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Relevant bibliographies by topics / Saskatchewan Valley

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Academic literature on the topic 'Saskatchewan Valley'

Author: Grafiati

Published: 4 June 2021

Last updated: 27 July 2025

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Journal articles on the topic "Saskatchewan Valley"

1

Christiansen, E. A. "Verendrye valley and the Glidden esker, Saskatchewan: subglacial and ice-walled features in southwestern Saskatchewan, Canada." Canadian Journal of Earth Sciences 24, no. 1 (1987): 170–76. http://dx.doi.org/10.1139/e87-014.

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Verendrye valley is more than 100 km long, about 1 km wide, and at least 225 m deep. Southward, the valley grades into the Glidden esker, the surface of which rises about 280 m above the lowest point in the valley. The sediments in the valley and esker are 205 and 75 m thick, respectively, and form a fining-upward sequence from sand and gravel at the base to silt with sand interbeds in the upper part of the sequence, which, in turn, is covered by a blanket of glacial lake clay.The concave-upward longitudinal profile of Verendrye valley, the genetic relationship between Verendrye valley and the

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2

Rains, Bruce, and James Welch. "Out-of-phase Holocene terraces in part of the North Saskatchewan River basin, Alberta." Canadian Journal of Earth Sciences 25, no. 3 (1988): 454–64. http://dx.doi.org/10.1139/e88-046.

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This study focuses on alluvial terraces in part of the North Saskatchewan River valley, near Edmonton, and in the small tributary valleys of Whitemud and Strawberry creeks. The characteristic terrace morphologies and alluvial sediment sequences are briefly described, but most importantly, the deposits are radiocarbon dated for many sites. Twenty-seven new 14C dates on bone, wood, charcoal, and shell materials, along with previously reported dates, provide the chronological framework for the study. Occurrences of the Mazama ash marker bed in terrace alluvium offer additional geochronological ev

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Eckel, B. F., E. Karl Sauer, and E. A. Christiansen. "The Petrofka landslide, Saskatchewan." Canadian Geotechnical Journal 24, no. 1 (1987): 81–99. http://dx.doi.org/10.1139/t87-008.

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Both abutments and all piers of the Petrofka bridge are on a landslide. The bridge has performed satisfactorily for 23 years, indicating the factor of safety of the Petrofka landslide is greater than unity. This stability is abnormal because landslide slopes on bedrock clays (shale) in this region are notoriously unstable. A dormant landslide is difficult to analyze because the input parameters must represent a condition of limiting equilibrium.The Petrofka landslide is 70 m high, 880 m long, 3000 m wide, and up to 100 m thick. The shear zone is in highly plastic, montmorillonitic clays in an

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4

Stauffer, Mel R., Don J. Gendzwill, and E. Karl Sauer. "Ice-thrust features and the Maymont landslide in the North Saskatchewan River valley." Canadian Journal of Earth Sciences 27, no. 2 (1990): 229–42. http://dx.doi.org/10.1139/e90-023.

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The Battleford glacier created shearing and softening of bedrock clays, contributing to widespread slope instability along the valley of the North Saskatchewan River. The Battleford glacier flowed southeastward down the valley of the North Saskatchewan River during its final stage in west-central Saskatchewan. It created flutings, crevasse fillings, folding and faulting in ice-thrust ridges, and extensive horizontal gouge zones filled with soft, malleable clay. Extensive drilling and testing for the foundations of the Maymont bridge provided definitive data outlining at least three gouge zones

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5

Klassen, Rudy W. "Late Wisconsinan and Holocene history of southwestern Saskatchewan." Canadian Journal of Earth Sciences 31, no. 12 (1994): 1822–37. http://dx.doi.org/10.1139/e94-162.

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The Late Wisconsinan Laurentide Ice Sheet reached the limit of glaciation along the north-facing slope of the unglaciated part of the Cypress Hills nunatak, but elsewhere around the Cypress Hills and Wood Mountain uplands of southwestern Saskatchewan it did not reach the limit of glaciation. An interval of deglaciation was followed by a readvance of the ice sheet, about 15 ka, to a position near the Late Wisconsinan limit, and was marked by strong flow of Keewatin ice from the north and weaker flow of Hudson ice from the northeast. Final deglaciation resulted in the formation of glacial lakes

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Christiansen, E. A., and E. K. Sauer. "Age of the Frenchman Valley and associated drift south of the Cypress Hills, Saskatchewan, Canada." Canadian Journal of Earth Sciences 25, no. 10 (1988): 1703–8. http://dx.doi.org/10.1139/e88-160.

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Frenchman Valley extends about 340 km from the Cypress Hills, Saskatchewan, to its confluence with the Milk River in Montana. In one area, the valley is 3 km wide, and it was 180 m deep prior to deposition of as much as 80 m of landslide debris, channel sand and gravel, and alluvial and colluvial deposits. Six radiocarbon ages ranging from 3440 to 11 460 BP suggest the Frenchman Valley is Wisconsinan. The Frenchman Valley could not have formed in its side-hill position if Late Wisconsinan ice had not been present south at the Cypress Hills.

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Edkins, Tera L., Christopher M. Somers, Mark C. Vanderwel, Miranda J. Sadar, and Ray G. Poulin. "Variable habitat selection and movement patterns among Bullsnake (Pituophis catenifer sayi) populations in Saskatchewan." Canadian Field-Naturalist 132, no. 2 (2019): 126–39. http://dx.doi.org/10.22621/cfn.v132i2.2041.

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Pituophis catenifer sayi (Bullsnake) is a sparsely studied subspecies of conservation concern in Canada. Basic ecological information is lacking for P. c. sayi, which reaches its northern range limit in western Canada. To address this gap, we used radio-telemetry to examine space use and habitat selection in three populations of Bullsnakes in disjunct river valley systems (Frenchman, Big Muddy, and South Saskatchewan River Valleys) across their Saskatchewan range. Bullsnakes in two valleys used up to three times more space, travelled 2.5-times farther from overwintering sites, and had lower ho

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Cruden, D. M., K. H. Tedder, and S. Thomson. "Setbacks from the crests of slopes along the North Saskatchewan River, Alberta." Canadian Geotechnical Journal 26, no. 1 (1989): 64–70. http://dx.doi.org/10.1139/t89-007.

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Setbacks from the crests of slopes along the North Saskatchewan River valley between Edmonton and Fort Saskatchewan can be estimated from the ultimate angle of the slope and the rate of lateral river erosion. The ultimate slope angle depends on the slope stratigraphy and the position of the water table in the slope. Three slopes, in overburden, with a bedrock base and dominantly in bedrock, typically having groundwater tables at respectively the toe of the slope, halfway up the slope, and at the lower quarter of the slope height, are studied. Theoretical estimates of the ultimate slope angle i

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Mahaney, William C., and A. MacS Stalker. "Stratigraphy of the North Cliff section, Wellsch Valley site, Saskatchewan." Canadian Journal of Earth Sciences 25, no. 2 (1988): 206–14. http://dx.doi.org/10.1139/e88-023.

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Eight separate till sheets are displayed at the North Cliff, which is part of the Wellsch Valley site in Saskatchewan. Those tills are differentiated by using physical characteristics, particle size, clay and primary mineralogy, and sediment chemistry. Grain size tends to fine downward in the section, and a significant increase in the mean [Formula: see text] centre of gravity indicates that some weathering occurred after deposition of the tills. Within the clay mineral suites, smectite tends to dominate in all eight tills, indicating that the paleoclimate was generally as dry as the present-d

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Barendregt, R. W., E. Irving, E. A. Christiansen, E. K. Sauer, and B. T. Schreiner. "Stratigraphy and paleomagnetism of Late Pliocene and Pleistocene sediments in the Wellsch Valley and Swift Current Creek areas, southwestern Saskatchewan, Canada." Canadian Journal of Earth Sciences 35, no. 12 (1998): 1347–61. http://dx.doi.org/10.1139/e98-068.

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The Late Pliocene and Pleistocene are represented in southern Saskatchewan by sequences of preglacial, glacial, and nonglacial deposits. These have been studied in surface exposures and bore cores and have been subdivided and correlated on the basis of their lithologies. In this study, new observations of magnetic polarity are presented. They reveal a lower preglacial sequence (Empress Group) with reversed polarity, and an upper normally magnetized sequence which contains glacial deposits of pre-Illinoian, Illinoian, and Wisconsinan age and which are correlative with the Saskatoon and Sutherla

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Dissertations / Theses on the topic "Saskatchewan Valley"

1

Westbroek, Hans-Henrik. "Seismic interpretation of two possible meteorite impact craters, White Valley, Saskatchewan and Purple Springs, Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0003/MQ31378.pdf.

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Lang, Amanda M. "Echoes of experience: the narrative forces of the Qu'Appelle Valley." 2010. http://hdl.handle.net/1993/3845.

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Echoes of Experience: The Narrative Forces of the Qu’Appelle Valley explores the possibility of playing on the picturesque notion of a ‘folly’ within this Southern Saskatchewan valley. By incorporating an understanding of the physical and narrative forces that have shaped the valley as both place and space, speculative interventions are proposed that generate an awareness of past conditions in order to provide some trace of those narratives within the future of the valley. This practicum endeavors to use landscape narrative inquiry as a tool that helps one to understand the landscape exp

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Books on the topic "Saskatchewan Valley"

1

Canada, Geological Survey of, ed. Notes on the geology and palæontology of the Lower Saskatchewan River Valley. Govt. Print. Bureau, 1997.

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2

Fehr, Wayne. A case study concerning relationships between principals and district boards of trustees in the Saskatchewan Valley School Division #49. Research Centre, Saskatchewan School Trustees Association, 1989.

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3

Nicholson, Joel. Utilization of air photo interpretation to locate prairie rattlesnake (Crotalus viridis viridis) hibernacula in the South Saskatchewan River Valley. Alberta Sustainable Resource Development, 2001.

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4

Company, International Securities, ed. The International Securities Company, Ltd. presents herein authentic facts, figures and photographic views of Weyburn: The present gateway of international traffic, the metropolis of the rich Souris River Valley, the fast developing agricultural, railway, commercial and distributing centre, and the future great and industrially commanding city of southeastern Saskatchewan, in Canada West. International Securities Company Ltd., 1996.

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5

Saskatchewan valley route: Time tables. s.n., 1994.

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6

Valley of Gold / a Tale of the Saskatchewan. Blurb, 2019.

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Valley of Gold / a Tale of the Saskatchewan. Blurb, 2019.

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8

The Valley of Gold / A Tale of the Saskatchewan. Blurb, 2019.

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9

Howarth, David. The Valley Of Gold: A Tale Of The Saskatchewan. Kessinger Publishing, LLC, 2007.

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10

Battle River Valley [microform]: A Pamphlet Describing the Advantages of the Country Drained by the Battle and Saskatchewan Rivers As a Field for Settlement. Creative Media Partners, LLC, 2021.

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Book chapters on the topic "Saskatchewan Valley"

1

McGhee, Robert. "A Distant Paradise: The Arctic in Ancient Thought." In The Last Imaginary Place. Oxford University PressNew York, NY, 2006. http://dx.doi.org/10.1093/oso/9780192807304.003.0003.

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Abstract On a Cold Summer Evening in 1959, I first heard the story of the mysterious tropical valley in the Arctic.The constructioncamp bunkhouse in the British Columbia mountains had settled into its after-supper routine. Most of the younger guys were out working on their pickup trucks or had disappeared down the rutted logging road to the town at the bottom of the valley.The elders of the camp were lying in their bunks, smoking and listening to rain on the tarpaper roof, staring at the ceiling or leafing through tabloid newspapers, too weary after a wet day on a chainsaw to do more than talk

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2

Papp, Theresa (Therri) A., and Michael Cottrell. "Post-Secondary Students’ Perceptions of Learning Remotely during and beyond the COVID-19 Pandemic in Saskatchewan, Canada." In Values, Education, Emotional Learning, and the Quest for Justice in Education. BRILL, 2024. http://dx.doi.org/10.1163/9789004706798_011.

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Conference papers on the topic "Saskatchewan Valley"

1

Holliday, Chris, Andy Young, Terri Funk, and Carrie Murray. "The North Saskatchewan River Valley Landslide: Slope and Pipeline Condition Monitoring." In 2020 13th International Pipeline Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/ipc2020-9532.

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Abstract Following a loss of containment incident in July 2016 on a 16-inch diameter pipeline on the south slope of the North Saskatchewan River located in Saskatchewan, Canada, Husky completed extensive studies to understand and learn from the failure. The cause of the incident was ground movement resulting from a landslide complex on the slope involving two deep-seated compound basal shear slides as well as a near surface translational slide in heavily over consolidated marine clays of the Upper Cretaceous Lea Park Formation. One aspect of the studies has been to undertake structural analysi

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2

Helie, T., R. Knudsen, and D. McLean. "Gas Well Liquid Unloading Using Automatic Valve Switching And Expert Systems Technology." In Technical Meeting / Petroleum Conference of The South Saskatchewan Section. Petroleum Society of Canada, 1997. http://dx.doi.org/10.2118/97-182.

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3

Johnston, Mark, Tim Williamson, and Dan Ohlson. "Climate Change Effects on Timber Yields and Soil Expectation Values in Northern Saskatchewan." In 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277262.

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Vakil, Mohammad, Reza Fotouhi, and Peter N. Nikiforuk. "Parameter Identification of a Friction Model for Robotic Joints." In ASME 2010 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. ASMEDC, 2010. http://dx.doi.org/10.1115/detc2010-29141.

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In this paper a new identification method to obtain the friction parameters in the joints of robotic manipulators is presented. These parameters are coulomb friction, static friction, Stribeck velocity constant and viscous damping coefficient. The available methods to find these parameters either require the design of a controller or the precise value of system parameters such as mass moment of inertia. In contrast, the new method proposed here finds these parameters by a nonlinear optimization approach which requires neither any knowledge of system’s parameters nor any controller design. The

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Fauchoux, Melanie, Carey Simonson, David Torvi, and Prabal Talukdar. "CFD Modelling With Buoyancy Effects for a Heat and Moisture Transfer Ceiling Panel." In ASME/JSME 2011 8th Thermal Engineering Joint Conference. ASMEDC, 2011. http://dx.doi.org/10.1115/ajtec2011-44121.

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A heat and moisture transfer panel (HAMP) capable of simultaneously transferring heat and moisture to/from a space to improve indoor air conditions is being developed at the University of Saskatchewan. Experiments have been performed for different air conditions to simulate heating, cooling, humidification and dehumidification of the air by the HAMP. A latent effectiveness value is calculated for each test to show the performance of the HAMP. The HAMP has the highest effectiveness (∼45%) when used to cool the airflow. When used to heat the airflow, the effectiveness is much lower (∼25%). This

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Hang, Jiayi, Da Shi, James House, and Jason Neufeld. "Prediction of protein and amino acid contents in whole and ground lentils using near-infrared reflectance spectroscopy." In 2022 AOCS Annual Meeting & Expo. American Oil Chemists' Society (AOCS), 2022. http://dx.doi.org/10.21748/pqtj3002.

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Lentil (Lens culinaris Medik) is an important source of plant-based protein, and the protein and amino acid contents have a significant influence on its nutritional value and use. This study developed near-infrared reflectance spectroscopy (NIRS) calibration models to predict the protein and 18 amino acid contents of lentil seeds. The effects of sample status (whole and ground), type of spectrometer (DA 7250 and FT 9700), and amino acid/protein correlation on model performance were analyzed and evaluated. In total, 361 lentil samples grown in Saskatchewan, Canada, were selected as a calibratio

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Anumah, Prosper, and Saman Azadbakht. "Application of ANN-Based Proxy and Metaheuristic Algorithms in Well Spacing Optimization in a Fractured Tight Reservoir." In SPE Nigeria Annual International Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/217095-ms.

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Abstract Optimizing well spacing is a critical step in the development of an oilfield. Several approaches have been employed over the past decades in an attempt to obtain an efficient and cost-effective well spacing methodology. The desire to achieve a fast-paced well spacing optimization outcome is not yet realized. This study explores the use of a data-driven surrogate model and metaheuristic optimization algorithms in optimizing the well spacing in a fractured tight reservoir in Saskatchewan, Canada. The wells considered drain oil from the Viking Formation located in the Avon Hill field. Mu

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O’Rourke, Dan J. "Corridor Pipeline: Hartley Creek Crossing." In 2002 4th International Pipeline Conference. ASMEDC, 2002. http://dx.doi.org/10.1115/ipc2002-27126.

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Construction of the 493 km Corridor Pipeline System commenced in summer 2000, and is scheduled for completion in 2002. The system connects the two major components of the Athabasca Oil Sands Project — the Muskeg River Mine, north of Ft. McMurray and the Upgrader adjacent to Shell Canada Limited’s Scotford Refinery, near Fort Saskatchewan. The pipeline will also link the Upgrader with terminals in the Edmonton Area. The system includes dual pipelines (610 mm and 323.9 mm O.D.) as well as associated pump stations and valve sites. Corridor Pipeline Limited is a wholly-owned subsidiary of BC Gas I

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McCauley, Dave, Douglas Metcalfe, Marcia Blanchette, and Tom Calvert. "The Government of Canada’s Programs for Radioactive Waste Cleanup and Long-Term Management." In ASME 2009 12th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2009. http://dx.doi.org/10.1115/icem2009-16133.

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The Government of Canada’s 1996 Policy Framework for Radioactive Waste Management establishes that waste owners are responsible for the management of their radioactive wastes. This includes the planning, funding, and implementation of long-term waste management initiatives. Within this context, the Government has established three separate programs aimed at addressing the long-term management of radioactive waste for which it has accepted responsibility. The largest of these programs is the Nuclear Legacy Liabilities Program (NLLP). The objective of the NLLP is to address radioactive waste and

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Pham, Quynh C., and Lesley A. James. "Considering the CO2 Source and Capture Technique to Reduce Minimum Miscibility Pressure (MMP) for Enriched Water Alternating Gas (WAG) Injection." In ASME 2021 40th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2021. http://dx.doi.org/10.1115/omae2021-62643.

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Abstract CO2 is a well-known and commonly used solvent for enhanced oil recovery (EOR). CO2-rich natural gas fields have been the source of CO2 for onshore EOR for more than 50 years. Offshore, the story is different. Some jurisdictions like offshore Norway and Gulf of Mexico send their gas to market, pipelines from offshore to Europe and the United States exist, and CO2 must be stripped from the natural gas to meet pipeline specifications. Oil rig power generation has, for the most part, been electrified. Other jurisdictions like offshore Newfoundland, Canada, have stranded uneconomic, sweet

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Reports on the topic "Saskatchewan Valley"

1

Huntley, D., D. Rotheram-Clarke, R. Cocking, J. Joseph, and P. Bobrowsky. Understanding plateau and prairie landslides: annual report on landslide research in the Thompson River valley, British Columbia, and the Assiniboine River valley, Manitoba-Saskatchewan (2020-2021 to 2021-2022). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329205.

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Open File 8838 is a publication of Interdepartmental Memorandum of Understanding (IMOU) 5170 between Natural Resources Canada (NRCAN), the Geological Survey of Canada (GSC), and Transport Canada Innovation Centre (TC-IC). IMOU 5107 aims to gain new insight into slow-moving landslides and the influence of climate changes through testing conventional and emerging monitoring technologies along strategically important sections of the national railway network in the Thompson River valley, British Columbia, and the Assiniboine River valley along the borders of Manitoba and Saskatchewan. The results

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2

Spence, C. D., and D. J. Sauchyn. Groundwater influence on valley-head geomorphology, upper Battle Creek basin, Alberta and Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/211122.

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Huntley, D., P. Bobrowsky, D. Rotheram-Clarke, R. Cocking, and J. Joseph. Understanding prairie landslides: current research in the Assiniboine River valley, Manitoba-Saskatchewan (2019-2020). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/326821.

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Oldenborger, G. A., D. R. Sharpe, A. J. M. Pugin, and H. A. J. Russell. Helicopter time-domain electromagnetic data over the Eastern Hatfield buried-valley aquifer system, Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292517.

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Huntley, D., D. Rotheram-Clarke, R. Cocking, J. Joseph, and P. Bobrowsky. Understanding plateau and prairie landslides: research plans for the Thompson River valley, British Columbia, and the Assiniboine River valley, Manitoba-Saskatchewan (2020-2025). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2020. http://dx.doi.org/10.4095/327127.

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Huntley, D., D. Rotheram-Clarke, R. Cocking, J. Joseph, and P. Bobrowsky. Current research on slow-moving landslides in the Thompson River valley, British Columbia (IMOU 5170 annual report). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331175.

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Interdepartmental Memorandum of Understanding (IMOU) 5170 between Natural Resources Canada (NRCAN), the Geological Survey of Canada (GSC) and Transport Canada Innovation Centre (TC-IC) aims to gain new insight into slow-moving landslides, and the influence of climate change, through testing conventional and emerging monitoring technologies. IMOU 5107 focuses on strategically important sections of the national railway network in the Thompson River valley, British Columbia (BC), and the Assiniboine River valley along the borders of Manitoba (MN) and Saskatchewan (SK). Results of this research ar

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