49 results
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2. Fuzzy set theory based methodology for the analysis of measurement uncertainties in river discharge and stage.
- Author
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Shrestha, Rajesh R. and Simonovic, Slobodan P.
- Subjects
FUZZY sets ,STREAM measurements ,ARITHMETIC ,QUALITY control ,RIVERS - Abstract
Copyright of Canadian Journal of Civil Engineering is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2010
- Full Text
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3. Reply to the comment by Bailey et al. on "Long-term decline of sugar maple following forest harvest, Hubbard Brook Experimental Forest, New Hampshire"1.
- Author
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Battles, John J., Cleavitt, Natalie L., Johnson, Chris E., and Fahey, Timothy J.
- Subjects
LOGGING ,SUGAR maple ,MAPLE ,RIVERS ,MOUNTAIN forests ,FOREST reserves - Abstract
Copyright of Canadian Journal of Forest Research is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2019
- Full Text
- View/download PDF
4. Sediment source identification: a review and a case study in some Canadian streams.
- Author
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Krishnappan, Bommanna G., Chambers, Patricia A., Benoy, Glenn, and Culp, Joseph
- Subjects
RIVER ecology ,RADIOISOTOPES ,CHEMICAL reactions ,GROUNDWATER ,RIVERS - Abstract
Copyright of Canadian Journal of Civil Engineering is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2009
- Full Text
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5. Recent advances in basic and applied research in cohesive sediment transport in aquatic systems.
- Author
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Krishnappan, Bommanna G.
- Subjects
RIVERS ,SEDIMENT transport ,SEDIMENTATION & deposition ,CHANNELS (Hydraulic engineering) ,FLUID dynamics ,FLUIDIZATION ,BULK solids flow ,DIVERSION structures (Hydraulic engineering) - Abstract
Copyright of Canadian Journal of Civil Engineering is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2007
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6. Structural analysis of the Miniss River and related faults, western Superior Province: post-collisional displacement initiated at terrane boundaries.
- Author
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Bethune, K. M., Helmstaedt, H. H., and McNicoll, V. J.
- Subjects
RIVERS ,GEOLOGIC faults ,STRUCTURAL geology ,CANADIAN provinces ,GEOLOGICAL time scales ,HISTORICAL geology ,GEOLOGY ,EARTH sciences - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2006
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7. Tectonic implications of 40Ar/39Ar muscovite dates from the Mt. Haley stock and Lussier River stock, near Fort Steele, British Columbia.
- Author
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Larson, Kyle P., Price, Raymond A., and Archibald, Douglas A.
- Subjects
STRUCTURAL geology ,ARGON ,MUSCOVITE ,RIVERS ,MOUNTAINS ,GEOLOGIC faults ,IGNEOUS intrusions ,PHYSICAL geology - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2006
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8. Early Turonian (Late Cretaceous) age of the Tuskoola sandstone Pine River area, northeastern British Columbia.
- Author
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Stelck, C R, Moore, W E, and Pemberton, S G
- Subjects
CRETACEOUS paleoceanography ,CRETACEOUS paleoecology ,CRETACEOUS stratigraphic geology ,RIVERS ,SANDSTONE ,EARTH sciences - Abstract
The presence of Watinoceras reesidei Warren, Watinoceras coloradoense (Henderson), Watinoceras thompsonense Cobban, and Mytiloides mytiloides (Mantell) within the Tuskoola sandstone beds of the Vimy Member of the Kaskapau (Blackstone) Formation, places these strata within the lower Turonian stage of the Upper Cretaceous, within the Watinoceras reesidei Zone. International discoveries of Watinoceras in the United States, the Arctic, west Africa, northern Africa, Europe, and Asia, in the past fifty years has allowed the authors, while updating the stratigraphy and taxonomy, to refine correlation of the Tuskoola sandstone, a sandy facies of the "Second White Specks" horizon of Western Canada.La présence de Watinoceras reesidei Warren, Watinoceras coloradoense (Henderson), Watinoceras thompsonense Cobban et Mytiloides mytiloides (Mantell) dans les lits de grès de Tuskoola du membre Vimy de la Formation de Kaskapau (Blackstone), place ces strates à l'étage Turonien inférieur du Crétacé supérieur, à l'intérieur de la zone à Watinoceras reesidei. Des découvertes internationales de Watinoceras aux États-Unis, dans l'Arctique, en Afrique occidentale, en Afrique du Nord, en Europe et en Asie au cours des cinquante dernières années ont permis aux auteurs, tout en mettant à jour la stratigraphie et la taxonomie, de préciser la corrélation du grès de Tuskoola, un faciès gréseux de l'horizon « Second White Specks » de l'Ouest du Canada.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
- Published
- 2002
- Full Text
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9. Late Quaternary glacial and interglacial environments of the Nechako River - Cheslatta Lake area, central British Columbia.
- Author
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Plouffe, A and Levson, V M
- Subjects
RIVERS ,LAKES ,GEOLOGY - Abstract
The Quaternary stratigraphy of the Nechako River – Cheslatta Lake area of central British Columbia is described and interpreted to reconstruct the late Quaternary history of the region. Exposures of glacial and nonglacial sediments deposited prior to the last glaciation (Fraser) are limited to three sites. Pollen assemblages from pre-Fraser nonglacial sediments at two of these sites reveal forested conditions around 39 000 BP. During the advance phase of the Fraser Glaciation, glacial lakes were ponded when trunk glaciers blocked some tributary valleys. Early in the glaciation, the drainage was free in easterly draining valleys. Subsequently, the easterly drainage was blocked either locally by sediments and ice or as a result of impoundment of the Fraser River and its tributaries east of the study area. Ice generally moved east and northeast from accumulation zones in the Coast Mountains. Ice flow was influenced by topography. Major late-glacial lakes developed in the Nechako River valley and the Knewstubb Lake region because potential drainage routes were blocked by ice.La stratigraphie du Quaternaire de la région de la rivière Nechako et du lac Cheslatta sise au centre de la Colombie Britannique est décrite et interprétée dans le but de reconstruire l'histoire du Quaternaire tardif de cette région. Seul trois coupes stratigraphiques mettent en évidence des sédiments glaciaires et non-glaciaires mis en place avant la dernière glaciation (Fraser). À deux sites, l'assemblage pollinique des sédiments non-glaciaires prédatant la Glaciation de Fraser reflète un environnement forestier aux environs de 39 000 BP. Lors de l'avancée des glaciers au début de la Glaciation de Fraser, des lacs glaciaires furent retenus dans les vallées secondaires par les glaciers qui occupaient les vallées primaires. Au début de cette glaciation, le drainage vers l'est fut tout d'abord ouvert mais subséquemment, il fut bloqué soit localement par des sédiments et de la glace ou en raison du blocage du fleuve Fraser et ses tributaires à l'est de la région d'étude. Les glaciers se sont écoulés vers l'est et le nord-est à partir de zones d'accumulation centrées sur la Chaîne Côtière. Les écoulements glaciaires furent influencés par la topographie. Des lacs post-glaciaires se sont formés dans la vallée de la rivière Nechako et dans la région du lac Knewstubb suite au blocage du drainage potentiel par la glace.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
- Published
- 2001
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10. Discovery of a significant cave entrance in stripe karst, Horsethief Creek Group, Wells Gray Provincial Park, British Columbia, Canada.
- Author
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Hickson, Catherine, Pollack, John, Struik, Lambertus, Hollis, Lee, and Yonge, Chas
- Subjects
PARKS ,KARST ,CAVES ,AERIAL photographs ,RIVERS - Abstract
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- Published
- 2020
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11. Remnants of Early Mesozoic basalt of the Central Atlantic Magmatic Province in Cape Breton Island, Nova Scotia, Canada.
- Author
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White, Chris E., Kontak, Daniel J., DeMont, Garth J., and Archibald, Douglas
- Subjects
BASALT ,RIVERS ,MAGMAS ,THOLEIITE ,ZEOLITES ,VOLCANISM - Abstract
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- Published
- 2017
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12. Assessment of seven Canadian rivers in relation to stages in oil sands industrial development, 1972-2010.
- Author
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Alexander, A. C. and Chambers, P. A.
- Subjects
OIL sands ,INDUSTRIALIZATION ,RIVERS ,OIL shales ,WATER quality - Abstract
Copyright of Environmental Reviews is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2016
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13. Low flow frequency analysis for stream with mixed populations.
- Author
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Hulley, Mike, Clarke, Colin, and Watt, Ed
- Subjects
STREAMFLOW ,HYDROLOGY ,HOMOGENEITY ,QUANTILES ,FREQUENCIES of oscillating systems ,RIVERS ,UNCERTAINTY (Information theory) ,STREAM measurements - Abstract
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- Published
- 2015
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14. Characteristics and distribution of natural flow regimes in Canada: a habitat template approach.
- Author
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Jones, Nicholas E., Schmidt, Bastian J., Melles, Stephanie J., and Brickman, David
- Subjects
RIVERS ,SPECIES ,HABITATS ,WATERSHEDS ,ECOLOGICAL research ,BIOTIC communities - Abstract
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- Published
- 2014
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15. Occurrence and magnitude of low flows for Canadian rivers: an ecozone approach.
- Author
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Hulley, Mike, Clarke, Colin, and Watt, Ed
- Subjects
RIVERS ,STREAMFLOW ,ECOLOGICAL zones ,REGRESSION analysis ,WATER management ,STREAM measurements ,QUANTILES - Abstract
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- Published
- 2014
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16. Comparative testing of numerical models of river ice jams.
- Author
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Carson, Rick, Beltaos, Spyros, Groeneveld, Joe, Healy, Dan, She, Yuntong, Malenchak, Jarrod, Morris, Mike, Saucet, Jean-Philippe, Kolerski, Tomasz, and Shen, Hung Tao
- Subjects
ICE ,RIVERS ,FLOODS ,CASE studies ,CALIBRATION ,NUMERICAL analysis - Abstract
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- Published
- 2011
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17. Ecological consequences of hybridization between native westslope cutthroat (Oncorhynchus clarkii lewisi) and introduced rainbow (Oncorhynchus mykiss) trout: effects on life history and habitat use.
- Author
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Rasmussen, Joseph B., Robinson, Michael D., and Heath, Daniel D.
- Subjects
SPECIES hybridization ,RAINBOW trout ,WESTSLOPE cutthroat trout ,LIFE history theory ,GENETIC polymorphisms ,HABITATS ,GENETIC research ,RIVERS - Abstract
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- Published
- 2010
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18. A temporal perspective on population structure and gene flow in Atlantic salmon (Salmo salar) in Newfoundland, Canada.
- Author
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Palstra, Friso P. and Ruzzante, Daniel E.
- Subjects
ATLANTIC salmon ,SALMON ,BIOLOGICAL variation ,GENES ,POPULATION biology ,DEEP-sea fisheries ,SIZE of fishes ,RIVERS - Abstract
Copyright of Canadian Journal of Fisheries & Aquatic Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2010
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19. Fish and harlequin ducks compete on breeding streams.
- Author
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LeBourdais, S. V., Ydenberg, R. C., and Esler, D.
- Subjects
BREEDING ,FISHES ,DUCKS ,RIVERS ,BENTHIC animals - Abstract
We investigated interactions among harlequin ducks (Histrionicus histrionicus (L., 1758)), fish, and their shared aquatic insect prey. We measured flow variability, benthic aquatic prey abundance, fish presence, and breeding density of harlequins on eight rivers in the Southern Coast Mountain Range in British Columbia, Canada, in 2003 and 2004. Rivers with lower flow variability had higher abundance of aquatic insects. Densities of harlequins and fish presence on the rivers were both significantly and positively related to insect abundance, but path analysis revealed a strong negative correlation between them. We interpret this as an indirect interaction between harlequins and fish mediated by anti-predator behaviour of insects in the presence of fish, which reduces insect availability, rather than as a reduction in the abundance of aquatic insects through consumption by fishes. We hypothesize that the ongoing and widespread introduction of fish into historically fishless waters throughout North America may have contributed to the current low productivity and recruitment measured in populations of harlequins by reducing quality of breeding habitat. Nous étudions les interactions entre les arlequins plongeurs (Histrionicus histrionicus (L., 1758)), les poissons et les insectes aquatiques qu’ils utilisent conjointement comme proies. Nous avons mesuré la variabilité du débit, l’abondance des proies aquatiques benthiques, la présence de poissons et la densité des arlequins plongeurs en reproduction dans huit rivières de la chaîne de montagnes de la côte sud de la Colombie Britannique, Canada, en 2003 et 2004. Les rivières à débit moins variable ont de plus fortes abondances d’insectes aquatiques. Il y a une relation significative et positive entre les densités des arlequins plongeurs et la présence de poissons, d’une part, et l’abondance des insectes, d’autre part, mais une analyse des coefficients de direction montre une forte corrélation négative entre ces deux variables. Nous interprétons ce phénomène comme une interaction indirecte entre les arlequins plongeurs et les poissons qui s’explique par le comportement anti-prédateur des insectes en présence des poissons, ce qui réduit la disponibilité des insectes, plutôt que par une réduction de l’abondance des insectes aquatiques à cause de la consommation par les poissons. Nous posons l’hypothèse selon laquelle les introductions courantes et répandues de poissons dans des eaux historiquement sans poissons dans toute l’Amérique du Nord peuvent avoir contribué à la productivité et au recrutement faibles mesurés actuellement chez les populations d’arlequins plongeurs en réduisant la qualité des habitats de reproduction. [ABSTRACT FROM AUTHOR]
- Published
- 2009
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20. Movement triggers and mechanisms of two earth slides in the Thompson River Valley, British Columbia, Canada.
- Author
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Eshraghian, Arash, Martin, C. Derek, and Morgenstern, Norbert R.
- Subjects
RIVERS ,VALLEYS ,EROSION ,CONSTRUCTION contracts ,SOIL infiltration ,LANDSLIDES - Abstract
Copyright of Canadian Geotechnical Journal is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2008
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21. Chemical, thermal, and physical properties of sites selected for overwintering by northern wood turtles (Glyptemys insculpta).
- Author
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Greaves, W. F. and Litzgus, J. D.
- Subjects
TURTLES ,GLYPTEMYS ,HIBERNACULA (Animal habitations) ,WINTER ,OXYGEN ,WATER temperature ,RIVER sediments ,RIVERS - Abstract
Northern ectotherms must seek refuge from winter conditions for a large portion of their annual activity cycle. The objective of this study was to quantify physical properties of overwintering sites selected by wood turtles (Glyptemys insculpta (LaConte, 1830)) at the species’ northern range limit. We mapped all structural features (e.g., root balls and log jams), water depth, and sediment types along a 1.5 km stretch of river that was available to turtles outfitted with radio transmitters (N = 8) during winter. Temperature selection was assessed by comparing thermal profiles from data loggers on turtles and temperature stations within the river and other riparian habitats (e.g., ephemeral pools and oxbows). Dissolved oxygen (DO) was measured at each temperature station and turtle location. Wood turtles overwintered in the river, which was colder (~0 °C), had more stable temperatures, and provided higher DO (12.64 ppm) compared with adjacent habitats. Some turtles selected structured refuges for overwintering. Winter movements were not related to temperature or DO, but may be related to maintaining a certain distance from shore and water depth to protect against accidental relocations during winter. We discuss hibernacula as potential factors limiting the northern distribution of wood turtles, a species at risk in Canada. Les ectothermes nordiques doivent trouver un refuge contre les conditions hivernales durant une partie importante de leur cycle annuel d’activités. L’objectif de notre étude est de mesurer les propriétés physiques des sites d’hivernage choisis par les tortues des bois (Glyptemys insculpta (LeConte, 1830)) à la limite boréale de la répartition de l’espèce. Nous avons cartographié tous les éléments structuraux (par ex., boules de racines et embâcles), la profondeur de l’eau et les types de sédiments sur une section de 1,5 km de rivière disponible à des tortues (N = 8) porteuses de radiotransmetteurs pendant l’hiver. La sélection de la température a été évaluée en comparant les profils de températures sur les enregistreuses fixées aux tortues et ceux des stations d’enregistrement dans la rivière et dans les autres habitats de la rive (par ex., les étangs temporaires et les bras morts). Nous avons mesuré l’oxygène dissous (DO) à chaque station d’enregistrement thermique et à chaque emplacement habité par une tortue. Les tortues des bois passent l’hiver dans la rivière qui présente des températures plus froides (~0 °C), mais plus stables et des concentrations de DO plus grandes (12,64 ppm) que les habitats adjacents. Quelques tortues ont choisi des refuges dans des structures pour passer l’hiver. Les déplacements en hiver ne sont pas reliés à la température, ni à la concentration de DO, mais s’expliquent peut-être par le besoin de maintenir une certaine distance de la berge et une certaine profondeur d’eau afin d’éviter les déplacements accidentels pendant l’hiver. Nous discutons des hibernacles comme facteurs potentiels qui peuvent limiter la répartition vers le nord de la tortue des bois, une espèce à risque au Canada. [ABSTRACT FROM AUTHOR]
- Published
- 2008
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22. Among- and within-tributary responses of riverine fish assemblages to habitat features.
- Author
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Reyjol, Yorick, Rodríguez, Marco A., Dubuc, Nathalie, Magnan, Pierre, and Fortin, Réjean
- Subjects
VARIATION in fishes ,FISH ecology ,AQUATIC ecology ,AQUATIC habitats ,REGRESSION analysis ,RIVERS - Abstract
Copyright of Canadian Journal of Fisheries & Aquatic Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2008
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23. Palynostratigraphy and lithostratigraphy of Carboniferous Upper Codroy Group and Barachois Group, southwestern Newfoundland.
- Author
-
Utting, John and Giles, Peter S.
- Subjects
LENTILS ,CRISES ,RIVERS ,LAKES ,COAL ,GEOLOGICAL formations ,CERVIDAE - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2008
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24. Population structure and mantle display polymorphisms in the wavy-rayed lampmussel, Lampsilis fasciola (Bivalvia: Unionidae).
- Author
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Zanatta, David T., Fraley, Stephen J., and Murphy, Robert W.
- Subjects
DNA ,FASCIOLA ,HUMAN ecology ,GENETIC polymorphisms ,WILDLIFE conservation ,ENDANGERED species ,GENETIC research ,RADIOACTIVE pollution of water ,RIVERS - Abstract
Copyright of Canadian Journal of Zoology is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2007
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25. Impacts of climate change on the frequency and severity of floods in the Châteauguay River basin, Canada.
- Author
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Mareuil, Arnaud, Leconte, Robert, Brissette, François, and Minville, Marie
- Subjects
CLIMATE change ,RIVERS ,ACCLIMATIZATION ,CLIMATOLOGY ,WATERSHEDS ,PRECIPITATION variability ,SEASONS ,STOCHASTIC analysis - Abstract
Copyright of Canadian Journal of Civil Engineering is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2007
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26. Hydrodynamic and physical assessment of ice-covered conditions for three reaches of the Athabasca River, Alberta, Canada.
- Author
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Katopodis, C. and Ghamry, H. K.
- Subjects
HYDRODYNAMICS ,ICE on rivers, lakes, etc. ,PHYSICAL measurements ,RIVERS ,WATER distribution ,FISH habitats ,PETROLEUM geology ,FLUID dynamics - Abstract
Copyright of Canadian Journal of Civil Engineering is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2007
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27. Individual variability in activity patterns of juvenile Atlantic salmon (Salmo salar) in Catamaran Brook, New Brunswick.
- Author
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Breau, Cindy, Weir, Laura K, and Grant, James WA
- Subjects
ATLANTIC salmon ,FISH behavior ,MARINE biology research ,EFFECT of temperature on fishes ,WATER temperature ,LOGISTIC regression analysis ,AQUACULTURE ,RIVERS - Abstract
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- Published
- 2007
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28. Riparian areas in the Canadian boreal forest and linkages with water quality in streams.
- Author
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Luke, Stacey H., Luckai, Nancy J., Burke, Janice M., and Prepas, Ellie E.
- Subjects
TAIGAS ,AQUATIC ecology ,BUFFER states (International relations) ,RIPARIAN areas ,RIVERS ,VEGETATION dynamics ,WATER quality - Abstract
Copyright of Environmental Reviews is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2007
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29. Structure of the Archean English River subprovince: implications for the tectonic evolution of the western Superior Province, Canada.
- Author
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Hrabi, R. B. and Cruden, A. R.
- Subjects
RIVERS ,CANADIAN provinces ,STRUCTURAL geology ,MORPHOTECTONICS ,GEOMORPHOLOGY ,PLATE tectonics ,METAMORPHISM (Geology) ,EARTH sciences - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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- 2006
- Full Text
- View/download PDF
30. Ovummuridae (calcareous microfossils) from a Late Devonian ramp: their distribution, preservation potential, and paleoecological significance.
- Author
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MacNeil, Alex J. and Jones, Brian
- Subjects
FOSSILS ,CARBONATES ,CEMENT ,STROMATOLITES ,PALEOZOIC stratigraphic geology ,RIVERS ,CRINOIDEA ,IGNEOUS rocks - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2006
- Full Text
- View/download PDF
31. Brittle faulting in the Thor–Odin culmination, Monashee complex, southern Canadian Cordillera: constraints on geometry and kinematics.
- Author
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Kruse, Stefan and Williams, Paul F.
- Subjects
GEOLOGIC faults ,STRIKE-slip faults (Geology) ,RIVERS ,CARTOGRAPHY ,GEOMETRY ,KINEMATICS - Abstract
Copyright of Canadian Journal of Earth Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2005
- Full Text
- View/download PDF
32. Risk analysis of dissolved organic matter-mediated ultraviolet B exposure in Canadian inland waters.
- Author
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Molot, L. A., Keller, W., Leavitt, P. R., Robarts, R. D., Waiser, M. J., Arts, M. T., Clair, T. A., Pienitz, R., Yan, N. D., McNicol, D. K., Prairie, Y. T., Dillon, P. J., Macrae, M., Bello, R., Nordin, R. N., Curtis, P. J., Smol, J. P., and Douglas, M. S. V.
- Subjects
RISK assessment ,ORGANIC compound content of seawater ,ULTRAVIOLET radiation ,RIVERS - Abstract
Copyright of Canadian Journal of Fisheries & Aquatic Sciences is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2004
- Full Text
- View/download PDF
33. Erosion of undisturbed clay samples from the banks of the St. Lawrence River.
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Gaskin, S.J., Pieterse, J., Al Shafie, A., and Lepage, S.
- Subjects
EROSION ,CLAY ,SOILS ,RIVERS - Abstract
Investigates the mechanism of erosion and the factors influencing erosion rates of clay banks of the Saint Lawrence River along the Montréal to Lac Saint Pierre n Quebec. Literature review; Details on the experiments; Results of the study; Conclusions.
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- 2003
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34. Midwinter breakup and jamming on the upper Saint John River: a case study.
- Author
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Beltaos, Spyros, Ismail, Sayed, and Burrell, Brian C.
- Subjects
ICE on rivers, lakes, etc. ,RIVERS ,FLOOD control - Abstract
Presents a case study of midwinter ice jams on the upper Saint John River in Canada. Background on the environmental effects of ice breakup and jamming; Analysis of several ice breakup and jamming events in the area during the 1990s; Results and implications for planning flood control measures.
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- 2003
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35. Relationships between lithofacies belts and conodont faunas, Gun River Formation (Lower Silurian), Anticosti Island, Quebec: a statistical approach.
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Zhang, Shunxin, Barnes, Christopher R, and Pohler, Susanne ML
- Subjects
LITHOFACIES ,SILURIAN paleoecology ,SILURIAN stratigraphic geology ,RIVERS - Abstract
Discriminant analysis of 80 samples from the Western Carbonate Platform Facies and the Eastern Transitional Carbonate–Siliciclastic Platform Facies of the Gun River Formation (Lower Silurian) on Anticosti Island, Quebec, indicates the degree to which different conodont communities were related to particular lithofacies. The statistical analysis reveals that during most of the Gun River Formation deposition, the conodont distributional pattern of the Western Carbonate Platform Facies and the Eastern Transitional Carbonate–Siliciclastic Platform Facies of the formation remained stable, and that the boundary of the two facies oscillated eastward and westward. The analysis indicates quantitatively that Icriodella deflecta had a nearshore environmental preference, whereas Rexroadus kentuckyensis tended to reside in offshore environments. These two species play the most important role in differentiating conodont communities and determining the relationship between conodont communities and lithofacies among all of the 22 species known from the Gun River Formation.Une analyse discriminante de 80 échantillons du faciès occidental de la plate-forme carbonatée et du faciès oriental de la plate-forme de transition carbonate–siliclastique de la Formation de Gun River (Silurien inférieur) sur l'île d'Anticosti, au Québec, indique le degré de relation entre les diverses communautés de conodontes et des lithofaciès particuliers. L'analyse statistique révèle que, lors de la déposition de la plus grande part de la Formation de Gun River, le patron de distribution des conodontes du faciès occidental de la plate-forme carbonatée et celui du faciès oriental de la plate-forme de transition carbonate–siliclastique de la formation sont demeurés stables et que la limite entre les deux faciès oscillait vers l'est et vers l'ouest. Les résultats quantitatifs de l'analyse indiquent que Icriodella deflecta préférait les environnements littoraux alors que Rexroadus kentuckyensis avait plus tendance à rester dans des environnements au large. Ces deux espèces sont les plus significatives pour différencier les communautés de conodontes et déterminer la relation entre les communautés de conodontes et les lithofaciès parmi toutes les 22 espèces connues dans la Formation de Gun River.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2002
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36. Hydrogeology of the Oak Ridges Moraine aquifer system: implications for protection and management from the Duffins Creek watershed.
- Author
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Gerber, Richard E and Howard, Ken
- Subjects
HYDROGEOLOGY ,RIVERS ,WATER supply - Abstract
The Oak Ridges Moraine aquifer feeds the headwaters of major rivers in the Greater Toronto Area and is an important source of domestic water supply. Recognizing the rapid rate of urban growth in the region, there is a concern that changing land use along the moraine must be strictly controlled if groundwater is to be adequately protected. To date, efforts to incorporate groundwater protection into the land use planning process have been hampered by an inadequate quantitative hydrogeological understanding of the aquifer system. Focusing on the Duffins Creek watershed, comprehensive hydrogeological studies including a numerical flow model now provide a quantitative insight into the hydrogeologic function of the moraine. These studies demonstrate that 60% of the entire basin groundwater discharge to streams occurs along the south flank of the moraine, and 60% of this headwater discharge occurs below the 275 m above sea level contour, one of the commonly accepted planning boundaries of the moraine. The remaining discharge is contributed by aquifers within and underlying deposits that extend to the south of the moraine. While 75–80% of the watershed discharge to streams is received from the uppermost aquifer, 20–25% is contributed by deeper aquifers underlying the extensive Northern–Newmarket till aquitard. This work shows that the moraine sediments represent just one component of a regional flow system that extends beyond the morphological boundary of the moraine. This has important implications for groundwater protection, as it demonstrates the need for management strategies that incorporate the regional groundwater flow system and not the moraine in isolation.L'aquifère de la moraine de Oak Ridges alimente le cours supérieur de grandes rivières dans la région du Grand Toronto et constitue une importante source d'alimentation en eau domestique. Conscient du taux rapide de croissance urbaine dans la région, on croit que le changement d'utilisation des terres le long de la moraine doit être rigoureusement contrôlé afin de protéger adéquatement l'eau souterraine. À ce jour, les efforts pour inclure la protection de l'eau souterraine dans le processus de planification d'utilisation des terres ont été retardés par une connaissance quantitative hydrogéologique inadéquate du système d'aquifères. Ciblant le bassin hydrographique de Duffins Creek, des études hydrogéologiques complètes, incluant un modèle numérique de l'écoulement, fournissent maintenant un aperçu quantitatif de la fonction hydrogéologique de la moraine. Il démontre que 60 % de tout le débit souterrain du bassin a lieu le long du flanc sud de la moraine. Soixante pour cent de ce débit a lieu sous le niveau amsl de 275 m, soit l'une des limites couramment utilisées comme limite de planification pour la moraine de Oak Ridges. Le débit restant est contrôlé par des aquifères à l'intérieur et sous des dépôts qui se prolongent au sud de la moraine. Alors que 75 à 80 % du débit du bassin hydrographique vers les ruisseaux provient de l'aquifère supérieur, 20 à 25 % provient d'aquifères plus profonds sous la grande couche de till semi-perméable capacitive de Northern–Newmarket. Cette étude montre que les sédiments de la moraine ne représentent qu'une composante d'un système régional d'écoulement qui s'étend au-delà de la limite morphologique de la moraine. Cela représente des implications importantes pour la protection de l'eau souterraine car cela démontre le besoin d'avoir des stratégies de gestion qui incorporent le système régional d'écoulement de l'eau souterraine et non seulement la moraine.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2002
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37. Analysis and reinterpretation of deformation features in the Rouge River valley, Scarborough, Ontario.
- Author
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Godin, Laurent, Brown, Richard L, Dreimanis, Aleksis, Atkinson, Gail M, and Armstrong, Derek K
- Subjects
RIVERS ,DEFORMATIONS (Mechanics) ,VALLEYS - Abstract
Geometry and timing of deformation affecting Ordovician bedrock and overlying Pleistocene sediments in the Rouge River valley near Scarborough, Ontario, are analysed to evaluate whether or not the structures are a result of glacial action or neotectonic activity. Extensive data on local and regional ice-flow directions are used to evaluate the kinematic compatibility between the observed faults and folds and the local ice-flow directions. Jointing and multiple episodes of faulting affect both the Ordovician bedrock and the overlying Pleistocene sediments. At one site, the bedrock is displaced by a normal fault by a minimum of 1.2 m. Crosscutting relationships constrain the majority of the faulting in the Rouge River valley as being coeval with deposition of the lower Bowmanville till during the Nissouri phase (ca. 23–15 ka), and possibly younger at one locality. The youngest regional ice-flow direction is northwestward; however, local ice-flow directions are highly variable. This can be explained by local perturbation enhanced by the presence of drumlinoid features in the area. Most deformation features are compatible with local and regional ice-flow directions. Glaciotectonic ice-push and ice-thrust deformation affected the Thorncliffe Formation after about 23 ka. Although some faults appear to be kinematically incompatible with ice-flow directions, six boreholes drilled to 52 m depth revealed only minor vertical offsets of bedrock strata in the uppermost 20 m, and an absence of obvious fault offsets deeper, precluding the possibility that the faults observed in the surface exposures were caused by deep-seated neotectonic stresses.Nous avons analysé la géométrie et le moment de la déformation touchant le socle ordovicien et les sédiments sus-jacents du Pléistocène dans la vallée de la rivière Rouge près de Scarborough, en Ontario, afin de déterminer si les structures résultent d'une action glaciaire ou d'une activité néotectonique. De nombreuses données sur les directions locales et régionales de l'écoulement glaciaire ont servi pour évaluer la compatibilité cinématique entre les failles et les plis observés et les directions locales des écoulements glaciaires. Le réseau de diaclases et les nombreux épisodes de failles affectent à la fois le socle ordovicien et les sédiments sus-jacents du Pléistocène. À un site, le socle est déplacé d'au moins 1,2 mètres par une faille normale. Des relations d'entrecroisements restreignent la plupart des failles de la vallée de la rivière Rouge à être contemporaines de la déposition du till Bowmanville inférieur au cours de la phase Nissouri (vers 23–15 ka) et possiblement plus jeunes à une localité. La direction de l'écoulement régional le plus jeune est vers le nord-ouest; toutefois, les directions locales de l'écoulement glaciaire sont hautement variables. Cela peut être expliqué par une perturbation locale rehaussée par la présence de formes drumlinoïdes dans la région. La plupart des paramètres de déformation sont compatibles avec les directions locales et régionales de l'écoulement glaciaire. La déformation glaciotectonique et de chevauchement glaciaire a affecté la Formation de Thorncliffe un peu après 23 ka. Bien que quelques failles semblent être incompatibles d'un point de vue cinétique avec les directions d'écoulement, six forages à une profondeur de 52 mètres ont révélé seulement de mineurs déplacements verticaux des strates du socle dans les 20 mètres supérieurs et une absence de déplacement évident de failles à de plus grandes profondeurs, écartant ainsi la possibilité que les failles observées dans les affleurements de surface aient été causées par des contraintes néotectoniques à de grandes profondeurs.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2002
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38. The Eureka River landslide and dam, Peace River Lowlands, Alberta.
- Author
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Miller, B G.N and Cruden, D M
- Subjects
RIVERS ,LANDSLIDES ,GEOMORPHOLOGY ,PHYSICAL geography - Abstract
The Eureka River landslide of June 1990, at 50 Mm[sup 3] , is one of the largest historical landslides on the Interior Plains of Canada. It is one of seven large translational landslides to have occurred in the Peace River Lowlands within the last 65 years. Each landslide occurred in Quaternary sediments deposited within a preglacial valley. Each landslide formed a dam. The rupture surface of the Eureka River landslide in preglacial lacustrine sediment, 125 m below the Peace River Lowlands plains, extended beneath the river channel causing the channel to be elevated. The resulting landslide dam was over 20 m high, forming a lake exceeding 8 km in length. The river cut a new channel around the toe of the landslide, abandoning the prelandslide channel. As the new channel is free of armour, incision has been rapid. After 10 years, the dam now stands approximately 5 m high.Key words: landslide, landslide dam, Peace River, Alberta, preglacial valley, geomorphology.Le glissement de la rivière Eureka de juin 1990, ayant un volume de 50 Mm[sup 3] , est un des plus importants glissements historiques des Plaines intérieures du Canada. Il est un des sept grands glissements translationnels à s'être produits dans les Basses-Terres de la rivière Peace au cours des 65 dernières années. Chaque glissement s'est produit dans les sédiments du Quaternaire déposés dans une vallée préglaciaire. Chaque glissement forme un barrage. La surface de rupture du glissement de la rivière Eureka dans le sédiment lacustre préglaciaire, localisée à 125 m sous les plaines des Basses-Terres de la rivière Peace, s'étendait sous le canal de la rivière produisant un soulèvement du canal. Le barrage du glissement résultant avait plus de 20 m de hauteur, formant un lac excédant 8 km de longueur. La rivière s'est frayé un nouveau canal autour du pied du glissement, abandonnant le canal existant avant le glissement. Comme le nouveau canal était libre d'armature, l'entaille a été rapide. Après 10 ans, le barrage mesure maintenant environ 5 m de hauteur.Mots clés : glissement, barrage de glissement, rivière Peace, Alberta, vallée préglaciaire, géomorphologie.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
- Published
- 2002
- Full Text
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39. Step-pool and cascade morphology, Mosquito Creek, British Columbia: a test of four analytical techniques.
- Author
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Wooldridge, C L and Hickin, E J
- Subjects
RIVERS ,MOUNTAINS - Abstract
The identification and geometric definition of individual cascade and step-pool bedforms are investigated in a steep, coarse-grained, mountain stream, Mosquito Creek, by testing four analytical techniques: visual identification, zero-crossing, bedform differencing, and power spectral analysis. The test is the first use of these techniques in a headwater stream, and the analysis of two bed profiles showed that visual identification was able to (i) identify, (ii) determine the geometry of, and (iii) classify the type of individual bedforms better than the other methods. The other techniques were not able to differentiate step-pools from cascades, and the large range of grain sizes and bedform heights hampered their ability to consistently identify stepped bedforms. The step-pool (pronounced, channel-spanning steps that alternate with channel-spanning pools) and cascade (multi-tiered, partially channel-spanning structures) morphology in Mosquito Creek has formed in the last 20 years as fluvial action has restructured its previously engineered, revetment-lined, planar bed. The channel bed exhibits a morphologic regularity that power spectral analysis captured as periodic fluctuations in the bed profiles, with mean wavelengths slightly greater than those identified by the other methods. Further, the active reorganization of revetment has formed stepped structures with geometries similar (i.e., height to wavelength ratios) to stepped features found in natural mountain streams. Channel slope partially controlled bedform geometry (wavelength and height), and bedform height weakly controlled individual step spacing, but there was no relation between wavelength and grain size (D[sub 90] ).L'identification et la définition géométrique de formes de lits de rivières individuels en cascades et en paliers d'accalmie sont étudiées dans le crique Mosquito, un ruisseau de montagne, abrupte et coulant sur un sol à grain grossier, en mettant à l'essai quatre techniques analytiques : l'identification visuelle, le passage par zéro, la différenciation de la forme du lit et une analyse spectrale de puissance. Ce test constitue la première utilisation de ces techniques dans un ruisseau d'amont et l'analyse de deux profils de lits a démontré que l'identification visuelle pouvait (i) identifier, (ii) déterminer la géométrie et (iii) classifier le type individuel de lit de rivière mieux que les autres méthodes. Les autres techniques ne permettaient pas de différencier entre les paliers d'accalmie et les cascades; de plus, la grande étendue des granulométries et de hauteurs de lits entravaient leur capacité d'identifier avec constance les formes de lits à paliers. Dans le crique Mosquito, la morphologie des paliers d'accalmie (des marches accentuées qui enjambent le chenal alternant avec des bassins calmes qui enjambent le chenal) et des cascades (des structures à plusieurs niveaux qui enjambent partiellement le chenal) s'est formée au cours des 20 dernières années alors que l'action de l'eau a restructuré son ancien lit planaire, artificiel et tapissé. Le lit du chenal montre une régularité morphologique que l'analyse spectrale de puissance a interprétée comme des fluctuations périodiques des profils du lit avec des longueurs d'onde moyennes légèrement supérieures à celles identifiées par les autres méthodes. De plus, la réorganisation active du revêtement a formé des structures en paliers dont les géométries (c.-à-d. les rapports de la hauteur sur la longueur d'onde) sont semblables aux caractéristiques des paliers trouvés dans les ruisseaux de montagne naturels. La pente du chenal a contrôlé en partie la géométrie de la forme du lit (longueur d'onde et hauteur) et la hauteur de la forme du lit a faiblement contrôlé l'espacement des gradins individuels mais il n'y avait aucune relation entre la longueur d'onde et la granulométrie (D[sub 90] ).[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2002
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40. Climate change and abundance cycles of two sympatric populations of smelt (Osmerus mordax) in the middle estuary of the St. Lawrence River, Canada.
- Author
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Mingelbier, M, Lecomte, F, and Dodson, J J
- Subjects
CLIMATE change ,CLIMATOLOGY ,SMELT fisheries ,RAINBOW smelt ,RIVERS - Abstract
Commercial catches of two ecologically distinct sympatric smelt (Osmerus mordax) populations segregated along the two shores of the St. Lawrence middle estuary exhibited inverse patterns with periodicities on the order of 30 years. The influence of water level in the St. Lawrence River and air temperature, chosen to reflect variations in hydrology and climate, differed markedly between the two populations. Analyses revealed that both water level and temperature were generally positively related with north-shore smelt landings and negatively related with south-shore smelt landings. For both populations, a number of significant climatic factors contributing to variance in smelt landings were lagged by one to three years relative to the year of landings, indicating that climatic variables influenced smelt recruitment. The contrasting role of hydroclimatic variables in driving these abundance cycles is likely related to differential exploitation of estuarine habitats; the south-shore population is associated with shallow shoal habitat, whereas the north-shore population is associated with deep channel habitat. The responses of the two smelt populations also reflect the fundamental ecological differences existing between shoal and channel habitats, indicating that future climate change may differentially affect other populations or species that are segregated between these two habitats.Les débarquements commerciaux de deux populations d'éperlans (Osmerus mordax) arc-en-ciel sympatriques, distinctes du point de vue écologique et ségréguées le long des deux rives de l'estuaire moyen du Saint-Laurent, montrent des variations cycliques inverses et une périodicité de l'ordre de 30 ans. L'influence du niveau d'eau du fleuve et de la température de l'air, choisis dans l'étude pour refléter les variations du régime hydrologique et du climat, diffèrent de façon marquée pour les deux populations. Les analyses révèlent que le niveau de l'eau et la température sont généralement corrélés positivement aux débarquements de la rive nord et négativement à ceux de la rive sud. Quelques un des principaux facteurs climatiques contribuant pour une grande part aux variations des débarquements des deux rives étaient décalés dans le temps, indiquant que les facteurs climatiques influencent le recrutement des éperlans. L'effet contrasté des variables hydroclimatiques sur les cycles d'abondance est vraisemblablement liée à l'utilisation différentielle des habitats de l'estuaire; la population de la rive sud est associée à un habitat peu profond et celle de la rive nord est à un chenal profond. Les réponses de ces deux populations d'éperlans reflètent aussi des différences écologiques existant entre des habitats peu profonds et un chenal profond, indiquant que les changements climatiques futurs pourraient avoir des effets différents sur d'autres populations ou d'autres espèces, qui sont ségréguées entre ces deux types d'habitats. [ABSTRACT FROM AUTHOR]
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- 2001
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41. Conodonts from the Kechika Formation and Road River Group (Lower to Upper Ordovician) of the Cassiar Terrane, northern British Columbia.
- Author
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Pyle, Leanne J and Barnes, Christopher R
- Subjects
CONODONTS ,FOSSIL animals ,RIVERS - Abstract
This study examines the lower Paleozoic stratigraphy of the Cassiar Terrane from three key sections comprising an east-west transect across the terrane. The Cassiar Terrane, west of the Northern Rocky Mountain Trench, consists of a Neoproterozoic to Triassic succession and is a fragment of the Cordilleran Miogeocline that has been displaced northward. The amount of displacement from its original position remains controversial. Conodonts from the Cassiar Terrane have been previously reported from only a few reconnaissance studies. More than 3000 m of strata have been measured and examined in detail and 85 conodont samples collected. A total of 926 identifiable conodont elements are assigned to 31 species representing 21 genera. The conodonts are mainly representative of the Midcontinent Faunal Realm, but some also represent the Atlantic Realm. Conodonts from the upper Kechika Formation and base of the Road River Group are Early Ordovician (Tremadocian) in age, and those from the upper Road River Group range into the Upper Ordovician (Caradocian). The detailed Ordovician stratigraphy and temporal constraints established by conodont biostratigraphy provide for correlation to coeval facies of ancestral North America. The onset of Road River sedimentation in the mid-Tremadocian is, however, older than that in the Macdonald Platform to the east (early Arenigian). This onset timing may help link the Cassiar Terrane to a specific part of the miogeocline from which it was transported.Cette étude examine la stratigraphie du Paléozoïque inférieur du terrane de Cassiar à partir de trois sections clefs comprenant un transect est-ouest à travers le terrane. Le terrane de Cassiar, à l'ouest du sillon septentrional des Rocheuses, comprend une séquence du néo-Protérozoïque au Trias et représente un fragment du miogéocline de la Cordillère qui a été déplacé vers le nord. La distance de déplacement par rapport à sa position originale demeure controversée. Les Conodontes du terrane de Cassiar n'ont été signalés antérieurement que dans quelques études de reconnaissance. Des strates ont été mesurées et examinées en détail sur plus de 3000 m et 85 échantillons de Conodontes ont été recueillis. Neuf cent vingt-six (926) éléments identifiables de Conodontes ont été assignés à 31 espèces représentant 21 genres. Les Conodontes sont surtout représentatifs du domaine faunique du centre du continent, mais quelques-uns représentent aussi le domaine de l'Atlantique. Les Conodontes de la partie supérieure de la Formation de Kechika et de la base du Groupe de Road River datent de l'Ordovicien précoce (Trémadocien) et ceux de la partie supérieure du Groupe de Road River atteignent l'Ordovicien supérieur (Caradocien). La stratigraphie détaillée de l'Ordovicien et les contraintes temporelles imposées par la biostratigraphie des Conodontes permettent une corrélation à des faciès contemporains dans l'ancienne Amérique du Nord. La sédimentation du Road River au Trémadocien moyen a toutefois débuté plus tard que dans la plate-forme de Macdonald vers l'est (Arénigien précoce). Ce moment du début peut aider à relier le terrane de Cassiar à une partie spécifique du miogéocline d'où il provient.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2001
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42. Comparison of models predicting invertebrate assemblages for biomonitoring in the Fraser River catchment, British Columbia.
- Author
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Reynoldson, T.B., Rosenberg, D.M., and Resh, V.H.
- Subjects
INVERTEBRATE populations ,RIVERS - Abstract
Describes a multivariate, predictive model based on the reference-condition approach for the Fraser River catchment in British Columbia. Study area and sampling sites; Assemblage metrics; Taxonomic resolution.
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- 2001
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43. Preglacial archaeological evidence at Grimshaw, the Peace River area, Alberta: Discussion.
- Author
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Driver, Jonathan C
- Subjects
ARCHAEOLOGY ,ANTHROPOLOGY ,RIVERS - Abstract
Comments on the preglacial archaeological evidence at Grimshaw, the Peace River area in Alberta presented by a study. Significance of the fractured quartzite cobbles from the base of a Wisconsinan Laurentide till in the area; Lack of contextual evidence of human presence in the area; Problems with the criteria and alternative explanations of the study.
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- 2001
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44. Preglacial archaeological evidence at Grimshaw, the Peace River area, Alberta: Reply.
- Author
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Chlachula, Jiri and Leslie, Louise
- Subjects
ARCHAEOLOGY ,ANTHROPOLOGY ,RIVERS - Abstract
Presents a response to comments concerning a study on preglacial archaeological evidence at Grimshaw, the Peace River area in Alberta. Debates concerning archaeological evidence potentially predating the Palaeo-Indian traditions; Cultural evidence presented by the study; Irrelevance of the references to naturally fractured flint collections from the British crags.
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- 2001
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45. New U–Pb and Ar/Ar isotopic age constraints on the timing of Eocene magmatism, Fort Fraser and Nechako River map areas, central British Columbia.
- Author
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Grainger, Nancy C, Villeneuve, Michael E, Heaman, Larry M, and Anderson, Robert G
- Subjects
RIVERS ,ROCKS ,GEOLOGY ,EARTH sciences - Abstract
Twenty-three new, precise, Eocene U–Pb and [sup 40] Ar/[sup 39] Ar age determinations for calc-alkaline volcanic rocks of the Ootsa Lake Group and associated intrusive rocks, widespread in the Nechako Plateau in central British Columbia, constrain the timing of the Eocene magmatism to 53.2–47.6 Ma, with a local duration of as little as 2–3 million years. The new dates show that magmatism in the study area is partly coeval with that responsible for the Babine Igneous Suite – Newman Volcanic Suite (53–50 Ma) to the north, and for the Endako Group (51–45 Ma), which overlies the Ootsa Lake Group; however, locally the three magmatic suites are distinct in age and (or) the strata record a magmatic hiatus of as much as 7.5 million years. The ages generally young from north to south (52–47 Ma) along the western portion of the study area. The Babine Igneous Suite – Newman Volcanic Suite represents the oldest member of this series. However, in the east, the Ootsa Lake Group volcanic rocks are generally older (53–51 Ma). The anomalously older ages may be related to the interaction of magmatism and formation of a nearby and coeval core complex, which ongoing studies show was uplifted at about the same time during the Eocene. Felsic plutonism associated with the Ootsa Lake Group occurred between 50.5 and 47.3 Ma. These plutons were emplaced in an extensional setting along north-northeast-trending faults. The new dates, stratigraphic relationships, and suggested correlations of Eocene strata in the study area with that to the west and north require a revision of the stratigraphic nomenclature for the Ootsa Lake and Endako groups.Vingt-trois nouvelles déterminations d'âge, précises, U–Pb et [sup 40] Ar/[sup 39] Ar sur des roches volcaniques calco-alcalines du Groupe d'Ootsa Lake et des roches intrusives associées, datant de l'Éocène, largement répandues dans le plateau de Nechako au centre de la Colombie-Britannique, limitent le magmatisme à l'Éocène à 53,2–47,6 Ma et à une durée aussi courte que 2 à 3 millions d'années. Les nouvelles dates montrent que le magmatisme dans la région étudiée est en partie contemporain avec celui qui est responsable de la suite ignée Babine – suite volcanique Newman (53–50 Ma) vers le nord et du Groupe Endako (51–45 Ma) qui repose sur le Groupe d'Ootsa Lake; localement, les trois suites magmatiques sont toutefois distinctes en âge et (ou) les strates enregistrent un hiatus magmatique allant jusqu'à 7,5 Ma. Les âges sont généralement plus jeunes du nord vers le sud (52–47 Ma) le long de la partie occidentale de la région à l'étude. La suite ignée Babine – suite volcanique Newman représente le membre le plus âgé de cette série. Toutefois, vers l'est, les roches volcaniques du Groupe d'Ootsa Lake sont généralement plus âgées (53–51 Ma). Les âges anormalement plus vieux peuvent être reliés à l'interaction du magmatisme et à la formation, à proximité, d'un complexe noyau contemporain, lequel, selon des études en cours, s'est soulevé à peu près à la même époque, à l'Éocène. Le plutonisme felsique associé au Groupe d'Ootsa Lake aurait eu lieu il y a environ 50,5 à 47,3 Ma. Ces plutons ont été mis en place dans un environnement extensionnel le long de failles de direction nord-nord-est. Les nouvelles dates, les relations stratigraphiques et les corrélations suggérées pour les strates de l'Éocène dans la région à l'étude et celles vers l'ouest et le nord demandent une révision de la nomenclature stratigraphique pour les groupes d'Ootsa Lake et d'Endako.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2001
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46. Quaternary stratigraphy and history of the Ootsa Lake - Cheslatta River area, Nechako Plateau, central British Columbia.
- Author
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Mate, D J and Levson, V M
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RIVERS ,LAKES ,EROSION - Abstract
Erosion along the Nechako Reservoir and Cheslatta River Spillway has resulted in unusually well-exposed late Quaternary and Holocene stratigraphy. Surficial sediments in the study area are mostly products of Late Wisconsinan glaciation. However, evidence for pre-Late Wisconsinan sedimentation has been found along the shores of the Nechako Reservoir, including till of an older glaciation and organic-bearing, blue-grey, lacustrine sediments of probable Middle Wisconsinan age. Stratigraphic correlation of the lake sediments suggests that an extensive lake system occurred in the region during the Olympia Nonglacial Interval. Late Wisconsinan ice initially moved along major valleys, with glaciofluvial outwash deposited in front of the advancing ice. Advance-phase glaciolacustrine sediments are rare but significant, as slope failures are spatially associated with areas where they are preserved. The distribution of these sediments and associated deltaic deposits indicates that advance-phase glacial lakes occurred up to approximately 855 m asl, at least several metres above the modern reservoir level. Sediments deposited in front of the ice margin were overridden during ice advance and are best preserved in large valleys. At the glacial maximum, ice flowed northeasterly throughout the study region. Crag and tails, flutings, and drumlinoid ridges with a generally consistent northeast trend are the dominant landforms. Till is the most common Pleistocene surficial sediment, covering approximately 80% of the area; large areas of exposed bedrock are rare. Late-glacial glaciofluvial and Holocene fluvial deposits are uncommon and occur mainly along the Cheslatta River valley. De l'érosion le long du réservoir Nechako et du déversoir de la rivière Cheslatta a produit de très beaux affleurements de la stratigraphie du Quaternaire tardif et de l'Holocène. Les sédiments de surface dans la région à l'étude sont surtout des produits de la glaciation du Wisconsinien tardif. Toutefois, des preuves de sédimentation au pré-Wisconsinien tardif ont été retrouvées le long des berges du réservoir Nechako; elles comprennent un till d'une glaciation plus ancienne et des sédiments lacustres gris-bleu contenant de la matière organique, datant probablement du Wisconsinien moyen. La corrélation stratigraphique des sédiments lacustres suggère qu'un système extensif de lacs était en place dans la région durant l'intervalle non glaciaire Olympia. La glace du Wisconsinien tardif a tout d'abord avancé le long des vallées majeures alors que du matériel stratifié fluvio-glaciaire était déposé en avant de la glace qui avançait. Des sédiments glacio-lacustres de phase avancée sont rares mais importants car les ruptures de pentes sont associées aux régions où ils sont préservés. La distribution de ces sédiments et des dépôts deltaïques associés indique que des lacs glaciaires de phase avancée se sont retrouvés à environ 855 m au-dessus du niveau de la mer, au moins plusieurs mètres au-dessus du niveau moderne du réservoir. Lors d'une avancée glaciaire, la glace passe par-dessus les sédiments déposés en avant du front glaciaire et ils sont ainsi mieux conservés dans les grandes vallées. Au maximum glaciaire, la glace coulait vers le nord-est dans toute la région à l'étude. Les formes de terrain dominantes, à direction généralement nord-est, sont les « crag and tail », les rainures glaciaires et les drumlinoïdes. Le till est le sédiment de surface le plus commun du Pléistocène, couvrant environ 80 % de la région; les grandes aires d'affleurements rocheux sont rares. Les dépôts fluvio-glaciaires tardi-glaciaires et les dépôts fluviaux de l'Holocène sont peu communs et se retrouvent surtout le long de la vallée de la rivière Cheslatta.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2001
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47. Imbricate architecture of the upper Paleozoic to Jurassic oceanic Cache Creek Terrane, central British Columbia.
- Author
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Struik, L C, Schiarizza, P, Orchard, M J, Cordey, F, Sano, H, MacIntyre, D G, Lapierre, H, and Tardy, M
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SUBMARINE topography ,OCEANIC plateaus ,ROCKS ,RIVERS - Abstract
Upper Paleozoic to Lower Jurassic oceanic rocks of the Cache Creek Terrane near Fort St. James, in central British Columbia, form a stack of thrust sheets cut by steeply dipping strike-slip faults. Paleontologically dated upper Paleozoic strata include bioclastic shallow-water limestone and ribbon chert. Isotopically dated Permian rocks consist of tonalite sills and stocks and rhyolite flows intercalated with basalt flows. Paleontologically dated lower Mesozoic rocks include greywacke, sandstone, siltstone, argillite, ribbon chert, conglomerate, limestone, and basalt tuff. Trembleur Ultramafite unit of the Cache Creek Complex, in places part of an ophiolite suite, forms thrust sheets and klippen that overlie lower Mesozoic sedimentary rocks. Sedimentological, lithochemical, paleontological, petrological, and textural comparisons with other areas and established models demonstrate that Cache Creek Terrane is an accretionary complex, a structurally stacked assemblage of rocks that originated in diverse and disparate oceanic paleoenvironments. These environments include spreading ridge, oceanic plateau, atoll, trench fill, and possibly arc. Internal imbrication of the terrane is as young as Early Jurassic, as determined from fossil evidence, and the minimum age of obduction of the thrust stack westward onto Stikine Terrane is Middle Jurassic, as determined from dating of a crosscutting pluton. Triassic blueschist and eclogite of Cache Creek Terrane are interpreted to have been primarily uplifted to upper crustal levels during Triassic subduction. Cache Creek Terrane, as a remnant of that subduction process, and caught in the collision between Stikine and Quesnel terranes, marks the position of a lithosphere-scale suture zone, the Pinchi Suture.Les roches océaniques du terrane de Cache Creek (Paléozoïque supérieur à Jurassique inférieur), près de Fort St. James, au centre de la Colombie-Britannique forment un empilement de nappes de charriage recoupé par des failles de décrochement à pendage abrupt. Les strates du Paléozoïque supérieur, datées par la paléontologie, comprennent des calcaires bioclastiques d'eau peu profonde et des cherts rubanés. Les roches du Permien, datées par analyse isotopique, comprennent des filons-couches et des petits intrusifs de tonalite ainsi que des écoulements de rhyolite intercalés avec des écoulements de basaltes. Les roches du Mésozoïque inférieur, datées par la paléontologie, comprennent des grauwackes, des grès, des microgrès, des argilites, des cherts rubanés, des conglomérats, des calcaires et des tufs basaltiques. L'unité ultramafique Trembleur du complexe de Cache Creek, qui à certains endroits fait partie d'une suite ophiolitique, forme des nappes de charriage et des klippes qui reposent sur les roches sédimentaires du Mésozoïque inférieur. Des comparaisons sédimentologiques, lithochimiques, paléontologiques, pétrologiques et texturales avec d'autres régions et avec des modèles établis démontrent que le terrane de Cache Creek est un complexe formé par accrétion, un assemblage de roches empilées structurellement qui proviennent de paléoenvironnements divers et disparates. Ces environnements océaniques comprennent des crêtes qui s'écartent, des plateaux océaniques, des atolls, des remplissages de fosses et possiblement des arcs. Une imbrication interne du terrane s'est effectuée aussi tôt que le Jurassique précoce, tel qu'il a été déterminé par des évidences de fossiles, et l'âge minimum pour l'obduction de l'empilement de charriage vers l'ouest sur le terrane de Stikine serait du Jurassique moyen, tel que déterminé par la datation d'un pluton qui le recoupe. Le schiste bleu et l'éclogite du terrane de Cache Creek (du Trias) sont interprétés comme ayant été principalement soulevés à des niveaux supérieurs de la croûte au cours de la subduction au Trias. Le terrane de Cache Creek, en tant que lambeau de ce processus de subduction pris dans la collision entre les terranes de Stikine et Quesnel, marque la position d'une zone de suture à l'échelle de la lithosphère, soit la suture Pinchi.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2001
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48. Biostratigraphic and biogeographic constraints on the Carboniferous to Jurassic Cache Creek Terrane in central British Columbia.
- Author
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Orchard, M J, Cordey, F, Rui, L, Bamber, E W, Mamet, B, Struik, L C, Sano, H, and Taylor, H J
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CARBONIFEROUS stratigraphic geology ,PALEOZOIC stratigraphic geology ,CONODONTS ,RIVERS - Abstract
Conodonts, radiolarians, foraminiferids, and corals provide constraints on the geology and tectonics of the Nechako region. They also support the notion that the Cache Creek Terrane is allochthonous with respect to the North American craton. The 177 conodont collections, assigned to 20 faunas, range in age from Bashkirian (Late Carboniferous) to Norian (Late Triassic); 70 radiolarian collections representing 12 zones range from Gzhelian (Late Carboniferous) to Toarcian (Early Jurassic); 335 collections assigned to 11 fusulinacean assemblages (with associated foram-algal associations) range from Bashkirian to Wordian (Middle Permian); and two coral faunas are of Bashkirian and Wordian age. The fossils document a long but sporadic history of sedimentary events within the Cache Creek Complex that included two major carbonate buildups in the Late Carboniferous (Pope limestone) and Middle Permian (Copley limestone), punctuated by intervening Early Permian deepening; basaltic eruptions during the mid Carboniferous and mid Permian; the onset of oceanic chert sedimentation close to the Carboniferous–Permian boundary and its persistence through the Late Triassic (Sowchea succession); latest Permian and Early Triassic mixed clastics and volcanics (Kloch Lake succession); Middle and Late Triassic reworking of carbonates (Whitefish limestone), including cavity fill in older limestones (Necoslie breccia), and fine-grained clastic sedimentation extending into the Early Jurassic (Tezzeron succession). Tethyan, eastern Pacific, and (or) low-latitude biogeographic attributes of the faunas are noted in the Gzhelian (fusulines), Artinskian (conodonts, fusulines), Wordian (fusulines, corals, conodonts), and Ladinian (conodonts, radiolarians). The Cache Creek Terrane lay far to the west of the North American continent during these times.Les conodontes, radiolaires, foraminiféridés et les coraux améliorent les données géologiques et tectoniques de la région de Nechako. Ils appuient aussi la notion que le terrane de Cache Creek est allochtone par rapport au craton nord-américain. Cent soixante-dix-sept collections de conodontes, assignés à 20 faunes, ont des âges allant du Bashkirien (Carbonifère tardif) au Norien (Trias tardif); 70 collections de radiolaires représentant 12 zones vont du Gzelien (Carbonifère tardif) au Toarcien (Jurassique précoce); 335 collections assignées à 11 assemblages de fusulinides (avec des associations foraminifères-algues associées) vont du Bashkirien au Wordien (Permien moyen) et deux faunes coralliennes sont du Bashkirien et du Wordien. Les fossiles enregistrent un historique long mais sporadique d'événements sédimentaires à l'intérieur du complexe de Cache Creek qui comprend deux grandes formation carbonatées au Carbonifère tardif (calcaire Pope) et au Permien moyen (calcaire Copley) ponctuées par un nouvel approfondissement au Permien précoce; des éruptions basaltiques au cours du Carbonifère moyen et du Permien moyen; le déclenchement de la sédimentation océanique de chert près de la limite Carbonifère–Permien et sa persistance à travers le Trias tardif (séquence de Sowchea); des mélanges de clastiques et de volcaniques au Permien terminal et au Trias précoce (séquence de Kloch Lake); le remaniement des carbonates (calcaire de Whitefish) au Trias moyen et tardif, comprenant le remplissage de cavités dans des calcaires plus âgés (brèche de Necoslie) et une sédimentation clastique à grains fins se poursuivant jusqu'au Jurassique précoce (séquence de Tezzeron). Des attributs biogéographiques du genre téthysien, de l'est du Pacifique et (ou) de basse latitude, sont notés dans les faunes du Gzelien (Fusulines) de l'Artinskien (conodontes, fusulines), du Wordien (fusulines, coraux, conodontes) et du Ladinien (conodontes, radiolaires). Le terrane de Cache Creek était potentillement très éloigné à l'ouest du continent nord-américain durant ces époques.[Traduit par la Rédaction] [ABSTRACT FROM AUTHOR]
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- 2001
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49. Discussion of "Smoothed particle hydrodynamics hybrid model of ice-jam formation and release".
- Author
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Beltaos, Spyros
- Subjects
INTERNAL friction ,ICE formation & growth ,HYDRODYNAMICS ,SEDIMENTATION analysis ,RIVERS - Abstract
The article discusses several inconsistencies in the treatment of the angle of internal friction in the modelling of dynamic ice-jam processes. It highlights the laboratory test conducted by researchers G. W. Timco and A. M. Cornett to eliminate uncertainties and errors arising from limitations of the study "Ice and sedimentation processes in the Saint John River, Canada." It is concluded that the findings concerning the spatial variability of the angle of internal friction is tenuous.
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- 2010
- Full Text
- View/download PDF
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