Antiphonarium (MS C.ö.III.20, "Michael Ericin antifonarium")

A copy of a Dominican antiphonary produced for Lutheran use in the second half of the sixteenth century. The sanctoral reflects Lutheran tastes, with St Henry, the patron of Finland, being the only non-biblical saint.

Estratégias periféricas sessenta anos depois do acordo de Bretton Woods

After sixty years, the Bretton Woods Agreement continuous to be a reference for the debates concerning institutional organization of the international monetary system. This paper compares some features of the arrangements that have emerged in that context with the recent wave of institutional reforms in the international financial architecture. We explore some arguments suggesting that, in an instable financial environment, is possible to envisage a strong rationality in strategies for emerging economies associated with a more active capital flows and exchange rate management. Apparently, those strategies are not dissimilar to the ones today's advanced countries had used in Bretton Woods Era.

La separación de los caminos (un análisis crítico del libro homónimo de Michael Friedman)

La filosofía contemporánea se hacaracterizadopor la presencia de un dualismo esquizoide entre la tradición analítica e la tradición fenomenológico hermenéutica. El origen histórico del mismo puede ser fijado en el Congreso de Davos, el cual, por otra parte, señala el comienzo del olvido de un otro programa, la filosofía de las formas simbólicas de E. Cassirer e que hoy puede ser considerado como alternativa e posible dirección de superación del dualismo mencionado. Tal es, en síntesis, la posición defendida por M. Friedman en su reciente monografía, escrita en el contexto de la convicción de una crisis derivada del agotamiento de las tradiciones y de la subsecuente necesidad de una reorientación. El texto que ofrecemos comenta críticamente el estudio de Friedman, mostrando donde y cómo él puede y debe ser completado o, eventualmente, corregido.

Das Grosfürstenthum Finland Augsburg, zu finden bey Johann Michael Probst, 1788

Janamittakaavat: Geographil Meile, Schwedische und Dännische, Norwegische, Franzöfische Meile.

[Charles Michael] Schwab (roi de l'acier) [américain en tenue de golf] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 58887

Résidence de Charles [Richard] Crane à Woods Hole (Mass.) [Massachusetts] qui sera probablement celle de Wilson [résidence d'été] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 58888

[Magnificentiores selectioresque Urbis Venetiarum prospectus quos olim Michael Marieschi, Venetus pictor et architectus in plerisque tabulis depinxit, nunc vero ab ipsomet acurate delineante, incidente, tyspisque mandante, iterum in sexdecim aereis tabulis in lucem aeduntur]. [21], Templum cum Platea Sanctae Mariae Formosae, ex archetiipo Jacobi Sansovini desumptum. : [estampe] / Mich.l Marieschi del.t et inci.t

Référence bibliographique : Toledano, Marieschi, 30

Conferencia de competitividad Doctor Michael Porter

Gestión del conocimiento

Dr. Michael Hornyansky

Professor of English Language and Literatre, Michael Hornyansky, in 1989. Dr. Hornyansky was one of the original Brock faculty members.

Dr. Michael Hornyansky

Professor of English Language and Literatre, Michael Hornyansky, in 1989. Dr. Hornyansky was one of the original Brock faculty members.

Michael Hornyansky

Michael Hornyansky was head of the Department of English at Brock and was one of the first 7 faculty members.

Physical volcanology, sedimentology, stratigraphy and petrochemistry of the Berry Creek metavolcanics: an Archean calc-alkaline complex, Lake of the Woods, Ontario

The steeply dipping, isoclinally folded early Precambrian (Archean) Berry Creek Metavolcanic Complex comprises primary to resedimented pyroclastic, epiclastic and autoclastic deposits. Tephra erupted from central volcanic edifices was dumped by mass flow mechanisms into peripheral volcanosedimentary depressions. Sedimentation has been essentially contemporaneous with eruption and transport of tephra. The monolithic to heterolithic tuffaceous horizons are interpreted as subaerial to subaqueous pumice and ash flows, secondary debris flows, lahars, slump deposits and turbidites. Monolithic debris flows, derived from crumble breccia and dcme talus, formed during downslope collapse and subsequent gravity flowage. Heterolithic tuff, lahars and lava flow morphologies suggest at least temporary emergence of the edifice. Local collapse may have accompanied pyroclastic volcanism. The tephra, produced by hydromagmatic to magmatic eruptions, were rapidly transported, by primary and secondary mechanisms, to a shallow littoral to deep water subaqueous fan developed upon the subjacent mafic metavolcanic platform. Deposition resulted from traction, traction carpet, and suspension sedimentation from laminar to turbulent flows. Facies mapping revealed proximal (channel to overbank) to distal facies epiclastics (greywackes, argillite) intercalated with proximal vent to medial fan facies crystal rich ash flows, debris flows, bedded tuff and shallow water to deep water lava flows. Framework and matrix support debris flows exhibit a variety of subaqueous sedimentary structures, e.g., coarse tail grading, double grading, inverse to normal grading, graded stratified pebbly horizons, erosional channels. Pelitic to psammitic AE turbidites also contain primary stru~tures, e.g., flames, load casts, dewatering pipes. Despite low to intermediate pressure greenschist to amphibolite grade metamorphism and variably penetrative deformation, relicts of pumice fragments and shards were recognized as recrystallized quartzofeldspathic pseudomorphs. The mafic to felsic metavolcanics and metasediments contain blasts of hornblende, actinolite, garnet, pistacitic epidote, staurolite, albitic plagioclase, and rarely andalusite and cordierite. The mafic metavolcanics (Adams River Bay, Black River, Kenu Lake, Lobstick Bay, Snake Bay) display _holeiitic trends with komatiitic affinities. Chemical variations are consistent with high level fractionation of olivine, plagioclase, amphibole, and later magnetite from a parental komatiite. The intermediate to felsic (64-74% Si02) metavolcanics generally exhibit calc-alkaline trends. The compositional discontinuity, defined by major and trace element diversity, can be explained by a mechanism involving two different magma sources. Application of fractionation series models are inconsistent with the observed data. The tholeiitic basalts and basaltic andesites are probably derived by low pressure fractionation of a depleted (high degree of partial melting) mantle source. The depleted (low Y, Zr) calc-alkaline metavolcanics may be produced by partial melting of a geochemically evolved source, e.g., tonalitetrondhjemite, garnet amphibolite or hydrous basalt.

Michael Hogue fonds

Michael H. [Henry] Hogue (1878-1963) was the son of Lemuel and Frances Hogue of Wainfleet Township, Welland County. In 1901 Michael Hogue was married to Margaret Case and they had five sons, William, Lemuel, Harry, Ross and Frank. In the 1911 Census of Canada he is residing in Welland and working as a blacksmith for Howard H. Lymburner. At Lymburner’s retirement, Hogue purchased the business and moved it from 15 Niagara Street, Welland to 12 Frazer Street, Welland. Mr. Hogue’s blacksmith activities included work with various industries in Welland including the expansion of blacksmithing work into the automobile industry. Mr. Hogue also worked for subcontractors Canadian Dredge & Dock and G.L. Campbell. These jobs included work related to the Welland Ship Canal in 1923. The business ceased operation in 1956.