Journal articles: 'Alberta and Northwest Conference'

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&NA;, &NA;. "NORTHWEST REGIONAL PERINATAL CONFERENCE." Journal of Perinatal & Neonatal Nursing 1, no. 4 (April 1988): 87. http://dx.doi.org/10.1097/00005237-198804000-00014.

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&NA;, &NA;. "NORTHWEST REGIONAL PERINATAL CONFERENCE." Journal of Perinatal & Neonatal Nursing 2, no. 1 (July 1988): 89. http://dx.doi.org/10.1097/00005237-198807000-00012.

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Levson, Vic. "Geology of northeast British Columbia and northwest Alberta: diamonds, shallow gas, gravel, and glaciersThis article introduces a selection of papers published in this Special Issue on the theme Geology of northeastern British Columbia and northwestern Alberta: diamonds, shallow gas, gravel, and glaciers." Canadian Journal of Earth Sciences 45, no. 5 (May 2008): 509–12. http://dx.doi.org/10.1139/e08-022.

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This special issue reports on some of the results of a multi-disciplinary research program conducted in the Boreal Plains of northwest Alberta and northeast British Columbia. Several innovative approaches to conducting geoscientific research in this remote drift-covered region are presented, including geochemical analysis of bentonites for evaluating kimberlite potential, the use of electromagnetic surveys for mapping buried aggregate deposits, and paleo-topographic mapping techniques to define buried channels. Results of the program include the discovery of several large aggregate deposits, the first kimberlite indicator minerals in northeast British Columbia, a significant sphalerite dispersal train in northwest Alberta, the first documented report of kimberlite-sourced bentonites, and numerous previously unknown interglacial sites. Together these papers provide a greatly enhanced understanding of the glacial history, Quaternary stratigraphy, and kimberlite geology of northwest Alberta and northeast British Columbia and provide an improved framework for resource exploration in the region.

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LeBoldus, Jared M., Peter V. Blenis, Barb R. Thomas, Nicolas Feau, and Louis Bernier. "Susceptibility of Populus balsamifera to Septoria musiva: A Field Study and Greenhouse Experiment." Plant Disease 93, no. 11 (November 2009): 1146–50. http://dx.doi.org/10.1094/pdis-93-11-1146.

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A greenhouse inoculation experiment and field study were conducted to determine the cause of an outbreak of Septoria musiva cankers on Populus balsamifera in a northern Alberta plantation. Four clones of P. balsamifera, five clones of putatively resistant P. deltoides, and one susceptible hybrid poplar clone, Northwest, were inoculated with seven isolates identified as S. musiva. Four of the isolates were from P. balsamifera in Alberta and the others were from P. deltoides in Quebec. Results indicated that disease severity was similar for Alberta and Quebec isolates (P = 0.243) and that P. balsamifera had the greatest mean disease severity (x-bar = 4.20), P. deltoides had the lowest (x-bar = 2.76), and Northwest was intermediate (x-bar = 3.45). A genetic analysis comparing six polymorphic polymerase chain reaction restriction fragment length polymorphism loci and the mitochondrial small subunit ribosomal DNA sequences of the seven isolates indicated that the Alberta population was made up of at least three distinct genotypes. Canker incidence and age on Northwest and 56 different clones of P. balsamifera in a plantation were recorded. Canker incidence (P = 0.726) and the canker age distributions (P = 0.994) were similar for the two species. In conclusion, contrary to what has been reported in the literature, P. balsamifera appears to be quite susceptible to Septoria canker.

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Thomson, R. B. "Atmospheric Environment Service Long Range Transport of Air Pollutant Activities in the Territories." Water Science and Technology 18, no. 2 (February 1, 1986): 109–15. http://dx.doi.org/10.2166/wst.1986.0020.

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Acid deposition monitoring and modelling in the Northwest Territories and Yukon Territories are reviewed. Data gathered since 1974 indicate that sulphur in precipitation is less than 1 kg/ha/yr. Trajectory calculations using numerical models are discussed that demonstrate a pattern of northeastward transport of pollutants from Alberta into southern sections of the Northwest Territories.

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De Souza, Wolan, Battochio, Christian, Hume, Johner, Lilley, et al. "Newborn Screening: Current Status in Alberta, Canada." International Journal of Neonatal Screening 5, no. 4 (October 1, 2019): 37. http://dx.doi.org/10.3390/ijns5040037.

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Newborn screening (NBS) in Alberta is delivered by a number of government and health service entities who work together to provide newborn screening to infants born in Alberta, the Northwest Territories, and the Kitikmeot region of the Nunavut territory. The Alberta panel screens for 21 disorders (16 metabolic, two endocrine, cystic fibrosis, severe combined immunodeficiency, and sickle cell disease). NBS is a standard of care, but is not mandatory. NBS performance is monitored by the Alberta Newborn Metabolic Screening (NMS) Program and NMS Laboratory, who strive for continuous quality improvement. Performance analysis found that over 99% of registered infants in Alberta received a newborn screen and over 98% of these infants received a screen result within 10 days of age.

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Steinhilber, M., and D. A. Neely. "A New Record of Deepwater Sculpin, Myoxocephalus thompsonii, in Northeastern Alberta." Canadian Field-Naturalist 120, no. 4 (October 1, 2006): 480. http://dx.doi.org/10.22621/cfn.v120i4.361.

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We present the first documented records of Deepwater Sculpin, Myoxocephalus thompsonii, from northern Alberta, and the second record for the province. Three specimens of Deepwater Sculpin were taken in gill nets set at 17 to 20 m depth in Colin Lake, Alberta, on 15 September 2001. Colin Lake, located in the Canadian Shield region of northeastern Alberta about 125 km northeast of Fort Chipewyan, drains into Lake Athabasca via the Colin River. The only other known Alberta population of Deepwater Sculpin inhabits Upper Waterton Lake in the southwestern corner of the province. This record is approximately 300 km SSE of the nearest verified record in the Northwest Territories and 400 km NW of the nearest verified record in Saskatchewan.

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DARWENT, A. L., and J. H. SMITH. "DELAYED SEEDING FOR WILD OAT CONTROL IN RAPESEED IN NORTHWEST ALBERTA." Canadian Journal of Plant Science 65, no. 4 (October 1, 1985): 1101–6. http://dx.doi.org/10.4141/cjps85-144.

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In a 4-yr study, rapeseed (Brassica campestris L.) was seeded where wild oats (Avena fatua L.) had been controlled either by various delayed seeding procedures or by an early spring application of trifluralin at 1.1 kg a.i./ha. The trifluralin treatment provided the best wild oat control. However, allowing wild oats to grow to the two-leaf stage, destroying them with cultivation and then seeding rapeseed resulted in commercially acceptable control (70% or more) with little or no loss of crop yield. Postponing cultivation until the wild oats reached the three- to four-leaf stage provided control that was almost equivalent to that attained with cultivation at the two-leaf stage but resulted in reduced crop yields. Destruction of wild oat seedlings at the two-leaf stage by paraquat or glyphosate did not improve the level of control over that provided by cultivation.Key words: Oat (wild), delayed seeding, rapeseed, trifluralin

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Egolf, Jeremy. "Pacific Northwest Labor History Association Annual Conference." International Labor and Working-Class History 28 (1985): 89–93. http://dx.doi.org/10.1017/s0147547900008838.

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Jacoby, Daniel. "1999 Pacific Northwest Labor History Association Conference." International Labor and Working-Class History 57 (April 2000): 117–19. http://dx.doi.org/10.1017/s0147547900212799.

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I cannot provide a definitive answer to those of us pondering what the best alternative to capitalism is, but after attending the Pacific Northwest Labor History Association (PNLHA) Conference in Westminster, British Columbia, over the weekend of May 28–30, 1999, I can tell you that this is certainly a preferable alternative to standard academic conferences. As usual, the PNLHA was able to produce a cadre of historians (from the trades as well as academia), active unionists, and old-timers whose memories are as tapable as a keg of beer. Although the association designates labor history as its subject, newly elected President Ross Rieder likes to say, “History ends the moment before now.”

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Foote, C. J., J. W. Clayton, C. C. Lindsey, and R. A. Bodaly. "Evolution of Lake Whitefish (Coregonus clupeaformis) in North America during the Pleistocene: Evidence for a Nahanni Glacial Refuge Race in the Northern Cordillera Region." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 4 (April 1, 1992): 760–68. http://dx.doi.org/10.1139/f92-085.

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Lake whitefish (Coregonus clupeaformis) could have survived through (at least) the Illinoisan and Wisconsinan Pleistocene glacial maxima in an area in the vicinity of the present Nahanni National Park in the Northwest Territories of Canada according to the geological evidence. This possibility was addressed by an analysis of the genetic makeup of 43 lake whitefish populations in the Northwest Territories, the Yukon Territory, British Columbia, and Alberta. Populations in the lower Liard, Tetcela, Fraser, and upper Peace River systems as well as the headwaters of the Athabasca River were distinguished from both the Bering glacial refuge race populations inhabiting the Yukon and upper Liard River basins in the Yukon Territory and the Mississippi–Missouri glacial refuge race populations inhabiting most of the Northwest Territories, Alberta, and areas further to the east by a specific combination of electrophoretic mobility alleles. This evidence supports the hypothesis of the survival and subsequent dispersal of lake whitefish from a Nahanni glacial refugium. Possible dispersal routes and the limited extent of introgression among races are discussed.

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Basu, Anup. "IEEE SMC 2017 in Banff, Alberta, Canada [Conference Reports]." IEEE Systems, Man, and Cybernetics Magazine 4, no. 3 (July 2018): 36–39. http://dx.doi.org/10.1109/msmc.2018.2831418.

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Cheung, Justin, Karen Goodman, Rachel Munday, Karen Heavner, Janis Huntington, John Morse, Sander Veldhuyzen van Zanten, et al. "Helicobacter PyloriInfection in Canada’s Arctic: Searching for the Solutions." Canadian Journal of Gastroenterology 22, no. 11 (2008): 912–16. http://dx.doi.org/10.1155/2008/614538.

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The Canadian NorthHelicobacter pylori(CANHelp) working group is a team composed of investigators, health officials and community leaders from Alberta and the Northwest Territories. The group’s initial goals are to investigate the impact ofH pyloriinfection on Canada’s Arctic communities; subsequent goals include identifying treatment strategies that are effective in this region and developing recommendations for health policy aimed at management ofH pyloriinfection. The team’s investigations have begun with the AklavikH pyloriProject in the Aboriginal community of Aklavik, Northwest Territories.

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Shaw, John, Bruce Rains, Ronald Eyton, and Lee Welssling. "Laurentide subgiacial outburst floods: landform evidence from digital elevation models." Canadian Journal of Earth Sciences 33, no. 8 (August 1, 1996): 1154–68. http://dx.doi.org/10.1139/e96-087.

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Various lines of landform evidence in many parts of Canada are comprehensively explicable as products of subglacial sheetfloods–outburst floods. In the Northwest Territories, northern Saskatchewan, and Alberta, landform associations such as scoured bedrock tracts, cavity-fill drumlins, erosional drumlins, erosional giant flutes–remnant ridges, tunnel channels, channeled scabland, and hummocky terrain with upstanding moraine plateaus reflect primary glaciofluvial erosional processes and secondary depositional activities. The Livingstone Lake event major sheetfloods path arcs obliquely upslope from the Keewatin District, Northwest Territories, through northern Saskatchewan and much of Alberta into Montana, U.S.A. Hill-shaded maps generated from digital elevation models, at widely varying scales, are used to illustrate regional to local examples of megaflood landform suites. Complementary maps and diagrams are derived from more conventional data sources. Speculations regarding extraglacial implications of the outburst floods in the Missouri–Mississippi basins, Mississippi Delta, and Gulf of Mexico are offered for testing by others.

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Marcus‐Smith, Miriam. "The Northwest Patient Safety Conference: keeping safety current." Clinical Governance: An International Journal 17, no. 4 (October 12, 2012): 343–49. http://dx.doi.org/10.1108/14777271211273224.

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Ghezzi, Pietro, and Marina Sironi. "Second International Cytokine Conference, Banff, Alberta October 1–5, 1994." Amyloid 2, no. 1 (January 1995): 66–68. http://dx.doi.org/10.3109/13506129509031888.

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Wilson, Donna M., and Doris M. Kieser. "Values and Canadian Health Care: an Alberta Exploration." Nursing Ethics 3, no. 1 (March 1996): 9–15. http://dx.doi.org/10.1177/096973309600300103.

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In March 1994, a health care conference was held in Edmonton, Alberta, at which the values of conference participants towards health care were systematically recorded and analysed. This exploration is significant because the values that underpin the structure of the current publicly-funded and administered Canadian health care system rarely enter current discussions regarding health care system reform. Rather, economic and other sociopolitical forces now seem to be having a major impact on plans and actual changes within the health care system. Thus, the underlying attitudes and beliefs of Canadians towards health care have not been articulated or given due credence. The conference par ticipants identified three dominant values: (1) the dignity of the human person as an indi vidual and social being; (2) respect for pluralism and difference; and (3) accountability These values were found to be robust, in that they sustain a focus on the 'common good'. The common good is the core of the Canadian health care system, and is enshrined in the 1984 Canada Health Act. Conceptually, these values could also lead to significant changes in health care, in keeping with the common good, particularly those changes focusing on the current deficiencies of the Canadian health care system.

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Majorowicz, Jacek, and Stephen E. Grasby. "Deep Geothermal Heating Potential for the Communities of the Western Canadian Sedimentary Basin." Energies 14, no. 3 (January 30, 2021): 706. http://dx.doi.org/10.3390/en14030706.

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We summarize the feasibility of using geothermal energy from the Western Canada Sedimentary Basin (WCSB) to support communities with populations >3000 people, including those in northeastern British Columbia, southwestern part of Northwest Territories (NWT), southern Saskatchewan, and southeastern Manitoba, along with previously studied communities in Alberta. The geothermal energy potential of the WCSB is largely determined by the basin’s geometry; the sediments start at 0 m thickness adjacent to the Canadian shield in the east and thicken to >6 km to the west, and over 3 km in the Williston sub-basin to the south. Direct heat use is most promising in the western and southern parts of the WCSB where sediment thickness exceeds 2–3 km. Geothermal potential is also dependent on the local geothermal gradient. Aquifers suitable for heating systems occur in western-northwestern Alberta, northeastern British Columbia, and southwestern Saskatchewan. Electrical power production is limited to the deepest parts of the WCSB, where aquifers >120 °C and fluid production rates >80 kg/s occur (southwestern Northwest Territories, northwestern Alberta, northeastern British Columbia, and southeastern Saskatchewan. For the western regions with the thickest sediments, the foreland basin east of the Rocky Mountains, estimates indicate that geothermal power up to 2 MWel. (electrical), and up to 10 times higher for heating in MWth. (thermal), are possible.

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Mulder, K. E., S. Ahmed, J. Davies, C. M. Doll, S. Dowden, S. Gill, V. Gordon, et al. "Report from the 17th Annual Western Canadian Gastrointestinal Cancer Consensus Conference; Edmonton, Alberta; 11–12 September 2015." Current Oncology 23, no. 6 (December 22, 2016): 425. http://dx.doi.org/10.3747/co.23.3384.

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The 17th annual Western Canadian Gastrointestinal Cancer Consensus Conference (wcgccc) was held in Edmonton, Alberta, 11–12 September 2015. The wcgccc is an interactive multidisciplinary conference attended by health care professionals from across Western Canada (British Columbia, Alberta, Saskatchewan, and Manitoba) who are involved in the care of patients with gastrointestinal cancer. Surgical, medical, and radiation oncologists; pathologists; radiologists; and allied health care professionals participated in presentation and discussion sessions for the purposes of developing the recommendations presented here. This consensus statement addresses current issues in the management of gastric cancer.

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Lee-Ying, Richard, Osama Ahmed, Shahid Ahmed, Shahida Ahmed, Oliver F. Bathe, Bryan Brunet, Laura Dawson, et al. "Report from the 21st Annual Western Canadian Gastrointestinal Cancer Consensus Conference; Calgary, Alberta; 20–21 September 2019." Current Oncology 28, no. 5 (September 21, 2021): 3629–48. http://dx.doi.org/10.3390/curroncol28050310.

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The 21st annual Western Canadian Gastrointestinal Cancer Consensus Conference (WCGCCC) was held in Calgary, Alberta, 20–21 September 2019. The WCGCCC is an interactive multi-disciplinary conference attended by health care professionals from across Western Canada (British Columbia, Alberta, Saskatchewan, and Manitoba) involved in the care of patients with gastrointestinal cancer. Surgical, medical, and radiation oncologists, pathologists, radiologists, and allied health care professionals such as dietitians and nurses participated in presentation and discussion sessions to develop the recommendations presented here. This consensus statement addresses current issues in the management of hepato-pancreato-biliary (HPB) cancers.

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Steel, Nancy, and Patrick J. Fahy. "Attracting, preparing, and retaining under-represented populations in rural and remote Alberta-North communities." International Review of Research in Open and Distributed Learning 12, no. 4 (May 13, 2011): 35. http://dx.doi.org/10.19173/irrodl.v12i4.936.

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<p>For several years, the government of the western Canadian province of Alberta has drafted policies and conducted research on the problem of populations under-represented in adult education. This Alberta-North and Athabasca University study, funded by the Alberta government’s Innovation Fund, uses the advice and educational experiences of northern former and present students, and of other community members, to identify ways of better attracting, preparing, and retaining under-represented populations in northern Alberta communities through provision and training in the use of distance delivery methods.</p><p>The research reported here commences with a review of the literature to investigate the following: 1) the contribution distance education makes globally to learning access in remote areas (and resulting economic growth for under-served populations); 2) how support is provided to retain isolated students; and 3) the help needed to assist remote students to complete distance programs. Community consultations with social service and education agencies in three communities were conducted in order to obtain their perspectives about what helps to attract and support students to educational programs and the barriers students typically encounter, which might be mitigated by distance methods. Finally, a survey was designed and distributed in 87 Alberta-North communities in northern Alberta and across Canada’s Northwest Territories to add perspective to the consultation results.</p>

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Turner, Robert E. "New acritarch taxa from the Middle and Upper Devonian (Givetian–Frasnian) of western Canada." Canadian Journal of Earth Sciences 28, no. 9 (September 1, 1991): 1471–87. http://dx.doi.org/10.1139/e91-129.

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Eight new acritarch species, four of which are assigned to new genera, are described from Givetian and Frasnian strata of Alberta and the Northwest Territories. The new taxa are Apectosphaeridium apoplanium n.gen. et sp., Asyncosmium isum n.gen. et sp., Cerastum pelorum n.gen. et sp., Variolidium omnium n.gen. et sp., Goniosphaeridium rallum n.sp., Leiosphaeridia gigantea n.sp., Polyedryxium leptum n.sp., and Saharidia perplexa n.sp.

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Wolfe, Stephen A., David J. Huntley, and Jeff Ollerhead. "Relict Late Wisconsinan Dune Fields of the Northern Great Plains, Canada*." Paleoenvironments 58, no. 2-3 (July 18, 2006): 323–36. http://dx.doi.org/10.7202/013146ar.

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Abstract Late Wisconsinan dune activity is investigated within the present-day boreal forest and parkland regions of the northern Great Plains, Canada, to extend the understanding of the spatial and temporal eolian record. Optical ages from stabilized sand dunes document the timing of past activity. Eolian activity ranges from about 16 ka in west-central Alberta to 9 ka in northwestern Saskatchewan. Between about 16 and 13 ka, dune activity in central Alberta occurred in an ice-proximal tundra setting along the margins of the Laurentide and Cordilleran ice sheets. Predominant dune-forming winds were from the west and northwest. Dune activity continued in this area between about 13 and 11 ka within parkland and grassland settings as the Laurentide Ice Sheet retreated to the northeast. Winds continued to blow from the west and northwest, and the climate was likely influenced by an increasingly dominant Pacific air mass. Also beginning at about 13 ka, dune-forming winds along the margins of the retreating Laurentide Ice Sheet were influenced by anticyclonic winds from the southeast that were maintained until about 9 ka. As the Laurentide Ice Sheet retreated, these southeasterly anticyclonic winds were successively replaced by winds from the northwest associated with the Pacific air mass. Dune activity across the region terminated in a time-transgressive manner from the southwest, at about 11 ka, to the northeast, at about 9 ka, with the establishment of boreal forest vegetation and reduced wind strength.

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BEAUDOIN, MARTIN, and MIKE LEVY. "Editorial." ReCALL 16, no. 2 (November 2004): 265–66. http://dx.doi.org/10.1017/s0958344004000126.

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This special issue of ReCALL is composed of 17 articles selected from presentations made at the WorldCALL 2003 conference, held May 7–10 2003 in Banff, Canada. Against all odds, during the heat of the war on terrorism, in the middle of the SARS crisis, approximately 250 people gathered in a breathtakingly beautiful town in the Rocky Mountains to discuss the latest advances in the field of Computer Assisted Language Learning (CALL). Registrants came to Banff for four spring days from fifty countries to take part in 158 lectures and poster sessions. The conference was steered by an international committee composed of members from twelve countries and organized by researchers from the Faculté Saint-Jean (Edmonton, Alberta), the University of Alberta (Edmonton, Alberta), and the University of Calgary (Calgary, Alberta). The programme committee was established at the University of Victoria (Victoria, British Columbia). The specificity of WorldCALL conferences is that they are truly international, taking place in various parts of the world and attracting specialists from all parts of the planet. One of the unique contributions of this conference is that participants from underserved regions of the world are particularly encouraged to share their experience in CALL. In this respect, the conference was very successful. This was made possible by awarding eleven scholarships to participants from selected countries. WorldCALL 2003 was particular in one respect: being held in Canada and organized by French and English speakers, the organizers decided to provide a bilingual environment where presentations could be made in either of Canada's official languages. This is reflected in the selected papers by the fact that some of the articles are in French.

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Bohach, Lisa L., and Emily K. Frampton. "Middle Cenomanian (Late Cretaceous) molluscs of the Shaftesbury Formation, Birch Mountains, northeastern Alberta, Canada." Canadian Journal of Earth Sciences 52, no. 8 (August 2015): 542–56. http://dx.doi.org/10.1139/cjes-2014-0166.

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Historical Resources Impact Assessment and Mitigation studies have documented a new middle Cenomanian invertebrate fauna from the Shaftesbury Formation in the Birch Mountains, northwest of Fort McMurray, in northeastern Alberta, Canada. Although older portions (Albian) of the Shaftesbury Formation in Alberta and British Columbia have yielded invertebrate fossils, this is the first fauna of middle Cenomanian age known for the unit. The fauna includes the ammonites Acanthoceras wyomingense and Borissjakoceras orbiculatum, the inoceramid bivalves Inoceramus dunveganensis and Inoceramus prefragilis stephensoni, and the gastropod Pirsila tensa. The occurrence of the late middle Cenomanian zonal fossil A. wyomingense allows correlation between the middle “Fish Scales Formation” of the Shaftesbury Formation and the lower part of the Labiche Formation of Alberta, and with five units farther to the south in the United States, namely the Greenhorn Limestone, Lincoln Formation, and Graneros Shale of Kansas, the Frontier Formation of Wyoming, and the Belle Fourche Shale of Montana.

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Roberts, D. G. "Petroleum geology of Northwest Europe: Proceedings of the 4th Conference." Marine and Petroleum Geology 11, no. 3 (June 1994): 412–13. http://dx.doi.org/10.1016/0264-8172(94)90060-4.

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Cruden, D. M., and T. M. Eaton. "Reconnaissance of rockslide hazards in Kananaskis Country, Alberta." Canadian Geotechnical Journal 24, no. 3 (August 1, 1987): 414–29. http://dx.doi.org/10.1139/t87-052.

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Kananaskis Country is situated in the Front Ranges of the Canadian Rockies in southwestern Alberta. Sedimentary rock thrust northeastwards forms mountain ridges that trend northwest–southeast parallel to the major thrust faults. Older, Palaeozoic rocks—mainly limestone and dolomite—form the ridges and peaks. Younger, Mesozoic rocks—sandstones, quartzites, siltstones, shales, conglomerates, and coals—are more easily eroded and form mountain passes and valleys.A reconnaissance mapped 228 rockslides, 8 km2 of rockslide debris and 96 km2 of talus. The largest rockslide exceeds 50 × 106 m3. Rockslides are most probable in the Devonian Palliser Formation, then in the Permo-Pennsylvanian Rocky Mountain Group, Mississippian Rundle Group, Devonian Fairholme Group, Mississippian Banff Formation, and the younger detrital rocks. Rockslides are most probable on dip and overdip slopes, followed by reverse-dip slopes, oblique and strike-dip slopes, and underdip slopes. Large rock masses have not slid on slopes below their basic friction angle, [Formula: see text]The reconnaissance shows that certain facilities in valleys below steep mountain slopes are exposed to rockslide hazards, and provides a guide for the location of new facilities. Analyses of two mountain slopes show that there are large, hypothetical hazards in Kananaskis. Rockslides are likely and could be destructive. Key words: Front Ranges, Rocky Mountains, Alberta, rockslides, hazards.

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Ginns, J. "The taxonomy and distribution of rare or uncommon species of Albatrellus in western North America." Canadian Journal of Botany 75, no. 2 (February 1, 1997): 261–73. http://dx.doi.org/10.1139/b97-028.

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Habitat data, although sparse, and occurrence are summarized for nine rare or uncommon species of Albatrellus. Significant range extensions are Albatrellus avellaneus in British Columbia, Oregon, and Washington, Albatrellus caeruleoporus in California, British Columbia, Oregon, and Washington, Albatrellus dispansus in Washington, Albatrellus ellisii in Colorado, Oregon, Washington, and Wyoming, Albatrellus flettii in Alaska, Alberta, northern British Columbia, Idaho, New Mexico, and Wyoming, Albatrellus subrubescens in Alberta, California, Northwest Territories, and Washington, Albatrellus syringae in North America (Alaska, Alberta, British Columbia, and Yukon Territory). Three additional collections of Albatrellus skamanius bring the total known collections of the species to four; all are from the same general locality. A key to the western species, emphasizing features of fresh basidiomes, is included. The basidiome features of these species are supplemented with data from additional collections. Spore sizes in several species are more critically defined. Amyloidity occurred in basidiospores and (or) hyphae of A. avellaneus, Albatrellus affin. cristatus, A. ellisii, A. flettii, A. skamanius, and A. subrubescens. Key words: systematics, ecology, Basidiomycetes, conservation, biodiversity, fungi.

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Thakor, Nehal, Ute Kothe, Hans-Joachim Wieden, and Trushar R. Patel. "Proceedings of the 14th annual RiboWest conference: perspectives and outcome." Biochemistry and Cell Biology 98, no. 1 (February 2020): vii—ix. http://dx.doi.org/10.1139/bcb-2019-0187.

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The RiboWest Conference brings together RNA researchers in Canada with the 2-fold goals of fostering internationally competitive RNA research and of training the next generation of scientists. The 14th Annual RiboWest conference (RiboWest 2018) was held at the University of Lethbridge (Lethbridge, Alberta) from June 10th to 13th, 2018. This meeting was focused on all major aspects of RNA research, ranging from understanding the cellular role of RNA, studying RNA interactions and structures, and employing them as a therapeutic tool. The invited keynote speakers (5) provided insights into the wide-range of RNA-based research. One of the unique features of this conference was that the majority of the oral presentations were given by the trainees (undergraduate/graduate students and postdoctoral researchers). Hosted by the Alberta RNA Research and Training Institute (ARRTI) at the University of Lethbridge as the leading center of RNA research in Western Canada, the RiboWest 2018 was well attended by researchers from across the country (>110 attendees in total). This conference proceedings editorial presents the overview of the conference, and briefly introduces articles published in this special issue of Biochemistry and Cell Biology.

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Loewen, Royden. "Faith, Life and Witness in the Northwest, 1903-2003: Centennial History of the Northwest Mennonite Conference (review)." Canadian Historical Review 86, no. 1 (2005): 155–57. http://dx.doi.org/10.1353/can.2005.0077.

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Jansson, T., and T. L. Powell. "The 13th Rochester Trophoblast Conference, Banff, Alberta, Canada 8–11 September 1996." Placenta 18, no. 2-3 (March 1997): 232–33. http://dx.doi.org/10.1016/s0143-4004(97)90099-0.

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Mei, S., and R. Paulen. "Using multi-beam RADARSAT-1 imagery to augment mapping surficial geology in northwest Alberta, Canada." Canadian Journal of Remote Sensing 35, no. 1 (January 2009): 1–22. http://dx.doi.org/10.5589/m08-077.

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Garzione, Carmala N., P. Jonathan Patchett, Gerald M. Ross, and JoAnne Nelson. "Provenance of Paleozoic sedimentary rocks in the Canadian Cordilleran miogeocline: a Nd isotopic study." Canadian Journal of Earth Sciences 34, no. 12 (December 1, 1997): 1603–18. http://dx.doi.org/10.1139/e17-129.

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Nd isotopes and trace elements in sedimentary rocks of the Yukon, the Northwest Territories, and northern British Columbia are used to examine the source of sediments in the Canadian Cordilleran miogeocline. Previous Nd isotope studies in southern Alberta demonstrated that strata of Neoproterozoic to Late Ordovician age were derived from Archean and Proterozoic Canadian Shield sources, whereas by the Late Devonian, a shift of 6 εNd units to younger crustal sources (εNd (T) = −6 to −9) had occurred. In this study, we found that the shift to younger crustal Nd isotopic signatures in the Yukon and Northwest Territories occurred much earlier than in southern Alberta. Cambrian and older strata have εNd(T) values of −10.0 to −21.1, consistent with derivation from Canadian Shield sources. Lower Ordovician through Permian strata in the Yukon and Northwest Territories, including the Innuitian-derived Imperial Assemblage, have εNd(T) values of −5 to −11.4. In northern British Columbia, the shift to a younger source reflects a wider range of εNd(T) values, from -−8.7 to −14.6 in Middle Ordovician through Middle Devonian strata, suggesting continued input from Canadian Shield sources. By the Middle Devonian, a complete shift to younger crustal signatures (εNd(T) = −5.9 to −10.5) had occurred in northern British Columbia. Several sources for the more juvenile sediments include (1) a mixture of locally erupted volcanic rocks with Canadian Shield sources, (2) a Grenville source, and (3) an Innuitian source. We propose that Ordovician to Lower Devonian strata were derived from a mixture of locally erupted, juvenile volcanics and pre-Cambrian Canadian Shield sources, and post-Middle Devonian strata were sourced from the Innuitian orogen in the Canadian Arctic.

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Hand, R. K., L. A. Goonewardene, B. J. Yaremcio, and R. Westra. "A study on the prevalence of cracked claws among beef cows." Canadian Journal of Animal Science 72, no. 1 (March 1, 1992): 165–68. http://dx.doi.org/10.4141/cjas92-019.

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A survey of the prevalence of vertical (sand) cracks on claws of cows on pasture in northwest Alberta found 261 out of 1183 or 22.7% cows affected. Among cows with cracks, 62% had a single crack while 29% had two cracks. There were significantly (P = 0.00001) more cracks on the outside (80.6%) compared with the inside (19.4%) claw. Significantly (P = 0.0002) more of the severe cracks were found on the outside claw. Key words: Claw, cracks, cows, severity, prevalence

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Brar, G. S., and H. R. Kutcher. "Race Characterization of Puccinia striiformis f. sp. tritici, the Cause of Wheat Stripe Rust, in Saskatchewan and Southern Alberta, Canada and Virulence Comparison with Races from the United States." Plant Disease 100, no. 8 (August 2016): 1744–53. http://dx.doi.org/10.1094/pdis-12-15-1410-re.

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Wheat stripe rust, caused by Puccinia striiformis f. sp. tritici, has been common across Saskatchewan, Canada since 2000. Fifty-nine isolates of P. striiformis f. sp. tritici, the majority of which were collected between 2011 and 2013 from Saskatchewan and southern Alberta, were analyzed for virulence frequency and diversity and compared with isolates characterized in the Pacific Northwest and Great Plains regions of the United States. In all, 31 wheat differentials, including 20 near-isogenic lines and 1 triticale variety, differentiated 59 P. striiformis f. sp. tritici isolates into 33 races, of which one race, C-PST-1, represented 31% of the isolates. None of the races were virulent on Yr5, Yr15, or YrSP. Virulence frequency ranged from 65 to 98% on YrA, Yr2, Yr8, Yr9, Yr27, Yr29, Yr32, YrSu, ‘Heines VII’, and ‘Nord Deprez’. Race C-PST-6 was virulent on the greatest number of the differentials (n = 25) and C-PST-18 on the fewest (n = 14). Discriminant analysis of principal components and multivariate cluster analyses detected three and four major groups, respectively, which differed from each other in terms of virulence spectrum and year of collection. The diversity of the P. striiformis f. sp. tritici population in southern Alberta was greater than in Saskatchewan, which indicated that, although P. striiformis f. sp. tritici is primarily windborne over great distances and does not usually overwinter, there are detectable differences in virulence between these regions of western Canada. Comparative analyses of virulence frequency of Saskatchewan or southern Alberta isolates with isolates representing races from the Great Plains and the Pacific Northwest of the United States indicated greater similarity of Saskatchewan races to the Great Plains despite strong correlations with both parts of the United States. This suggests that the P. striiformis f. sp. tritici population in Saskatchewan is a mixture of inoculum from both parts of the United States.

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Eberth, David A., and Phil R. Bell. "Stratigraphy of the Danek Bonebed (Upper Cretaceous Horseshoe Canyon Formation, central Alberta) and correlations with strata in the Drumheller and Grande Prairie regions." Canadian Journal of Earth Sciences 51, no. 11 (November 2014): 975–81. http://dx.doi.org/10.1139/cjes-2014-0069.

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Although considerable work has been conducted on the stratigraphy and dinosaur assemblages of the Horseshoe Canyon Formation of southern Alberta, equivalent strata and assemblages in central Alberta remain poorly understood. Data from the Danek Bonebed (Edmonton, Alberta) are beginning to fill this gap. The bonebed occurs 4 m above the #9 Big Island Coal Seam. This stratigraphic position lies just below the middle of the Horseshoe Canyon Formation in the Edmonton region, and also lies below a thick, stratigraphically significant non-coaly interval that is expressed throughout central and southern Alberta. The stratigraphic position of the Danek Bonebed equates best with the uppermost Horsethief Member of the Horseshoe Canyon Formation in the Drumheller region and the upper part of Unit 4 of the Wapiti Formation in the Grande Prairie region. In both Drumheller and Grande Prairie, the correlated position of the bonebed underlies a zone of marine transgression (Drumheller Marine Tongue), which, in turn, includes the Campanian–Maastrichtian boundary. In the context of Geologic Time Scale 2004, we infer a late Campanian age of 71.0–71.3 Ma for the bonebed. The Danek’s dinosaurian assemblage is limited taxonomically, but compares well with the Edmontosaurus regalis – Pachyrhinosaurus canadensis fossil assemblage zone in the Drumheller region. We propose that a mega-herbivore faunal assemblage, characterized by Edmontosaurus and Pachyrhinosaurus, extended continuously across the climatically wet coastal plain of latest Campanian southern and central Alberta, and likely extended northwest into the North Slope of Alaska, where it persisted into the early Maastrichtian.

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Shen, S. S. P., H. Yin, K. Cannon, A. Howard, S. Chetner, and T. R. Karl. "Temporal and Spatial Changes of the Agroclimate in Alberta, Canada, from 1901 to 2002." Journal of Applied Meteorology 44, no. 7 (July 1, 2005): 1090–105. http://dx.doi.org/10.1175/jam2251.1.

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Abstract This paper analyzes the long-term (1901–2002) temporal trends in the agroclimate of Alberta, Canada, and explores the spatial variations of the agroclimatic resources and the potential crop-growing area in Alberta. Nine agroclimatic parameters are investigated: May–August precipitation (PCPN), the start of growing season (SGS), the end of the growing season (EGS), the length of the growing season (LGS), the date of the last spring frost (LSF), the date of the first fall frost (FFF), the length of the frost-free period (FFP), growing degree-days (GDDs), and corn heat units (CHUs). The temporal trends in the agroclimatic parameters are analyzed by using linear regression. The significance tests of the trends are made by using Kendall’s tau method. The results support the following conclusions. 1) The Alberta PCPN has increased 14% from 1901 to 2002, and the increment is the largest in the north and the northwest of Alberta, then diminishes (or even becomes negative over two small areas) in central and southern Alberta, and finally becomes large again in the southeast corner of the province. 2) No significant long-term trends are found for the SGS, EGS, and LGS. 3) An earlier LSF, a later FFF, and a longer FFP are obvious all over the province. 4) The area with sufficient CHU for corn production, calculated according to the 1973–2002 normal, has extended to the north by about 200–300 km, when compared with the 1913–32 normal, and by about 50–100 km, when compared with the 1943–72 normal; this expansion implies that the potential exists to grow crops and raise livestock in more regions of Alberta than was possible in the past. The annual total precipitation follows a similar increasing trend to that of the May–August precipitation, and the percentile analysis of precipitation attributes the increase to low-intensity events. The changes of the agroclimatic parameters imply that Alberta agriculture has benefited from the last century’s climate change.

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Landry, Bernard, and Jean-François Landry. "The genus Alucita in North America, with description of two new species (Lepidoptera: Alucitidae)." Canadian Entomologist 136, no. 4 (August 2004): 553–79. http://dx.doi.org/10.4039/n03-095.

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AbstractThe North American fauna of Alucitidae is shown to include three widespread species: Alucita montana Barnes et Lindsey, 1921 (nec Cockerell), Alucita adriendenisisp. nov. (type locality: Manitoulin Island, Ontario, Canada), and Alucitalalanneisp. nov. (type locality: Maynooth, Ontario, Canada). Alucita hexadactyla (L., 1758) and A. huebneri Wallengren, 1862 do not occur in North America. The three North American species are described and illustrated. Alucita montana is found from southwestern Quebec and Vermont, west to British Columbia, and south to Arizona, California, and Texas; its caterpillar is associated with Symphoricarpos spp. (Caprifoliaceae). Alucita adriendenisi is known from northwestern Quebec and New York, west to Alberta and the Northwest Territories, with more southern populations (isolated?) in West Virginia, Arizona, and Texas; its caterpillar feeds on flowers of Lonicera dioica L. (Caprifoliaceae) in Michigan. Alucita lalannei has been found in Ontario, Manitoba, and Alberta, Canada; its host plant is unknown.

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Jozsa, L. A., and J. M. Powell. "Some climatic aspects of biomass productivity of white spruce stem wood." Canadian Journal of Forest Research 17, no. 9 (September 1, 1987): 1075–79. http://dx.doi.org/10.1139/x87-165.

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Biomass productivity was determined for white spruce (Piceaglauca (Moench) Voss) in the boreal forests of Alberta, the Northwest Territories, and Manitoba. Comparisons were made between southern and northern locations, between eastern and western transect locations, and between older (200 + years) and younger (110 years) trees. At 13 sampling locations, X-ray densitometric tree ring data were obtained from the base of the stem, breast height, and from five points equidistant along the stem. Markedly higher stem wood biomass productivity was found for the 110-year-old trees than for the 210-year-old trees in Alberta; average ring weights were 3.8 and 1.2 g for the first 100 years of growth in 1 cm thick disks at breast height. These results suggest that climatic warming since the end of the Little Ice Age (ca. 1850) has resulted in higher biomass productivity in the Canadian boreal forest.

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Chen, Zhuoheng, Kirk G. Osadetz, and Maowen Li. "Spatial characteristics of Middle Devonian oils and non-associated gases in the Rainbow area, northwest Alberta." Marine and Petroleum Geology 22, no. 3 (March 2005): 391–401. http://dx.doi.org/10.1016/j.marpetgeo.2004.12.005.

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Langenberg, Willem. "The geometry of folded and thrusted rocks in the Rocky Mountain Foothills near Grande Cache, Alberta." Canadian Journal of Earth Sciences 22, no. 11 (November 1, 1985): 1711–19. http://dx.doi.org/10.1139/e85-179.

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Lower Cretaceous clastic rocks make up the Inner Foothills of the Rocky Mountains along the Smoky River near Grande Cache, Alberta. Shortening of these rocks is accomplished by folding and thrusting and averages 33% over the area studied.Folds in the area are of the chevron variety. They are caused by shortening of a multilayered sequence of alternating competent and incompetent strata, where the thickness of the competent layers is fairly constant. The folds are generally cylindrical and maintain their shapes over distances of up to 2 km along trend. However, at their tapering ends they are conical.The majority of the faults are southwest-dipping thrusts, displaying ramps that cut up stratigraphic section and flats that are parallel to bedding. The best exposed fault in the area is the Mason Thrust. Displacements along this fault increase from 150 m in the northwest to 1500 m in the southeastern part of the area. A prominent anticline below the Mason Thrust diminishes gradually towards the southeast. A conical fold with a half apical angle of 7° describes this geometry. Shortening by this fold decreases from about 30% in the northwest to 10% in the southeastern part of the area. This indicates that a decrease in shortening by folding is compensated by an increase in thrust fault displacement. It is an example of fault-to-fold displacement transfer.

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Stubbs, Barbara E. "2012 Canadian Conference on Medical Education (CCME) (14-18 April, Banff, Alberta, Canada)." Medical Education 46 (April 10, 2012): 1. http://dx.doi.org/10.1111/j.1365-2923.2012.04281.x.

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43

Blay-Palmer, Alison. "FLEdGE (Food: Locally Embedded, Globally Engaged) Partnership." Canadian Food Studies / La Revue canadienne des études sur l'alimentation 8, no. 2 (August 5, 2021): 1–5. http://dx.doi.org/10.15353/cfs-rcea.v8i2.539.

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The Food: Locally Embedded, Globally Engaged (FLEdGE) SSHRC-funded Partnership has deep roots in relationships developed over time among academics and community-based practitioners. FLEdGE emerged from community-driven research in Ontario on food hubs and community resilience dating from 2010. From there it expanded to include seven research nodes across Canada and three thematic international working groups, with over 90 researchers, students, and community partners involved in the project. As a multi-institutional project, FLEdGE has nodes in British Columbia (Kwantlen Polytechnic University)/Alberta (University of Alberta), Northwest Territories (Wilfrid Laurier University), northern Ontario (Lakehead University), eastern Ontario (Carleton University), southern Ontario (Wilfrid Laurier University; University of Guelph; University of Waterloo); Quebec (McGill University; Dawson College); and Atlantic Canada (Dalhousie University; Carleton University). There are two or more lead researchers in each node, typically from different disciplines and several community partners in each node. In this way, FLEdGE branched out to include more than 90 partners and collaborators.

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44

van Marle, Guido, and Trushar R. Patel. "Proceedings of the Alberta Virology Conference, University of Alberta, 1–2 June 2017; edited by Guido van Marle and Trushar R. Patel." Biotechnology and Genetic Engineering Reviews 34, no. 1 (January 2, 2018): 1–2. http://dx.doi.org/10.1080/02648725.2018.1478662.

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Pratt, Brian R., and Johan van Heerde. "An arborescent lycopsid stem fragment from the Palliser Formation (Famennian) carbonate platform, southwestern Alberta, Canada, and its paleogeographic and paleoclimatic significance." Canadian Journal of Earth Sciences 54, no. 2 (February 2017): 141–45. http://dx.doi.org/10.1139/cjes-2016-0117.

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A partially silicified stem fragment of an arborescent lycopsid, tentatively identified as Leptophloeum rhombicum, is documented from peritidal carbonates in the Palliser Formation (Upper Devonian; Famennian) of southwestern Alberta. An unlikely inhabitant of these tidal flats, the log must have rafted in from a relatively nearby land area. The most probable candidate sources are either the Kootenay island arc to the paleo-northwest or hypothetical Montania to the southwest. The specimen is evidence that either or both these equatorial areas had a humid paleoclimate and vegetated coastal marshes and swamps.

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Baracos, Vickie E. "Nutrition and Athletic Performance." Canadian Journal of Applied Physiology 26, S1 (October 2001): S1—S3. http://dx.doi.org/10.1139/h2001-036.

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This supplement is based on presentations made at the “First International Congress on Nutrition and Athletic Performance” held at the Shaw Conference Centre, Edmonton, Alberta, Canada, August 8-11, 2001. This conference was stimulated by an increasing awareness of the potential benefits and risks of diet modification and supplementation for elite athletic performance. This supplement summarizes recentfindings and commentary on new research directions in nutrition and athletic performance by 22 invited plenary speakers from around the world.

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Wilson, Steve, Glenn Sutherland, Nicholas Larter, Allicia Kelly, Ashley McLaren, James Hodson, Troy Hegel, Robin Steenweg, Dave Hervieux, and Tom Nudds. "Spatial structure of boreal woodland caribou populations in northwest Canada." Rangifer 40, no. 1 (May 5, 2020): 1–14. http://dx.doi.org/10.7557/2.40.1.4902.

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Local population units (LPUs) were delineated in Canada’s recovery strategy for threatened boreal woodland caribou (Rangifer tarandus caribou). Population viability analyses central to contemporary integrated risk assessments of LPUs implicitly assume geographic closure. Several LPUs in northwest Canada, however, were in part delineated by geopolitical boundaries and/or included large areas in the absence of evidence of more finely resolved population spatial structure. We pooled >1.2 million locations from >1200 GPS or VHF-collared caribou from northeast British Columbia, northwest Alberta and southwestern Northwest Territories. Bayesian cluster analysis generated 10 alternative candidate LPUs based on a spatial cluster graph of the extent of pairwise co-occurrence of collared caribou. Up to four groups may be artifacts in as yet under-sampled areas. Four were mapped LPUs that were conserved (Prophet, Parker, Chinchaga and Red Earth). One small group between Parker and Snake-Sahtaneh known locally as the “Fort Nelson core,” and outside any mapped LPU, was also conserved. Finally, one large group, at >136000 km2, spanned all three jurisdictions and subsumed all of six delineated LPUs (Maxhamish, Snake-Sahtaneh, Calendar, Bistcho, Yates, Caribou Mountains) and part of southern Northwest Territories. These results suggest less geographic closure of LPUs than those currently delineated, but further analyses will be required to better reconcile various sources of knowledge about local population structure in this region.

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Vajda, Edward J., and A. Sumru Ozsoy. "Proceedings of the Conference on Northwest Caucasian Linguistics, 10-12 October 1994." Language 76, no. 4 (December 2000): 929. http://dx.doi.org/10.2307/417211.

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Widenor, Marcus. "Pacific Northwest Labor History Association Conference Highlights Organizing Strategies, Past and Present." International Labor and Working-Class History 55 (April 1999): 142–45. http://dx.doi.org/10.1017/s0147547999253227.

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Facey, Martha. "Report of a Session at the CALL/ACBD Conference, Calgary 2011: The Effects of Interdisciplinary Research on Law Libraries." Legal Information Management 11, no. 4 (December 2011): 298–300. http://dx.doi.org/10.1017/s1472669611000892.

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AbstractMartha Facey summarises the answers given by three panellists during the seminar “Thinking beyond the Law: Effects of Interdisciplinary Research on Law Libraries” delivered at the conference of the Canadian Association of Law Libraries/Association Canadienne des Bibliotheques de Droit (CALL/ACBD) which took place in May 2011 in Calgary, Alberta.

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Journal articles on the topic 'Alberta and Northwest Conference'

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