DOCSLIB.ORG

Willmore Wilderness

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Willmore Wilderness THE ALBERTA GAZETTE, DECEMBER 31, 1968 Township 57 -All of ranges 10 to 12 inclusive and all those portions of range 13 lying easterly of the McLeod River; Township 58 -All of ranges 10 to 17 inclusive; Township 59 Township 60 the Athabasca River; Township 61 Township 62 Township 63 Township 64 the Athabasca River, and all of ranges 4 to 13 -All of those portions of range 3 lying westerly of the Athabasca River, and all of ranges 4 to 7 inclusive; . erly of the Athabasca River, and all of ranges 4 to 7 inclusive. All of the above lands lying west of the fifth meridian, excepting therefrom the area contained within the limits of any town or village, as the case may be. MINISTERIAL ORDER NO. 428/68 To Provide for Establishment of Improvement District No. 16. THE JMPROVEhllbl’ DISTRICTS ACT, 1965 Edmonton, December 19, 1968. Whereas under the provisions of The Improvement Districts Act, 1965, the Minister may, by order, amalgamate any two or more Im- provement Districts, or alter the boundaries thereof; Therefore, I, Edgar H. Gerhart, Minister of Municipal Affairs, by virtue of the powers vested in me by section 4 of the said Act, do hereby order, that the undernoted Improvement Districts, be am- algamated: Nos. 110, 111 and 126. 3155 THE ALBERTA GAZETTE, DECEMBER 31, 1968 It is further ordered, that the amalgamated district thus created, be numbered 16 and shall comprise the lands described in the Schedule hereto. This order shall be effective as of January 1, 1969, except for assessment purposes where the effective date will be December 31, 1968. E. H. GERHART, 4 Minister of Municipal Affairs. SCHEDULE IMPROVEMENT DISTRICT NO. 16 Township 57 -All those portions of ranges 20 to 23 inclusive lying north and east of the Berland River; Township 58 -All those portions of range 19 lying north of the Athabasca River and all those Portions of ranges 20 to 26 inclusive lying north of the Bedand River, and all of range 27; Township 59 -All those portions of ranges 18 and 19 lying north of the Athabasca River, and all of ranges 20 to 27 inclusive; Township 60 -All tdke portions of ranges 16, 17 and 18 lmg north of the Athabasca River, and all of ranges 19 to 27 inclusive; Township 61 -All those portions of range 16 lying north and west of the Athabasca River and all of ranges 17 to 27 inclusive; Township 62 -All of ranges 15 to 27 inclusive; Townships 63 to 67 -All of ranges 14 to 27 inclusive; inclusive Townships 68 to 73 -All of ranges 20 to 26 inclusive; inclusive Townships 74 and 75-All of ranges 24 to 26 inclusive; Township 76 -All those portions of ranges 24, 25 and 26 lying south and east of the Smoky River; Township 77 -All those portions of range 24 lying east of the Smoky River and south of the Little Smoky River; I All of the above lands lying west of the fifth meridian, excepting therefrom the area contained within the limits of any town or village, as the case may be. JTownship 53 -All those portions of ranges 11, 12 and 13 lying north of Pauline Creek and Jackpine River in the Province of Alberta; /Township 54 -All those portions of ranges 10 to 13 inclusive 7. lying west of Jackpine and Smoky Rivers in the d Province of Alberta; 3156 r * TRE ALBERTA GAZETTE, DECEMBER 91, 1968 (Township 55 -All those portions of ranges 9 and 10 lying west of the Smoky River, all of ranges 11 and 12, and all of those portions of ranges 13 and 14 in the Province of Alberta; ,/Townships 56 and 57-All those portions of ranges 8 and 9 lying west of . the Smoky River, and all of ranges 10 to 14 in- clusive in the Province of Alberta; Townships 58 to 68 -All of ranges 1 to 14 inclusive; hclusive Township 69 -All of ranges 1 to 9 inclusive and all those por- tions of ranges 10 and 11 lying south and east of the Wapiti River; Township 70 -All of ranges 1 and 2 and all those portions of ranges 3 to 9 inclusive lying south of the Wapiti River; Township 71 -All of range 1 and all those portions of ranges 2 and 3 lying east of the Wapiti River; Townships 72 to 74 -All of range 1 and all those portions of ranges 2 inclusive and 3 ly4Fg east of the Smoky River; Township 75 -All those portions of ranges 1 and 2 lying east and south of the Smoky River; Township 76 -All those portions of range 1 lying south of the Smoky River; All of the above lands lying west of the sixth meridian, excepting therefrom the area con- tained within the limits of any town or village, as the case may be. MINISTERIAL ORDER NO. 429/68 To Provide for Establishment of Improvement District No. 17. THE IMPROVEhlENT DISTRICTS ACT, 1965 algamated: Nos. 107, 122, 123, 124, 125,J’28,// 129 and 131. J It is further ordered,,&t the amalgamated district thus created, be numbered 17, and sPI1 comprise the lands described in the Schedule hereto. be effective as of January 1, 1969, except for assessment purboses where the effective date will be December 31, E. H. GERHART, Minister of Municipal Affairs. 3157 .
Load more

Recommended publications
  • A Preliminary Assessment of the Native Fish Stocks of Jasper National Park
    A Preliminary Assessment of the Native Fish Stocks of Jasper National Park David W. Mayhood Part 3 of a Fish Management Plan for Jasper National Park Freshwater Research Limited A Preliminary Assessment of the Native Fish Stocks of Jasper National Park David W. Mayhood FWR Freshwater Research Limited Calgary, Alberta Prepared for Canadian Parks Service Jasper National Park Jasper, Alberta Part 3 of a Fish Management Plan for Jasper National Park July 1992 Cover & Title Page. Alexander Bajkov’s drawings of bull trout from Jacques Lake, Jasper National Park (Bajkov 1927:334-335). Top: Bajkov’s Figure 2, captioned “Head of specimen of Salvelinus alpinus malma, [female], 500 mm. in length from Jaques [sic] Lake.” Bottom: Bajkov’s Figure 3, captioned “Head of specimen of Salvelinus alpinus malma, [male], 590 mm. in length, from Jaques [sic] Lake.” Although only sketches, Bajkov’s figures well illustrate the most characteristic features of this most characteristic Jasper native fish. These are: the terminal mouth cleft bisecting the anterior profile at its midpoint, the elongated head with tapered snout, flat skull, long lower jaw, and eyes placed high on the head (Cavender 1980:300-302; compare with Cavender’s Figure 3). The head structure of bull trout is well suited to an ambush-type predatory style, in which the charr rests on the bottom and watches for prey to pass over. ABSTRACT I conducted an extensive survey of published and unpublished documents to identify the native fish stocks of Jasper National Park, describe their original condition, determine if there is anything unusual or especially significant about them, assess their present condition, outline what is known of their biology and life history, and outline what measures should be taken to manage and protect them.
    [Show full text]
  • Exploration in the Rocky Mountains North of the Yellowhead Pass Author(S): J
    Exploration in the Rocky Mountains North of the Yellowhead Pass Author(s): J. Norman Collie Source: The Geographical Journal, Vol. 39, No. 3 (Mar., 1912), pp. 223-233 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1778435 Accessed: 12-06-2016 07:31 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 155.69.24.171 on Sun, 12 Jun 2016 07:31:04 UTC All use subject to http://about.jstor.org/terms EXPLORATION IN THE ROCKY MOUNTAINS. 223 overtures to Bhutan and Nepal, which have been rejected by these states, and I am very glad they have been. The Chinese should not be allowed on the Indian side of the Himalayas. The President : We will conclude with a vote of thanks to Mr. Rose for his excellent paper. EXPLORATION IN THE ROCKY MOUNTAINS NORTH OF THE YELLOWHEAD PASS.* By J. NORMAN OOLLIE, Ph.D., LL.D., F.R.S., F.R.G.S., etc. The part of the Koeky mountains, that run north through what is now the Dominion of Canada, have only in the last twenty-five years been made accessible to the ordinary traveller.
    [Show full text]
  • Wapiti River Water Management Plan Summary
    Wapiti River Water Management Plan Summary Wapiti River Water Management Plan Steering Committee February 2020 Summary The Wapiti River basin lies within the larger Smoky/Wapiti basin of the Peace River watershed. Of all basins in the Peace River watershed, the Wapiti basin has the highest concentration and diversity of human water withdrawals and municipal and industrial wastewater discharges. The Wapiti River Water Management Plan (the Plan) was developed to address concerns about water diversions from the Wapiti River, particularly during winter low-flow periods and the potential negative impacts to the aquatic environment. In response, a steering committee of local stakeholders including municipalities, Sturgeon Lake Cree Nation, industry, agriculture, the Department of Fisheries and Oceans Canada, and the Mighty Peace Watershed Alliance (MPWA), supported by technical experts from Alberta Environment and Parks (AEP), was established. The steering committee initiated the development of a water management plan that includes a Water Conservation Objective (WCO) and management recommendations for the Wapiti River basin from the British Columbia border to its confluence with the Smoky River. A WCO is a limit to the volume of water that can be withdrawn from the Wapiti River, ensuring that water flow remains in the river system to meet ecological objectives. The Plan provides guidance and recommendations on balancing the needs of municipal water supply, industry uses, agriculture and other uses, while maintaining a healthy aquatic ecosystem in the Alberta portion of the Wapiti River basin. Wapiti River Water Management Plan | Summary 2 Purpose and Objectives of the Plan The Plan will be provided as a recommendation to AEP and if adopted, would form policy when making water allocation decisions under the Water Act, and where appropriate, under the Environmental Protection and Enhancement Act by establishing a WCO for the Wapiti River.
    [Show full text]
  • BYLAW NO. 20-850 of the Municipal District of Greenview No. 16
    BYLAW NO. 20-850 of the Municipal District of Greenview No. 16 A Bylaw of the Municipal District of Greenview No. 16, in the Province of Alberta to establish the ward boundaries within the M.D of Greenview and the number of Councillors elected to represent each ward. WHEREAS, Section 143(4) of the Municipal Government Act enables a Council to pass a bylaw specifying the number of Councillors to serve on the Council of a Municipal District; and WHEREAS, Section 148(2) of the Municipal Government Act enables a Council to pass a bylaw to establish ward boundaries for its municipality, including the number of wards and number for each ward in the M.D. of Greenview; and WHEREAS, Section 148(5) of the Municipal Government Act enables a Council to pass a bylaw requiring each Councillor to be nominated by ward and that each Councillor shall serve as the Councillor for the ward in which they were nominated; and NOW THEREFORE, under the authority and subject to the provisions of the Municipal Government Act, the Council of the M.D. of Greenview No. 16, in the Province of Alberta enacts as follows: 1. Title 1.1 This bylaw shall be cited as the “Municipal Ward Boundaries and Council Composition”. 2. Definitions a. Greenview means the municipal corporation of the M.D. of Greenview No. 16. b. Local Authorities Election Act means the Local Authorities Election Act, R.S.A 2000, Chapter L-21. 3. Greenview shall be divided into nine (9) Wards. 4. The number and designation of each Ward shall be as described herein and as per Schedule ‘A’, and shall exclude all incorporated municipalities, as well as Sturgeon Lake Cree Nation and Alexander First Nation situated therein.
    [Show full text]
  • Appendix 9A Hydrogeological Baseline Report
    Proposed HR Milner Expansion Project Environmental Impact Assessment Report Appendix 9A: Hydrogeological Baseline Report Appendix 9A Hydrogeological Baseline Report Maxim Power Corp. Page 9A-1 January 2009 REPORT TO MAXIM POWER CORPORATION and ALBERTA ENVIRONMENT HYDROGEOLOGICAL BASELINE REPORT, HR MILNER GENERATING STATION, NEAR GRANDE CACHE, ALBERTA PROJECT NO.: PR08-04 Prepared By July 28, 2008 Executive Summary Maxim Power Corporation (MAXIM) is currently in the process of a major expansion of their existing HR Milner thermal power generating station located approximately 20km north east of Grande Cache, Alberta. The HR Milner Generating Station and facilities are located in the north half of Section 10 and the south half of Section 15, Township 58, Ranges 7 and 8, West of the 6th Meridian. The expansion will require a number of initiatives including the development of both a baseline environmental assessment and an environmental impact assessment. This section provides the hydrogeological information requested in Section 4.3.1 of Alberta Environment’s (AENV) April 8, 2008 Draft Terms of Reference. Impact assessment and monitoring/mitigation components are provided in Section 9 of the Impact Assessment Report. The HR Milner Generating Station is located on a flood plain terrace on the northwest bank of the Smoky River immediately down-gradient from the Grande Cache Coal Corporation’s Coal Processing Plant. The terrace that underlies the Station is approximately five metres above river elevation. Surface drainage is toward the Smoky
    [Show full text]
  • Milner Expansion – 2010 Supplementary Fisheries Information
    Milner Expansion – 2010 Supplementary Fisheries Information November 2010 Prepared for: MAXIM Power Corp. Calgary, Alberta Prepared by: Stantec Consulting Ltd. Calgary, Alberta Project Number: 123510029 Milner Expansion – 2010 Supplementary Fisheries Information Table of Contents November 2010 Table of Contents 1.0 INTRODUCTION...........................................................................................................................1-1 2.0 PROJECT LOCATION .................................................................................................................2-1 3.0 METHODS ....................................................................................................................................3-1 3.1 HABITAT SURVEY.......................................................................................................................3-1 3.2 FISH COMMUNITY SAMPLING...................................................................................................3-1 4.0 RESULTS .....................................................................................................................................4-1 4.1 FISH HABITAT .............................................................................................................................4-1 4.2 FISH COMMUNITY.......................................................................................................................4-5 5.0 SUMMARY....................................................................................................................................5-1
    [Show full text]
  • Metallic Mineral Deposits and Occurrences in the Phanerozoic Succession North of Latitude 55ºn, Alberta
    METALLIC MINERAL DEPOSITS AND OCCURRENCES IN THE PHANEROZOIC SUCCESSION NORTH OF LATITUDE 55ºN, ALBERTA Alberta Geological Survey Geo-Note 2000-02 D. Roy Eccles Contents 1.0 INTRODUCTION.................................................................................................................1 2.0 METHODOLOGY AND FORMAT......................................................................................1 3.0 GEOLOGY OF THE PHANEROZOIC STRATA IN NORTHERN ALBERTA ...................4 4.0 PREVIOUS MINERAL POTENTIAL STUDIES AND EXPLORATION SUMMARY........4 5.0 REFERENCES......................................................................................................................7 6.0 METALLIC MINERAL DEPOSITS AND OCCURRENCES IN THE PHANEROZOIC SUCCESSION OF NORTHERN ALBERTA........................................................................9 7.0 SUMMARY OF OCCURRENCES OF PLACER GOLD....................................................36 Figure Figure 1. Mineral deposits and occurrences in the Phanerozoic strata of northern Alberta...........3 1.0 INTRODUCTION The geological setting of Phanerozoic rocks in northern Alberta is similar to many productive metalliferous districts in the world, where formation or emplacement of mineral deposits is often controlled, in part, by coeval volcanism and extensional faults or fracture zones associated with regional fault systems, arches and other structural zones that transect overlying Phanerozoic cover rocks. Selected examples, include: Early Cambrian marine black shale Ni-Mo deposits
    [Show full text]
  • Resources Development Table
    AECOM Alberta Environment and Appendix A – Stakeholder Issues Map ID Sustainable Resources Development Table Appendix A Stakeholder Issues Map ID Table AECOM: 2012-01-06 © 2009-2015 AECOM Canada Ltd. All Rights Reserved. AECOM Alberta Environment and Sustainable Resource Development Peace River Basin Flood Mitigation Feasibility Study Appendix A - Stakeholder Consultation Flood Issues Summary Table Stakeholder Identified Flood Risk Summary Table Table A-1 summarizes stakeholder identified issues and specifies the flood risk for each issue. The map ID in column one corresponds to “Stakeholder Identified Historical Flood Issues” figures found in Figures 5-1-1 to 5-10-1 and can be found at the end of each sub-section in Sections 5, for the respective municipality. These flood risks were identified during the stakeholder meeting. Table A-1: Stakeholder Consultation Flood Risk Summary Map ID Tribe Municipality Reserve Name Flood Issues Flood Risk Notes 1 - MD of Smoky River No. 130 - Little Smokey Bridge Low risk High water at bridge. 2 - MD of Smoky River No. 130 - Gravel Pit Low risk Was flooded 1 week, no impacts to access. 3 - MD of Smoky River No. 130 - River banks flooded Low risk - 4 - MD of Smoky River No. 130 - River banks flooded Low risk - 5 - MD of Smoky River No. 130 - Flood area Low risk Floods annually due to overtopping of east-west canal. Railway track on south extents of flood area is at a high elevation and acts as a barrier. Building or developing the area is prohibited. 6 - MD of Smoky River No. 130 - Water reservoir No risk Water from Smoky River intake is pumped to reservoir, and then pumped to Town of Falher WTP.
    [Show full text]
  • Natural Regions and Subregions of Alberta
    Natural Regions and Subregions of Alberta Natural Regions Committee 2006 NATURAL REGIONS AND SUBREGIONS OF ALBERTA Natural Regions Committee Compiled by D.J. Downing and W.W. Pettapiece ©2006, Her Majesty the Queen in Right of Alberta, as represented by the Minister of Environment. Pub # T/852 ISBN: 0-7785-4572-5 (printed) ISBN: 0-7785-4573-3 (online) Web Site: http://www.cd.gov.ab.ca/preserving/parks/anhic/Natural_region_report.asp For information about this document, contact: Information Centre Main Floor, 9920 108 Street Edmonton, Alberta Canada T5K 2M4 Phone: (780) 944-0313 Toll Free: 1-877-944-0313 FAX: (780) 427-4407 This report may be cited as: Natural Regions Committee 2006. Natural Regions and Subregions of Alberta. Compiled by D.J. Downing and W.W. Pettapiece. Government of Alberta. Pub. No. T/852. Acknowledgements The considerable contributions of the following people to this report and the accompanying map are acknowledged. Natural Regions Committee 2000-2006: x Chairperson: Harry Archibald (Environmental Policy Branch, Alberta Environment, Edmonton, AB) x Lorna Allen (Parks and Protected Areas, Alberta Community Development, Edmonton, AB) x Leonard Barnhardt (Forest Management Branch, Alberta Sustainable Resource Development, Edmonton, AB) x Tony Brierley (Agriculture and Agri-Food Canada, Edmonton, AB) x Grant Klappstein (Forest Management Branch, Alberta Sustainable Resource Development, Edmonton, AB) x Tammy Kobliuk (Forest Management Branch, Alberta Sustainable Resource Development, Edmonton, AB) x Cam Lane (Alberta Sustainable Resource Development, Edmonton, AB) x Wayne Pettapiece (Agriculture and AgriFood Canada, Edmonton, AB [retired]) Compilers: x Dave Downing (Timberline Forest Inventory Consultants, Edmonton, AB) x Wayne Pettapiece (Pettapiece Pedology, Edmonton, AB) Final editing and publication assistance: Maja Laird (Royce Consulting) Additional Contributors: x Wayne Nordstrom (Parks and Protected Areas, Alberta Community Development, Edmonton, AB) prepared wildlife descriptions for each Natural Region.
    [Show full text]
  • Willmore-Wilderness-Park-Map.Pdf
    Ancient glaciers, high mountain Park Guide peaks, thick forests and raging Wildlife Backcountry Hiking Contact rivers define these 4,597 km² of untamed wilderness. Backpackers and horseback riders seeking a true Willmore’s wildlife thrives in the natural Safety Many of the park’s well-established trails follow Alberta Parks backcountry experience can explore surroundings of the park. Grassy slopes provide in the historic footsteps of Aboriginal hunters, Web: albertaparks.ca over 750 km of trails where wildlife excellent winter ranges for sheep and goats. fur traders, coal miners and trappers. The Rock Hinton Office: 780–865–8395 abounds. Visitors to Willmore must Almost 20% of Alberta’s mountain goats and The wild and rugged nature of Willmore Lake staging area provides a popular access Visitor Centre: 780–865–5600 be experienced and well equipped 20% of the province’s bighorn sheep live in Wilderness is an irresistible draw for many into the Willmore via the Mountain Trail. For Toll Free: 1–866–427–3582 Willmore for backcountry adventure. Willmore and the park is also home to woodland visitors. Yet, the dangers of Willmore can provide those with only a few days to explore, Seep caribou, moose, elk, grizzly bears, black bears, a challenge for even the most seasoned outdoor Creek Trail soon heads north off the Mountain Fire Bans in Alberta Wilderness Park cougars, wolves, wolverine, and numerous small enthusiasts. Trail to provide quick entry into alpine country Web: albertafirebans.ca mammals. with plentiful wildlife and extensive views. Further Park Access • Only minimal trail maintenance occurs and along, Mountain Trail bends southwest and Emergency (Police, Fire, Ambulance) there are no developed campsites in the climbs to Eagle’s Nest Pass, offering a fine base Phone: 911 Hunting & Fishing park.
    [Show full text]
  • Glaciers of the Canadian Rockies
    Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter
    [Show full text]
  • Update on the Little Smoky Landslide
    UPDATE ON THE LITTLE SMOKY LANDSLIDE Roger Skirrow, Alberta Infrastructure and Transportation, Edmonton, Alberta, Canada Don Proudfoot, Thurber Engineering Ltd, Edmonton, Alberta, Canada Corey Froese, AMEC Earth & Environmental, Edmonton, Alberta, Canada Stan Thomson, Professor Emeritus, University of Alberta, Edmonton, Alberta, Canada ABSTRACT The Little Smoky River valley is cut into a preglacial channel infilled with very soft deposits. Valley slope instability is pervasive and very deeply seated. Highway 49 crosses the valley along an alignment that involves long sidehill traverses connected by a relatively low level bridge crossing. The south bridge abutment and land-based piers, and a significant portion of the southern valley slope exhibited movements shortly after construction in 1957. Stabilization efforts were undertaken at that time, as documented by Hayley and Thomson, 1975. Over the past 30 years more movements have occurred on both valley slopes. Numerous investigations and studies were undertaken on both valley slopes, and both slopes are being monitored at discrete instrumented locations. An InSAR study was completed to provide a widescale interpretation of the valley movements. This paper provides an overview of the salient issues and a discussion of short term and long-term mitigation options. RÉSUMÉ Le Little Smoky River Valley est coupé en canal preglacial infilled avec les dépôts très mous. L'instabilité de pente de vallée est dominante et très profondément assise. La Route 49 traverse la vallée le long d'un alignement qui implique de longues traversées reliées par un croisement de pont de niveau relativement bas. La butée du sud de pont et les piliers sur terre, et une partie significative de la pente méridionale de vallée ont montré des mouvements peu de temps après la construction en 1957.
    [Show full text]