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Core 1..4 Bill (PRISM::Advent3b2 15.50)
C-493 C-493 First Session, Forty-first Parliament, Première session, quarante et unième législature, 60-61-62 Elizabeth II, 2011-2012-2013 60-61-62 Elizabeth II, 2011-2012-2013 HOUSE OF COMMONS OF CANADA CHAMBRE DES COMMUNES DU CANADA BILL C-493 PROJET DE LOI C-493 An Act to amend the Navigable Waters Protection Act Loi modifiant la Loi sur la protection des eaux navigables (Ashuapmushuan River, Mistassini River and Peribonka (rivières Ashuapmushuan, Mistassini et Péribonka) River) FIRST READING, APRIL 22, 2013 PREMIÈRE LECTURE LE 22 AVRIL 2013 NOTE NOTE 2nd Session, 41st Parliament 2e session, 41e législature This bill was introduced during the First Session of the 41st Le présent projet de loi a été présenté lors de la première session de la Parliament. Pursuant to the Standing Orders of the House of 41e législature. Conformément aux dispositions du Règlement de la Commons, it is deemed to have been considered and approved at all Chambre des communes, il est réputé avoir été examiné et approuvé à stages completed at the time of prorogation of the First Session. The toutes les étapes franchies avant la prorogation de la première session. number of the bill remains unchanged. Le numéro du projet de loi demeure le même. MR.CHOQUETTE M. CHOQUETTE 411730 SUMMARY SOMMAIRE This enactment amends the Navigable Waters Protection Act in order to add Le texte modifie la Loi sur la protection des eaux navigables pour ajouter les the Ashuapmushuan River, the Mistassini River and the Peribonka River to the rivières Ashuapmushuan, Mistassini et Péribonka aux eaux navigables navigable waters listed in the schedule to that Act, as it will read immediately mentionnées à l’annexe de cette loi, dans sa version postérieure à l’entrée en after the coming into force of section 331 of the Jobs and Growth Act, 2012. -
Downscaling of Global Climate Model Outputs for Flood Frequency
Science Sub-Component Climate Change Action Fund, Environment Canada Downscaling of Global Climate Model Outputs for Flood Frequency Analysis in the Saguenay River System Project no. S02-15-01 Paulin Coulibaly and Yonas B. Dibike Department of Civil Engineering / School of Geography and Geology McMaster University Hamilton, ON L8S 4L7 Collaborators: François Anctil and Bruno Larouche Hamilton, ON June 2004 Downscaling and Climate Change Impact Study in Saguenay Watershed Downscaling Global Climate Model Outputs for Flood Frequency Analysis in the Saguenay River System Final Report by Paulin Coulibaly and Yonas B. Dibike Financial Support: The Government of Canada Climate Change Action Fund June, 2004 Project participants: Mr. Jean Paquin, Hydrologist, ALCAN Company, Jonquiere, Quebec Mr. Sajjad M. Khan, PhD candidate, Department of Civil Engineering, McMaster University Mr. Xiaogong Shi, M.A.Sc. candidate, Department of Civil Engineering, McMaster University Starting date: November 1, 2002 Ending date: June 30, 2004 Project summary: The Global Climate Models (GCMs) used to simulate the present climate and project future climate are generally not designed for local or regional climate change impact studies. While GCMs demonstrated significant skill at the continental and hemispherical scales, they are inherently unable to represent local or subgrid-scale features and dynamics such as local topographical features and convective cloud processes. However, most hydrological models used in climate change impact studies need to simulate sub-grid scale phenomenon and therefore require input data (such as precipitation and temperature) at similar sub-grid scale (i.e. high resolution). Therefore, there is a need to convert (or ‘downscale’) the GCM outputs into high resolution daily precipitation and temperature series appropriate for local or regional scale hydrological impact studies. -
Winter 2016 Vol
Winter 2016 Vol. 43 No. 1 Quarterly Journal of the Wilderness Canoe Association Start at Whitefish Lake From Whitefish Lake to Great Slave Lake: Tundra, Trees and Cliffs Story and photos by John McInnes Having spent several summers in the 1990s exploring some the drainages entering the lake from the south are no more of the small rivers falling into the East Arm of Great Slave than tiny creeks. The only river of any size entering Lake (McLeod Bay) from the north, I was curious if it Christie Bay is the Snowdrift. Rising in the Barrens at were possible to canoe into the East Arm (Christie Bay) Sandy Lake, it flows southwest parallel to the axis of the from the south. Geology was an obstacle here since the East Arm until finally plunging through the McDonald steep north-facing cliffs of the McDonald Fault, which Fault to Great Slave. runs along the south shore of the lake here, mean that the This final plunge was the problem. The surveyor Guy height of land is only a few kilometres inland, and most of Blanchet had followed the Snowdrift in 1925. Missing the Browning estimated the portage, which took several days, to be at least thirteen miles – “enough portaging to last us forever.” 2 Perusing maps of the area, I won - dered if it might be possible to bypass this last difficult section of the Snowdrift. My attention was drawn to a possible portage route, leaving the Snowdrift further upstream, and fol - lowing a chain of lakes – Robert, Dion, and Daisy – to what appeared to be a gap in the steep contours of the McDonald Fault and a possible descent to Meridian Lake and Charlton Bay, at the far east end of Great Slave. -
Université Du Québec Mémoire Présenté À L
UNIVERSITÉ DU QUÉBEC MÉMOIRE PRÉSENTÉ À L'UNIVERSITÉ DU QUÉBEC À CHICOUTIMI COMME EXIGENCE PARTIELLE DE LA MAÎTRISE EN SCIENCES DE LA TERRE PAR DAPHNE SILVA PINO B.A.A. STRUCTURAL HYDROGEOLOGY IN THE KENOGAMI UPLANDS, QUEBEC, CANADA AOÛT 2012 "Those were the stories that stayed with you, that meant something. (...) Folk in those stories had lots of chances of turning back, only they didn't. They kept going, because they were holding on to something." J. R. R. Tolkien (The Lord of the rings - The two towers) To my parents, Francisco and Marina, my sister, Ingrid, and my best friend, Vitor. For always giving me something to hold on to. Ill ABSTRACT Characterizing the joint system is a very significant component of investigations on fractured rock aquifers, as the secondary porosity controls the groundwater flow. It is also important to analyze the types of interactions between the joints, e.g., the types of termination and the dominancy of a certain joint set, since such information helps to understand the tectonic events that were responsible for the generation of the joint systems in the aquifer. Moreover, the current stress field is usually the most significant in controlling joint aperture, which plays a major role in groundwater flow. The main objective of this work is to characterize an aquifer in fractured crystalline rocks with a fairly homogeneous lithology, defining a hydrogeological model of the study area, through structural surveys at different scales and hydrogeologic data analyses. This study was carried out in the Kenogami uplands, within the Saguenay graben, Quebec. It aimed to answer the following questions: (1) is there a structured joint system in the bedrock, that is, is it possible to identify preferential joint orientations and structural domains? (2) Can joint systems be defined at different scales, e.g.