ACTS OF THOUGHT AND RE-ENACTMENT IN COLLINGWOOD'S PHILOSOPHY OF HISTORY

This article explores one of Collingwood's most puzzling claims—that, in re-enacting a past act of thought, I can revive not just the propositional content of that act but also the very act of thought itself. This aspect of Collingwood's ideas has been largely ignored, and, when not ignored, it has been almost universally rejected. After all, we might ask, how can it be that two acts of thought—one, say, had by Carol in the library on Wednesday and another act of thought had by Harold in his study on Thursday—are literally identical? I explore this baffling claim and, in particular, Collingwood's argument that acts of thought can have the identity of a continuant. I try to show how the idea of the identity of the continuant might be used to remove some of the puzzlement in Collingwood's claim about literal identity between acts of thought; I thus show how Harold, on Thursday, might be able to experience the exact same act of thought that Carol had on Wednesday.     

Contesting Commerce: Gibbons v. Ogden, Steam Power, and Social Change

The U.S. Supreme Court case Gibbons v. Ogden (1824) ¹ represents one of the most significant yet least understood cases in the history of American jurisprudence. Most accounts depict the case as a constitutional showdown between former New Jersey Governor Aaron Ogden and his estranged business partner, a Georgian businessman and planter named Thomas Gibbons. Ogden charged Gibbons with operating a steamboat on the Hudson River in violation of the Fulton–Livingston Steamboat monopoly that controlled steam travel in the state of New York. In March 1824, Chief Justice John Marshall ruled for the Supreme Court that Gibbons' federal coasting license trumped a state grant issued to Ogden by the Fulton–Livingston syndicate. ²     

Mobilization of ore fluids during Alpine metamorphism: evidence from hydrothermal veins in the Variscan basement of Western Carpathians,Slovakia

Hydrothermal polymetallic veins of the Gemeric unit of the Western Carpathians are oriented coherently with the foliation of their low‐grade Variscan basement host. Early siderite precipitated from homogeneous NaCl‐KCl‐CaCl₂‐H₂O brines with minor CO₂, while immiscible gas–brine mixtures are indicative of the superimposed barite, quartz–tourmaline and quartz–sulphide stages. The high‐salinity aqueous fluid (18–35 wt%) found in all mineralization stages corresponds to formation water modified by interaction with crystalline basement rocks at temperatures between 140 and 300°C. High brominity (around 1000 ppm in average) resulted from evaporation and anhydrite precipitation in a Permo‐Triassic marine basin, and from secondary enrichment by dissolution of organic matter in the marine sediments at diagenetic temperatures. Sulphate depletion reflects thermogenic reduction during infiltration of the formation waters into the Variscan crystalline basement. Crystallization temperatures of the siderite fill (140–300°C) and oxygen isotope ratios of the parental fluids (4–10‰) increase towards the centre of the Gemeric cleavage fan, probably as a consequence of decreasing water/rock ratios in rock‐buffered hydrothermal systems operating during the initial stages of vein evolution. In contrast, buoyant gas–water mixtures, variable salinities and strongly fluctuating P–T parameters in the successive mineralization stages reflect transition from a closed to an open hydrothermal system and mixing of fluids from various sources. Depths of burial were 6–14 km (1.7–4.4 kbar, in a predominantly lithostatic fluid regime) during the siderite and barite sub‐stages of the north‐Gemeric veins, and up to 16 km (1.6–4.5 kbar, in a hydrostatic to lithostatic fluid regime) in the quartz–tourmaline stage of the south‐Gemeric veins. The fluid pressure decreased down to approximately 0.6 kbar during crystallization of sulphides. U‐Pb‐Th, ⁴⁰Ar/³⁹Ar and K/Ar geochronology applied to hydrothermal muscovite–phengite and monazite, as well as cleavage phyllosilicates in the adjacent basement rocks and deformed Permian conglomerates corroborated the opening of hydrothermal veins during Lower Cretaceous thrusting and their rejuvenation during Late Cretaceous sinistral transpressive shearing and extension.     

LES ACCIDENTS DE LA ROUTE ET LES CONTRAVENTIONS ROUTIÈRES AU QUÉBEC: ANALYSE GÉOGRAPHIQUE

Cet article traite de la relation géographique entre les accidents de la route et l'intervention policière sur les routes en milieu rural. On pose la question à savoirsi les accidents se produisent généralement là ou les policiers assurent une certaine intervention et surveillance et si, réciproquement, les caractéristiques géographiques des accidents incitent des interventions spécifiques des forces publiques. L'analyse permet de constater la distribution géographique des accidents et des contraventions. If existe également des lieux communs regroupant en nombre considérable les deux types d'événements. Les courbes de distribution selon les mois, jours et heures sont toutes spécifiques. En conclusion, l'article constate que la correspondance géographique entre accidents et contraventions est caractéristique du milieu étudié mais l'inadéuation temporelle en limite la relation. On s'interroge enfin sur le fait que l'intervention policièe pourrait ne pas etre suffisamment planifiée. This article deals with the geographical aspects of highway safety in a rural area. Using two different databanks, the research attempts to establish a correlation between car accidents and the frequency of police intervention (traffic tickets) in specific geographical locations. Is there a higher frequency of highway accidents in areas where patrolmen frequently hand out tickets to motorists? Research results indicate a concentration of accidents occurring in geographic areas where tickets are frequently given out. However, the period in time when tickets are given out does not correspond to the period in time when accidents happen. In conclusion, the authors question the nature of police intervention.     

Mead-Halls of the Oiscingas: A New Kentish Perspective on the Anglo-Saxon Great Hall Complex Phenomenon

THE GREAT HALL complex represents one of the most distinctive and evocative expressions of the Anglo-Saxon settlement record, and is widely cited as a metaphor for the emergence of kingship in early medieval England. Yet interpretation of these sites remains underdeveloped and heavily weighted towards the excavated findings from the well-known site of Yeavering in Northumberland. Inspired by the results of recent excavations at Lyminge, Kent, this paper undertakes a detailed comparative interrogation of three great hall complexes in Kent, and exploits this new regional perspective to advance our understanding of the agency and embodied meanings of these settlements as ‘theatres of power’. Explored through the thematic prisms of place, social memory and monumental hybridity, this examination leads to a new appreciation of the involvement of great hall sites in the genealogical strategies of 7th-century royal dynasties and a fresh perspective on how this remarkable, yet short-lived, monumental idiom was adapted to harness the symbolic capital of Romanitas.