970 resultados para Anselm of Canterbury


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This article analyses the convoluted path of the Romanian communist regime's rapprochement with the West in the early 1960s. While, officially, the church supported the regime, the hierarchs strengthened their contacts with the West. This article argues that, paradoxically, church participation in international religious dialogue represented direct support for the nationalist stance of Romanian Communism. The increased number of ecumenical relations between Romania and the West reached its climax with the visit of Michael Ramsey, the Archbishop of Canterbury, to Romania in 1965, a few months before the country became the Socialist Republic of Romania.

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Anställningsotrygghet – en oro för att mot sin vilja förlora jobbet – är något som de flesta anställda idag upplever under sina yrkesliv. Den beteendevetenskapliga forskningen inom detta område har skjutit fart sedan millennieskiftet, vilket motiverar behovet av en uppdaterad litteraturöversikt. Översikten omfattar prediktorer och konsekvenser av anställningsotrygghet samt vilka faktorer som har identifierats som viktiga när det gäller att mildra anställningsotrygghetens konsekvenser.

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La perdurabilidad empresarial ha sido un tema recurrente en la literatura sobre dirección de empresas. A pesar de los avances, la liquidación de las empresas aumenta permanentemente. Buscando alternativas de mejora se estudia el caso de dos empresas cuadragenarias dedicadas a prestar servicios de consultoría en ingeniería eléctrica y civil que, en condiciones de crisis, implementaron acciones que les permitieron, no sólo mantenerse en el mercado sino también fortalecer su estructura financiera. Los resultados demostraron que un enfoque equilibrado caracterizado por la toma oportuna de decisiones y la definición e implementación de estrategias de negocio efectivas constituyen herramientas óptimas para asegurar un mayor grado de resiliencia empresarial.

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Resumen: La prueba de la existencia de Dios, sacada de su sola idea, fue, y es aún, una de esas experiencias metafísicas de las que se puede decir que nacen eternas, porque alcanzan el último término de uno de los caminos por donde el espíritu humano puede encauzarse. La presencia de Dios en el alma vivifica la fórmula que da san Anselmo y el análisis que hace de ella no tiene otro fin que llevar a la clara luz de la inteligencia una presencia realmente, pero oscuramente, sentida. Situados, dice, entre la fe y la visión, considera que “la inteligencia que alcanzamos en esta vida es intermedia”; los modos de aproximación difieren, pero sus términos no.

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Ocean Drilling Program (ODP) Site 1119 is located at water depth 395 m near the subtropical front (STF; here represented by the Southland Front), just downslope from the shelf edge of eastern South Island, New Zealand. The upper 86.19 metres composite depth (mcd) of Site 1119 sediment was deposited at an average sedimentation rate of 34 cm/kyr during Marine Isotope Stages (MIS) 1-8 (0-252 ka), and is underlain across a ~25 kyr intra-MIS 8 unconformity by MIS 8.5-11 (277-367 ka) and older sediment deposited at ~14 cm/kyr. A time scale is assigned to Site 1119 using radiocarbon dates for the period back to ~39 ka, and, prior to then, by matching its climatic record with that of the Vostok ice core, which it closely resembles. Four palaeoceanographic proxy measures for surface water masses vary together with the sandy-muddy, glacial-interglacial (G/I) cyclicity at the site. Interglacial intervals are characterised by heavy delta13C, high colour reflectance (a proxy for carbonate content), low Q-ray (a proxy for clay content) and light delta18O; conversely, glacial intervals exhibit light delta13C, low reflectance, high Q-ray and heavy delta18O signatures. Early interglacial intervals are represented by silty clays with 10-105-cm-thick beds of sharp-based (Chondrites-burrowed), shelly, graded, fine sand. The sands are rich in foraminifera, and were deposited distant from the shoreline under the influence of longitudinal flow in relatively deep water. Glacial intervals comprise mostly micaceous silty clay, though with some thin (2-10 cm thick) sands present also at peak cold periods, and contain the cold-water scallop Zygochlamys delicatula. Interglacial sandy intervals are characterised by relatively low sedimentation rates of 5-32 cm/kyr; cold climate intervals MIS 10, 6 and 2 have successively higher sedimentation rates of 45, 69 and 140 cm/kyr. Counter-intuitively,and forced by the bathymetric control of a laterally-moving shoreline during G/I and I/G transitions, the 1119 core records a southeasterly (seaward) movement of the STF during early glacial periods, accompanied by the incursion of subtropical water (STW) above the site, and northwesterly (landward) movement during late glacial and interglacial times, resulting in a dominant influence then of subantarctic surface water (SAW). The history of passage of these different water masses at the site is clearly delineated by their characteristic delta13C values. The intervals of thin, graded sands-muds which occur within MIS 2-3, 6, 7.4 and 10 indicate the onset at times of peak cold of intermittent bottom currents caused by strengthened and expanded frontal flows along the STF, which at such times lay near Site 1119 in close proximity to seaward-encroaching subantarctic waters within the Bounty gyre. In common with other nearby Southern Hemisphere records, the cold period which represents the last glacial maximum lasted between ~23-18 ka at Site 1119, during which time the STF and Subantarctic Front (SAF) probably merged into a single intense frontal zone around the head of the adjacent Bounty Trough.

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At head of title v. 1: Canterbury College (University of New Zealand).

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Mode of access: Internet.

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Pt.2 reprinted 1881; Pt.3 reprinted 1896; Pts. 5-6 reprinted 1900.