Historical Research
Bob Carlson (University of Georgia)
Under the guidance of Dr. Aaron Fisk and Dr. James Peterson of the University of Georgia, USA, I am assessing the delivery of nutrients and contaminants to Quesnel Lake via sockeye salmon for my undergraduate thesis. With the help of the Quesnel River Research Centre (QRRC) staff and the Canadian government, I was permitted to sample in the fall of 2005. The knowledge the QRRC staff possess pertaining to the catchment area was an intricate part in making my study a success. In this pilot study, I sampled sockeye (Oncorhynchus nerka), lake trout (Salvelinus namaycush), rainbow trout (Oncorhynchus mykiss), mountain whitefish (Prosopium williamsoni), burbot (Lota Lota), and forage fishes.
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Filippo Ferri, Trygve Höy and Richard M. Friedman
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C.J.N Fletcher and HJ Greenwood (University of British Columbia)
The Quesnel Lake area lies within the Omineca Crystalline Belt, and is underlain by the northern extremity of the Shuswap Metamorphic Complex. Closely spaced and steeply dipping isograds mark the margins of the metamorphic belt. In the Penfold Creek area only one and one-half miles separate the biotite and sillimanite isograds. Related to this sharp increase in metamorphic grade there is a marked change in the fold style. In the chlorite zone are similar folds, showing a strong axial-plane cleavage, and tight refolded isoclines dominate in the sillimanite zone. Three periods of deformation and two periods of prograde metamorphism have been recognized, with the first metamorphic period being associated with Phase 2 deformation and the second being post-Phase 2.
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Hume, Jeremy, Ken Shortreed, and Timber Whitehouse
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J. Lu(Visiting Scholar, Ministry of Metallurgical Industry, China)
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Melling DR, D. H. Watkinson, P. E. Fox and R. S. Cameron
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Melling, DR and David H. Watkinson
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Valhalla Wilderness Watch
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Bloodgood, Mary Anne (UBC MSc Program Geological Science)