barcelona, Abadía de Montserrat-Institut de Filología Valenciana, 1990, pp. 125-149

El món cultural d'Isabel de Villena

Descripción basada en: en D'Eiximenis a Sor Isable de Villena. Aportació a l'estudi de la nostra cultura medieval, Barcelona, Abadía de Montserrat-Institut de Filología Valenciana, 1990, pp. 303-321

El Congreso por la Libertad de la Cultura y su apoyo a la disidencia intelectual durante el franquismo

El artículo reconstruye los principales aspectos de la labor del Congreso por la Libertad de la Cultura entre la oposición antifranquista del interior. Se describen las circunstancias políticas que motivaron la fundación del Comité Español (1959-1977), así como las principales características de esa célula intelectual antifranquista. El artículo indaga en los objetivos ideológicos y políticos de la actividad del Congreso por la Libertad de la Cultura entre las elites intelectuales y culturales disidentes durante el tardofranquismo. Nos concentramos especialmente en el capítulo que atañe a la ayuda directa dispensada por el Congreso por la Libertad de la Cultura a los intelectuales y artistas españoles mediante la concesión de becas de libros y bolsas de viaje a través del Comité d’Ecrivains et d’Editeurs pour une Entraide Européenne. Reconstruimos asimismo los nombres de los principales beneficiarios españoles de esas ayudas, así como la principal problemática vinculada al desarrollo del programa. El análisis histórico se apoya en documentos procedentes de diversos archivos nacionales e internacionales.

Una Girona poc il·luminada [Ressenya del llibre Girona a l'època de la Il·lustració, de Ramon Alberch, Javier Antón, Montserrat Jiménez i Josep Quer]

Ressenya d'aquesta obra historiogràfica sobre la Girona del segle XVIII. Es presenten tres treballs, dos d'ells entorn l’àmbit clerical i el tercer entorn la poca evolució de l’estructura econòmica i social de la Girona d’aquell temps

Història de les dones : estat actual i noves aportacions. 'Historia de las mujeres : estado actual y nuevas aportaciones'.

Resumen tomado de la revista

Història de les dones (II) : estat actual i noves aportacions. 'Historia de las mujeres (II) : estado actual y nuevas aportaciones'.

Resumen tomado de la revista. Incluye resumen de las ponencias de Vicenç Jasso, Bàrbara Genovard, Catalina Valriu, Joana Maria Escartín y Aina Serrano, David Ginard y Francesca Mas

Una manera de treballar la història : l'amplicació del món conegut. 'Una manera de trabajar la historia : la ampliación del mundo conocido'.

Resumen basado en el de la autora en catalán

Història de vida de Seis experiencias de educación Freinet en Cataluña antes de 1939, de Fernando Jiménez

Treball destinat a totes les persones interessades en la història de l’educació i la pràctica quotidiana del mètode Freinet. El centre d’interès és una publicació sobre experiències de mestres durant la Segona República Espanyola. Les sis experiències són el fruit de les entrevistes que en Fernando Jiménez va realitzar a alguns mestres que van tenir contacte amb la impremta escolar durant aquest període

Tracking the magmatic evolution of island arc volcanism : insights from a high-precision Pb isotope record of Montserrat, Lesser Antilles

The volcanic succession on Montserrat provides an opportunity to examine the magmatic evolution of island arc volcanism over a ∼2.5 Ma period, extending from the andesites of the Silver Hills center, to the currently active Soufrière Hills volcano (February 2010). Here we present high-precision double-spike Pb isotope data, combined with trace element and Sr-Nd isotope data throughout this period of Montserrat's volcanic evolution. We demonstrate that each volcanic center; South Soufrière Hills, Soufrière Hills, Centre Hills and Silver Hills, can be clearly discriminated using trace element and isotopic parameters. Variations in these parameters suggest there have been systematic and episodic changes in the subduction input. The SSH center, in particular, has a greater slab fluid signature, as indicated by low Ce/Pb, but less sediment addition than the other volcanic centers, which have higher Th/Ce. Pb isotope data from Montserrat fall along two trends, the Silver Hills, Centre Hills and Soufrière Hills lie on a general trend of the Lesser Antilles volcanics, whereas SSH volcanics define a separate trend. The Soufrière Hills and SSH volcanic centers were erupted at approximately the same time, but retain distinctive isotopic signatures, suggesting that the SSH magmas have a different source to the other volcanic centers. We hypothesize that this rapid magmatic source change is controlled by the regional transtensional regime, which allowed the SSH magma to be extracted from a shallower source. The Pb isotopes indicate an interplay between subduction derived components and a MORB-like mantle wedge influenced by a Galapagos plume-like source.

Submarine pyroclastic deposits formed during the 20th May 2006 dome collapse of the Soufrière Hills Volcano, Montserrat

The 20th May 2006 lava dome collapse of the Soufrière Hills Volcano, Montserrat, had a total non-dense rock equivalent (non-DRE) collapse volume of approximately 115 × 10 6 m 3. The majority of this volume was deposited into the ocean. The collapse was rapid, 85% of the mobilized volume being removed in just 35 min, giving peak pyroclastic flow flux of 66 × 10 3 m 3 s -1. Channel and levee facies on the submarine flanks of the volcano and formation of a thick, steep-sided ridge, suggest that the largest and most dense blocks were transported proximally as a high concentration granular flow. Of the submerged volume, 30% was deposited from the base of this granular flow, forming a linear, high-relief ridge that extends 7 km from shore. The remaining 70% of the submerged volume comprises the finer grain sizes, which were transported at least 40 km by turbidity currents on gradients of <2°. At several localities, the May 2006 distal turbidity currents ran up 200 m of topography and eroded up to 20 cm of underlying substrate. Multiple turbidites are preserved, representing current reflection from the graben margins and deflection around topography. The high energy of the May 2006 collapse resulted in longer submarine run out than the larger (210 × 10 6 m 3) Soufrière Hills dome collapse in July 2003.

Anatomy of a submarine pyroclastic flow and associated turbidity current : July 2003 dome collapse, Soufrière Hills volcano, Montserrat, West Indies

The 12 to 13 July 2003 andesite lava dome collapse at the Soufrière Hills volcano, Montserrat, provides the first opportunity to document comprehensively both the sub-aerial and submarine sequence of events for an eruption. Numerous pyroclastic flows entered the ocean during the collapse, depositing approximately 90% of the total material into the submarine environment. During peak collapse conditions, as the main flow penetrated the air–ocean interface, phreatic explosions were observed and a surge cloud decoupled from the main flow body to travel 2 to 3 km over the ocean surface before settling. The bulk of the flow was submerged and rapidly mixed with sea water forming a water-saturated mass flow. Efficient sorting and physical differentiation occurred within the flow before initial deposition at 500 m water depth. The coarsest components (∼60% of the total volume) were deposited proximally from a dense granular flow, while the finer components (∼40%) were efficiently elutriated into the overlying part of the flow, which evolved into a far-reaching turbidity current.