Équité d’utilisation des services de santé et de disponibilité des ressources en matière de santé dans la province de Québec

Objectif : L’objectif général de cette étude est de comprendre en quoi l’utilisation des services de santé et de disponibilité des ressources en santé au Québec sont équitables. Méthodes : De type transversal et corrélationnel, cette étude intéresse les 95 territoires CSSS du Québec, et couvre les années 2006-2007 et 2008-2009. L’indice de défavorisation matérielle et sociale de Pampalon est mis en lien avec deux séries de variables, soit celles d’utilisation des services par CSSS (services hospitaliers; services médicaux; services CLSC) et celles de disponibilité des ressources (capacité financière; capacité matérielle, capacité humaine; viabilité). Pour ce faire, des analyses de variance ont été effectuées. Le modèle intégrateur de la performance des services de santé EGIPSS et celui de l’utilisation des services de santé de Donabedian servent de cadre d’analyse. Résultats : L’utilisation des services de santé est équitable en ce qui concerne la défavorisation matérielle, mais pas en ce qui a trait à la défavorisation sociale. L’utilisation des services médicaux dispensés par les omnipraticiens est plus élevée chez les populations les plus favorisées socialement comparativement aux populations les plus défavorisées. Toutefois, l’utilisation des médecins spécialistes est plus équitable que celle des omnipraticiens, cela, chez les populations défavorisées autant matériellement que socialement. Les hospitalisations évitables sont plus élevées chez les populations les défavorisées socialement comparativement aux populations les plus favorisées. En termes de disponibilité des ressources, les populations défavorisées disposent de plus de ressources que les plus favorisées, sauf en ce qui concerne la répartition du personnel. Conclusion : En général, il existe très peu d’iniquités dans l’utilisation des services de santé au Québec. Par ailleurs, la disponibilité des ressources en santé est relativement équitable au Québec, exception faite de la disponibilité du personnel.

Mapping surface deformation in open pit iron mines of Carajas Province (Amazon Region) using an integrated SAR analysis

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

Hazard index maps for woody material recruitment and transport in alpine catchments

A robust and reliable risk assessment procedure for hydrologic hazards deserves particular attention to the role of transported woody material during flash floods or debris flows. At present, woody material transport phenomena are not systematically considered within the procedures for the elaboration of hazard maps. The consequence is a risk of losing prediction accuracy and of underestimating hazard impacts. Transported woody material frequently interferes with the sediment regulation capacity of open check dams and moreover, when obstruction phenomena at critical crosssections of the stream occur, inundations can be triggered. The paper presents a procedure for the determination of the relative propensity of mountain streams to the entrainment and delivery of recruited woody material on the basis of empirical indicators. The procedure provided the basis for the elaboration of a hazard index map for all torrent catchments of the Autonomous Province of Bolzano/Bozen. The plausibility of the results has been thoroughly checked by a backward oriented analysis on natural hazard events, documented since 1998 at the Department of Hydraulic Engineering of the aforementioned Alpine Province. The procedure provides hints for the consideration of the effects, induced by woody material transport, during the elaboration of hazard zone maps.

Geology of the Haliburton and Bancroft areas, province of Ontario,

Mode of access: Internet.

Memoirs, maps, &c., issued by the Geological Survey of the United Kingdom and the Museum of Practical Geology.

At head of title: List F.

Annales de la propagation de la foi pour la province de Québec.

"table des maitères des Annales de la Propagation de la foi pour la province de Québec depuis le premier numéro, février 1877, jusqu'au trente-sixième numéro, octobre 1888 inclusivement": no. 36, Oct. 1888, p. [275]-288.

Évolution de l'autonomie des commissaires d'écoles de la province de Québec de 1846 à 1967

Il est assez difficile d’évaluer en termes d’autonomie, du moins jusqu’en 1961, l’évolution de la loi concernant les dépenses des commissions scolaires : elles dépendent en partie de leurs sources de revenus, mais il nous semble clair que leur autonomie, du moins théoriquement, a diminué de beaucoup à partir de 1961, à cause de la nécessité de faire approuver leur budget annuel. Si de façon générale on peut dire que les commissaires d’écoles ont moins d’autonomie aujourd’hui qu’en 1846, l’évolution de la législation n’a cependant pas, durant toute cette période, suivi une courbe générale unique pour les six secteurs analysés. Nous avons remarqué deux tendances opposées jusqu’en 1961 : d’une part le législateur a graduellement diminué l’autonomie des commissaires dans leurs relations avec les instituteurs et le domaine pédagogique, et d’autre part il a augmenté leurs pouvoirs dans le domaine financier. Mais à partir de 1961, il a beaucoup diminué leur autonomie financière. En résumé, les commissaires d’écoles sont moins libres aujourd’hui qu’en 1846, mais leurs responsabilités générales sont cependant plus considérables.

Spatiotemporal analysis of indigenous and imported dengue fever cases in Guangdong province, China

Background Dengue fever has been a major public health concern in China since it re-emerged in Guangdong province in 1978. This study aimed to explore spatiotemporal characteristics of dengue fever cases for both indigenous and imported cases during recent years in Guangdong province, so as to identify high-risk areas of the province and thereby help plan resource allocation for dengue interventions. Methods Notifiable cases of dengue fever were collected from all 123 counties of Guangdong province from 2005 to 2010. Descriptive temporal and spatial analysis were conducted, including plotting of seasonal distribution of cases, and creating choropleth maps of cumulative incidence by county. The space-time scan statistic was used to determine space-time clusters of dengue fever cases at the county level, and a geographical information system was used to visualize the location of the clusters. Analysis were stratified by imported and indigenous origin. Results 1658 dengue fever cases were recorded in Guangdong province during the study period, including 94 imported cases and 1564 indigenous cases. Both imported and indigenous cases occurred more frequently in autumn. The areas affected by the indigenous and imported cases presented a geographically expanding trend over the study period. The results showed that the most likely cluster of imported cases (relative risk = 7.52, p < 0.001) and indigenous cases (relative risk = 153.56, p < 0.001) occurred in the Pearl River Delta Area; while a secondary cluster of indigenous cases occurred in one district of the Chao Shan Area (relative risk = 471.25, p < 0.001). Conclusions This study demonstrated that the geographic range of imported and indigenous dengue fever cases has expanded over recent years, and cases were significantly clustered in two heavily urbanised areas of Guangdong province. This provides the foundation for further investigation of risk factors and interventions in these high-risk areas.

Eruption centres of the Hamilton area of the Newer Volcanics Province, Victoria, Australia: Pinpointing volcanoes from a multifaceted approach to landform mapping

Volcanic eruption centres of the mostly 4.5 Ma-5000 BP Newer Volcanics Province in the Hamilton area of southeastern Australia were examined in detail using a multifaceted approach, including ground truthing and analysis of ArcGIS Total Magnetic Intensity and seamless geology data, NASA Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) digital elevation models and Google Earth satellite image interpretation. Sixteen eruption centres were recognised in the Hamilton area, including three previously unrecorded volcanoes-one of which, the Cas Maar, constitutes the northernmost maar-cone volcanic complex in the Western Plains subprovince. Seven previously allocated eruption centres were placed into question based on field and laboratory observations. Three phases of volcanic activity have been suggested by other authors and are interpreted to correlate with ages of >4 Ma, ca 2 Ma and <0.5 Ma, which may be further subdivided based on preservation of outcrop. Geochemical compositions of the dominantly basaltic products become increasingly alkaline and enriched in incompatible elements from Phases 1 to 2, with Phase 3 eruptions both covering the entire geochemical range and extending into increasingly enriched compositions. This research highlights the importance of a multifaceted approach to landform mapping and demonstrates that additional volcanic centres may yet be discovered in the Newer Volcanics Province

Victoria erupts: The Newer Volcanics Province of south-eastern Australia

The Newer Volcanics Province of south-eastern Australia is often overlooked, though it comprises a multitude of volcanic features worthy of exploration. The province contains > 416 eruption centres varying in nature from simple to complex, ranging from lava shields and scoria cones to some of the largest maar volcanoes in the world. Explorable caves and lava tubes showcase well-preserved lava flow features, while the province is a fossickers dream, containing abundant mantle xenolith and megacryst collecting localities. As the most recent eruption was ~5000 bp at Mt. Gambier, the Newer Volcanics is considered an active province, and may yet provide Australia with more eruptions, adding to the glorious volcanic features of the wonderful landscape.

Petrology and textural classification of the Jericho kimberlite, northern Slave Province, Nunavut, Canada

The paper presents data on petrology, bulk rock and mineral compositions, and textural classification of the Middle Jurassic Jericho kimberlite (Slave craton, Canada). The kimberlite was emplaced as three steep-sided pipes in granite that was overlain by limestones and minor soft sediments. The pipes are infilled with hypabyssal and pyroclastic kimberlites and connected to a satellite pipe by a dyke. The Jericho kimberlite is classified as a Group Ia, lacking groundmass tetraferriphlogopite and containing monticellite pseudomorphs. The kimberlite formed, during several consecutive emplacement events of compositionally different batches of kimberlite magma. Core-logging and thin-section observations identified at least two phases of hypabyssal kimberlites and three phases of pyroclastic kimberlites. Hypabyssal kimberlites intruded as a main dyke (HK1) and as late small-volume aphanitic and vesicular dykes. Massive pyroclastic kimberlite (MPK1) predominantly filled the northern and southern lobes of the pipe and formed from magma different from the HK1 magma. The MPK1 magma crystallized Ti-, Fe-, and Cr-rich phlogopite without rims of barian phlogopite, and clinopyroxene and spinel without atoll structures. MPK1 textures, superficially reminiscent of tuffisitic kimberlite, are caused by pervasive contamination by granite xenoliths. The next explosive events filled the central lobe with two varieties of pyroclastic kimberlite: (1) massive and (2) weakly bedded, normally graded pyroclastic kimberlite. The geology of the Jericho pipe differs from the geology of South African or the Prairie kimberlites, but may resemble Lac de Gras pipes, in which deeper erosion removed upper fades of resedimented kimberlites.

Geology alive. GeoBizirik.org

Geology is the science that studies the Earth, its composition, structure and origin in addition to past and present phenomena that leave their mark on rocks. So why does society need geologists? Some of the main reasons are listed below: - Geologists compile and interpret information about the earth’s surface and subsoil, which allows us to establish the planet’s past history, any foreseeable changes and its relationship with the rest of the solar system. - Society needs natural resources (metals, non-metals, water and fossil fuels) to survive. The work of geologists is therefore a key part of finding new deposits and establishing a guide for exploring and managing resources in an environmentally-friendly way. - The creation of geological maps allows us to identify potential risk areas and survey different land uses; in other words, they make an essential contribution to land planning and proposing sustainable development strategies in a region. - Learning about Geology and the proper use of geological information contributes to saving lives and reducing financial loss caused by natural catastrophes such as earthquakes, tsunamis, volcanic eruptions, flooding and landslides, while also helping to develop construction projects, public works, etc. Through the proposed activities we aim to explain some of the basic elements of the different specialities within the field of Geological Sciences. In order to do this, four sessions have been organised that will allow for a quick insight into the fields of Palaeontology, Mineralogy, Petrology and Tectonics.