DOCSLIB.ORG

Surficial Geology Compilation Map Series -- SG

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Surficial Geology Compilation Map Series -- SG 10 R 29 W R 28 W R 27 W R 26 W R 25 W R 24 W R 23 W R 22 W R 21 W R 20 W R 19 W 102° Dropmore 83 100° 300,000 325,000 350,000 375,000 400,000 425,000 0 0 0 , 51° 0 51° SURFICIAL GEOLOGY COMPILATION MAP SERIES 5 6 , 5 Tp 23 The Surficial Geology Compilation Map Series (SGCMS) addresses an increasing demand for Tp 23 0 consistent surficial geology information for applications such as groundwater protection, 0 0 , 0 industrial mineral management, protected lands, basic research, mineral exploration, 5 6 , 5 engineering, and environmental assessment. The SGCMS will provide province-wide coverage Inglis at scales of 1:500 000, 1:250 000 and a final compilation at 1:1 000 000. Shellmouth The unit polygons were digitized from paper maps originally published by the Geological Edwards Survey of Canada and Manitoba Geological Survey (MGS). In several areas, digital polygons derived from soils mapping were used to fill gaps in the geological mapping. The 1:250 000 Tp 22 L Tp 22 scale maps provide a bibliography for the original geological mapping. 10 Edge-matching of adjoining 1:250 000 scale map sheets is based on data from the Shuttle Radar Topography Mission Digital Elevation Model (SRTM DEM1) as interpreted by the MGS. Gunn Other polygon inconsistencies were modified in a similar manner. Geology (colour) is draped Cracknell Lake over a shaded topographic relief map (grey tones) derived from the SRTM DEM. 1 United States Geological Survey 2002: Shuttle radar topography mission, digital elevation model, Manitoba; United 83 States Geological Survey, URL <ftp://edcsgs9.cr.usgs.gov/pub/data/srtm/>, portions of files N48W88W.hgt.zip through N60W102.hgt.zip, 1.5 Mb (variable), 90 m cell, zipped hgt format [Mar 2003]. Tp 21 Tp 21 ek re Whitewater C LEGEND Lake 0 Quaternary Russell 0 0 , 5 2 6 Silverton Lake , 16 5 ORGANIC DEPOSITS: peat, muck; <1–5 m thick; very low Harrowby Audy O relief wetland deposits; accumulated in fen, bog, swamp, and 0 0 0 marsh settings , 45 5 2 Angusville 6 , Tp 20 5 Tp 20 SHORELINE SEDIMENTS: sand and gravel; 1–2 m thick; Lm beaches; formed by waves at the margins of modern lakes Millwood 10 16 Clear COLLUVIUM: landslide debris, eroded slopes, sheet flood Clear C deposits associated with steep slopes Lake Waywayseecappo Rossburn Lake Wasagaming EOLIAN: sand and minor silt; dunes, blowouts and undulating E plains; generally overlies deltaic sediments, coarse lacustrine 45 Tp 19 Tp 19 sediments, or glaciofluvial deposits Binscarth Onanole Vista L i t ALLUVIAL SEDIMENTS: sand and gravel, sand, silt, clay, t l e A organic detritus; 1–20 m thick; channel and overbank The Corners Gambler sediments; reworked by existing rivers and deposited primarily as bars l i a t Oakburn MARGINAL GLACIOLACUSTRINE SEDIMENTS: sand and d r i 0 Ls 0 gravel; 1–20 m thick; beach ridges, spits, bars, littoral sand and B Sandy 0 , Tp 18 Tp 18 0 gravel; formed by waves at the margin of glacial Lake Agassiz Keeseekoowenin 0 6 , Rackham 5 Menzie Elphinstone Lake 0 OFFSHORE GLACIOLACUSTRINE SEDIMENTS: clay, silt, minor 0 45 45 0 45 , Foxwarren 16 0 Lc sand; 1–20 m thick; very low relief massive and laminated deposits; 0 6 , 5 deposited from suspension in offshore, deep water of glacial Lake Agassiz; commonly scoured and homogenized by icebergs Solsgirth 16 Kelloe DISTAL GLACIOFLUVIAL SEDIMENTS: fine sand, minor gravel, S a Gs thin silt and clay interbeds; 1–75 m thick; subaqueous outwash fans; 21 sk R Tp 17 Tp 17 at deposited in glacial Lake Agassiz by meltwater turbidity currents; ch o e l l St-Lazare w i a n commonly reshaped by wave erosion and reworked by wind n g 41 A Shoal Lake s 42 42 PROXIMAL GLACIOFLUVIAL SEDIMENTS: sand and gravel; s Birtle Shoal G in 1–20 m thick; complex deposits, belts with single or multiple esker ib ridges and kames, as well as thin, low-relief deposits; deposited in Strathclair R o Lake iv contact with glacial ice by meltwater i er n 16 R e iv er Tp 16 TILL: diamicton; 1–75 m thick; low-relief, commonly streamlined deposits; subglacial Tp 16 deposits; largely derived from shale above the Manitoba Escarpment, carbonate rocks Salt in the central lowlands, and crystalline rocks in areas of Precambrian terrane; Raven Newdale Lake thicker sequences consist of multiple units of varying texture; commonly scoured by icebergs; Lake covered discontinuously by thin veneers (<1 m) of glaciolacustrine and glaciofluvial sediments 0 0 0 , 5 7 5 , 5 Basswood Calcareous clay diamicton, predominantly derived from Mesozoic 0 0 Tm 0 shale , 5 7 5 16 Tp 15 , Tp 15 5 Lavinia Decker Calcareous silt diamicton, predominantly derived from Paleozoic Birdtail Sioux Isabella McConnell McAuley Beulah Tc dolomite and limestone R iv Uno e Cardale Non-calcareous sand diamicton, predominantly derived from r O a Tp Pre-cambrian crystalline rock k 83 21 Tp 14 Tp 14 Pre-Quaternary Hamiota Moline ROCK: > 75% bedrock outcrop; Cretaceous shales above the Willen R Manitoba Escarpment, Paleozoic carbonate-dominated rocks in areas west and south of Lake Winnipeg, exposed typically as 41 Crandall glacially striated, low-relief surfaces; in Precambrian terrane, generally Miniota Arrow River Manson Oak River 10 unweathered intrusive, metasedimentary, and metavolcanic rocks Quadra 24 24 24 Rapid City having a glacially scoured irregular surface with high local relief 24 R Pope i v Reeder e 0 0 Tp 13 Uncoloured legend blocks indicate units that do not appear on this map. Tp 13 r Pettapiece 0 , 0 To aid the reader a shadow effect has been added to exaggerate the topographic relief. 5 5 , Oakner 5 Published by: Manitoba Industry, Economic Development and Mines 0 0 0 , Manitoba Geological Survey, 2004 0 5 5 , 5 Compiled by: G.L.D. Matile and G.R. Keller Rivers Modifed from: Chimo Resort Tp 12 Tp 12 1Kirkella Two Creeks Klassen, R.W. 1978. Surficial geology of Riding Mountain, west of principle meridian Manitoba- Wheatland 25 25 Saskatchewan; Geological Survey of Canada, "A" Series Map, Map 1479A, 1 map. Scale 1:250 000. 50° 50° Kenton Geology polygons in the Riding Mountain National Park area are based on data from the Shuttle 300,000 325,000 350,000 375,000 Bradwardine 400,000 425,000 102° 83 Harding 100° Radar Topography Mission Digital Elevation Model as interpreted by the MGS. R 29 W R 2E8l kWhorn R 27 W R 26 W R 25 W R 24 W R 23 W R 22 W R 21 W R 20 W Printed 2004 Scale 1:250 000 U p 0 10 20 30 p e r e C Kilometres n i a a m r p o b e M ll a b Major landforms: southern Manitoba Major landforms:r NTS 62K ea A brief description of the Quaternary landscape of southern Manitoba u c l h 100° 98° 96° 102° t 100° e P G 53° Eastward-facing bedrock escarpments culminating in cuestas which form the Manitoba Escarpment provide a foundation for the 53° e 51° 51° The Pas Moraine or M ge present-day landscape of southern Manitoba. To the east, the landscape is dominated by Precambrian rocks and bedrock structure, o Is SURFICIAL GEOLOGY COMPILATION MAP SERIES ra l i an such as faulting, is commonly visible. ne d Dead-ice SG-62K Above the Manitoba Escarpment, the landscape is dominated by hummocky moraine or dead-ice topography, streamlined topography Streamlined landforms topography and glacial spillways. Many areas are covered by thick sequences of glacial till representing numerous glacial episodes Dead-ice Precambrian topography dating back more than 100,000 years. The most recent glacial advances were from the northwest. Glacial till tends to be clay rich. shield 52° Dead-ice The Interlake is dominated by streamlined landforms and in lower areas, glaciolacustrine depositional basins. Quaternary sediments 52° topography Surficial geology of the Riding Mountain map sheet tend to be relatively thin and the preservation of older sediments is uncommon, limited to bedrock protected areas such as Dead-ice B e escarpments. Bedrock outcrops are common. Glacial advance was generally from the northwest, parallel to the streamlined topography d (NTS 62K), Manitoba r o c A landforms. Glacial till is typically silt rich. Glacial retreat occurred in a series of steps marked by moraines: the Darlingford Moraine k f s y a u s a l 100° 96° 92° 88° (~11,000 years old); the Sandilands Moraine, which represents the interlobate position of the Rainy lobe from the northeast and the t i w s n l l i i b Red River lobe from the northwest; the Birds Hill–Belair Moraine; the Teulon Moraine; and The Pas Moraine (~9000 years old). p 60° o s U i l p M n i Index Map pe 51° 64N 64P 54M George Island Moraine, contemporaneous with and to the east of The Pas Moraine, is another ice margin of the retreating Rainy 51° r e a 64O C Precambrian t i a G Saskatchewan s n A m la d n c shield p r lobe. s p ia i e s b l f il d e e o i lu l n l w B l te n s 54L 54K Dead-ice i a 64K 64J 64I 58° i w s a b a s y topography a r M In the Precambrian shield, rock outcrops dominate the landscape.
Load more

Recommended publications
  • Stra Th Cla Ir Co-Op Sells Food Store
    F RIDAY , J ANUARY 19, 2018 Volume 10 Number 44 S ERVING E RICKSON , O NANOLE , W ASAGAMING , S ANDY L AKE , E LPHINSTONE , R OLLING R IVER , K EESEEKOOWENIN AND SU RROUNDING AREA FREE TAKE ONE Strathcla ir Co-op sells food store >> Sa le to loca lly ow n ed J& P G roceries ta kes effect Ap ril 8 MARCIE HARRISON So uth M o unta in Press With the sale of the Strathclair Co-op food store to locally owned J&P Groceries, Strath - clair will soon become a one-grocery-store town. Details of the sale, which was finalized on Jan. 7, were discussed at a pubic meeting on The Board Thursday, Jan. 18, along wanted to with the reasons behind it. make sure that In an interview prior to the meeting, Strath - th e co m m u n ity clair Co-op General COLOUR GUARD Manager Valerie Collins ha s a s tro n g CINDY MURRAY/FOR SOUTH MOUNTAIN PRESS said it wasn’t an over - A blue jay stands at attention, adopting the crest up, chest out posture befitting this winter colour guard. Of all the birds that brave the food store in night decision, and that elements during Manitoba’s coldest months, the blue jay provides the brightest flash of colour in a landscape dominated by white. Often the store’s inability to th e co m m u n ity referred to as aggressive, the blue jay is not always a welcome guest at backyard feeders. However, if you enjoy watching their colourful turn a profit was just antics, be sure to put out some peanuts, black oil sunflower seeds or corn.
    [Show full text]
  • Mar 01 Manitoba --+
    BROWNLEE'S INDEXED RAILWAY AND GUIDE maR 01 manitoba --+----- PUBUSHED tlQcQ¥vY OF THE PROVI4I.@~MENT. ----- A COMPLETE ENCYCLOPJEDIA -OF-- THE PRAIRIE PROVINCE. -- -+ --- +- ----. PUBLIEHED BY J. H. BROWNLEE, BRANDON, MAN., NORTH\\ .. " 1 AhEN 1 FOk "The Dominion Illustrated." II IN-~ENDING SETTLERS In Manitoba and the Northwest Territories will find it to their advantage to call at the Northwest head office of the Massey Man­ ufacturing Co., Market Square; Winnipeg, or at their permanent local offices through­ out the country, where they will in a few hours gain more reliable information about the surrounding district' than they could learn in weeks by ordinary methods. Wherever you Pitch your Tent Look up the Massey Agent. He can tell you all about the settlers, the kind of soil, wood, water, proximity to schools and churches, the average price of land per acre, where the Free Grant Government Lands Are located, the average price of horses, Oxen, Cows, Lumber, &c., &c., and If you don't like his Plows, Harrows, Seeders, Drills, Wagons, Mowers. Horse Rakes, Self Binding Harvesters, &c., profit by his experience. SEE THE BACK COYER. {jr.2J" Cons u I r your' fl'iencls ca nnot get this CUIDE supply it by rnail on ,'eceipt or ~5 <·ts. nevvs dealers, the Publisher vvill 1. H . BROWNLEE, Brandon, Man. The Glory of a Man is his Strength 1l'he Great Strength Giver It is· not a Illere Extract or Meat, but contai"ns all the nutritious and life giving eleIllents of Meat. ., '" I A PERFECT FOOD FOR THE SICK. L " A WARMING AND NUTRITIOUS BEVERAGE.
    [Show full text]
  • Groundwater in Manitoba: Hydrogeology, Quality Concerns, Management
    Robert Betcher Water Resources Branch Manitoba Natural Resources Gary Grove National Hydrology Research Institute Environment Canada and Christian Pupp State of Environment Reporting Environment Canada Environmental Sciences Division National Hydrology Research Institute Environment Canada Saskatoon, Saskatchewan S7N 3H5 GROUNDWATER IN MANITOBA: HYDROGEOLOGY, QUALITY CONCERNS, MANAGEMENT NHRI Contribution No. CS-93017 March, 1995 ERRATA: Page 13, the first sentence beneath the heading “Groundwater Flow Systems” should read “The point-water potentionmetric surface…” Page 13, the caption for Figure 8 should read “Point-water potentionmetric surface and expected regional groundwater flow in the Winnipeg Formation” Groundwater in Manitoba: Hydrogeology, Quality Concerns, Management ABSTRACT Groundwater forms an important source of municipal, rally occurring constituents exceed drinking water guide- industrial, agricultural and residential water supply in lines locally. Many aquifers are poorly protected from Manitoba. Groundwater is available from a number of near-surface contamination sources and, as a result, extensive bedrock aquifers along the margins of Hudson anthropogenic contamination has been found in some Bay and within the Western Canada Sedimentary Basin areas. The major groundwater quality management con- and from sand and gravel aquifers found within glacial cerns include underground storage tanks, agricultural deposits in many parts of the province. The geological activities, saline water intrusion and waste disposal. framework for these aquifers is presented and the major aquifer units discussed in terms of occurrence, ground- Provincial legislation relating to water resources and water availability, yield and water quality. groundwater protection is summarized. Two agencies, Manitoba Natural Resources and Manitoba Environment, Groundwater quality is highly variable in most aquifer have primary responsibility for the development and units in Manitoba.
    [Show full text]
  • ROUTING GUIDE - Less Than Truckload
    ROUTING GUIDE - Less Than Truckload Updated December 17, 2019 Serviced Out Of City Prov Routing City Carrier Name ADAM LAKE MB WINNIPEG, MB Interline Point ALEXANDER MB WINNIPEG, MB Interline Point ALONSA MB WINNIPEG, MB Interline Point ALTAMONT MB WINNIPEG, MB Interline Point ALTONA MB WINNIPEG, MB Direct Service Point AMARANTH MB WINNIPEG, MB Interline Point ANGUSVILLE MB WINNIPEG, MB Interline Point ANOLA MB WINNIPEG, MB Interline Point ARBORG MB WINNIPEG, MB Interline Point ARDEN MB WINNIPEG, MB Interline Point ARGYLE MB WINNIPEG, MB Interline Point ARNAUD MB WINNIPEG, MB Interline Point ARNES MB WINNIPEG, MB Interline Point ARROW RIVER MB WINNIPEG, MB Interline Point ASHERN MB WINNIPEG, MB Interline Point ATIKAMEG LAKE MB WINNIPEG, MB Interline Point AUBIGNY MB WINNIPEG, MB Interline Point AUSTIN MB WINNIPEG, MB Interline Point BADEN MB WINNIPEG, MB Interline Point BADGER MB WINNIPEG, MB Interline Point BAGOT MB WINNIPEG, MB Interline Point BAKERS NARROWS MB WINNIPEG, MB Interline Point BALDUR MB WINNIPEG, MB Interline Point BALMORAL MB WINNIPEG, MB Interline Point BARROWS MB WINNIPEG, MB Interline Point BASSWOOD MB WINNIPEG, MB Interline Point BEACONIA MB WINNIPEG, MB Interline Point BEAUSEJOUR MB WINNIPEG, MB Direct Service Point BELAIR MB WINNIPEG, MB Interline Point BELMONT MB WINNIPEG, MB Interline Point BENITO MB YORKTON, SK Interline Point BERESFORD MB WINNIPEG, MB Interline Point BERESFORD LAKE MB WINNIPEG, MB Interline Point BERNIC LAKE MB WINNIPEG, MB Interline Point BETHANY MB WINNIPEG, MB Interline Point BETULA MB WINNIPEG,
    [Show full text]
  • Geomorphic and Sedimentological History of the Central Lake Agassiz Basin
    Electronic Capture, 2008 The PDF file from which this document was printed was generated by scanning an original copy of the publication. Because the capture method used was 'Searchable Image (Exact)', it was not possible to proofread the resulting file to remove errors resulting from the capture process. Users should therefore verify critical information in an original copy of the publication. Recommended citation: J.T. Teller, L.H. Thorleifson, G. Matile and W.C. Brisbin, 1996. Sedimentology, Geomorphology and History of the Central Lake Agassiz Basin Field Trip Guidebook B2; Geological Association of CanadalMineralogical Association of Canada Annual Meeting, Winnipeg, Manitoba, May 27-29, 1996. © 1996: This book, orportions ofit, may not be reproduced in any form without written permission ofthe Geological Association ofCanada, Winnipeg Section. Additional copies can be purchased from the Geological Association of Canada, Winnipeg Section. Details are given on the back cover. SEDIMENTOLOGY, GEOMORPHOLOGY, AND HISTORY OF THE CENTRAL LAKE AGASSIZ BASIN TABLE OF CONTENTS The Winnipeg Area 1 General Introduction to Lake Agassiz 4 DAY 1: Winnipeg to Delta Marsh Field Station 6 STOP 1: Delta Marsh Field Station. ...................... .. 10 DAY2: Delta Marsh Field Station to Brandon to Bruxelles, Return En Route to Next Stop 14 STOP 2: Campbell Beach Ridge at Arden 14 En Route to Next Stop 18 STOP 3: Distal Sediments of Assiniboine Fan-Delta 18 En Route to Next Stop 19 STOP 4: Flood Gravels at Head of Assiniboine Fan-Delta 24 En Route to Next Stop 24 STOP 5: Stott Buffalo Jump and Assiniboine Spillway - LUNCH 28 En Route to Next Stop 28 STOP 6: Spruce Woods 29 En Route to Next Stop 31 STOP 7: Bruxelles Glaciotectonic Cut 34 STOP 8: Pembina Spillway View 34 DAY 3: Delta Marsh Field Station to Latimer Gully to Winnipeg En Route to Next Stop 36 STOP 9: Distal Fan Sediment , 36 STOP 10: Valley Fill Sediments (Latimer Gully) 36 STOP 11: Deep Basin Landforms of Lake Agassiz 42 References Cited 49 Appendix "Review of Lake Agassiz history" (L.H.
    [Show full text]
  • RM of Birtle Information Bulletin 98-6
    Rural Municipality of Birtle Information Bulletin 98-6 Rural Municipality of Birtle Information Bulletin 98-6 Page 1 Rural Municipality of Birtle Information Bulletin 98-6 Prepared by: Land Resource Unit, Brandon Research Centre, Research Branch, Agriculture and Agri-Food Canada. Department of Soil Science, University of Manitoba. Manitoba Soil Resource Section, Soils and Crops Branch, Manitoba Agriculture. Printed December, 1998 Page 2 Information Bulletin 98-6 Rural Municipality of Birtle PREFACE ACKNOWLEDGMENTS This is one of a new series of information bulletins for individual Continuing support for this project has been provided by Brandon rural municipalities of Manitoba. They serve to introduce the newly Research Centre and PFRA Manitoba. The project was initiated by developed digital soil databases and illustrate several typical derived the Land Resource Unit under the Canada-Manitoba Agreement of and interpretive map products for agricultural land use planning Agricultural Sustainability. applications. The bulletins will also be available in diskette format for each rural municipality. The following individuals and agencies contributed significantly to the compilation, interpretation, and derivation of the information Information contained in this bulletin may be quoted and utilized contained in this report. with appropriate reference to the originating agencies. The authors and originating agencies assume no responsibility for the misuse, Managerial and administrative support was provided by: alteration, re-packaging, or re-interpretation of the information. R.G. Eilers, Head, Land Resource Unit, Brandon Research Centre, This information bulletin serves as an introduction to the land Research Branch, Agriculture and Agri-Food Canada. resource information available for the municipality. More detailed G.J.
    [Show full text]
  • Guide to Manitoba Memorial Types
    GUIDE TO MANITOBA MEMORIAL TYPES War Memorials in Manitoba: An Artistic Legacy GUIDE TO MANITOBA MEMORIAL TYPES he memorials honouring Manitoba’s dead of World War I are a profound historical legacy. They are also a major artistic achievement. This section of the study of Manitoba war memorials explores the Tmost common types of memorials with an eye to formal considerations – design, aesthetics, materials, and craftsmanship. For those who look to these objects primarily as places of memory and remembrance, this additional perspective can bring a completely different level of understanding and appreciation, and even delight. Six major groupings of war memorial types have been identified in Manitoba: Tablets Cairns Obelisks Cenotaphs Statues Architectural Monuments Each of these is reviewed in the following entries, with a handful of typical or exceptional Manitoba examples used to illuminate the key design and material issues and attributes that attend the type. Guide to Manitoba Memorial Types 1 War Memorials in Manitoba: An Artistic Legacy Tablets The apparently simple and elemental form of the tablet, also known as a stele (from the ancient Greek, with stelae as the plural), is the most common form of gravesite memorial. Given its popularity and cultural and historical resonance, its use for war memorials is understandable. The tablet is economical—in form and often in cost—but also elegant. And while the simple planar face is capable of conveying a great deal of inscribed information, the very form itself can be seen as a highly abstracted version of the human body – and thus often has a mysterious attractive quality.
    [Show full text]
  • Upper Cretaceous Colorado Group in the Pasquia Hills, Northeastern Saskatchewan: a Multidisciplinary Study in Progress
    Upper Cretaceous Colorado Group in the Pasquia Hills, Northeastern Saskatchewan: A Multidisciplinary Study in Progress 1 1 4 Claudia J Schroder-Adams , Dale A. Leckie , Jim Craig J' and John Bloch Schroder-Adams, C.J ., Leckie. D.A .. Craig, J. and Bloch, J. ( 1998): Upper Cretaceous Colorado Group in the l'asquia 11 ills. northeastern Sac;katchewan: A multidisciplinary study in progress; in Summary of Investigations 1999. Volumt.: I. Saskatchewan Geological Survey, Sask. Energy Mines, Misc. Rep. 99-4. 1. I. Introduction this volume; Cumbaa et al., 1992). It contains late Cretaceous bird bones (Tokaryk et al. , 1997). This and The upper part of the Upper Cretaceous Colorado the authors' continuous work on the Colorado Group Group (Cenomanian to Campanian) represents the led to a week's fieldwork in the Pasquia Hills during Cenomanian/middle Turonian Greenhorn and late the summer of 1997. Turonian/Santonian Niobrara sea-level cycles (Kauffman, 1984) and is widely distributed in the Western Canada Sedimentary Basin (WCSB). Both cycles reflect times of high sea level and inundation of 2. Stratigraphic Framework the western side of North America when the Boreal Stratigraphic nomenclature used in this study (Figure and Tethyan seas were connected. Resulting sequences 1) is based on the comprehensive lithological and are dominated by organic-rich shale and approximately forarniniferal study of Cretaceous outcrops in the contemporaneous episodes of global anoxia (Arthur et Manitoba Escarpment including the Pasquia Hills by al., 1987). Tectonic events and relative sea-level McNeil and Caldwell ( 1981 ). The stratigraphic interval fluctuations resulted in coarser elastic units found of interest here includes the Cenomanian Belle Fourche particularly in the western part of this fore land basin.
    [Show full text]
  • Municipal Officials Directory 2021
    MANITOBA MUNICIPAL RELATIONS Municipal Officials Directory 21 Last updated: September 23, 2021 Email updates: [email protected] MINISTER OF MUNICIPAL RELATIONS Room 317 Legislative Building Winnipeg, Manitoba CANADA R3C 0V8 ,DPSOHDVHGWRSUHVHQWWKHXSGDWHGRQOLQHGRZQORDGDEOH0XQLFLSDO2IILFLDOV'LUHFWRU\7KLV IRUPDWSURYLGHVDOOXVHUVZLWKFRQWLQXDOO\XSGDWHGDFFXUDWHDQGUHOLDEOHLQIRUPDWLRQ$FRS\ FDQEHGRZQORDGHGIURPWKH3URYLQFH¶VZHEVLWHDWWKHIROORZLQJDGGUHVV KWWSZZZJRYPEFDLDFRQWDFWXVSXEVPRGSGI 7KH0XQLFLSDO2IILFLDOV'LUHFWRU\FRQWDLQVFRPSUHKHQVLYHFRQWDFWLQIRUPDWLRQIRUDOORI 0DQLWRED¶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erek Johnson 0LQLVWHU TABLE OF CONTENTS MANITOBA EXECUTIVE COUNCIL IN ORDER OF PRECEDENCE ............................. 2 PROVINCE OF MANITOBA – DEPUTY MINISTERS ..................................................... 5 MEMBERS OF THE LEGISLATIVE ASSEMBLY ............................................................ 7 MUNICIPAL RELATIONS ..............................................................................................
    [Show full text]
  • Manitoba Outdoor Adventures Guide
    Manitoba Outdoor 2011 Adventures Guide Bloodvein River EXPLORE RIDING MOUNTAIN NATIONAL PARK OF CANADA EXPLOREZ LE PARC NATIONAL DU CANADA DU MONT-RIDING 1 888 773-8888 www.pc.gc.ca PARKS CANADA CAMPGROUND RESERVATION SERVICE SERVICE DE RÉSERVATION DES EMPLACEMENTS DE CAMPING DE PARCS CANADA www.pccamping.ca 1 877 RESERVE (1 877 737-3783) TTY only/ATS seulement : 1 866 787-6221 Your Guide to Adventure Wildlife & Bird Watching ..................................................... 3 Canoeing / Kayaking .........................................................15 Hiking ..................................................................................21 Cycling .................................................................................31 Skiing ...................................................................................39 Cross-Country ...........................................................................40 Downhill .....................................................................................47 Snowmobiling ....................................................................48 Winnipeg Interlake Grab Bag of Adventures Central Plains Aurora Borealis (Northern Lights) ....................................50 Pembina Valley Dogsledding / Skijoring ......................................................51 Western Parkland Geocaching ..............................................................................52 North of 53˚ Rock / Ice Climbing ...............................................................53 Eastern Skateboarding
    [Show full text]
  • Public Accounts of the Province of Manitoba for the Fiscal Year Ending
    200 CASH PAYMENTS TO CORPORATIONS, ETC., 1967 -1968 GOVERNMENT OF THE PROVINCE OF MANITOBA Cash Paid to Corporations, Firms, Individuals, Municipalities, Cities, Towns and Villages, Arranged in Alphabetical Order to Show the Amount Paid to Each Payee Where the Total Payments Exceed $1,000.00 for the Year Ended 31st March, 1968. For Salaries, Page No. 178 Name Address Amount Name Address Amount “A” Acme Welding & Supply Ltd., Winnipeg . 7,281.88 A Active Electric Co., Acres & Company Ltd., Winnipeg .$ 2,287.40 H. C., Niagara Falls, Ont. 81,967.21 A. & A. Frozen Foods Ltd., Acres Western Ltd., Winnipeg . 1,031.29 Winnipeg . 12,926.22 A. E. I. Telecommunication, Winnipeg . 4,745.67 Adam, A., Ste. Rose . 1,232.79 Adams Supply Company A. & F. Trucking Service, Ltd., A., Winnipeg . 1,645.22 Virden . 1,829.88 Adams, Alfred Lloyd & A. & H. Equipment Leasing Adams, Laura, Winnipeg 21,312.75 Ltd., Winnipeg . 4,264.79 Adams, Lorraine M., A. & N. Groceteria, Dauphin . 1,250.53 Thompson . 5,020.75 Adam’s Store, Skowman .... 1,959.37 Abbott Laboratories Ltd., Adams, Walter, Montreal, Que. 6,576.29 Portage la Prairie . 1,078.00 Abelard-Schuman Canada Adanac Household Supply Ltd., Toronto, Ont. 2,152.56 (1961) Ltd., Winnipeg . 24,919.97 Aberhart Memorial Sana¬ Addison-Wesley Canada torium, Edmonton, Alta... 2,376.00 Ltd., Don Mills, Ont. 13,983.59 Abex Industries of Canada Addison’s, Carberry . 1,498.60 Limited, Montreal, Que..... 2,305.00 Addressograph-Multigraph Abitibi Manitoba Paper of Canada Ltd., Ltd., Pine Falls . 7,540.03 Toronto, Ont.
    [Show full text]
  • OCTOBER 2013 the ONLY ALL CANADIAN DISTRICT in 5M Just Ask!
    ManitobaLion VOLUME 28 Number 02 OCTOBER 2013 THE ONLY ALL CANADIAN DISTRICT IN 5M Just Ask! istrict 5M13 needs more Lions to maintain Global Membership Team (GMT) of 5M13 is seeking your help in getting Dbeing 5M13! At the beginning of Septem- our membership up to at least 1,250 members by the end of January 2014 so we ber we had 1,195 members and we need 1,250 may celebrate this accomplishment at the district convention in mid-February, to maintain present district status. and from there to 1,300 members by the end of June this Lion year. For clubs with 20 or less members who bring in +3 members and How do we do this? clubs over 20 members have a net gain of +4 will get ONE free convention registration per club for the new member of their WE JUST ASK OTHERS TO choice. JOIN the best service club in the world. Have you asked a neighbor to be a LION? Have Each cabinet member has pledged to invite two new members as well. you made sure present LIONS are being treated properly so they remain being a LION? You see we Th en we need to start up some new Lions clubs, or branch clubs in areas lost more Lions last year than we gained and we that do not have the privilege to have a Lions club in their community. So if you brought over 120 new Lions BUT lost over 140 – know of any areas that we should address, please do contact your zone chair whom why? they will share with the GMT of our district.
    [Show full text]