998 resultados para upper house


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View to landscape beyond through windows of upper level of tower (shown open).

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Detail view of timber cross-bracing with polycarbonate sheeting behind as seen from upper level dining studio.

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Detail view of timber cross-bracing to dining studio, as seen from upper living area.

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Detail view of timber cross-bracing with polycarbonate sheeting behind as seen from upper level dining studio.

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View through courtyard to lower studio dining room, as seen from upper living area.

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View through courtyard to lower studio dining room, as seen from upper living area.

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View through courtyard to lower studio dining room, as seen from upper living area.

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View through courtyard to dining studio as seen from upper living room.

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Detail view of cladding to upper level dining studio.

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BACKGROUND: Rhinovirus is the most common cause of respiratory viral infections and leads to frequent respiratory symptoms in lung transplant recipients. However, it remains unknown whether the rhinovirus load correlates with the severity of symptoms. OBJECTIVES: This study aimed to better characterize the pathogenesis of rhinoviral infection and the way in which viral load correlates with symptoms. STUDY DESIGN: We assessed rhinovirus load in positive upper respiratory specimens of patients enrolled prospectively in a cohort of 116 lung transplant recipients. Rhinovirus load was quantified according to a validated in-house, real-time, reverse transcription polymerase chain reaction in pooled nasopharyngeal and pharyngeal swabs. Symptoms were recorded in a standardised case report form completed at each screening/routine follow-up visit, or during any emergency visit occurring during the 3-year study. RESULTS: Rhinovirus infections were very frequent, including in asymptomatic patients not seeking a specific medical consultation. Rhinovirus load ranged between 4.1 and 8.3 log copies/ml according to the type of visit and clinical presentation. Patients with highest symptom scores tended to have higher viral loads, particularly those presenting systemic symptoms. When considering symptoms individually, rhinovirus load was significantly higher in the presence of symptoms such as sore throat, fever, sputum production, cough, and fatigue. There was no association between tacrolimus levels and rhinovirus load. CONCLUSIONS: Rhinovirus infections are very frequent in lung transplant recipients and rhinoviral load in the upper respiratory tract is relatively high even in asymptomatic patients. Patients with the highest symptom scores tend to have a higher rhinovirus load.

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The correspondence from D.W. [David William] Smith to President Peter Russell regarding Smith’s desire to sell a certain piece of property in Newark (now Niagara-on-the-Lake, Ont.) to be used as a location for a common grammar school. The notice gives a description of the building situated on the property as being adaptable for the use of a school. The Board of Survey convened in December 1798 to examine Smith’s property and gave an appropriate valuation of the properties and buildings Smith was offering for sale. Smith was the deputy surveyor general of lands for Upper Canada.

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Original advertisement for William Still's Boarding House, No. 832 South Street, below 9th, south side Philad'a [sic]. Not dated. The advertisement includes handwritten marginalia, possibly by William Still, on the left-hand side referring to St. Catharines. There is a small embossed stamp on the upper left-hand corner of the advertisement. This item was in the possession of the Rick Bell Family of St. Catharines.Handwritten marginalia (original spelling and punctuation): "Do remember me very kindly to all my enquiring friends _ I but seldom hear of late from St. Catherines" The street number printed in the original advertisement (374) has been crossed out in black ink and a handwritten "832" has been inserted. William Still was an African-American abolitionist from Philadelphia and clerk of the Anti-Slavery Society who by his own account assisted 649 slaves receive freedom. He kept records on fugitive slaves so their relatives could find them later. In 1872, he published his records in a book entitled, The Underground Railroad. Source: William Still Underground Railroad Foundation: http://www.undergroundrr.com/foundation/about.htm

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George Upper is a Niagara area artist. His limited edition prints feature local scenes, many from Port Dalhousie, Ontario.

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Ce mémoire propose une analyse du discours et de l’expérience corporelle des adeptes de la scène musicale électronique underground-house de Montréal. Il cherche à contribuer au champ des études sur les formations culturelles expressives contemporaines sur deux axes. Sur le plan méthodologique, cette recherche illustre la portée de l’entretien d’explicitation lorsqu’il s’agit d’accompagner la mise en mots d’impressions sensorielles, d’émotions, de pensées ou d’actions. Combinée à une démarche immersive de longue haleine sur le terrain, cette méthode innovante développée par le chercheur Pierre Vermersch (1994) s’avère ici un outil rigoureux donnant accès à la mémoire incarnée des sujets, laquelle regorge d’informations d’une étonnante précision. Sur le plan ethnographique, cette étude s’intéresse aux nouveaux espaces de solidarité et d’expression balisant l’expérience des Québécois de parents haïtiens issus des classes moyenne et moyenne élevée. Les résultats de cette recherche démontrent, en premier lieu, que l’expérience de la « vibe », expression idiomatique largement utilisée par les acteurs, constitue la clé de voûte maintenant la cohésion entre les représentations, les croyances et les activités corporelles des participants. En deuxième lieu, la scène underground-house se présenterait comme l’expression d’une nouvelle contre-culture en établissant une distance critique avec, d’une part, la « culture hip hop » commerciale et sa représentation médiatique « ghettoïsée » et, d’autre part, l’espace culturel dominant en promouvant une expérience de corps et d’esprit subversive. Cet espace de transmission et de communion inédit propose des modèles de sociabilités nouveaux qui contribuent de manière inusuelle au dialogue interculturel urbain montréalais.

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At various times during the Quaternary, north-eastern England was a zone of confluence between dynamic ice lobes sourced from the Pennines, northern Scotland, the Cheviots, and Scandinavia. The region thus has some of the most complex exposures of Middle to Late Pleistocene sediments in Britain, with both interglacial and glacial sediments deposited in terrestrial and marine settings. We investigated sedimentary sequences exposed on the coastline of County Durham at Warren House Gill, and present a new model of British and Fennoscandian Ice Sheet interaction in the North Sea Basin during the Middle Pleistocene. The stratigraphy at Warren House Gill consists of a lower diamicton and upper estuarine sediments, both part of the Warren House Formation. They are separated from the overlying Weichselian Blackhall and Horden tills by a substantial unconformity. The lower diamicton of the Warren House Formation is re-interpreted here as an MIS 8 to 12 glaciomarine deposit containing ice-rafted lithics from north-eastern Scotland and the northeast North Sea, and is renamed the ‘Ash Gill Member’. It is dated by lithological comparison to the Easington Raised Beach, Middle Pleistocene Amino Acid Racemisation values, and indirectly by optically stimulated luminescence. The overlying shallow subaqueous sediments were deposited in an estuarine environment by suspension settling and bottom current activity. They are named the ‘Whitesides Member’, and form the uppermost member of the Warren House Formation. During glaciation, ice-rafted material was deposited in a marine embayment. There is no evidence of a grounded, onshore Scandinavian ice sheet in County Durham during MIS 6, which has long been held as the accepted stratigraphy. This has major implications for the currently accepted British Quaternary Stratigraphy. Combined with recent work on the Middle Pleistocene North Sea Drift from Norfolk, which is now suggested to have been deposited by a Scottish ice sheet, the presence of a Scandinavian ice sheet in eastern England at any time during the Quaternary is becoming increasingly doubtful.