Discurso sobre las aguas minerales en general,y en particular sobre las de la Fuente del Toro,en la villa del Molar /

Mode of access: Internet.

Disertacion sobre las aguas minerales termales de Panticosa [Manuscrito] /

Mode of access: Internet.

Memoria de las aguas minerales de Tiermas : madrid 28 de junio de 1833 /

Mode of access: Internet.

Sobre varias aguas minerales : Puertollano y Fuencaliente /

Mode of access: Internet.

[Memoria sobre las aguas minerales de Tiermas leida por D. Jose Abades y Rezano en la oposicion de 1833]

Mode of access: Internet.

Disertación sobre un punto de hidrología médica, y Monografía de las aguas y baños minero-medicinales de Caldelas de Tuy /

Antigua Signatura Ca 2861F(37)

Memoria sobre las aguas minerales termo-salinas de Guesalaga comunmente llamadas de Cestona en la provincia de Guipuzcoa /

Mode of access: Internet.

Guía del enfermo en las aguas minero-medicinales de Marmolejo /

Mode of access: Internet.

Memoria sobre las aguas y baños minero-medicinales sulfurosos de Betelu (Navarra) /

Mode of access: Internet.

Aguas minerales acidulo-salinas de Caldas de Besaya en la provincia de Santander /

Mode of access: Internet.

Baños minero-medicinales de Carratraca, año de 1848 : memoria del número y caracter de las enfermedades en que se han aplicado estas aguas en el presente año, metodo hidropatico y efectos obtenidos, llebando de preliminar el diario de las variaciones atmosfericas, y su influjo en la salud de los bañistas /

Incluye cuadros estadísticos y, al final, una instancia en papel sellado del director del establecimiento.

Disertacion sobre los baños de Solan de Cabras /

Carece de portada.

Fauxciutto- Is Italian-American Cuisine Really Italian?

Chef and Florida International University faculty member Mike D'Alessandro lectures on the evolution of Italian and Itlalian-American cuisines in the United States. Event is a part of the Food for Thought lecture series, and was held at the Village Gardens at the Vizcaya Museum and Gardens on October 9, 2013.

Preserving Beauty

Individuals from the Center for Humanities in an Urban Environment and the Vizcaya Museum and Gardens discuss the issue of "Preservation vs. Beauty". Lecture held on September 18, 2013 at the Vizcaya Museum and Gardens.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.