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Journal articles on the topic 'Winnipeg River'

Author: Grafiati

Published: 4 June 2021

Last updated: 2 March 2023

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1

Enders, Eva C., Colin Charles, Douglas A. Watkinson, et al. "Analysing Habitat Connectivity and Home Ranges of Bigmouth Buffalo and Channel Catfish Using a Large-Scale Acoustic Receiver Network." Sustainability 11, no. 11 (2019): 3051. http://dx.doi.org/10.3390/su11113051.

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The determination if fish movement of potadromous species is impeded in a river system is often difficult, particularly when timing and extent of movements are unknown. Furthermore, evaluating river connectivity poses additional challenges. Here, we used large-scale, long-term fish movement to study and identify anthropogenic barriers to movements in the Lake Winnipeg basin including the Red, Winnipeg, and Assiniboine rivers. In the frame of the project, 80 Bigmouth Buffalo (Ictiobus cyprinellus) and 161 Channel Catfish (Ictalurus punctatus) were tagged with acoustic transmitters. Individual f

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Kristofferson, A. H., and J. W. Clayton. "Subpopulation Status of Lake Whitefish (Coregonus clupeaformis) in Lake Winnipeg." Canadian Journal of Fisheries and Aquatic Sciences 47, no. 8 (1990): 1484–94. http://dx.doi.org/10.1139/f90-166.

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Spawning lake whitefish in Lake Winnipeg from Dauphin River–Lake St. Martin, Traverse Bay, Berens River–Poplar River–Big Black River and Grand Rapids and in Little Playgreen Lake are accorded subpopulation status based on morphometric measurements, meristic counts, and differences in frequencies of alleles at the muscle glycerol-3-phosphate dehydrogenase (g-3-pdh-b) locus. The frequency of the g-3-pdh-b-3 allele in samples from Dauphin River–Lake St. Martin was 0.77 compared with 0.46 for whitefish from the remainder of Lake Winnipeg and Little Playgreen Lake. Two loci for isocitrate dehydroge

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3

Hrabi, R. B., and A. R. Cruden. "Structure of the Archean English River subprovince: implications for the tectonic evolution of the western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (2006): 947–66. http://dx.doi.org/10.1139/e06-023.

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The English River subprovince is one of two metasediment-dominated terranes in the western Superior Province. It has been interpreted as an accretionary complex, a foreland, or a fore-arc basin that developed and was subsequently deformed between the metavolcanic-rich Uchi subprovince and the orthogneiss- and metaplutonic-dominated Winnipeg River subprovince during a prolonged transpressive orogeny. To test these hypotheses, we combined a satellite image, aeromagnetic image, and Lithoprobe reflection seismic profile interpretation with detailed structural mapping to better characterize the int

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4

Patalas, K., and A. Salki. "Crustacean Plankton in Lake Winnipeg: Variation in Space and Time as a Function of Lake Morphology, Geology, and Climate." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 5 (1992): 1035–59. http://dx.doi.org/10.1139/f92-116.

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Rivers draining different geological basins have the most important impact on the formation of the planktonic community in Lake Winnipeg. Very diverse patterns of distribution of individual species reflected the complexity of the water masses structured by lake morphology and the configuration of river inflows. Of the 34 species identified (15 copepods and 19 cladocerans), 12 were found exclusively in the South Basin, 7 exclusively in the North Basin, and 15 were common to both basins. A "core" group of 12 species was distributed over the whole lake, but the remaining 22 species ("unsuccessful

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5

Burn, Donald H., and N. K. Goel. "Flood frequency analysis for the Red River at Winnipeg." Canadian Journal of Civil Engineering 28, no. 3 (2001): 355–62. http://dx.doi.org/10.1139/l00-122.

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This paper reviews the flood frequency characteristics of the Red River at Winnipeg. The impacts of persistence in the flood series on estimates of flood quantiles and their associated confidence intervals are examined. This is done by generating a large number of data sequences using a mixed noise model that preserves the short-term and long-term correlation structures of the observed flood series. The results reveal that persistence in the data series can lead to a slight increase in the expected flood magnitude for a given return period. More importantly, persistence is shown to dramaticall

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6

Wyman, Jeffrey M. "Affinities of Skeletal Material from the Winnipeg River System." Plains Anthropologist 38, no. 142 (1993): 65–78. http://dx.doi.org/10.1080/2052546.1993.11931665.

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Kimiaghalam, Navid, Masoud Goharrokhi, and Shawn P. Clark. "Estimating cohesive sediment erosion and deposition rates in wide rivers." Canadian Journal of Civil Engineering 43, no. 2 (2016): 164–72. http://dx.doi.org/10.1139/cjce-2015-0361.

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Sediment erosion and deposition rates are two of the most important factors that influence fluvial geomorphology. Several experimental devices have been constructed to estimate cohesive sediment erosion rate. However, estimated erosion rates may not be reliable for large rivers due to limited soil sampling and a high dependency of cohesive sediment behaviour on several physical, mechanical, and electrochemical properties of the sediment and eroding fluid. A new methodology has been developed to estimate the erosion and deposition rate of wide rivers using in situ measurements. To test this met

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Percival, J. A., V. McNicoll, and A. H. Bailes. "Strike-slip juxtaposition of ca. 2.72 Ga juvenile arc and >2.98 Ga continent margin sequences and its implications for Archean terrane accretion, western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (2006): 895–927. http://dx.doi.org/10.1139/e06-039.

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The North Caribou terrane of the western Superior Province attained continental thickness (~35 km) by 2997 Ma. It records a subsequent 300 million years history of continental fragmentation, arc magmatism, and terrane accretion. At Lake Winnipeg the ~2978 Ma Lewis–Storey quartzite–komatiite–iron formation assemblage marks Mesoarchean breakup. Unlike the relatively continuous 2980–2735 Ma stratigraphic record of the Red Lake and Birch–Uchi greenstone belts to the east, little of this interval is recorded at Lake Winnipeg. Rather, two belts of younger, juvenile rocks are tectonically juxtaposed:

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9

Bethune, K. M., H. H. Helmstaedt, and V. J. McNicoll. "Structural analysis of the Miniss River and related faults, western Superior Province: post-collisional displacement initiated at terrane boundaries." Canadian Journal of Earth Sciences 43, no. 7 (2006): 1031–54. http://dx.doi.org/10.1139/e06-017.

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Mountain building in the western part of the Archean Superior Province culminated with the formation of regional strike-slip faults. This paper reports on the kinematics and timing of several major faults at the juncture between the Uchi, English River, Winnipeg River, and western Wabigoon subprovinces. Sinistral-oblique mylonitization along the northeast-striking Miniss River fault occurred at 2681 [Formula: see text] Ma. This involved ~40 km of sinistral offset and a scissor-like motion whereby vertical displacement increased southwestward toward a restraining bend near Sioux Lookout. To the

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10

Mckillop, W. B., W. B. Preston, and A. R. Westwood. "RANGE EXTENSION FOR THE EUROPEAN SKIPPER, THYMELICUS LINEOLA (OCHSENHEIMER), 1808 (LEPIDOPTERA: HESPERIIDAE), IN MANITOBA." Canadian Entomologist 124, no. 5 (1992): 943–44. http://dx.doi.org/10.4039/ent124943-5.

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Preston and Westwood (1981) reported on the distribution of Thymelicus lineola (Ochsenheimer) in Manitoba. They suggested that the species arrived here about 1970 by way of northwestern Ontario. At that time the population in central Winnipeg was the most western known in the Prairie region and they suggested that the spread of the species might be impeded by the arid nature of the Great Plains to the west. Klassen et al. (1989) noted that specimens subsequently had been taken 70 km west of Winnipeg at Rathwell(49°39'N; 98°33'W) near the western edge of the Red River Valley soils on the easter

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Rannie, W. F., L. H. Thorleifson, and J. T. Teller. "Holocene evolution of the Assiniboine River paleochannels and Portage la Prairie alluvial fan." Canadian Journal of Earth Sciences 26, no. 9 (1989): 1834–41. http://dx.doi.org/10.1139/e89-156.

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The Portage la Prairie alluvial fan was constructed by numerous successive paleochannels of the Assiniboine River along the western side of the Lake Agassiz basin as the level of the lake rapidly declined beginning 9500 years ago. The history of the paleochannels during the first several thousand years is not known. Paleochannel morphologies and cross-cutting relations, soil maturity, and radiocarbon dates, however, indicate that by 6000–7000 years ago flow was northward into Lake Manitoba. This direction was maintained until about 3000 years ago, when avulsion redirected the Assiniboine eastw

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Booy, C., and D. R. Morgan. "The effect of clustering of flood peaks on a flood risk analysis for the Red River." Canadian Journal of Civil Engineering 12, no. 1 (1985): 150–65. http://dx.doi.org/10.1139/l85-015.

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The nearly 100 year record of spring flood peaks on the Red River at Winnipeg, Manitoba, shows a clustering of high annual peak flows that is possibly, but not likely, due to chance. A similar degree of clustering has been observed in other long-term geophysical records. It can be measured by means of the Hurst statistic. Clustering increases the uncertainty in the parameters of the probability distribution of peak flows estimated from the record. As such it profoundly affects the weight that must be given to the unusually high historical floods that preceded the period of record, in particula

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13

St. George, Scott. "Streamflow in the Winnipeg River basin, Canada: Trends, extremes and climate linkages." Journal of Hydrology 332, no. 3-4 (2007): 396–411. http://dx.doi.org/10.1016/j.jhydrol.2006.07.014.

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Percival, J. A., M. Sanborn-Barrie, T. Skulski, G. M. Stott, H. Helmstaedt, and D. J. White. "Tectonic evolution of the western Superior Province from NATMAP and Lithoprobe studies." Canadian Journal of Earth Sciences 43, no. 7 (2006): 1085–117. http://dx.doi.org/10.1139/e06-062.

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Five discrete accretionary events assembled fragments of continental and oceanic crust into a coherent Superior craton by 2.60 Ga. They exhibit similar sequences of events at ~10 million year intervals: cessation of arc magmatism, early deformation, synorogenic sedimentation, sanukitoid magmatism, bulk shortening, regional metamorphism, late transpression, orogenic gold localization, emplacement of crust-derived granites, and postorogenic cooling. The Northern Superior superterrane recorded 3.7–2.75 Ga events prior to 2.72 Ga collision with the 3.0 Ga North Caribou superterrane. Following 2.98

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McCulloch, W. J., C. Militano, and S. Rizkalla. "Behavioral load testing of the Disraeli facility." Canadian Journal of Civil Engineering 14, no. 1 (1987): 103–10. http://dx.doi.org/10.1139/l87-013.

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The Disraeli facility, which was completed in 1960, consists of several overpasses utilizing rolled steel beam construction and a riveted steel plate girder bridge crossing the Red River in Winnipeg, Manitoba. The total length of the facility is approximately 707 m (2320 ft). In 1984, the City of Winnipeg commissioned Reid Crowther and Partners Limited to perform a load test on the facility to ascertain the possibility of increasing the maximum gross vehicle weight limit. The tests were performed on three consecutive Sundays, from September 23 to October 7, 1984.Three spans were tested. One no

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Booy, C., and L. M. Lye. "Accumulated basin storage as a factor in the correlation structure of annual peak flows on the Red River." Canadian Journal of Civil Engineering 13, no. 3 (1986): 365–74. http://dx.doi.org/10.1139/l86-049.

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The well-established occurrence of exceptionally high floods on the Red River prior to the record of annual peak flows at Winnipeg is an important factor in the flood risk assessment for that city and for the entire Red River valley. But the weight given to this occurrence is quite dependent on the autocorrelation structure assumed for the spring peak time series. It is therefore important to decide whether the clustering of high peak flows, which can be observed in the record, is a mere chance phenomenon or indeed a characteristic of the runoff process. In earlier studies this clustering was

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17

Rigby, J. Keith, and Edward I. Leith. "Tiddalickia manitobensis, a new dictyosponge, and an unusual specimen of the lithistid sponge, Aulocopella winnipegensis Rauff, from the Ordovician of Manitoba." Journal of Paleontology 63, no. 5 (1989): 550–53. http://dx.doi.org/10.1017/s0022336000041172.

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The new thin-walled vasiform dictyospongid hexactinellid, Tiddalickia manitobensis, is described from the Ordovician Red River Formation at McBeth Point on Lake Winnipeg, Manitoba. Vertical spicule bundles are an outer? part of the wall and horizontal spicule bundles an inner? different level within the wall. Bundle quadrules are only half the size of those in Tiddalickia quadrata Rigby and Webby, 1988. A complete anthaspidellid lithistid, Aulocopella winnipegensis Rauff, 1895, is described from a glacial erratic recovered from near Reston, Manitoba.

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18

Camacho, A., H. Baadsgaard, D. W. Davis, and P. Cerny. "RADIOGENIC ISOTOPE SYSTEMATICS OF THE TANCO AND SILVERLEAF GRANITIC PEGMATITES, WINNIPEG RIVER PEGMATITE DISTRICT, MANITOBA." Canadian Mineralogist 50, no. 6 (2012): 1775–92. http://dx.doi.org/10.3749/canmin.50.6.1775.

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Strong, J. W. D., A. R. Cruden, P. A. Cawood, and D. W. Davis. "Eo-Paleoarchean detrital zircon in the Winnipeg River terrane, Western Superior Province: Provenance and implications." Precambrian Research 379 (September 2022): 106802. http://dx.doi.org/10.1016/j.precamres.2022.106802.

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20

Robin Stewart, A., Gary A. Stern, W. Lyle Lockhart, et al. "Assessing Trends in Organochlorine Concentrations in Lake Winnipeg Fish Following the 1997 Red River Flood." Journal of Great Lakes Research 29, no. 2 (2003): 332–54. http://dx.doi.org/10.1016/s0380-1330(03)70438-9.

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21

Melnyk, M., D. W. Davis, A. R. Cruden, and R. A. Stern. "UPb ages constraining structural development of an Archean terrane boundary in the Lake of the Woods area, western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (2006): 967–93. http://dx.doi.org/10.1139/e06-035.

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Layered gneisses in the Winnipeg River subprovince contain magmatic zircon with UPb ages of 3317 ± 9 and 3055 ± 4 Ma at Tannis Lake, and ~3170 and 3255 ± 5 Ma at Cedar Lake, indicating widespread occurrence of Mesoarchean crust. This is in contrast to the well-documented Neoarchean age of the western Wabigoon subprovince. Further geochronology using both SHRIMP (sensitive high resolution ion microprobe) and ID-TIMS (isotope dilution thermal ionization mass spectrometry), combined with structural observations, in the Kenora area and Lake of the Woods greenstone belt show the effects of juxtapo

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Sanborn-Barrie, M., and T. Skulski. "Sedimentary and structural evidence for 2.7 Ga continental arc–oceanic-arc collision in the Savant–Sturgeon greenstone belt, western Superior Province, Canada." Canadian Journal of Earth Sciences 43, no. 7 (2006): 995–1030. http://dx.doi.org/10.1139/e06-060.

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The western Superior Province sustained rapid crustal growth in the interval 2.72–2.68 Ga through amalgamation of microcontinental crustal blocks and juvenile oceanic terranes. Recent field, isotopic, and geophysical surveys provide insight on the nature, timing, and scale of this accretionary growth. However, few places offer the rich tectono-stratigraphic and structural detail with which to establish accretion of oceanic and continental blocks as does the Savant–Sturgeon area. Here, 3.4–2.8 Ga continental crust of the Winnipeg River terrane is juxtaposed with 2.775–2.718 Ga juvenile oceanic

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St. George, Scott, David M. Meko, and Michael N. Evans. "Regional tree growth and inferred summer climate in the Winnipeg River basin, Canada, since AD 1783." Quaternary Research 70, no. 2 (2008): 158–72. http://dx.doi.org/10.1016/j.yqres.2008.04.009.

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AbstractA network of 54 ring-width chronologies is used to estimate changes in summer climate within the Winnipeg River basin, Canada, since AD 1783. The basin drains parts of northwestern Ontario, northern Minnesota and southeastern Manitoba, and is a key area for hydroelectric power production. Most chronologies were developed from Pinus resinosa and P. strobus, with a limited number of Thuja occidentalis, Picea glauca and Pinus banksiana. The dominant pattern of regional tree growth can be recovered using only the nine longest chronologies, and is not affected by the method used to remove v

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Kimiaghalam, Navid, Masoud Goharrokhi, Shawn P. Clark, and Habib Ahmari. "A comprehensive fluvial geomorphology study of riverbank erosion on the Red River in Winnipeg, Manitoba, Canada." Journal of Hydrology 529 (October 2015): 1488–98. http://dx.doi.org/10.1016/j.jhydrol.2015.08.033.

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Corfu, Fernando. "Multistage zircon and titanite growth and inheritance in an Archean gneiss complex, Winnipeg River Subprovince, Ontario." Earth and Planetary Science Letters 141, no. 1-4 (1996): 175–86. http://dx.doi.org/10.1016/0012-821x(96)00064-7.

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Parks, J. W., P. J. Craig, B. P. Neary, G. Ozburn, and D. Romani. "Biomonitoring in the mercury-contaminated Wabigoon-English-Winnipeg river (Canada) system: selecting the best available bioindicator." Applied Organometallic Chemistry 5, no. 6 (1991): 487–95. http://dx.doi.org/10.1002/aoc.590050606.

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Smith, Mauri, and Stephen Bend. "Geochemical analysis and familial association of Red River and Winnipeg reservoired oils of the Williston Basin, Canada." Organic Geochemistry 35, no. 4 (2004): 443–52. http://dx.doi.org/10.1016/j.orggeochem.2004.01.008.

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Cordeiro, Marcos R. C., Kang Liang, Henry F. Wilson, et al. "Simulating the hydrological impacts of land use conversion from annual crop to perennial forage in the Canadian Prairies using the Cold Regions Hydrological Modelling platform." Hydrology and Earth System Sciences 26, no. 22 (2022): 5917–31. http://dx.doi.org/10.5194/hess-26-5917-2022.

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Abstract. The Red River is one of the largest contributing sources of discharge and nutrients to the world's 10th largest freshwater lake, Lake Winnipeg. Conversion of large areas of annual cropland to perennial forage has been proposed as a strategy to reduce both flooding and nutrient export to Lake Winnipeg. Such reductions could occur either via a reduction in the concentration of nutrients in runoff or through changes in the basin-scale hydrology, resulting in a lower water yield and the concomitant export of nutrients. This study assessed the latter mechanism by using the physically base

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Barth, Cameron C., and W. Gary Anderson. "Factors influencing spatial distribution and growth of juvenile lake sturgeon (Acipenser fulvescens)." Canadian Journal of Zoology 93, no. 11 (2015): 823–31. http://dx.doi.org/10.1139/cjz-2015-0058.

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Understanding biotic and abiotic factors that influence spatial distribution patterns, condition factor, and growth of lotic fish species within river impoundments is essential for the development of effective management and conservation strategies. This study aimed to compare relative abundance, condition factor, and growth rate of juvenile lake sturgeon (Acipenser fulvescens Rafinesque, 1817) among eight sections of a 41 km long impoundment of the Winnipeg River, Manitoba, Canada. Relative abundance of juvenile lake sturgeon, as measured by catch per unit effort (CPUE), was 3–6 times greater

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VanTassel, N. M., C. E. Beaver, D. A. Watkinson, T. J. Morris, and D. T. Zanatta. "Absence of genetic structure reflects post-glacial history and present-day host use in Mapleleaf (Quadrula quadrula) mussel from Manitoba, Canada." Canadian Journal of Zoology 98, no. 8 (2020): 551–56. http://dx.doi.org/10.1139/cjz-2019-0227.

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Our study documents and analyzes the absence of genetic diversity and structure of the Mapleleaf (Quadrula quadrula (Rafinesque, 1820)) (Bivalvia: Unionidae) mussel in the Lake Winnipeg, Assiniboine River, and Red River drainages (Manitoba, Canada). Previous studies have revealed patterns of genetic diversity and structure in the Mississippi and Ohio river drainages, as well as in the Laurentian Great Lakes drainage. Genotypes from six variable microsatellite loci showed that the Q. quadrula population in Manitoba was significantly differentiated from the population in the Great Lakes drainage

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Benoy, Glenn A., R. Wayne Jenkinson, Dale M. Robertson, and David A. Saad. "Nutrient delivery to Lake Winnipeg from the Red—Assiniboine River Basin – A binational application of the SPARROW model." Canadian Water Resources Journal / Revue canadienne des ressources hydriques 41, no. 3 (2016): 429–47. http://dx.doi.org/10.1080/07011784.2016.1178601.

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Rao, Yerubandi R., and Jun Zhao. "Numerical simulation of the influence of a Red River flood on circulation and contaminant dispersion in Lake Winnipeg." Natural Hazards 55, no. 1 (2010): 51–62. http://dx.doi.org/10.1007/s11069-010-9534-5.

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Struthers, Daniel P., Lee F. G. Gutowsky, Eva C. Enders, et al. "Factors influencing the spatial ecology of Lake Sturgeon and Walleye within an impounded reach of the Winnipeg River." Environmental Biology of Fishes 100, no. 9 (2017): 1085–103. http://dx.doi.org/10.1007/s10641-017-0629-7.

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Lewis, Catherine, and Blanche Kingdon. "CELBAN: A 10-Year Retrospective Catherine Lewis & Blanche Kingdon." TESL Canada Journal 33, no. 2 (2016): 69. http://dx.doi.org/10.18806/tesl.v33i2.1238.

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This article provides a 10-year review by the test developers of the Canadian English Language Benchmark Assessment for Nurses (CELBAN™). From 2004 to 2014, the development, implementation, national administration, and operations of CELBAN and CELBAN-related products and services were the responsibility of the test developers and team at the Canadian English Language Assessment Services (CELAS) Centre at Red River College, Winnipeg, Manitoba. The CELAS Centre team experienced both challenges and opportunities during this 10-year period. As CELBAN expands, and in light of its current profile as

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de Trémaudan, A. H. "Louis Riel’s Account of the Capture of Fort Garry, 1870." Canadian Historical Review 102, s1 (2021): s44—s55. http://dx.doi.org/10.3138/chr-102-s1-002.

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The capture of Fort Garry, now Winnipeg, by the Red River expedition under Colonel Garnet Wolseley, on August 24, 1870, is an event in Canadian history about which some misapprehensions have been current. It has frequently been said, for example, that the arrival of Colonel Wolseley’s forces took Louis Riel and his associates completely by surprise. That such was not the case is made clear by the following narrative written by Louis Riel himself. For this narrative the present editor is indebted to the late Joseph Riel, who died on the old homestead at St. Vital on May 27, 1921. The manuscript

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Camacho, Alfredo, Halfdan Baadsgaard, Brian J. Paul, and Petr Černý. "RADIOGENIC ISOTOPE SYSTEMATICS OF THE HURON CLAIM PEGMATITE AND THE SHATFORD LAKE PEGMATITE GROUP, WINNIPEG RIVER PEGMATITE DISTRICT, MANITOBA." Canadian Mineralogist 52, no. 5 (2014): 857–72. http://dx.doi.org/10.3749/canmin.1400041.

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Barth, C. C., W. G. Anderson, S. J. Peake, and P. Nelson. "Seasonal variation in the diet of juvenile lake sturgeon, Acipenser fulvescens , Rafinesque, 1817, in the Winnipeg River, Manitoba, Canada." Journal of Applied Ichthyology 29, no. 4 (2013): 721–29. http://dx.doi.org/10.1111/jai.12193.

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Rannie, W. F. "Breakup and freezeup of the Red River at Winnipeg, Manitoba Canada in the 19th century and some climatic implications." Climatic Change 5, no. 3 (1990): 283–96. http://dx.doi.org/10.1007/bf00140185.

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Ma, Chong, Mostafa Naghizadeh, Ademola Adetunji, Robert W. D. Lodge, David Snyder, and Ross Sherlock. "Imaging Neoarchean crustal structures: An integrated geologic-seismic-magnetotelluric study in the western Wabigoon and Winnipeg River terranes, Superior craton." Precambrian Research 364 (September 2021): 106339. http://dx.doi.org/10.1016/j.precamres.2021.106339.

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Lockhart, W. L., D. A. Metner, D. A. J. Murray, and D. C. G. Muir. "Hydrocarbons and Complaints About Fish Quality in the Mackenzie River, Northwest Territories, Canada." Water Quality Research Journal 22, no. 4 (1987): 616–28. http://dx.doi.org/10.2166/wqrj.1987.050.

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Abstract The Mackenzie River in northwestern Canada is the largest North American source of freshwater to the Arctic Ocean There are continuous discharges of petroleum into the river from an oil field at Norman Wells both from refinery and natural seepage sources. Recently oil production was expanded using several artificial islands constructed in the river Coincident with the expansion native DENE fishermen in downstream communities complained that the quality of fish deteriorated. Specifically, the liver of burbot (Lota lota) was reported to have become small and dark in colour, and our inve

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Larbi, Y., R. Stevenson, F. Breaks, N. Machado, and C. Gariépy. "Age and isotopic composition of late Archean leucogranites: implications for continental collision in the western Superior Province." Canadian Journal of Earth Sciences 36, no. 4 (1999): 495–510. http://dx.doi.org/10.1139/e98-113.

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U-Pb and Sm-Nd isotopic data are presented for leucogranites and pegmatites from the boundary zones of the English River, Winnipeg River, and Wabigoon subprovinces in the late Archean Superior Province of northwestern Ontario. The Ghost Lake batholith and the Separation Rapids pluton are posttectonic, rare-metal-bearing, S-type leucogranites that were generated during the final stages of the amalgamation of the Superior Province. U-Pb dating of monazites yields ages of 2650 ± 3 Ma for a pegmatite from the Dryden area and 2646 ± 2 Ma for the Separation Rapids pluton. Sm-Nd data from these grani

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Beakhouse, G. P., R. H. McNutt, and T. E. Krogh. "Comparative RbSr and UPb zircon geochronology of late- to post-tectonic plutons in the Winnipeg River belt, Northwestern Ontario, Canada." Chemical Geology: Isotope Geoscience section 72, no. 4 (1988): 337–51. http://dx.doi.org/10.1016/0168-9622(88)90046-2.

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43

Corfu, F. "Differential response of U-Pb systems in coexisting accessory minerals, Winnipeg River Subprovince, Canadian Shield: implications for Archean crustal growth and stabilization." Contributions to Mineralogy and Petrology 98, no. 3 (1988): 312–25. http://dx.doi.org/10.1007/bf00375182.

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44

Bruyneel, Kevin. "Exiled, Executed, Exalted: Louis Riel, Homo Sacer and the Production of Canadian Sovereignty." Canadian Journal of Political Science 43, no. 3 (2010): 711–32. http://dx.doi.org/10.1017/s0008423910000612.

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Abstract. In this article, I argue that Louis Riel is a necessary invention for the production of Canadian sovereignty. The argument builds on the work of Giorgio Agamben. I see Riel as a Canadian version of homo sacer, “who may be killed but not sacrificed,” and thereby serves as the exception that proves the rule of Canadian sovereignty. I carry out this argument in three stages, focusing first on Riel's exile in 1870 after the Red River Rebellion. I then bring Agamben's insights into an examination of the tensions between French and English Canada over Riel's execution in 1885. Finally, I l

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45

Wendt, I. "Comparative RbSr and UPb zircon geochronology of late- to post-tectonic plutons in the Winnipeg River belt, northwestern Ontario, Canada — Comments." Chemical Geology: Isotope Geoscience section 79, no. 1 (1989): 95. http://dx.doi.org/10.1016/0168-9622(89)90010-9.

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46

Beakhouse, G. P., R. H. McNutt, and T. E. Krogh. "Comparative RbSr and UPb zircon geochronology of late- to post-tectonic plutons in the Winnipeg River belt, northwestern Ontario, Canada — Reply." Chemical Geology: Isotope Geoscience section 79, no. 1 (1989): 96–97. http://dx.doi.org/10.1016/0168-9622(89)90011-0.

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de Trémaudan, A. H. "Louis Riel and the Fenian Raid of 1871." Canadian Historical Review 102, s1 (2021): s32—s43. http://dx.doi.org/10.3138/chr-102-s1-001.

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Just two years ago Joseph Riel, a younger brother of Louis Riel, the famous Metis chieftain of 1869–70 and 1885, died at the old homestead of the Riel family, at St. Vital, near Winnipeg. Until his last breath Joseph Riel resided in the little white house on the east side of the Red River in which his brother had lived. It has been my privilege, on repeated occasions, to be a guest at this house, either on a friendly call or when attending one of the meetings of the Union Nationale Métisse which has been so kind as to elect me one of its honorary members. During such visits I have been allowed

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Thiessen, Kendall J., Marolo C. Alfaro, and James A. Blatz. "Measuring the load–deformation response of rockfill columns by a full-scale field test on a natural riverbank." Canadian Geotechnical Journal 48, no. 7 (2011): 1032–43. http://dx.doi.org/10.1139/t11-019.

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A full-scale field test loading of a riverbank stabilized with rockfill columns was used to measure the load–deformation characteristics of the reinforced slope. The test site is located on the natural banks of the Red River in the city of Winnipeg. Rockfill column technology has evolved from granular shear key methods for stabilizing slopes. The relatively weak lacustrine clays are stabilized with compacted columns of limestone rockfill. The columns typically extend through the clay stratum and are anchored in the underlying till. The project involved an extensive site investigation, and soil

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Ma, Susan, Kathleen R. Laird, Melanie V. Kingsbury, CF Michael Lewis, and Brian F. Cumming. "Diatom-inferred changes in effective moisture during the late Holocene from nearshore cores in the southeastern region of the Winnipeg River Drainage Basin (Canada)." Holocene 23, no. 4 (2012): 568–78. http://dx.doi.org/10.1177/0959683612463103.

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Plotkin, Howard. "The Iron Creek Meteorite: The Curious History of the Manitou Stone and the Claim for its Repatriation." Earth Sciences History 33, no. 1 (2014): 150–75. http://dx.doi.org/10.17704/eshi.33.1.2457k54466405851.

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Canada's Iron Creek meteorite, a 320 lb (145 kg) Group IIIAB medium octahedrite iron, was long venerated by the First Nations in Alberta as their sacred Manitou Stone, but it was taken without authority from them by Methodist missionaries in 1866. That began the meteorite's long odyssey, as it was transferred first to the Methodist Mission in Victoria (now Pakan) Alberta; then to the Red River Mission in Winnipeg, Manitoba; then to the Wesleyan Methodist Church's Mission Rooms in Toronto, Ontario; then to Victoria College in Cobourg, Ontario; then to the campus of the University of Toronto in

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