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Relevant bibliographies by topics / Geology - Nunavut - Bathurst Island

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Academic literature on the topic 'Geology - Nunavut - Bathurst Island'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 July 2025

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Journal articles on the topic "Geology - Nunavut - Bathurst Island"

1

Poole, Kim G., Anne Gunn, Jack Wierzchowski, and Morgan Anderson. "Peary caribou distribution within the Bathurst Island Complex relative to the boundary proposed for Qausuittuq National Park, Nunavut." Rangifer 35, no. 2 (2015): 81. http://dx.doi.org/10.7557/2.35.2.3635.

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How caribou (Rangifer tarandus), including Peary caribou (R. t. pearyi), use their annual ranges varies with changes in abundance. While fidelity to some seasonal ranges is persistent, use of other areas changes. Consequently, understanding changes in seasonal distribution is useful for designing boundaries of protected areas for caribou conservation. A case in point is the proposed Qausuittuq (Northern Bathurst Island) National Park for Bathurst Island and its satellite islands in the High Arctic of Canada. Since 1961, Peary caribou have been through three periods of high and low abundance. W

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2

Harrison, Christopher. "Intersecting fold belts in the Bathurst Island region, Nunavut." Journal of Geodynamics 118 (July 2018): 82–105. http://dx.doi.org/10.1016/j.jog.2017.11.003.

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3

Anderson, Morgan. "Trends in high arctic muskox (Ovibos moschatus) harvest, 1990-2015." Rangifer 37, no. 1 (2017): 47–58. http://dx.doi.org/10.7557/2.37.1.4182.

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Harvest reporting has been in place for High Arctic muskoxen in Nunavut, Canada, since 1990-91. The communities of Resolute, Grise Fiord, and Arctic Bay harvest muskoxen in the region. Overall, muskox harvest has declined in Resolute and Grise Fiord since the 1990s. The recovery of Peary caribou populations on the Bathurst Island Complex, which provides an alternate preferred source of country food, may be a factor behind Resolute’s decreased muskox harvest. The proportion of harvest for domestic use has also declined relative to sport hunts, which have remained relatively constant since the 1

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4

Young, Kathy L., Laura Brown, and Claude Labine. "Snow cover variability at Polar Bear Pass, Nunavut." Arctic Science 4, no. 4 (2018): 669–90. http://dx.doi.org/10.1139/as-2017-0016.

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Information on arctic snow covers is relevant for climate and hydrology studies and investigations into the sustainability of both arctic fauna and flora. This study aims to (1) highlight the variability of snow cover at Polar Bear Pass (PBP) at a range of scales: point, local, and regional using both in situ snow cover measurements and remote sensing imagery products; and (2) consider how snow cover at PBP might change in the future. Terrain-based snow surveys documented the end-of-winter snowpacks over several seasons (2008–2010, 2012–2013), and snowmelt was measured daily at typical terrain

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5

Nelson, R. John, Kelly V. Young, and William J. Williams. "Marine zooplankton of Coronation Gulf and Bathurst Inlet, Nunavut, Canada." Continental Shelf Research 191 (December 2019): 104003. http://dx.doi.org/10.1016/j.csr.2019.104003.

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6

Namayandeh, Armin, and David V. Beresford. "A new species in the Rheocricotopus (R.) effusus group from Canada with a review of the Nearctic species of Rheocricotopus and Parametriocnemus (Chironomidae: Orthocladiinae)." CHIRONOMUS Journal of Chironomidae Research, no. 31 (December 27, 2018): 16–29. http://dx.doi.org/10.5324/cjcr.v0i31.2531.

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Rheocricotopus (Rheocricotopus) reduncusoides sp. n. is described from Bathurst Island, Nunavut, Canada. Its discovery was made while curating and examining specimens deposited by H. V. Danks in 1969 at the Canadian National Collection in Ottawa, Canada. We also report the first Canadian record of Parametriocnemus hamatus (Johannsen, 1934) from Québec, based on previously unsorted material deposited at the Canadian National Collection. In this paper we provide distributional records of the Nearctic species of Rheocricotopus Thienemann and Harnisch and Parametriocnemus Goetghebuer, and present

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7

Bischof, Jens F., and Dennis A. Darby. "Quaternary ice transport in the Canadian Arctic and extent of Late Wisconsinan Glaciation in the Queen Elizabeth Islands." Canadian Journal of Earth Sciences 36, no. 12 (1999): 2007–22. http://dx.doi.org/10.1139/e99-096.

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Most of the ice-rafted debris in channels off the Queen Elizabeth Islands, Nunavut, is of local origin, particularly in the inner part of the archipelago, but samples from the Arctic shelf contain as much as 40% grains from sources as far away as 2000 km, including the Siberian shelves. Particle transport by drifting sea ice from distant shelves is an important process on the Arctic continental shelf of the Queen Elizabeth Islands. In the interior of the Queen Elizabeth Islands and in the Viscount Melville and Lancaster sounds, particle transport is limited to distances of approximately 200 km

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8

Young, Kathy L., and Claude Labine. "Summer hydroclimatology of an extensive low-gradient wetland: Polar Bear Pass, Bathurst Island, Nunavut, Canada." Hydrology Research 41, no. 6 (2010): 492–502. http://dx.doi.org/10.2166/nh.2010.219.

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Polar Bear Pass (PBP) (75°40′N, 98°30′W) is considered a critical wetland area for migratory birds, caribou and muskox. Little is known of its climatology and hydrology. Here we evaluate both the short-term and long-term summer climatic record for this wetland. A 10 m high automatic weather station (AWS) was established here 27 years ago, and in 2007 this centrally located AWS was supplemented by three more weather stations placed across the wetland pass. The long-term climate record here indicates little significant departure when compared to the long-term climate means (1971–2005) at Resolut

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9

Young, Kathy L., Jane Assini, Anna Abnizova, and Elizabeth A. Miller. "Snowcover and melt characteristics of upland/lowland terrain: Polar Bear Pass, Bathurst Island, Nunavut, Canada." Hydrology Research 44, no. 1 (2012): 2–20. http://dx.doi.org/10.2166/nh.2012.083.

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The seasonal snowcover and snowmelt (2008–2010) of an extensive low-gradient wetland at Polar Bear Pass, Bathurst Island, Nunavut, Canada (75°40′ N, 98°30′ W) was examined. This wildlife sanctuary is characterized by two large lakes and numerous tundra ponds, and is bordered by rolling hills with incised hillslope stream valleys. In arctic environments snow remains one of the most important sources of water for wetlands. End-of-winter snowcover measurements (snow depth, density, water equivalent) together with direct and modeled estimates of snowmelt provided an assessment of the seasonal snow

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10

Abnizova, Anna, Kathy L. Young, and Melissa J. Lafrenière. "Pond hydrology and dissolved carbon dynamics at Polar Bear Pass wetland, Bathurst Island, Nunavut, Canada." Ecohydrology 7, no. 1 (2012): 73–90. http://dx.doi.org/10.1002/eco.1323.

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Dissertations / Theses on the topic "Geology - Nunavut - Bathurst Island"

1

Copeland, David A. "The structural and metamorphic geology of Big Island, southwest Baffin Island, Nunavut Territory, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0002/MQ46458.pdf.

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2

Courtney, Mustaphi Colin John. "Analysis of laminated sediments from Lake DV09, northern Devon Island, Nunavut, Canada." Thesis, University of Ottawa (Canada), 2009. http://hdl.handle.net/10393/28123.

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A 147cm sediment core from Lake DV09, northern Devon Island, Nunavut, Canada (75° 34'34"N, 89° 18'55"W) contains annually-laminated (varved) sediments, providing a 1600-year record of climate variability. A minerogenic lamina deposited during the annual thaw period and a thin deposit of organic matter deposited during the summer and through the winter, together form a clastic-organic couplet each year. The thinnest varves occur from AD800-1050, and the thickest from AD1100-1300, during the Medieval Warm Period. The relative sediment density is also highest during this period suggesting

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3

McDonald, Juliet Carleton University Dissertation Geology. "Palynology of the triporate pollen and paleoecology of the tertiary fossil forests of eastern Axel Heiberg Island, N.W.T., Canada." Ottawa, 1992.

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4

Lewis, Edward. "Normal and extreme sedimentation and physical processes in Lake Tuborg, Ellesmere Island, Nunavut." 2009. https://scholarworks.umass.edu/dissertations/AAI3379980.

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Lake Tuborg is a large lake on west-central Ellesmere Island, Nunavut. Part of the lake is meromictic, and contains trapped saltwater below about 55 m depth. The lake receives meltwater and sediments from multiple sources, including snowmelt and glacier melt. A lake process study was undertaken from 2001-2003 at Lake Tuborg that involved obtaining profiles of water temperature, salinity, transmissivity, and dissolved oxygen. Networks of short and long sediment cores were also obtained throughout the lake. During the last year of monitoring the lake and its sediments, a large catastrophic drain

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5

"Geology of the Qaqqanituaq Area and mafic and ultramafic geochemistry of the Hall Peninsula, Baffin Island, Nunavut." Thesis, 2014. http://hdl.handle.net/10388/ETD-2014-12-1887.

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Recent regional bedrock mapping carried out on the Hall Peninsula, Baffin Island, Nunavut has revealed previously unknown rock units, structural relationships and metamorphic conditions achieved. Mafic and ultramafic rocks occur primarily intercalated with metasedimentary rocks in the east-central region of the Hall Peninsula. Focused mapping was carried out in the Quaqqanituaq Area (QA), now the type locality for metasedimentary-mafic/ultramafic occurrences on the Hall Peninsula. The QA records an east-west compression event, D1, which produced in the dominant regional S1 fabric and tight,

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6

Cook, Timothy. "Climate and environmental change in Arctic Canada: Observations from Upper and Lower Murray Lakes, Ellesmere Island, Nunavut." 2009. https://scholarworks.umass.edu/dissertations/AAI3379950.

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This study was designed with the overriding goal of improving our understanding of the nature, causes, and impacts of past climatic conditions in the High Arctic and to evaluate the potential impacts of future climatic warming. Specifically, the focus of this project was centered on Upper and Lower Murray Lakes (81° 21' N, 69° 32' W) on northern Ellesmere Island, Nunavut, Canada. Sediment cores were collected from each of the lakes in order to reconstruct past climate and environmental variability and space-borne synthetic aperture radar (SAR) data were used to evaluate recent variability in t

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7

Hooper, James Matthew. "Late quaternary glacial and sea level history of the Bernier Bay area, northwestern Baffin Island, N.W.T. /." 1990. http://collections.mun.ca/u?/theses,109545.

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Books on the topic "Geology - Nunavut - Bathurst Island"

1

Jackson, G. D. Geology of the Clyde-Cockburn Land map area, north-central Baffin Island, Nunavut. Geological Survey of Canada, 2000.

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2

Canada, Geological Survey of. Geology and paleontology of the southeast Arctic platform and southern Baffin Island, Nunavut. Edited by McCracken Alexander D and Bolton Thomas Elwood 1924-. Geological Survey of Canada, 2000.

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3

Canada. Natural Resources Canada. Geological Survey. Geology and paleontology of the Southeast Arctic Platform and Southern Baffin Island, Nunavut. Natural Resources Canada., 2000.

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Reports on the topic "Geology - Nunavut - Bathurst Island"

1

Bednarski, J. Surficial geology, northeast Bathurst Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213750.

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2

Harrison, J. C., and T. de Freitas. Bedrock geology, Bathurst Island Group (NTS 68G, 68H, 69A, 69B; small parts of 78H and 79A), District of Franklin (Nunavut), Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209408.

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3

Bednarski, J. M. Deglaciation of Bathurst Island Group, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214279.

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4

Dyke, A. S. Surficial geology, Elder Island, Baffin Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215639.

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5

Kerr, D. E., V. N. Rampton, and R. D. Thomas. Surficial geology, Hepburn Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/221204.

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6

Dyke, A. S., and J. M. Savelle. Surficial geology, Koch Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/223035.

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7

Dyke, A. S., and J. M. Savelle. Surficial geology, Rowley Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/223037.

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8

St-Onge, M. R., D. J. Scott, and D. Corrigan. Geology, central Baffin Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212237.

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9

St-Onge, M. R., D. J. Scott, and D. Corrigan. Geology, north Tweedsmuir Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213224.

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10

Sanborn-Barrie, M., M. Young, and J. B. Whalen. Geology, Qikiqtarjuaq, Baffin Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292016.

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