Una pintura d'Antoni Viladomat i Manalt (1678-1755) a Manresa : l'Assumpta de Santa Maria de l'Alba

This painting with an exceptional iconography of the Assumption of the Virgin with All the Saints, was saved from a altarpiece in the church of Santa Maria de l'Alba in Manresa, which was burnt during the Spanish Civil War. The article attributes this painting to Antoni Viladomat i Manalt (1678-1755), one of the most relevant figures in the Catalan artistic scene in the 18th century, and it dates it to the latter years of his extensive artistic career. An analysis of the work shows that the Catalan painter incorporated some figurative elements that he borrowed from an engraving of the Swiss engraver, Jakob Frey (1681-1752), interpreted from a canvas of the Italian painter Sebastiano Conca (1680-1764). This helps to relate the canvas of the Barcelona painter-based on his previous figurative work with high Roman baroque- to the new proposals of the so-called Roman barrochetto. In addition the study hopes to offer the reader an artistically cultural view of Antoni Viladomat, openly concerned by the novelties that constantly reached Catalonia by means of the engravings

El pintor Antoni Viladomat i Manalt (1678-1755): Biografia i Catàleg crític

La tesi és un estudi integral de la figura i l'obra del pintor Antoni Viladomat i Manalt (1678-1755), un dels artífexs més destacats del panorama artístic català del Set-cents. El primer volum aborda la revisió de la seva biografia partint de les aportacions de la historiografia i de les noves dades inèdites d'arxiu. S'hi fa també un anàlisi de la seva cultura visual i figurativa, una panoràmica sobre la relació del pintor amb el seu ambient artístic més proper i immediat, i un estudi de l'encaix de la seva personalitat artística en el context de la pintura precedent i contemporània peninsular i europea. El primer volum inclou, també, un epíleg on s'aborden temes com els detonants i les conseqüències de la seva extraordinària fortuna crítica. El segon volum és un catàleg crític de la seva obra, organitzat a partir de fitxes individuals de cadascuna de les obres. L'autor considera que dues-centes cinquanta obres conservades, comptant dibuixos i pintures, són autògrafes, quaranta-una de les quals són inèdites. El catàleg també te recull i classifica les obres descartades i les perdudes. Les principals aportacions de la tesi, a banda de l'actualització del coneixement de la seva biografia i de l'elaboració per primera vegada d'un catàleg crític complet de la seva obra, són la localització del testament del pintor, la revisió de la relació de Viladomat amb els artistes de la cort de l'Arxiduc Carles d'Àustria, la proposta d'una nova cronologia per als treballs dels anys vint del segle XVIII, una interpretació nova dels plets contra el col·legi de pintors de Barcelona, la revisió de la seva intervenció a la Capella dels Dolors de Santa Maria de Mataró, bona part de la qual l'autor d'aquesta Tesi atribueix al pintor Joan Gallart; la definició dels usos que el pintor fa amb l'estampa de traducció, la relació amb la pintura siscentista dels Juncosa o la importància de l'aprenentatge en un context tradicional, etcètera.

Silvos del pastor divino, a todos los sacerdotes y Padres de Almas, sus Pastores [Texto impreso]

Signaturizado hasta A8 en la p. 13

Honras a la.... memoria del... Señor D.Francisco Perez de Prado y Cuesta Obispo de Teruel... con el motiuo del traslado de su cadauer... y sermon que predico en ellas... [Texto impreso]

Sign. : []4, A-D4, E.

Collection académique, composée des mémoires, actes, ou journaux des plus célèbres académies & sociétés littéraires étrangères, des extraits des meilleurs ouvrages périodiques, des traités particuliers, & des pièces fugitives les plus rares; concernant l'histoire naturelle et la botanique, la physique expérimentale et la chymie, la médecine et l'anatomie.

Vol. 7: cancel p. 31-32 bound in following p. 670.

Memoirs of odd adventures, strange deliverances, &c. in the captivity of John Gyles, Esq; commander of the garrison on St. George's River /

"Erratum."--p. [44].

L'obra d'Antoni Viladomat a la Capella dels Dolors de Mataró

Amb aquest treball de final de carrera vull divulgar en format hipertextual el conjunt dels Dolors de Santa Maria de Mataró, que és segurament el conjunt de pintures més complet i més ben conservat del Barroc català. Totes són obra d'Antoni Viladomat i Manalt, el pintor barceloní més destacat de la seva època.

James Parkinson (1755-1824): A pioneer of child care

James Parkinson (1755-1824) of Parkinson's disease, is well recognized as a pioneer of clinical neurology; and is even more famous as a founder of modem palaeontology. We have reviewed from primary sources his extensive contributions to clinical child care and his pioneering advocacy for child welfare, protection and safety. His writings, outreach and advocacy for children's health characterizes him as one whose influence was an important springboard from which evolved the modern specialty of paediatrics. Parkinson was one of the first to write on child-rearing practices and in this context antedated Benjamin Spock by 150 years. Parkinson was a pioneer of child safety and the prevention of childhood trauma. He wrote of the resuscitation of near-drowned children and of first aid for injured children. This critical analysis reviews his pioneering description of child abuse and the development of post-abuse hydrocephalus. He wrote the datum description (in English) of the pathophysiology and pathology of appendicitis in children, of fatal rabies in children and highlighted the risk of death even when the biting dog was not clinically rabid. His advocacy for social reform for children's welfare was courageous and pioneering. James Parkinson, hitherto unacknowledged, was a significant founder of the evolving discipline of paediatrics and child health.

Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: A study case of the 1755 Lisbon tsunami in Algarve, Portugal

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

Impact of a 1755-like tsunami in Huelva, Spain

Coastal areas are highly exposed to natural hazards associated with the sea. In all cases where there is historical evidence for devastating tsunamis, as is the case of the southern coasts of the Iberian Peninsula, there is a need for quantitative hazard tsunami assessment to support spatial planning. Also, local authorities must be able to act towards the population protection in a preemptive way, to inform 'what to do' and 'where to go' and in an alarm, to make people aware of the incoming danger. With this in mind, we investigated the inundation extent, run-up and water depths, of a 1755-like event on the region of Huelva, located on the Spanish southwestern coast, one of the regions that was affected in the past by several high energy events, as proved by historical documents and sedimentological data. Modelling was made with a slightly modified version of the COMCOT (Cornell Multi-grid Coupled Tsunami Model) code. Sensitivity tests were performed for a single source in order to understand the relevance and influence of the source parameters in the inundation extent and the fundamental impact parameters. We show that a 1755-like event will have a dramatic impact in a large area close to Huelva inundating an area between 82 and 92 km(2) and reaching maximum run-up around 5 m. In this sense our results show that small variations on the characteristics of the tsunami source are not too significant for the impact assessment. We show that the maximum flow depth and the maximum run-up increase with the average slip on the source, while the strike of the fault is not a critical factor as Huelva is significantly far away from the potential sources identified up to now. We also show that the maximum flow depth within the inundated area is very dependent on the tidal level, while maximum run-up is less affected, as a consequence of the complex morphology of the area.

Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: A study case of the 1755 Lisbon tsunami in Algarve, Portugal

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

Potential inundation of Lisbon downtown by a 1755-like tsunami

In this study, we present 10 m resolution tsunami flooding maps for Lisbon downtown and the Tagus estuary. To compute these maps we use the present bathymetry and topographic maps and a reasonable estimate for the maximum credible tsunami scenario. Tsunami modeling was made with a non-linear shallow water model using four levels of nested grids. The tsunami flood is discussed in terms of flow depth, run-up height and maximum inundation area. The results show that, even today, in spite of the significant morphologic changes in the city river front after the 1755 earthquake, a similar event would cause tsunami flow depths larger than one meter in a large area along the Tagus estuary and Lisbon downtown. Other areas along the estuary with a high population density would also be strongly affected. The impact of the tide on the extent of tsunami inundation is discussed, due to the large amplitude range of the tide in Lisbon, and compared with the historical descriptions of the 1755 event. The results presented here can be used to identify the potential tsunami inundation areas in Lisbon; this identification comprises a key element of the Portuguese tsunami emergency management system.

Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: Astudy case of the 1755 Lisbon tsunami in Algarve, Portugal (vol 182, pg 187, 2010)

Storm- and tsunami-deposits are generated by similar depositional mechanisms making their discrimination hard to establish using classic sedimentologic methods. Here we propose an original approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism. To test our method, we investigate the tsunami deposit of the Boca do Rio estuary generated by the 1755 earthquake in Lisbon which is well described in the literature. We first test the 1755 tsunami scenario using a numerical inundation model to provide physical parameters for the tsunami wave. Then we use concentration (MS. SIRM) and grain size (chi(ARM), ARM, B1/2, ARM/SIRM) sensitive magnetic proxies coupled with SEM microscopy to unravel the magnetic mineralogy of the tsunami-induced deposit and its associated depositional mechanisms. In order to study the connection between the tsunami deposit and the different sedimentologic units present in the estuary, magnetic data were processed by multivariate statistical analyses. Our numerical simulation show a large inundation of the estuary with flow depths varying from 0.5 to 6 m and run up of similar to 7 m. Magnetic data show a dominance of paramagnetic minerals (quartz) mixed with lesser amount of ferromagnetic minerals, namely titanomagnetite and titanohematite both of a detrital origin and reworked from the underlying units. Multivariate statistical analyses indicate a better connection between the tsunami-induced deposit and a mixture of Units C and D. All these results point to a scenario where the energy released by the tsunami wave was strong enough to overtop and erode important amount of sand from the littoral dune and mixed it with reworked materials from underlying layers at least 1 m in depth. The method tested here represents an original and promising tool to identify tsunami-induced deposits in similar embayed beach environments.

La concepció evolucionista de la natura en el programa de difusió de la cultura cientí­fica d'Antoni Bergnes de las Casas (1801-1879)

La recerca es centra en l'™obra de divulgació cientí­fica d'™Antoni Bergnes de las Casas al llarg del segle XIX a Barcelona. En les obres i revistes que publicà destaca la difusió de noves concepcions en la història natural. En elles es divulga la teoria evolucionista de Lamarck i d'altres models evolutius similars, però que defensen la intervenció divina en el procés. Aquests fets posen de manifest la presència de teories evolutives a Catalunya i a Espanya en la primera meitat del segle XIX, i de la teoria evolucionista de Lamarck a principi dels anys seixanta del segle.