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Relevant bibliographies by topics / Bathurst Island

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Academic literature on the topic 'Bathurst Island'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "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 (December 17, 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. We examined caribou distribution and composition mapped during nine systematic aerial surveys (1961–2013), unsystematic helicopter surveys (1989–98), and limited radio-collaring from 1994–97 and 2003–06. While migration patterns changed and use of southern Bathurst Island decreased during lows in abundance, use of satellite islands, especially Cameron Island for winter range, persisted during both highs and lows in abundance. The northeast coast of Bathurst Island was used to a greater extent during the rut and during summer at low abundance. We suggest that Park boundaries which include Cameron Island and the northeast coast of Bathurst Island will be more effective in contributing to the persistence of Peary caribou on the Bathurst Island Complex.

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2

Kotyk, Michele E., and James F. Basinger. "The Early Devonian (Pragian) zosterophyll Bathurstia denticulata Hueber." Canadian Journal of Botany 78, no. 2 (April 7, 2000): 193–207. http://dx.doi.org/10.1139/b99-179.

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Approximately 86 specimens of Bathurstia denticulata Hueber were collected from upper Bathurst Island and lower Stuart Bay beds of Bathurst Island, Canadian Arctic Archipelago. Bathurstia was a component of a zosterophyll-dominated flora of Pragian age (Lower Devonian) that existed at low paleolatitudes in northern Canada. The large collection of well-preserved materials permits reconstruction of the plant as a robust scrambler of about 30 cm in height. Stems bear short, shelf-like emergences in two rows, and branch isotomously, although sparsely. Rooting organs, representing some of the oldest known for land plants, arise from the main aerial axes, although they are also associated with small, subordinate shoots interpreted as plantlets. Numerous specimens are fertile, with sporangia borne in dense terminal spikes. Spikes include two rows of overlapping, discoid sporangia. Isospores are round and featureless, and assignable to the genus Calamospora. While Bathurstia apparently originated from among the isotomously branching bilaterally symmetrical zosterophylls, the phylogenetic relationships of Bathurstia to known taxa is unclear, although some resemblance to Serrulacaulis, Barinophytaceae, and the Gosslingiaceae can be documented. Bathurstia denticulata is now one of the best known of early land plants, and contributes significantly to our understanding of zosterophylls and their role in Early Devonian vegetation.Key words: Bathurstia, zosterophyll, Devonian, Canada, Arctic, evolution.

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3

Miller, Frank L., and Samuel J. Barry. "Single-island home range use by four female Peary caribou, Bathurst Island, Canadian High Arctic, 1993-94." Rangifer 23, no. 5 (April 1, 2003): 267. http://dx.doi.org/10.7557/2.23.5.1710.

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Spatial and temporal use of seasonal, and collectively, annual ranges by four female Peary caribou (Rangifer taran-dus pearyi) was investigated using satellite telemetry. Knowledge of how caribou use space allows a better understanding of their demands on those ranges and enhances evaluation of associated environmental stressors. The study took place during an environmentally favorable caribou-year with high reproduction and calf survival and low (none detected) 1+ yr-old mortality, 1 August 1993 to 31 July 1994, Bathurst Island, south-central Queen Elizabeth Islands, Canadian High Arctic. All four females exhibited a pattern of single-island seasonal, and collectively, annual range use. Estimates of the maximum area encompassed by each individual during the course of the annual-cycle varied from 1735 to 2844 km2 (mean±SE = 2284±250 km2). Although, there was 46% spatial overlap among individual ranges, temporal isolation resulted in the four individuals maintaining seasonal ranges distinctly separate from each other. This collective area encompassed 4970 km2 and equaled about 31% and 18% of Bathurst Island and the Bathurst Island complex, respectively. Individual wintering areas formed a relatively small portion of each individual's annual range (mean±SE=71±17 km2): 24 km2, 158 days of occupation, <1% of the annual area; 70 km2, 187 days, 4%; 95 km2, 200 days, 4%; and 94 km2, 172 days, 6%. Seasonal movements were greatest during pre-rut and pre-calving.

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4

Fjellberg, Arne. "Collembola of the Canadian high arctic. Review and additional records." Canadian Journal of Zoology 64, no. 10 (October 1, 1986): 2386–90. http://dx.doi.org/10.1139/z86-355.

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A revised list of species from the Queen Elizabeth Islands is given, including new records from Ellesmere, Devon, Cornwallis, Bathurst, King Christian, and Ellef Ringnes islands. Fifty species are reported (43 named and 7 unnamed), with the highest number from Ellesmere Island (41). About 75% of the species in the area have a circumpolar or holarctic distribution.

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5

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 (December 1, 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. Mixing is more common among grains of coarse silt to fine sand than in the >250 µm fraction, but even the latter contains debris from sources far apart. During the Late Wisconsinan, the northern, southern, and eastern Queen Elizabeth Islands were covered by glaciers flowing radially from ice centers on the islands into the inter-island channels. Queens Channel was completely filled by ice, and a glacier lobe moved north from an ice divide northwest of Devon Island to Peary Channel. This lobe redistributed crystalline and carbonate erratics that are derived in part from a strongly weathered and degraded till that was deposited by a pre-Late Wisconsinan glaciation, and in part from glacial erratics that were deposited below the marine limit by icebergs during the Late Wisconsin deglaciation. Tills from eastern Bathurst Island are locally derived and devoid of erratics, but submarine tills west of Bathurst Island contain crystalline erratics that could be from either the Canadian Shield or Victoria Island.

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6

Young, Kathy L., Melissa J. Lafrenière, Scott F. Lamoureux, Anna Abnizova, and Elizabeth A. Miller. "Recent multi-year streamflow regimes and water budgets of hillslope catchments in the Canadian High Arctic: evaluation and comparison to other small Arctic watershed studies." Hydrology Research 46, no. 4 (August 12, 2014): 533–50. http://dx.doi.org/10.2166/nh.2014.004.

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This study evaluates whether a recent decline in snowcover extent for circumpolar regions is matched by changes in the seasonal streamflow regime of several small hillslope catchments on Bathurst and Melville Islands. This includes shifts in the timing of initiation, peak discharge and impacts on the spring–summer water budgets. Paired catchments (West and East) at the Cape Bounty Arctic Watershed Observatory (CBAWO) on Melville Island (74.9°N, 109.5°W) have been studied from the pre-snowmelt season to early August since 2003. They are low-rolling tundra catchments between 8.0 and 11.6 km2 in area. Likewise, within the Polar Bear Pass (PBP) watershed, Bathurst Island (75.7°N 98.7°W), two hillslope basins, Windy Creek (4.2 km2) and Landing Strip Creek (0.2 km2) have been investigated since 2007. Detailed snow surveys were conducted each spring and streamflow estimates were made using the mid-section velocity method. Nival regimes continue to dominate in these basins but runoff ratios are variable between catchments, across islands, and from year-to-year. In comparison to earlier streamflow studies across the Queen Elizabeth Islands (QEIs), an earlier response to peak discharge and start of flow for these hillslope streams is confirmed. Water budgets for PBP, CBAWO differ from other small Arctic watersheds.

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7

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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8

Anderson, Morgan. "Trends in high arctic muskox (Ovibos moschatus) harvest, 1990-2015." Rangifer 37, no. 1 (July 27, 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 1990s. We compared muskox harvest from tag records and reported harvest, i.e., the voluntary surveys to the Nunavut Wildlife Harvest Study for muskoxen. It is clear that voluntarily reported harvest underestimates actual harvest, but not consistently enough to predict the actual harvest. Muskox populations are at historic high levels on Bathurst Island, southern Ellesmere Island, and Devon Island and could support more harvest than is currently taken. Changes to Total Allowable Harvests and management unit boundaries in 2015, combined with a decline in the availability of Baffin Island caribou as country food, may result in increased harvest pressure on muskoxen in the High Arctic.

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Ferguson, Michael A. D. "Status and trends of Rangifer tarandus and Ovibos moschatus populations in Canada." Rangifer 12, no. 3 (October 1, 1992): 127. http://dx.doi.org/10.7557/2.12.3.1017.

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We identified 97 Rangifer tarandus and 17 Ovibos moschatus populations in Canada. In July 1991, the Canadian populations totalled 1.9 to 2.6 million caribou, 13 600 reindeer and 108 600 muskoxen. Seven barren-ground caribou populations contributed about 75% to Canada's total number of caribou. Most population trends of these barren-ground caribou had shiftet from increasing in the early 1980s to stable or decreasing in the late 1980s. The George River herd of Quebec and Labrador has been decreasing since 1987, but remains the largest Canadian caribou population. The ecological factors driving barren-ground caribou population dynamics are not well understood. Arctic islands caribou are about 17% of all Canadian caribou. Over 60% of Arctic islands caribou occurred on Baffin Island. Most Arctic islands populations were decreasing with the exceptions of Southampton, Bathurst, Victoria and Baffin islands. Movements within and between islands are not well understood, and probably limit the usefulness of small surveys for indicating long-term trends of Arctic islands caribou populations. Woodland caribou form about 7% of all Canadian caribou, with about 40% of these occurring on the island of Newfoundland. Most Canadian woodland caribou have not been well studied or censused. In many areas, they were faced with an increasing rate of habitat loss. Exceptions included: some eastern Yukon populations and most Newfoundland populations which were increasing. Over 70% of the Canadian muskox population occurred on Banks and Victoria islands. Almost all muskox populations were increasing, especially those on Banks, Victoria, Melville and Bathurst islands. Muskoxen on the mainland Northwest Territories are re-colonizing southern portions of their historical distribution.

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West, B. G., and V. L. Passmore. "HYDROCARBON POTENTIAL OF THE BATHURST ISLAND GROUP, NORTHEAST BONAPARTE BASIN, IMPLICATIONS FOR FUTURE EXPLORATION." APPEA Journal 34, no. 1 (1994): 626. http://dx.doi.org/10.1071/aj93048.

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Despite 20 years of exploration between 1965 and 1992 in the northeastern part of the Bonaparte Basin, the region remains underexplored. Exploration has produced modest encouragement. The seven wells drilled in the area totalling more than 70 000 km2 include one dry gas and two gas/condensate discoveries. Explorers have targeted the Jurassic Plover Formation and Flamingo Group, but reservoir quality has often been poor in both units due largely to depth of burial.Recent regional studies of the northeastern part of the Bonaparte Basin, undertaken by the Bureau of Resource Sciences, indicate there is potential for generation and entrapment of hydrocarbons in the Cretaceous Bathurst Island Group. Geochemical results show the lower Bathurst Island Group contains good source rocks that are largely gas prone, but have the potential to charge large Cretaceous traps. Geohistory modelling suggests that the Bathurst Island Group may have entered the oil window around the Middle Cretaceous, after most of the structuring had occurred, and continued until the Middle Miocene or later. Potential reservoirs have been identified in Santonian, Campanian and Maastrichtian sands, and in fractured Albian Carbonates.Recent reports have predicted that by early next century there will be a significant increase in natural gas consumption in Australia, due to increased use for power generation and transportation, as well as further sales to the Asian market. New methanol technology could commercialise some marginal gas fields. The theme for this years APEA conference is `New Age—New Opportunities'. The Bonaparte Basin may provide the opportunity to explore for and develop new gas accumulations.

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Dissertations / Theses on the topic "Bathurst Island"

1

Lim, Darlene S. S. "An examination of the limnology and freshwater diatom autoecology of Bathurst Island, Northwest Territories, Canadian High Arctic." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0001/MQ45525.pdf.

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2

Campbell, Robert John. "Calcareous nannofossil and foraminiferal analysis of the middle to upper cretaceous Bathurst Island Group, Northern Bonaparte Basin and Darwin Shelf, Northern Australia." University of Western Australia. School of Earth and Geographical Sciences, 2003. http://theses.library.uwa.edu.au/adt-WU2003.0025.

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[Truncated abstract] The Northern Bonaparte Basin and adjacent Darwin Shelf form part of a major petroleum province on the northwestern margin of Australia. The middle to Late Cretaceous Bathurst Island Group consists of siliciclastic and pelagic carbonate strata that form the regional seal to underlying Upper Jurassic and Lower Cretaceous reservoir sandstones. The Bathurst Island Group has previously been subdivided into four stratigraphic sequences or ‘play intervals’ bound by regional disconformities in the Valanginian (KV horizon), Lower Aptian (KA horizon), upper Lower Cenomanian (KC horizon), Middle Campanian (KSC horizon), and at the CretaceousPaleocene boundary (T horizon). Correlation of these sedimentary packages and stratigraphic surfaces requires high-resolution calcareous microfossil biostratigraphy, while palaeobathymetric determinations based on benthonic foraminiferal assemblages are important for determining the subsidence history of the area and relative sea-level changes. This study presents the first detailed stratigraphic distributions, taxonomic lists and illustrations of foraminifera and calcareous nannofossils from the Bathurst Island Group of the Northern Bonaparte Basin and Darwin Shelf. A biostratigraphic framework has been constructed for the study area incorporating ‘standard’ (Tethyan) Cretaceous planktonic foraminiferal and calcareous nannofossil events where applicable, and integrating locally defined events where necessary. This framework allows Cretaceous strata to be correlated regionally across the study area and to the global chronostratigraphic scale. Correlation of the Northern Bonaparte Basin and Darwin Shelf strata to the Cretaceous Stages and international time scale is based on recent ties of nannofossil and foraminiferal events to macrofossil zones and palaeomagnetic polarity chrons at ratified and proposed Global Stratotype Sections and Points (GSSPs). Calcareous nannofossil events recorded in the study area that are critical for defining stage boundaries include the lowest occurrences of Prediscosphaera columnata, Micula decussata, Lithastrinus grillii, and Aspidolithus parcus parcus, and the highest occurrences of Helenea chiastia, Lithastrinus moratus, Aspidolithus parcus constrictus, and Eiffellithus eximius. Important planktonic foraminiferal events for correlation include the lowest occurrences of Rotalipora gr. globotruncanoides, and Dicarinella asymetrica, and the highest occurrences of Planomalina buxtorfi, Rotalipora cushmani, and Dicarinella asymetrica. During the middle to Late Cretaceous the Northern Bonaparte Basin and Darwin Shelf occupied mid-high palaeolatitudes between 35ºS to 45ºS. These palaeolatitudes are reflected in the transitional character of the planktonic microfossil assemblages, which combine elements of the low-latitude, warm-water Tethyan Province to the north and the cool-water high-latitude Austral Province to the south. ‘Standard’ Tethyan zonations are most applicable for uppermost AlbianMiddle Campanian strata because equator-to-pole temperature gradients were weakly developed, and global climate was warm and equable during this interval. These conditions resulted in broad latitudinal distributions for Tethyan marker species, and consequently most UC calcareous nannofossil zones and European-Mediterranean planktonic foraminiferal zones are recognised. In contrast, the EarlyLate Albian and the late Middle CampanianMaastrichtian were intervals of greater bioprovinciality and stronger palaeotemperature gradients. In these intervals application of the Tethyan zonations is more difficult, and a number of the Tethyan biostratigraphic markers are absent from the study area (e.g. Ticinella species in the Albian and Radotruncana calcarata in the Late Campanian). Cretaceous palaeobathymetric reconstruction of the study area is based on comparison of the foraminiferal assemblages with those of previous Cretaceous palaeobathymetric studies. Marginal marine assemblages consist solely of low diversity siliceous agglutinated foraminifera (e.g. Trochammina). Inner and middle neritic water depths (0-100 m) contain rare to common planktonic foraminifera (mainly globigerine forms), robertinids (e.g. Epistomina), siliceous agglutinates, lagenids, buliminids (e.g. Neobulimina), and rotaliids. The outer neritic zone (100-200 m water depth) contains abundant planktonic foraminifera (keeled and globigerine), calcareous agglutinates (e.g. Dorothia), and diverse lagenids, buliminids, and rotaliids. Upper-middle bathyal water depths (200-1000 m) are characterised by abundant planktonic foraminifera, common siliceous agglutinated taxa (e.g. Glomospira), rare to common Osangularia, and globular species of Gyroidinoides, Pullenia, and Paralabamina.

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3

Rose, Scott Richard Andrew. "Sedimentology and diagenesis of the lower blue fiord formation carbonates in a prospective Mississippi Valley-type (Pb-Zn) setting, Bathurst Island, Northwest Territories." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ38607.pdf.

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Books on the topic "Bathurst Island"

1

Miller, Frank L. Peary caribou conservation studies, Bathurst Island complex, Northwest Territories, July-August 1993. Edmonton, Alta: Canadian Wildlife Service, Prairie and Northern Region, 1995.

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2

Miller, Frank L. Peary caribou conservation studies, Bathurst Island Complex, Northwest Territories, April-August 1994 and June-July 1995. Edmonton: Canadian Wildlife Service, 1997.

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3

Rachebœuf, Patrick. Upper Lower and Lower Middle Devonian chonetacean brachiopods from Bathurst, Devon, and Ellesmere Islands, Canadian Arctic Archipelago. Ottawa, Canada: Geological Survey of Canada, 1987.

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4

Evans, Nicholas. Polysynthesis in Northern Australia. Edited by Michael Fortescue, Marianne Mithun, and Nicholas Evans. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199683208.013.19.

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This chapter surveys the polysynthetic languages of northern Australia, across four families in three non-contiguous regions: Gunwinyguan (Arnhem Land), Tiwi (Bathurst and Melville Islands), and Southern and Western Daly (Daly River). All are non-Pama-Nyungan. It contextualizes the more detailed treatments of Dalabon (Ch. 43), Southern and Western Daly (Ch. 44), and the acquisition of Murrinh-patha (Ch. 26) by bringing out the typological similarities and differences in polysynthetic languages, with a particular focus on pathways of change between more and less polysynthetic structures. Australian polysynthetic languages exhibit little morphological fusion, and all are basically templatic. However, there are significant differences in noun and verb incorporation, applicatives and other valency-changing operations, and the degree of subordinating morphology, illustrated by comparing the closely related Dalabon and Bininj Gun-wok. Perhaps the biggest difference is the presence of a bipartite structure in the Southern Daly languages. The chapter closes by surveying the main trajectories by which morphological complexity increases or diminishes in the languages of northern Australia.

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5

Lim, Darlene S. S. Examination of the limnoloogy and Freshwater Diatom Autoecology of Bathust Islands, N. W. T., Canadian High Arctic. 1999.

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6

Rachebeuf, Patrick. Upper Lower and Lower Middle Devonian chonetacean brachiopods from Bathurst, Devon, and Ellesmere Islands, Canadian Arctic Archipelago (Bulletin / Geological Survey of Canada). Canadian Govt. Pub. Centre, Supply and Services [distributor], 1987.

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Observations on the government, trade, fisheries, and agriculture of Newfoundland: In a series of letters addressed to the Right Honourable the Earl Bathurst, His Majesty's principal secretary of state for the colonies : by an inhabitant of the colony : with an appendix containing a report on the state of the island, addressed to his lordship by the committee of the inhabitants of St. John's, and also a statement of the revenues arising from the customs and crown rents. London: W. Simkin, R. Marshall, J. Bigg, 1987.

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Book chapters on the topic "Bathurst Island"

1

Lamoureux, Scott F., and Ashley C. A. Rudy. "Melville, Bathurst, and Cornwallis Islands: Low to Moderate Relief Innuitia." In World Geomorphological Landscapes, 315–32. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35137-3_14.

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Venbrux, Eric. "Communicating with the Dead in an Australian Aboriginal Culture: The Tiwi from Melville and Bathurst Islands." In Death Across Cultures, 317–33. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-18826-9_19.

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Reports on the topic "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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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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McCann, S. B. Coastal Geology Maps, Northwest Devon Island and Northeast Bathurst Island, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130636.

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Harrison, J. C. Parry Islands and Cornwallis fold belts in the Bathurst Island region, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/299549.

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Edlund, S. A. Surficial Materials, Bathurst Island area and Byam Martin Island, District of Franklin, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130057.

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Bednarski, J. M. Surficial geology and sea level history of Bathurst Island, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207432.

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7

Basinger, J. F., M. E. Kotyk, and P. G. Gensel. Early land plants from the Late Silurian-Early Devonian of Bathurst Island, Canadian Arctic Archipelago. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207431.

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8

Budkewitsch, P., M. A. D'Iorio, and J. C. Harrison. C-band radar signatures of lithology in arctic environments: preliminary results from Bathurst Island, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207433.

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Harrison, J. C., T. De Freitas, and R. Thorsteinsson. New field observations on the geology of Bathurst Island, Arctic Canada: part B, structure and tectonic history. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/134218.

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10

Anglin, C. D., and J. C. Harrison. Mineral and energy resource assessment of Bathurst Island area, Nunavut (parts of NTS 68G, 68H, 69A, 69B and 79A). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210386.

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