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Relevant bibliographies by topics / Fjords – British Columbia – Jervis Inlet

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Academic literature on the topic 'Fjords – British Columbia – Jervis Inlet'

Author: Grafiati

Published: 4 June 2021

Last updated: 10 February 2022

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Journal articles on the topic "Fjords – British Columbia – Jervis Inlet"

1

Friedman, R. M., J. W. H. Monger, and H. W. Tipper. "Age of the Bowen Island Group, southwestern Coast Mountains, British Columbia." Canadian Journal of Earth Sciences 27, no. 11 (1990): 1456–61. http://dx.doi.org/10.1139/e90-154.

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A new U–Pb date of [Formula: see text] for foliated felsic metavolcanic rocks of the Bowen Island Group, from Mount Elphinstone in the southwesternmost Coast Mountains of British Columbia, indicates that there the age of this hitherto undated unit is early Middle Jurassic. These rocks grade along strike to the north-northwest into a more sedimentary facies, which north of Jervis Inlet contains a probable Sinemurian (Lower Jurassic) ammonite. The Bowen Island Group thus appears to include Lower and Middle Jurassic rocks and to be coeval in part with volcanic rocks of the Bonanza Formation on Va

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2

Wolfe, A. Megan, Susan E. Allen, Michal Hodal, Rich Pawlowicz, Brian P. V. Hunt, and Desiree Tommasi. "Impact of advection loss due to wind and estuarine circulation on the timing of the spring phytoplankton bloom in a fjord." ICES Journal of Marine Science 73, no. 6 (2015): 1589–609. http://dx.doi.org/10.1093/icesjms/fsv151.

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Abstract A coupled biophysical model is used to explore the physical controls involved in the timing of the spring phytoplankton bloom in fjords. Observations from Rivers Inlet, British Columbia, are used to force and evaluate the model. It is found that the interannual variation in timing is due primarily to variations in retention, in particular, to variations in horizontal advection out of the fjord. The two dominant processes are (i) strong outflow winds rapidly advecting the surface layer and thus the phytoplankton population out of the fjord and (ii) losses due to high river flux increas

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3

Morris, Sandra A., and Raymond J. Andersen. "Nitrogenous metabolites from the deep water sponge Hexadella sp." Canadian Journal of Chemistry 67, no. 4 (1989): 677–81. http://dx.doi.org/10.1139/v89-102.

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The secondary metabolites of the sponge Hexadella sp., collected by SCUBA (−40 m) and manned submersible (−100 to −200 m) in Jervis Inlet, British Columbia, have been examined. The submersible-collected material contained only the previously reported compound topsentin B2 (1). Sponge material collected in shallower water via SCUBA contained hexadellins A (2) and B (3), two new dibromotyrosine derived metabolites. The structures of 2 and 3 were determined by spectroscopic analysis of the diacetyl derivatives 6 and 7. Keywords: sponge, metabolite, Hexadella, nitrogenous.

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4

Sutherland, T. F., A. M. Sterling, and M. Ou. "Influence of salmonid aquaculture activities on a rock-cliff epifaunal community in Jervis Inlet, British Columbia." Marine Pollution Bulletin 127 (February 2018): 297–309. http://dx.doi.org/10.1016/j.marpolbul.2017.12.005.

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5

Albright, L. J., S. Johnson, and A. Yousif. "Temporal and Spatial Distribution of the Harmful Diatoms Chaetoceros concavicornis and Chaetoceros convolutus along the British Columbia Coast." Canadian Journal of Fisheries and Aquatic Sciences 49, no. 9 (1992): 1924–31. http://dx.doi.org/10.1139/f92-213.

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The harmful phytoplankters Chaetoceros concavicornis and Chaetoceros convolutus are normal components of the phytoplankton assemblage along the British Columbia coast. During 1988, these diatoms occurred at their highest concentrations in the spring and fall from the Strait of Georgia to Queen Charlotte Strait. North of Queen Charlotte Strait, the maximal concentrations appeared to be delayed until summer. The greatest concentrations occurred in the waters of the Strait of Georgia and its contiguous bays and inlets, especially Jervis Inlet, where concentrations of C. concavicornis and C. convo

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6

Olesiuk, Peter F., Michael A. Bigg, and Graeme M. Ellis. "Recent Trends in the Abundance of Harbour Seals, Phoca vitulina, in British Columbia." Canadian Journal of Fisheries and Aquatic Sciences 47, no. 5 (1990): 992–1003. http://dx.doi.org/10.1139/f90-114.

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Aerial censuses of harbour seals (Phoca vituiina) were conducted in the Strait of Georgia (1966–88), the lower Skeena River (1977–87), off the southwest coast of Vancouver island (1976–87), off the northeast coast of the Queen Charlotte Islands (1986), in Jervis Inlet (1987), and at the entrance to Queen Charlotte Strait (1988). The estimated number of seals in the Strait of Georgia, the primary study area, increased from 2170 in 1973 to 15 810 in 1988; the number in the lower Skeena River from 520 in 1977 to 1590 in 1987; and the number off south western Vancouver Island from 210 in 1976 to 1

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7

Todd, James F., Robert J. Elsinger, and Willard S. Moore. "The distributions of uranium, radium and thorium isotopes in two anoxic fjords: Framvaren Fjord (Norway) and Saanich Inlet (British Columbia)." Marine Chemistry 23, no. 3-4 (1988): 393–415. http://dx.doi.org/10.1016/0304-4203(88)90107-7.

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8

Lewis, T. J., A. M. Jessop, and A. S. Judge. "Heat flux measurements in southwestern British Columbia: the thermal consequences of plate tectonics." Canadian Journal of Earth Sciences 22, no. 9 (1985): 1262–73. http://dx.doi.org/10.1139/e85-131.

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Measured heat fluxes from previously published data and 34 additional boreholes outline the terrestrial heat flow field in southern British Columbia. Combined with heat generation representative of the crust at 10 sites in the Intermontane and Omineca belts, the data define a heat flow province with a reduced heat flow of 63 mW m−2 and a depth scale of 10 km. Such a linear relationship is not found or expected in the Insular Belt and the western half of the Coast Plutonic Complex where low heat fluxes are interpreted to be the result of recent subduction. The apparent boundary between low and

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9

Stocks, Allison P., Evgeny A. Pakhomov, and Brian P. V. Hunt. "A simple method to assess the marine environment residence duration of juvenile sockeye salmon (Oncorhynchus nerka) using laser ablation." Canadian Journal of Fisheries and Aquatic Sciences 71, no. 10 (2014): 1437–46. http://dx.doi.org/10.1139/cjfas-2014-0073.

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Monitoring habitat utilization and early marine growth of sockeye salmon juveniles (Oncorhynchus nerka) in fjords of the Pacific Northwest is currently hampered by difficulties in estimating residence times, limiting scientific advances in certain aspects of this species’ fisheries management and conservation. Combining otolith microchemistry and conventional daily ring counts, we were able to obtain the date of first entry and the residence time of sockeye juveniles in Rivers Inlet, British Columbia. This operationally inexpensive method builds upon variable microelement concentrations in fre

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10

Evans, Ian S. "Climatic Effects on Glacier Distribution Across the Southern Coast Mountains. B.C., Canada." Annals of Glaciology 14 (1990): 58–64. http://dx.doi.org/10.1017/s0260305500008272.

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Over a distance of 150 km inland across British Columbia, glaciation level (altitudinal threshold for glacier generation) rises north-eastward from 1800 m near Jervis Inlet, to 2800m near Lillooet on Fraser River. The methods of Østrem (1966b) are revised for more detailed work from air photographs; inclusion of small but active glaciers gives a glaciation level some 200 m below Østrem’s from 1:250 000 maps, or 110 m below that from 1:50 000 maps. Mountains which rise slightly above the altitudinal threshold invariably support glaciers only on their northerly slopes. Mountain crests need to be

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Books on the topic "Fjords – British Columbia – Jervis Inlet"

1

Phillips, Ray. Royal Fjord: Memories of Jervis Inlet. Harbour Publishing Company, Limited, 2015.

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