Selection of Illustrations

Total Page:16

File Type:pdf, Size:1020Kb

Selection of Illustrations Selection of Illustrations From Harrison, John Christopher. (1991) "Melville Island's salt-based fold belt (Arctic Canada)." Doctoral Thesis, Rice University. http://hdl.handle.net/1911/16447. LIST OF ILLUSTRATIONS Figures 2. Colour satellite mosaic of Melville Island . • . • . 4 3. Map of reflection seismic proflles, wells and structural cross-sections, Mel ville Island . 12 7. Correlation of sonic, density, lithology and various synthetic logs of the logs of the Panarctic et al. Sabine Bay A-07 well with a nearby portion of reflection seismic line P1192 . 29,30 10. Topography and bathymetty of Melville Island-area . 44 11. Bouguer gravity anomaly map of the western Arctic Islands-area . 48 12. Magnetic anomaly map of the western Arctic Islands-area . 50 21. Isopach map of the upper unreflective succession (sP3, sPC) ............. 70 22. Suggested correlation of Precambrian units • • • . • • • • • • • • . • . 75 25. Generalized stratigraphic cross-section of the Franldinian Succession, northern Victoria Island to northwestern Melville Island . 81,82 28. Representative stratigraphy: ?Precambrian to Devonian shelf rim stratigraphy and cover, west central Melville Island . 89 29. Representative lithostratigraphy: ?Precambrian to Devonian intra -shelf basin,·embayment and cover, central Melville Island . 91 30. Representative lithostratigraphy: ?Precambrian to Devonian of the Towson Point Carbonate Build-up and cover, northeastern Melville Island . 93 33. Suggested correlation of ?Cambrian and Lower Ordovician seismic units . 107 34. Correlation chart, Lower Ordovician through Upper Silurian strata . • . 113 41. Correlation chart, Devonian strata of Melville Island . 132 59. Bar graphs of sedimentation rate plotted against time (540-355 Ma) . • . • . 188 60. Isopach map of ?Lower Cambrian and ?Middle Cambrian units . 190 64. Isopach map of ?Middle and ?Upper Cambrian, and ?Lower Ordovician units 197 67. Paleogeography of late Arenig-early Llanvirn; isopachs of the halite facies . 203 68. Isopach map of the Cornwallis Group and age equivalent strata . 205 69. Isopach map of the Cape Phillips Fonnation and age equivalent strata . 207 77. Deltaic lobes of the Hecla Bay Sequence, and of the shelf-slope break above the Cape De Bmy Fonnation . 225 79. Isopach map of the Hecla Bay Sequence • . 229 80. Palinspastic cross-sections of the Hecla Bay Sequence . 230 81. Devonian paleogeographic maps and schematic cross-sections, Arctic Islands 233 82. Isopach map of the Beverley Inlet Sequence • • • • • . • • • . 235 84. Isopach map of the lower Parry Islands Sequence . 238 88. Correlation chart, Carboniferous through Holocene strata . 250 99. Bar graphs of sedimentation rate plotted against time (322-57 Ma) • . 286 100. Fold trends of the Franklinian Mobile Belt, western Arctic Islands . 293 134. Subsurface tectonic elements on the Thumb Mountain Formation . 393 142. Beverley Inlet Anticline, on a portion of seismic proflle P1660 . 407 168. Structure contour map on the Eleanor River Formation . 467 169. Sub- Carboniferous geology of Sabine Peninsula ................... 468 172. Stereonet plots of kinematic indicators collected at numerous sites in the Canrobert Hills . 475 179. Stereonet plots of kinematic data from Kitson River Inlier ............. 491 182. Weatherall Depression on a portion of seismic proflle P1921 ........... 500 195. Paleogeographic map of Melville Island area for mid-Permian time . 527 200. Map of Mesozoic gabbro dykes, extension faults and related magnetic anomaliM1 203. Eurekan fold trends (D8) and recent earthquake epicentres (D9) plotted on the Bouguer anomaly for land areas and on the isostatic anomaly for marine areas 553 208. Kinematic model for the Eurekan Orogen in the Canadian Arctic Islands . 566 210. Commodity occurrences map of Melville Island .................... 586 4 12 3sl;f 23 ~... s HECLA AND 34~ 14 -¢.3 8 I ( 'f-1o GRIPER BAy REA POINT ... "'0 MELVILLE --STRUcTURAL CROSS-SECTION SOUND --- REPROCESSED SEISMIC DATA ~KILOMETRES 0 ~iJ5LLre 3. ------7~7;6;o;-·-----------------:TJ}:4oo-------------------~·;-2~o-------------------~·1o~o~----------------~~~6~afo~--------- 29 30 0 TWO-WAY TRAVEL TIME 0 "'0 (s.) "' 0 0 0 ON 0 00> 8 0 8 8 LEGEND DEPTH 0 ~ ... ~;;:; (m.) '"' SEISMIC CONFIGURATION LITHOFACIES SYMBOLS ~ Rl!lleclion-lree (RF) Conglomerate (CGL), Breccia (BRX) nonmarine Anticline {arrow Indicates direction of plunge; ~ upright and inclined, overturned) ... .. ... --- Wavy (W) ; hummocky; mounded --- Sandstone (SS); deltaic, nonmarine STRATIGRAPHIC UNITS E2J Syncline (arrow indicates direction of plunge; upright and inclined, overturned) . .. ...... Low amplitude (WL) Sandstone, siltstone, shale; inner shelf, delta-front t u LITHOLOGY LOG Jhrust {defined, approximate, assumed) High amplitude (WH) Shale (SH), siltstone (SLn; outer shelf Normal fault {defined, approximale) .. .... • . ----- Parallel discontinuous (PO) ---- Anhydrite (ANHY) , gypsum (GYP) ; rastricted shelf VELOCITY LOG Fault {arrow indicates relative movement; 1 1 I Low amplitude (POL) Bedded salt (SALn; restricted shell (m.s- ) dextral, sinistral) ~ --- / I High amplitude (PDH) Dolostone (DOL); shell Fault, undetermined (tick indicates downthrown side; defined, approximate) ------Parallel, continuous------ Umestone (LSn; open shelf DENSITY LOG 2 -soo--- (kg.m' ) lsopachs {approximate, assumed) -100---- Low amplituda Limestone clinoforms; slope 00000~ Facies front {plan; section) ... .. .. .. .. .. .. .. ACOUSTIC IMPEDANCE High amplitude Mudrock clinoforms; slope 1 (kg.m·'s- ) Unconformity (defined, approximate) . ..... .. • . incised valley fill {IVF) Siliciclastic sediment gravity flows Une of section . .. .. ... .. .. .. ................ Growth fault Dark mudrock, bedded chert, resadimented carbonate; starved basin or shell lsochron (seconds, two way time) . .. .. .. ...... --}9-- REFLECTION COEFFICIENTS Clinoforms (CL) ...... Bedded chert; starved basin or starved shelf .. D11ta point {thickness in metres) . Divergent (DIV) WAVE LET (REVERSE RICKER) Correlated seismic reflection (0° 26 Hz 30 ms) Toplap (T) MODIFYING TERMS SYNTHETIC SEISMOGRAM Coal Type section ... (REVERSE POLARITY) Downlap (D) 8 Bentonite * G Glauconitic Fossil locality; kinematic indicators ®® Onlap {0) R Redbeds v 1\ Volcanic flows; basic {vb), felsic Minor fold (north vergent, south vergent) N NV SV Angular unconformity (AU) l:l. Replacement chert ~ ~ Calcareous, dolomitic SEISMIC PROFILE NEAR WELL Disconlormity Sandy, minor sandstone Silty, minor siltstone Nonconformity Argillaceous, shale partings TWO-WAYTRAVEL TIME Figure 7. (continued) Legend to accompany the figure on the previous page. This figure (s.) 0 "'ci is universally applicable to most other text illustrations. 44 souND MELVILLE VISCOUNT Kilometres 0 50 48 -27.5 - - 25.0 30.0 - - 30.0 - - 27.5 27.5 - - 32.5 - - 30.0 25.0 - - 35.0 - - 32.5 22.5 - - 37,5 - - 35.0 20.0 - - 40.0 - -37.5 17.5 - - - 42.5 - -40.0 15.0 - 17.5 - - 45.0 - -42.5 12.5 - 15.0 - - 47.5 - -45.0 10.0 - 12.5 - - 50.0 - - 4'1 .5 7.5 - 10.0 --52.5 - - 50,0 5.0 - 7.5 --55.0 - - 52.5 2.5 - 5.0 --57.5 - - 55.0 0.0 - 2.5 --60.0 - -57.5 - 2.5 - 0.0 --62.5 - - 60.0 - 5.0 - - 2.5 - - 65.0 - ~ 62.5 - 7.5 - - 5.0 --67.5 - - 65.0 - 10.0 - - 7.5 --70.0 -- 67.5 - 12.5 - - 10.0 -- 72.5 - - 70.0 -16.0 - - 12.6 -- ·75.0 - -72.5 - 17.5 - -15.0 -- 77.5 - - 75.0 - 20.0 - -17.5 -- 80.0 - - 77.5 - 22.5 - - 20.0 -- 82.5 - -80.0 -25.0 - -22.5 - -82. Figure 11. 1000- 750- 1000 500 - 750 - 400 - 500 - 350- 400 - 300- 350 - 275- 300 - 250- 275 - 225 - 250 - 200- 225 - 175- 200 - 150- 175 125- 150 100 - 125 75- 100 50 - 75 25 - 50 0- 25 -25- 0 -50- - 25 - 75 - - 50 -100- - 75 - 125- - 100 - 150- -125 - 175- -200- -275- -300- -325 - - 350 - -325 - 400- -350 -500- -400 -750- -500 -1000- - 750 -1500 - -1000 <-1500 NANOTESLAS Figure 12. V\ 0 70 4!) c~ DESBARA TS S TRAIT lOWSON F' OlNl ,,/ ) I / I ,' ! ! II I I ! I / I Vtsc OUNr MELVILLE SOUND ~T_ r, c RES ' i 1JO·,) -----------;b:}I " (.) MACKENZIE INTERIOR VICTORIA MELVILLE NORTHERN I w I WERNECKE IRICHARDSON I I 0... <!) I MOUNTAINS MOUNTAINS MOUNTAINS PLATFORM I ISLAND I ISLAND BAFFIN ISLAND <( <{ 0:: (.!) () MINTO UPLIFT, SUBSURFACE ~ C/) a: (? 0:: !:: 1- PLATEAU OGILVIE RICHARDSON COPPERMINE BORDEN ~ z w HADLEY, I (f) ::) ~ 5 OF DUNDAS 0 0 WELLINGTON z 0 THRUST ARCH TROUGH HOMOCLINE BASIN 0 <{ PENINSULA I 0:: INLIERS I a: (.) en VAMPIRE FM sh sit ss 6 ~ ~ Uz~<(N a: BACKBONE 0 al z 570-----l UJ :E <( RANGES ..J <( != <( u 0 a.. :E :E 0 1- z <( a:<( u <( wCi EKWI SUPERGP 700 a:w a.. a.. ::JI 800 I LIL...UI\>JI z AND LITTLE DAL GP NUNATSIAO ~z MACKENZIE GPS a:>- 0 a.. HIGHL Y dol 1st ss <( (.9 1st gyp ::r: MOUNTAINS sit 13 2-37.3 ffi sl1 vb 22 a.. ~ ;:) (/) (/) ~ SUPERGP REFLECTIVE 900 I~ KATHERINE GP <: ;:) a.. I EOUALULIK sh ss gyp 1st 10 + (.9 0 PINGUICULA GP SHALER GROUP a: :::!: UJ ss sh 20 a.. ~ ;:) (/) ~ UJ RAE GP SUCCESSION 1- u~ 0 s=l GP Q) ~ TSEZOTENE FM I I (sP2) 1000 I I sh dol 16 I I I (upper par1) UNITH-1 I dol A .. I I I I I II Iss 1st 1100 n= I I I (.) 6 N 0 a: UJ 1- I 1200 olwla: ...J a.. 0 0 :E Iz 1300 <( S2 ::J w ::r: I WERNECKE 1400 I I I I I II I I covered SUPERGP covered 1500 sh ss dol 130 1600 a: w ~~z 0 <( covered ...J iii w ::r: Cl. <( 2500 (1900 ' rna) z SLA VE CRATON GRANITOIDS SEISMIC UNIT <( w :I: (2390 ma) (.) GRANITOIDS sAP II: <( Figure 22. Suggested correlation of Precambrian lithostratigraphic units (Northern Cordillera and Arctic Islands), and -.l ?Precambrian seismic stratigraphic units (Melville Island). Vl 82 81 I SOUTH NORTH ISOUTHEAST NORTHWEST I 1-------------
Recommended publications
  • Ellesmere Light Expedition Report
    Ellesmere Light Expedition Report The aim of Ellesmere Light was to make a lightweight north-south hiking traverse of Ellesmere Island. In the months leading up to the expedition my team mate Clive Rubens and I refined the plan in order to attempt the journey unsupported i.e. without food caches en route. This change was mainly brought on by worries that we would not reliably and economically be able to put in one of our caches; namely at Vendom Fiord. The upside of trying for an unsupported traverse is that it is much more satisfying to just head out with two months of food and supplies and be totally immersed in the wilderness; rather than having the deadlines of trying to reach a cache. The downside it that you have to move all your stuff at once! Now obviously one cannot carry 55 or 60 days of food in a backpack, so we planned to start with sledding over the sea ice, then put wheels on the sled and finally to cache the sled and hike. See overview map on page 5. After three days in Resolute Bay, hub of high arctic logistics, we were keen to be away. Our pilot was pretty confident that he could fly north of Eureka and land at a strip beside Otto Fiord. This sounded good, since it would get us closer to the Arctic Ocean. At Eureka the melt was well underway; all the snow had gone and there was already a shore lead of water between the land and the sea ice.
    [Show full text]
  • An Aerial Survey of Caribou On
    AN AERIAL SURVEY OF CARIBOU ON WESTERN VICTORIA ISLAND (5–17 JUNE 1994) JOHN S. NISHI AND LAURIE BUCKLAND DEPARTMENT OF RESOURCES, WILDLIFE, AND ECONOMIC DEVELOPMENT GOVERNMENT OF THE NORTHWEST TERRITORIES 1KUGLUKTUK, NT. X0E 0E0 2YELLOWKNIFE, NT. X1A 3S8 2000 FILE REPORT NO. 128 iii ABSTRACT Concerns over the sharp decline in numbers of the Minto Inlet caribou herd on northwest Victoria Island and increased hunting pressure on the Dolphin and Union caribou herd on southwestern Victoria Island prompted a survey of western Victoria Island. We used two fixed-wing aircraft and flew a systematic strip transect survey of western Victoria Island in June 1994. Our objectives were two-fold: 1) to determine the abundance of caribou in northwest Victoria Island (Minto Inlet calving area), and 2) to delineate the calving distribution of caribou on southwestern Victoria Island (Dolphin and Union calving area), re- survey any high density areas, and estimate population size based on the calving ground survey. We conducted the survey from 5–16 June 1994. The area surveyed was 138 185 km² in size and accounted for ca. 63% of the entire land area of Victoria Island. We estimated a total of 14 539 ± 1015 (SE) caribou on western Victoria Island at an overall density of 0.11 caribou / km2. Although our survey area included the entire known seasonal range of the Minto Inlet herd, we only observed 4 caribou on-transect in that area. Our results corroborated previous aerial surveys (March 1992, March 1993 and June 1993) where few caribou were observed and added confirmation to the decline of the Minto Inlet herd.
    [Show full text]
  • Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
    Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands.
    [Show full text]
  • Diamondiferous Kimberlites on Victoria Island, Canada: a Northern Extension of the Slave Craton
    DIAMONDIFEROUS KIMBERLITES ON VICTORIA ISLAND, CANADA: A NORTHERN EXTENSION OF THE SLAVE CRATON Mark Kolebaba1, George Read2, Bernard Kahlert1 and Dave Kelsch1, 1 Diamonds North Resources Ltd, Canada; 2 Canabrava Diamond Corporation, Canada basalt (Natkusiak Formation 723 Ma) and INTRODUCTION agglomerate which make up the Shaler Mountains that are intruded by gabbro sills. The lower sandstone and gabbro units of the Shaler Group are also found Victoria Island, located in the Northwest Territories along the southern coast of Victoria Island, and as and Nunavut in the High Arctic of Canada (Figure 1) small inliers south of Washburn Lake. has been a diamond exploration target since 1993 when exploration companies recognized the possibility Archean age rocks beneath the eastern half of Victoria Island under thin Paleozoic carbonate cover. Much evidence has been collected through work since 1993 that suggests Victoria Island has the potential to become a world-class diamond-producing district. Recent exploration efforts have identified kimberlites with high diamond counts and robust diamond size distributions trending toward large 1 to 2 mm stones from small kimberlite samples. Supportive mineral chemistry including major oxides and trace element analyses suggests a cool geotherm, presence of potential peridotitic diamond sources and a strong diamond bearing eclogite signature. Figure 1: Location and geology map for Victoria Island. GEOLOGY Regional magnetics indicate the basement rocks have been intruded by NW-SE trending Mackenzie (1270 Archean rocks exist in the eastern half of Victoria Ma) and Franklin (720 Ma) diabase dykes and a Island. Paleozoic sediments including dolomite, previously undocumented north-south trending minor limestone, sandstone and shale of the Arctic diabase dyke system dated at 425 Ma (Diamonds Platform have been preserved within post- North Internal Report, 1999).
    [Show full text]
  • Canadian Manuscript Report of Fisheries and Aquatic Sciences No. 1577
    DFO L bra 111 11 1 y111 / MPO11 1 1111 B bliotheque 12021433 Ringed Seal, Phoca hispida, Breeding Habitat Survey of Bridport Inlet and Adjacent Coastal Sea Ice LIBRARY FISHERIES AND OCEA NS T. G. Smith and M. O. Hammill BIBLIOTHÈQUE PÉCHES ET OCÉANS Arctic Biological Station Department of Fisheries and Oceans 555 St. Pierre Blvd. Ste. Anne de Bellevue, Quebec H9X 3R4 July 1980 Canadian Manuscript Report of Fisheries and Aquatic Sciences No.1577 H a a 3 F 4k c. of Govemment of Canada Gouvernement du Canada Fisheries and Oceans Pêches et Océans Canadian Manuscript Report of Fisheries and Aquatic Sciences These reports contain scientific and technical information that represents an important contribution to existing knowledge but which for some reason may not be appropriate for primary scientific (i.e. Journal) publication. They differ from Tech- nical Reports in terms of subject scope and potential audience: Manuscript Reports deal primarily with national or regional problems and distribution is generally restrict- ed to institutions or individuals located in particular regions of Canada. No restriction is placed on subject matter and the series reflects the broad interests and policies of the Department of Fisheries and Oceans, namely, fisheries management, technology and development, ocean sciences, and aquatic environments relevant to Canada. Manuscript Reports may be cited as. full publications. The correct citation appears above the abstract of each report. Each report will be abstracted by Aquatic Sciences and Fisheries Abstracts and will be indexed annually in the Department's index to scientific and technical publications. Numbers 1-900 in this series were issued as Manuscript Reports (Biological Series) of the Biological Board of Canada, and subsequent to 1937 when the name of the Board was changed by Act of Parliament, as Manuscript Reports (Biological Series) of the Fisheries Research Board of Canada.
    [Show full text]
  • Nolocene Deglacial and Sea Level History of Dobbin Bay, Eastern Ellesmere Island, Arctic Canada
    University of Alberta NOLOCENE DEGLACIAL AND SEA LEVEL HISTORY OF DOBBIN BAY, EASTERN ELLESMERE ISLAND, ARCTIC CANADA SCOTT M. ROBERTSON 0 A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Science Department of Earth and Atmospheric Sciences Edmonton, Alberta Spnng 1999 National Library Bibliotheque nationale du Canada Acquisitions and Acquisitions et Bibliographie Services services bibliographiques 395 WeIAngton Street 395, nie Wellington Ottawa ON KIA ON4 WwaON K1A ON4 Canada Canada Your f~ieVotre refënmar Our füe Notre reldrenu, The author bas granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant à la National Library of Canada to Bibliothèque nationale du Canada de reproduce, loan, distribute or seil reproduire, prêter, distribuer ou copies of this thesis in microfonn, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfichelfh, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fkom it Ni la thèse ni des extraits substantiels may be printed or otherwise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation. ABSTRACT This thesis presents the Holocene deglacial and sea level history at the head of Dobbin Bay, east Ellesmere Island. An ice-contact delta at the fiord head contains two tills separated by deltaic foreset beds dated 23.3 ka BP.
    [Show full text]
  • Canada's Arctic Marine Atlas
    Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King
    [Show full text]
  • Canada Topographical
    University of Waikato Library: Map Collection Canada: topographical maps 1: 250,000 The Map Collection of the University of Waikato Library contains a comprehensive collection of maps from around the world with detailed coverage of New Zealand and the Pacific : Editions are first unless stated. These maps are held in storage on Level 1 Please ask a librarian if you would like to use one: Coverage of Canadian Provinces Province Covered by sectors On pages Alberta 72-74 and 82-84 pp. 14, 16 British Columbia 82-83, 92-94, 102-104 and 114 pp. 16-20 Manitoba 52-54 and 62-64 pp. 10, 12 New Brunswick 21 and 22 p. 3 Newfoundland and Labrador 01-02, 11, 13-14 and 23-25) pp. 1-4 Northwest Territories 65-66, 75-79, 85-89, 95-99 and 105-107) pp. 12-21 Nova Scotia 11 and 20-210) pp. 2-3 Nunavut 15-16, 25-27, 29, 35-39, 45-49, 55-59, 65-69, 76-79, pp. 3-7, 9-13, 86-87, 120, 340 and 560 15, 21 Ontario 30-32, 40-44 and 52-54 pp. 5, 6, 8-10 Prince Edward Island 11 and 21 p. 2 Quebec 11-14, 21-25 and 31-35 pp. 2-7 Saskatchewan 62-63 and 72-74 pp. 12, 14 Yukon 95,105-106 and 115-117 pp. 18, 20-21 The sector numbers begin in the southeast of Canada: They proceed west and north. 001 Newfoundland 001K Trepassey 3rd ed. 1989 001L St: Lawrence 4th ed. 1989 001M Belleoram 3rd ed.
    [Show full text]
  • Floristische Studien Auf Victoria Island, N. W. T. (Kanada)
    Polarforschung 56 (112): 93-98, 1986 Floristische Studien auf Victoria Island, N. W. T. (Kanada) Von Dietbert Thannhciscr" Zusammenfassung: Währendgeoökologischer Untersuchungen auf Victorla lslund wurden Indct Umgcbuug VOll Holmnn, Cambridgc Bay, Wellington Bay, Mt. Pelly, Richardson lstands, Hadley Bay und Minto lnlct 277 Neufunde l:!~'ll\ndll, von denen RGcfüßpflunzon als Erst­ nachweise für Vierorte lsland und 6 Arten für den westlichen kanadischen urktlschcn Ardlipcl unzusprcchcn xlttd. Summary: While engaged in geoecological field work on Victoria Island, 277 ncw plunt« could bc rccordcd Fot rhc vldllilin 01' Hohnun. CambridgeBay, Wellington Bay, Mt. Pelly, Richardson Islands, Hadley Bay, undMin!u lnlet ; R01' thcm wen- Il('W fot VlrIPfl11I.... tnnd. 6 1'01 the western Canadian arctic archipelago. Die Flora des westlichen kanadischen Arktis-Archipels ist weit weniger bekannt als dic dcs Östlichen Teils. Die Liste der 277 Gefäßpflanzen, die während pflanzensoziologischer Untcrsuchungcu auf Victoria Island neu gefunden wurden, soll dazu beitragen, diese unzureichenden Kenntnisse W verbessern. Der Verfasser registrierte im Gebiet von Holman in der Zeit vom 7. bis 17. August 1973 und 1I1il 26. Au­ gust 1986 verschiedene Neufunde. Die nähere und weiterc Umgebung von Cambridge Bay wurde in der Zeit vom 21. Juli bis 5. August 1983, vom 27. Juli bis 1. August 1984, vom 8. Juli bis 20, Juli 1986 lind vom 27. bis 29. August 1986 eingehend floristisch untersucht. Die Wcllington Bay an der Mündung des Ekulluk River wurde vom 6. bis 9. August 1983 besucht. Weitere floristische Bcobachtuugcn wurden am Mt. Pelly vom 19. bis 26. Juli 1984 sowie an der Hadlcy BlIY (71 "37'N, 107 045'W) vom 7.
    [Show full text]
  • The Glacial, Sea Level, and Sea Ice Histories of Melville and Eglinton Islands, Western Canadian High Arctic: Last Glacial Maximum to Present
    University of Alberta The glacial, sea level, and sea ice histories of Melville and Eglinton islands, western Canadian High Arctic: Last Glacial Maximum to present by Francis Chantel Nixon A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth and Atmospheric Sciences ©Francis Chantel Nixon Spring 2012 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. Library and Archives Bibliotheque et Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-87893-4 Our file Notre reference ISBN: 978-0-494-87893-4 NOTICE: AVIS: The author has granted a non­ L'auteur a accorde une licence non exclusive exclusive license allowing Library and
    [Show full text]
  • Escholarship@Mcgill
    " " 1] • " ., , if - • - THE AlLOCHTItONOUS ·ORIGIN Of "BIOHERMS" IN THE EARLY DEVONiAN STUART SAY FORMA~IeN , ' OF BATHURST IS~ND,'~RCTic.CANADA. / 1 / / KEVIN PATRICK POLAN, / / OEPARTMENT OF GEOLOGICA~ SCIENCES" , ~ McGItL UNIV~RSITY, MONTREAL~ '., ( DECEMBER, 1982. A the~i s submi t'ted to the Facul ty . of Graduate Stùdies and Researeh in' partial fulfillment of the requirements, l for the degree of Master of Sci ence. , " 3 ~ ,~ ~ ~ ~ .. ! ~ j J . J ~ .{ " ~ @ Kevin P. Palan, 1982. , i! 1 ~" . ~ o i ; ~ j - \ /1' , ABSTRACT Blocks of limestone and dol9,mite 'up to tens of metres i1\ sfz.e occur • near the base of the Lower Oevonian (Siegenian-Emsian) Stuart Bay Formation 1\, . at s~x sites, on eastern Bathurst Island. These blocks occur in gro~ps of up . " , , ",. 1 : ta thirty individuals and, at the two localit'ies with the greatest numer 'of , . • 1 blacks, are disposed in two roughly linear groups reflecting,their occurrence on two beddin9 planes. Stromatoporoids (genera: 'Cl..a.t:hJr.od.rj.ctyon, Atopo.4.tJwma., GeJrJUmO.4.t1r.om4, Acünccli.c.t.yon. IJr,u.pe.t:o.!).tJwma.,. 'P.6eu.d.ot:Jw.pet.o.4~IfIIJ., Sa.lai.Ir.eUa . and S~ngo.!)~ma.l and favositid corals are the MOst co~n framebuilders. <1 ,<:, . The blacks have weathered from a matrix of finelY-la~~nated deePj . water siltstone. Neighbourin9 bloc~~ differ i~ bedding orientatiqp. Although they, h~ve been described as' bioherms in place~ this evidence indicates tha~ l th~ are blocks deri~ed during cata~trophic events such as earthqu~kes from ( " a Devonian reef tract developed on the western flank of the Cornwallis Fold- belt.
    [Show full text]
  • Inuvialuit Settlement Region Polar Bear Joint Management Plan 2017
    Inuvialuit Settlement Region Polar Bear Joint Management Plan 2017 As recommended by: to: Minister of Environment and Climate Change, Canada Minister of Environment and Natural Resources, Government of Northwest Territories Minister of Environment, Government of Yukon Recommended citation: Joint Secretariat. 2017. Inuvialuit Settlement Region Polar Bear Joint Management Plan. Joint Secretariat, Inuvialuit Settlement Region. vii + 66 pp. © 2017 Joint Secretariat, Inuvik, NWT All rights reserved. ISBN: 978-0-7708-0251-6 Cover photo: Jodie Pongracz, University of Alberta Inuvialuit Settlement Region Polar Bear Joint Management Plan PREFACE The Inuvialuit Settlement Region Polar Bear Joint Management Plan is intended to describe the management goal and objectives for polar bears in the entire Inuvialuit Settlement Region (ISR), including the Northwest Territories (NWT) and Yukon. This plan was developed to meet the requirements of a management plan under the territorial Species at Risk (NWT) Act and the ISR (Yukon and NWT) regional component of the national management plan under the federal Species at Risk Act while respecting the joint management process legislated by the Inuvialuit Final Agreement (IFA). Management authority for polar bears in the ISR is jurisdictionally complex and the plan is intended to facilitate an integrated and common approach by all jurisdictions. To facilitate this process, a companion document, Framework for Action for Management of Polar Bears in the Inuvialuit Settlement Region has been developed. This document outlines actions and areas where further work should be directed. The framework is meant to be used by management partners to develop an implementation table. Implementation of this joint management plan and companion document is subject to budgetary appropriations, priorities, and constraints of the participating management organizations.
    [Show full text]