Burton Tower - June, 1948; Percival Price, Carillonneur

Albert Kahn, architect

Sapientia, 1971, Vol. XXVI, nº 100-102 (número completo)

Contenido: Sapientia, Veinticinco años después / Octavio N. Derisi – Tomás de Aquino, peregrino de Dios / Adolfo Muñoz Alonso – Qu’est-ce que la philosophie? / A. Dondeyne – La subordinación de la lógica a la ciencia / A. Furlán – Volición y voluntad en Aristóteles / B. Raffo Magnasco – Entendement et imagination selon Aristote / A. Guy – Le problème de l’existence de Dieu dans le Commentaire de Saint Thomas sur la Physique d’Aristote / F. Van Steenberghen – Individuación, analogía y participación en el plano físico / J. E. Bolzán – La “Summa Physicorum” y la filosofía natural de Grosseteste / C. Lértora Mendoza – El infinito actual en Santo Tomás / O. Argerami – Tomás de Aquino en la Universidad de París / G. E. Ponferrada – Dante y la filosofía / G. Terán – El ámbito del objeto de la fenomenología en E. Husserl / O. N. Derisi – Orígenes doctrinales de la Tercera Escolástica en la filosofía argentina del siglo XIX / A. Caturelli – Hegel e Cristo / C. Fabro – Sapientia reconsidered / A. G. M. Van Melsen – El punto de partida de la metafísica : ¿abstracción o intuición? / J. R. Sanabria – La catégorie hégélienne de contradiction / R. Verneaux – La ontología modificada / C. A. Iturralde Colombres – L’acte moral et le sujet / J. de Finance – La crítica de Monseñor Derisi a la ciencia política empírica / A. E. Sampay – Notas y comentarios -- Bibliografía

Citizens’ Savings and Loan Association, Cleveland, Ohio passbook

Citizens’ Savings and Loan Association, Cleveland, Ohio passbook issued to Isabel G. Price, 1882- 1901.

Meninices de uma poetisa: um estudo de O menino poeta, de Henriqueta Lisboa

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

(Table 1) Sulfur isotopes and description of anhydrite in DSDP Holes 70-504B and 83-504B

Anhydrite occurs in veins in hydrothermally altered basalts recovered from Hole 504B during Leg 83 of the Deep Sea Drilling Project. Sulfur isotopic data indicate that the anhydrites formed from fluids with sulfur isotopic compositions similar to seawater sulfate. Anhydrite probably formed as a pulse of relatively unreacted seawater was heated when it entered a relatively hot hydrothermal system containing evolved fluids. Reheating and continued evolution of the system followed anhydrite deposition. Preservation of anhydrite in Hole 504B was probably favored by the high temperatures and by the low permeability that resulted from the sealing of cracks with secondary minerals. Evidence also indicates that anhydrite was partly replaced by laumontite and prehnite at relatively high temperatures, and possibly by calcite at lower temperatures.

Population redistribution and economic growth: United States, 1870-1950 /

Includes bibliographical references.