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Relevant bibliographies by topics / Canadian River

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Academic literature on the topic 'Canadian River'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Canadian River"

1

Ouellet Dallaire, Camille, Bernhard Lehner, and Irena Creed. "Multidisciplinary classification of Canadian river reaches to support the sustainable management of freshwater systems." Canadian Journal of Fisheries and Aquatic Sciences 77, no. 2 (February 2020): 326–41. http://dx.doi.org/10.1139/cjfas-2018-0284.

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Climate change is altering the hydrology of Canadian rivers to an unprecedented degree. Consequently, sustainable freshwater management practices need to adapt, which include the development of integrated water resource strategies and environmental flow recommendations. A particular challenge arises for these assessments due to the highly diverse nature of river ecosystems across Canada. This diversity can be addressed by using a classification system to create manageable spatial units. Building upon and adapting the results of a global river reach classification scheme, we present a multidisciplinary K-means clustering approach to categorize all river reaches of Canada into 23 types at fine spatial resolution. The typology is based on classifier variables related to hydrology, mostly derived from modelled long-term means of monthly discharges, physiography, climate, and fluvial geomorphology. Resulting maps provide baseline information for rivers of all size classes, from small headwater streams to very large rivers, across the entire country, including unmonitored regions such as the High Arctic. The classification system also points to some strategic expansion opportunities for the current Canadian monitoring network of river gauging stations.

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Peden, Alex E., and Grant W. Hughes. "Sympatry in four species of Rhinichthys (Pisces), including the first documented occurrences of R. umatilla in the Canadian drainages of the Columbia River." Canadian Journal of Zoology 66, no. 8 (August 1, 1988): 1846–56. http://dx.doi.org/10.1139/z88-267.

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Four species of Rhinichthys (R. cataractae, R. falcatus, R. osculus, and R. umatilla) are recognized in Canadian sections of the Columbia River, with sympatry occuring between all species except R. falcatus and R. osculus. Species status of the latter is supported by morphological dissimilarity between it and the morphologically similar R. falcatus and R. umatilla. Populations of R. umatilla from the Similkameen, Kettle, and Columbia (including Kootenay and Slocan) rivers have morphological and pigmentary differences, but are identifiable with R. umatilla of the lower Columbia River. Canadian R. osculus are similar to historically known populations near the Colville and Little Spokane rivers of northeastern Washington. Populations from more distant tributaries of the Columbia system are variable in morphology and habitat and require separate study to determine their relationships to Canadian populations. Rhinichthys osculus was apparently replaced by R. umatilla in the Colville River, an event that may have been correlated with historical changes of water quality or flooding by the Roosevelt Reservoir. Because R. umatilla prefers swift clear portions of large rivers, it is potentially in conflict with hydroelectric projects. Though not immediately threatened, the status of this species in Canada should be monitored in connection with future development of river systems.

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Hickin, Edward J. "Fluvial facies models: a review of Canadian research." Progress in Physical Geography: Earth and Environment 17, no. 2 (June 1993): 205–22. http://dx.doi.org/10.1177/030913339301700207.

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Canadian river scientists made significant contributions to the early development (1960-80) of fluvial facies models, particularly to those for braided rivers. More recent Canadian studies (1980-92) have centred on understanding the facies sedimentology of anastomosed and wandering gravel-bed rivers. River planform facies models are distinctly limited as indicators of fluvial style because of: (1) spurious environmental correlations; (2) the difficulty of river planform definition; (3) differential preservation potential of facies; (4) inadequate and unsystematic field sampling; (5) flawed statistical testing; and (6) the inappropriate space scale adopted for analysis. The scale problems of facies analysis may be overcome by employing architectural element analysis in conjunction with modem geophysical methods such as shallow reflection seismology and ground-penetrating radar. Future research should focus on devising specific tests of element-scale sedimentological relationships based on the contemporary fluvial enrivonment.

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Williams, M. M. R. "Deep River: A Canadian Story." Annals of Nuclear Energy 30, no. 15 (October 2003): 1597–98. http://dx.doi.org/10.1016/s0306-4549(03)00104-x.

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Marsalek, J., B. J. Dutka, A. J. McCorquodale, and I. K. Tsanis. "Microbiological pollution in the Canadian upper great lakes connecting channels." Water Science and Technology 33, no. 4-5 (February 1, 1996): 349–56. http://dx.doi.org/10.2166/wst.1996.0525.

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The faecal microbiological pollution was investigated in the Upper Great Lakes Connecting Channels by focusing on the near-shore zones of the St. Marys River in Sault Ste. Marie, the St. Clair River in Sarnia and the Detroit River in Windsor (Ontario). Water samples from these rivers and various sources of faecal pollution were analyzed for the indicator organismrecommended by Health and Welfare Canada --Escherichia coli . The observed bacterial counts were characterized by probabilistic distributions and assessed for compliance with the Ontario recreational water quality guideline (100 E. coli/100 mL). The degree and extent of microbiological pollution were related to dry weather sources (malfunctioning sewer systems) and wet weather discharges, particularly combined sewer overflows (CSOs). Excellent water quality was found in Sault Ste. Marie (no CSOs), but poor quality was found in the St. Clair River along a relatively short Sarnia waterfront (5 CSOs) and in a long stretch of the Detroit River in Windsor (25 CSOs). Among the remedial measures, the highest priorities were assigned to both dry and wet weather source controls. Local improvements in microbiological water quality can be achieved by manipulating bacteria transport in rivers - preventing influx of contaminated waters to the areas used for water-based recreation.

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Banks, Daniel, and Thad A. Harroun. "Seventy years of scientific impact using neutron beams at the Chalk River Laboratories." FACETS 4, no. 1 (June 1, 2019): 507–30. http://dx.doi.org/10.1139/facets-2019-0003.

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The 31 March 2018 closure of the National Research Universal reactor marked the end of over 70 years of materials research using neutron beams from major neutron sources at the Chalk River Laboratories in Chalk River, Ontario, Canada. This closure will have a major impact on the Canadian materials research community, including researchers in the physics, chemistry, and engineering of materials. After a brief review of the history of neutron beams at the Chalk River Laboratories, we present the results of a bibliometric study of the scientific output of the research with neutron beams. In this study, we compiled a complete bibliographic record of the research papers beginning with the first neutron scattering experiments at the National Research Experimental reactor in 1947, analyzed the citations from 1980 onward, and benchmarked the results against major neutron beam facilities in other countries and against other major research facilities in Canada. We also conducted a broader bibliometric analysis of the use of neutron scattering data among all Canadians, regardless of where the data were taken. The results provide a useful metric of the size of the Canadian neutron scattering community and places into context the importance of access to this research tool.

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Kaiser, Ted, Wilma Godon, Ron Whitehorne, Erich R. Gundlach, and Bart J. Baca. "CANADIAN-U.S. SPILL RESPONSE COOPERATION ALONG THE GREAT LAKES." International Oil Spill Conference Proceedings 1987, no. 1 (April 1, 1987): 177–80. http://dx.doi.org/10.7901/2169-3358-1987-1-177.

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ABSTRACT The United States and Canada share more than 1,400 miles of aquatic border between the St. Lawrence River and western Lake Superior. To effectively deal with regional oil and hazardous material spills that can equally affect either side of the border, Canadian and U.S. agencies have formed a cooperative agreement under the CANUSLAK plan to share resources and information before and during spill occurrences. Primary agencies involved include the Canadian and U.S. coast guards, U.S. National Oceanic and Atmospheric Administration, and the Canadian Environmental Protection Service (Emergencies Program). Examples of prespill cooperation, as discussed in this paper, include the joint preparation of contingency plan annexes and shoreline sensitivity atlases for the St. Lawrence River, Detroit-St. Clair River area, and St. Marys River. Cooperation during spills, also discussed, is illustrated by the exchange of information either by direct participation of both countries during response and cleanup or by advisory representation.

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Wirgin, Isaac I., Tun-Liang Ong, Lorraine Maceda, John R. Waldman, David Moore, and Simon Courtenay. "Mitochondrial DNA Variation in Striped Bass (Morone saxatilis) from Canadian Rivers." Canadian Journal of Fisheries and Aquatic Sciences 50, no. 1 (January 1, 1993): 80–87. http://dx.doi.org/10.1139/f93-010.

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Mitochondrial DNA(mtDNA)was analysed to determine the genetic relatedness of striped bass (Morone saxatilis) populations in tributaries to the Gulf of St. Lawrence and the Bay of Funday. Mitochondrial DNA genotype frequencies were compared with those of striped bass from the Shubenacadie River (Bay of Fundy) and the Miramichi and Tabusintac rivers (Gulf of St. Lawrence). These mtDNA genotype frequencies were compared with those of striped bass representative of the Atlantic coastal migratory stock originating in the Hudson River and Chesapeake Bay. Differences in the frequencies of mtDNA length variants permitted discrimination of the Shubenacadie River from the Miramichi River and Tabusintac River populations and all three Canadian populations from the U S. spawned costal migratory stock. No difference in the frequency of mtDNA length variants was observed between Tabusintac River and Miramichi River striped bass. Heteroplasmy for mtDNA length variants was observed in 35% of Gulf of St. Lawrence fish, the highest frequency observed in any striped bass population. These results highlight the genetic heterogeneity of these Canadian striped bass populations and their distinctiveness from U S. stocks. Future efforts to restore these depleted Canadian striped bass populations should consider the impact of stock transfer on endemic striped bass gene pools.

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Beltaos, S., and B. C. Burrell. "Hydrotechnical advances in Canadian river ice science and engineering during the past 35 years." Canadian Journal of Civil Engineering 42, no. 9 (September 2015): 583–91. http://dx.doi.org/10.1139/cjce-2014-0540.

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Greater opportunity now exists compared to 35 years ago for civil engineers to apply river ice knowledge to practical problems of planning, designing, and operating hydro-power facilities, water intakes, bridges, and other infrastructure along ice-covered rivers. This is due to major advancements made during this period in understanding the physical processes of river ice formation, growth and breakup, in developing instrumentation for acquisition of information on winter environments, and in developing numerical modelling tools. An increasing number of journal articles, as well as papers presented at the river ice workshops of the CGU Committee on River Ice Processes and the Environment (CRIPE) and the ice symposia of the International Association for Hydro-Environment Engineering and Research (IAHR) attest to the advancement in river ice science and engineering knowledge that has occurred during the past 35 years. This paper reviews the developments in river ice science and engineering from a Canadian perspective and briefly discusses future directions.

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Venkiteswaran, Jason J., Sherry L. Schiff, and Brian P. Ingalls. "Quantifying the fate of wastewater nitrogen discharged to a Canadian river." FACETS 4, no. 1 (June 1, 2019): 315–35. http://dx.doi.org/10.1139/facets-2018-0028.

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Addition of nutrients, such as nitrogen, can degrade water quality in lakes, rivers, and estuaries. To predict the fate of nutrient inputs, an understanding of the biogeochemical cycling of nutrients is needed. We develop and employ a novel, parsimonious, process-based model of nitrogen concentrations and stable isotopes that quantifies the competing processes of volatilization, biological assimilation, nitrification, and denitrification in nutrient-impacted rivers. Calibration of the model to nitrogen discharges from two wastewater treatment plants in the Grand River, Ontario, Canada, show that ammonia volatilization was negligible relative to biological assimilation, nitrification, and denitrification within 5 km of the discharge points.

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Dissertations / Theses on the topic "Canadian River"

1

Batten, Douglas James. "Nonlinear time series modeling of some Canadian river flow data." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ54860.pdf.

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St, George Scott. "Hydrological and Paleo-Drought Variability in the Winnipeg River Basin, Canada and the Canadian Prairies." Diss., The University of Arizona, 2007. http://hdl.handle.net/10150/194832.

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Changing hydroclimatic conditions are the primary source of risk to hydroelectric power generation. The research described in this dissertation investigates hydrological and drought variability in the Winnipeg River basin, Canada, during the last several hundred years using instrumental hydroclimate data and paleoclimatic records derived from tree rings. The basin drains parts of northwestern Ontario, northern Minnesota and southeastern Manitoba, and is the most important component of the hydrological system used to generate power in Manitoba. Extreme low annual flows in the Winnipeg River are associated with enhanced meridional flow across western Canada during summer and autumn, which suppresses precipitation over the watershed and reduces runoff from spring snowmelt. In contrast to the declining flows observed for other regional rivers, mean annual discharge in the Winnipeg River basin has increased substantially since the early 1920s. For a longer perspective, fifty-four ringwidth chronologies (mainly Pinus resinosa and P. strobus) were used to assess changes in summer climate in the Winnipeg River region since AD 1783. Tree growth in this region is significantly, but weakly, correlated with both temperature and precipitation during summer. Synthetic tree-ring records produced by the Vaganov-Shashkin model of tree-ring formation are consistent with these relationships with climate, and suggest that the primary factor limiting tree growth switches from temperature to moisture in mid-summer. The Winnipeg River tree-ring record indicates that summer droughts were more persistent in the 19th and late 18th century than during the last 100 years, but there is no evidence that drought was more extreme prior to the onset of direct monitoring.This dissertation also examines past changes in summer drought over the broader region using 138 ringwidth records from the Canadian Prairies provinces and adjacent areas. Regional ringwidth signals are primarily related to summer moisture and drought conditions. These summer-sensitive records are not linearly related to major modes of climate variability, including ENSO and the PDO, which mainly affect the climate of western Canada during winter. Extended drought records inferred from regional tree-ring series indicate that drought on the Canadian Prairies has exhibited considerable spatial heterogeneity over the last several centuries.

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De, Pascale Gregory P. "Massive ice in coarse-grained sediments, Western Canadian Arctic." Thesis, McGill University, 2005. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82217.

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Destruction of ecosystems and infrastructure can be caused by melting of massive ice within permafrost. To predict potential melting caused by natural and human disturbance, we need to know the nature and origin of massive ice deposits. The purpose of this research was to evaluate the nature of massive ice in coarse-grained sediments that accepted theories suggest should not occur.
Degradation of ice-rich granular resources is expensive and difficult to rehabilitate and can cause developmental thermokarst, overestimation of granular resources, disturbance of wildlife habitat and create conflicts with traditional land uses.
To locate massive ice we used a resistivity geophysical technique and to characterize the ice we used geochemical, petrographic and stratigraphic techniques. The resistivity technique detected bodies of massive ice and ice-rich sediments and coarse-grained sediments at high resolutions and laboratory analysis reveal that the ice was of glacial origin.
These findings indicate that massive ice of glacial origin occurs in coarse-grained sediments in permafrost. The techniques used in this study could form the basis of a predictive model of massive ice occurrence.

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Bickers, Margaret A. "Three cultures, four hooves and one river : the Canadian river in Texas and New Mexico, 1848-1939." Diss., Manhattan, Kan. : Kansas State University, 2010. http://hdl.handle.net/2097/4186.

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Zalatan, R., and K. Gajewski. "Dendrochronological Potential of Salix Alaxensis from the Kuujjua River Area, Western Canadian Arctic." Tree-Ring Society, 2006. http://hdl.handle.net/10150/262624.

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This study presents the first annually-resolved chronology using Salix alaxensis (Anderss.) Cov from Victoria Island, Northwest Territories, Canada, an area well north of treeline. Forty-one samples were collected and examined for subsequent analysis. However, crossdating was difficult because of locally absent or missing rings and the narrowness of the rings, and ultimately thirteen stems were crossdated and used to evaluate their dendroclimatological potential. The chronology spans 74 years (1927-2000) and could potentially be extended further using subfossil wood. Precipitation data from December of the previous year to March of the current year were the most consistently and highly correlated with ring width. This suggests that the recharge of the soil moisture by early summer snowmelt is a key factor limiting growth of these shrubs.

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Davey, Chad E. "Longitudinal trends in grain size, shear stress and sediment mobility along sedimentary links of a Canadian Shield river, Saguenay Region : a geomorphic perspective on assessing Atlantic salmon (Salmo salar) productivity in rivers." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82215.

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The segmenting of gravel-bed rivers into 'sedimentary links', characterized by single-sediment sources and downstream fining of alluvial sediments, is a relatively new technique which has had limited application. The sedimentary link concept has been primarily applied to alpine river environments where link formations are supplied by coarse sediment from active point sources. The purpose of this study is to apply the sedimentary link concept on the Ste Marguerite River in the Saguenay region of the Canadian Shield, where valley-segment deposits of coarse sediment from ancient glacial processes are dominant in forming links.
Specifically, this study examines link-scale trends in surface grain size and channel slope. This study also uses the sedimentary link concept within an ecological context to explain the spatial organization and quality of Atlantic salmon spawning and rearing habitat. (Abstract shortened by UMI.)

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Hawkins, Emily. "Demography, Movement Patterns, and Habitat Selection of Blanding's Turtles at Canadian Nuclear Laboratories in Chalk River, Ontario." Thesis, Université d'Ottawa / University of Ottawa, 2016. http://hdl.handle.net/10393/35563.

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The development and implementation of effective species and population-specific management strategies requires population-specific information. To demonstrate the relative extirpation risk associated with various road mortality scenarios for a population of Blanding’s turtles at Canadian Nuclear Laboratories in Chalk River, Ontario, a Population Viability Analysis was conducted. Road mortality of two adult females every ten years resulted in population extirpation within 200 years relative to a stable population not experiencing road mortality. To accommodate informed decision-making for the management of this species at risk, the movement patterns and habitat selection of this Blanding’s turtle population were described. There was no significant difference between males and females in distance moved between relocations in either the spring or the summer, but turtles moved greater distances in the spring than in the summer. Annual and seasonal home range size did not differ between the sexes or between spring and summer periods. A compositional analysis indicated Blanding’s turtles preferred marsh habitats over bog, swamp, lake, and upland. Matched-paired logistic regression was used to determine selection of microhabitat features, such as type of vegetation, in the spring and summer. Turtles preferred sites with warmer air temperatures, shallower water, a higher availability of open water, and greater coverage of emergent and floating vegetation types in the spring period. In the summer period, turtles preferred sites characterized by cooler, deeper water, a higher availability of open water, and greater coverage of emergent and floating vegetation types. This population of Blanding’s turtles appears to be relatively small and the continued threat of road mortality indicates a delicate situation for its persistence. Considering seasonally preferred habitats will best inform management decisions for seasonal work restrictions and future development plans.

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Friesen, Wilbert J. "Development ethics and the Canadian North : a case study analysis of the Churchill-Nelson Rivers Hydro Diversion Project." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0018/NQ55332.pdf.

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Clarke, Margaret L. "Reconstituting the fur trade community of the Assiniboine basin, 1793 to 1812." Ottawa : Library and Archives Canada, 1998. http://www.nlc-bnc.ca/obj/s4/f2/dsk3/ftp04/mq23256.pdf.

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Burge, Leif M. "Dynamics of a transitional river pattern : a multi-scale investigation of controls on the wandering pattern of Miramichi rivers, New Brunswick, Canada." Thesis, McGill University, 2003. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=84484.

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The wandering river pattern represents one of the last remaining river patterns that are not well understood. Many aspects of these rivers are not well known, particularly the processes of their creation and maintenance. The term wandering describes gravel or cobble bedded rivers, transitional between braided and meandering, with multiple channel sections around semi-permanent islands connected by single channel sections. This dissertation investigates the controls on the characteristics of wandering rivers within the Miramichi region of New Brunswick through time and at three nested spatial scales.
At the scale of rivers, three factors appear to be needed for wandering to occur: (1) wide valleys, (2) channel energy between braiding and meandering, and (3) avulsion triggers, frequent overbank flows caused by icejams in the Miramichi. Principal component analysis showed that larger wandering rivers displayed greater anabranching intensity than smaller rivers, perhaps related to higher stage ice jams within larger rivers.
At the scale of channels, the wandering pattern of the Renous River was found to be in a state of dynamic equilibrium, with channel creation balanced by channel abandonment. The anabranch cycle model was developed to illustrate the temporal dynamics of anabranch creation, maintenance and abandonment within wandering rivers.
Also at the channel scale, principal component analysis of channel reaches within the Renous River displayed differences in grain size and hydraulic efficiency between side-channels and main-channels. Energy and sediment mobility within side-channels was related to their formation, maintenance and abandonment. Energy and sediment mobility within main-channels was related to mega bedforms called bedwaves. The apex of some bedwaves occurred at diffluences.
At the scale of channel elements, diffluences are stable where a large bar is formed and accretes upstream, creating a large reservoir of sediment upstream of anabranch channels to buffer their degradation. Where diffluences are unstable, a large bar forms within one anabranch channel to partially block flow and may cause its abandonment. The dissertation illustrates that within wandering rivers, processes occurring at multiple spatial and temporal scales interact to create and maintain the pattern.

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Books on the topic "Canadian River"

1

Lane, M. Travis. River readings. Fredericton, N.B: Wild East, 1993.

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Sawdon, Robert Gordon. Another river to cross. Gilbert Plains, Man: Peckham's Family History Research/Publishing, 2000.

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MacDonald, Jake. Raised by the river. Winnipeg: Turnstone, 1992.

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1962-, Chevrier Mike, and Lalouette Jacques 1930-, eds. Lights over the river. Oakville, Ont: Mosaic Press, 1989.

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MacDonald, Jake. Raised by the river. Winnipeg: Turnstone, 1992.

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Bloomfield, Lori Ann. The last river child. Toronto: Second Story Press, 2009.

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Bloomfield, Lori Ann. The last river child. Toronto: Second Story Press, 2009.

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The last river child. Toronto: Second Story Press, 2009.

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Geddes, Hilda. The Canadian Mississippi River: Hilda Geddes. Burnstown, Ont., Canada: General Store Pub. House, 1992.

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Raised by the river: Jake MacDonald. Winnipeg, Manitoba, Canada: Turnstone Press, 1992.

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Book chapters on the topic "Canadian River"

1

Flamini, Enrico, Alessandro Coletta, Maria Libera Battagliere, and Maria Virelli. "Steen River, Canada." In Encyclopedic Atlas of Terrestrial Impact Craters, 617–19. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-05451-9_171.

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Prowse, Terry. "Lake and River Ice in Canada." In Changing Cold Environments, 163–81. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781119950172.ch9.

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Murray, Anne. "Fraser River Delta: Southern British Columbia (Canada)." In The Wetland Book, 1–11. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_191-3.

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Murray, Anne. "Fraser River Delta: Southern British Columbia (Canada)." In The Wetland Book, 565–75. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_191.

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Curtis, R. S., A. P. Finch, and R. P. Lovat. "New St Clair River tunnel, Canada-USA." In Tunnelling’ 94, 69–86. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2646-9_5.

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Shatford, Jeffrey. "The Peace-Athabasca Delta: MacKenzie River Basin (Canada)." In The Wetland Book, 1–8. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_13-1.

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Shatford, Jeffrey. "The Peace-Athabasca Delta: MacKenzie River Basin (Canada)." In The Wetland Book, 549–56. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_13.

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Flannagan, J. F., J. Alba-Tercedor, R. G. Lowen, and D. G. Cobb. "Emergence of Ephemeroptera from the Assiniboine River, Canada." In Trends in Research in Ephemeroptera and Plecoptera, 97–106. Boston, MA: Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1257-8_13.

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Law, K. Tim, and C. F. Lee. "The retrogressive slide at Nipigon River, Ontario, Canada." In Slope Stability Engineering, 1129–34. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203739600-87.

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Michael, E., and P. Chadwick. "Relationship Between Atlantic Salmon Smolts and Adults in Canadian Rivers." In Atlantic Salmon, 301–24. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-1235-9_16.

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Conference papers on the topic "Canadian River"

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Huntley, David H., Peter Bobrowsky, Roger MacLeod, Robert Cocking, Jamel Joseph, and Drew Rotheram-Clarke. "CANADIAN GEOSCIENCE MAP: RIPLEY LANDSLIDE, THOMPSON RIVER VALLEY, BRITISH COLUMBIA, CANADA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339684.

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Bender, Michael, Rolf Oswald, Mark Vandersluis, Mark Deutschman, and Slobodan Simonovic. "Red River Basin Canadian Flood Management Virtual Database." In Joint Conference on Water Resource Engineering and Water Resources Planning and Management 2000. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40517(2000)115.

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Hepburn, B., and B. Beekman. "Reverse Circulating Cement Technique for Subsurface Pipeline River Crossing." In Canadian International Petroleum Conference. Petroleum Society of Canada, 2005. http://dx.doi.org/10.2118/2005-265.

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Erwin, M. D., C. R. Pierson, and D. B. Bennion. "Brine Imbibition Damage in the Alpine/Colville River Field, Alaska." In Canadian International Petroleum Conference. Petroleum Society of Canada, 2003. http://dx.doi.org/10.2118/2003-050.

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Brissenden, S. J. "Steaming Uphill: Using J-Wells for CSS at Peace River." In Canadian International Petroleum Conference. Petroleum Society of Canada, 2005. http://dx.doi.org/10.2118/2005-107.

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Makhanov, Kaiyrzhan, Hassan Dehghanpour, and Ergun Kuru. "An Experimental Study of Spontaneous Imbibition in Horn River Shales." In SPE Canadian Unconventional Resources Conference. Society of Petroleum Engineers, 2012. http://dx.doi.org/10.2118/162650-ms.

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Kimiaghalam, N., and S. Clark. "River morphodynamics in the Canadian Prairies: An overview of recent studies in Manitoba." In The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742: CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-198.

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Pond, Jennifer, Tyler Zerbe, and Kirk W. Odland. "Horn River Frac Water: Past, Present, and Future." In Canadian Unconventional Resources and International Petroleum Conference. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/138222-ms.

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Novlesky, Alex, Anjani Kumar, and Stefan Merkle. "Shale Gas Modeling Workflow: From Microseismic to Simulation -- A Horn River Case Study." In Canadian Unconventional Resources Conference. Society of Petroleum Engineers, 2011. http://dx.doi.org/10.2118/148710-ms.

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Hildebrande, A. R., M. J. Mazur, R. R. Stewart, A. Schafer, D. W. Hladiuk, L. Scheonthaler, and M. Pilkington. "Seismic Velocity Imaging of the Steen River Crater: Technique Development for Exploring Crater Reservoirs." In Canadian International Petroleum Conference. Petroleum Society of Canada, 2000. http://dx.doi.org/10.2118/2000-101-ea.

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Reports on the topic "Canadian River"

1

Irvine, M., I. R. Smith, and T. Bell. Community-scale hazard mapping in the Canadian Arctic: a case study of Clyde River, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/286264.

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Fritz, W. H. The basal contact of the Road River group-a proposal for its location in the type area and in other selected areas in the northern Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120246.

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Fallas, K. M., and T. D. Finley. A GIS dataset of geological features from mineral exploration of the Gayna River Property by Rio Tinto Canadian Exploration Ltd., 1975-1976, northern Mackenzie Mountains, Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328243.

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Ashmore, P., and M. Church. The impact of climate change on rivers and river processes in Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/211891.

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Day, T. J. River Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131644.

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Christian, H. A., T. Mulder, and R. C. Courtney. Seabed slope instability on the Fraser River Delta, Vancouver, British Columbia, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205044.

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Rivera, A., M. A. Pétré, F. Létourneau, and F. Audet-Gagnon. Groundwater atlas of the Milk River Transboundary Aquifer, Alberta, Canada and Montana, U.S.A. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/302719.

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McCracken, A. D. Middle ordovician conodonts from the Cordillera Road River Group, northern Yukon Territory, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132433.

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Bell, J. S., and P. F. Lloyd. Modelling of Stress Refraction in Sediments Around the Peace River Arch, western Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126688.

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Pétré, M. A., and A. Rivera. A synthesis of knowledge of the Milk River Transboundary Aquifer (Alberta, Canada - Montana, USA). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/295754.

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