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Saskatchewan Regional Newcomer Gateways
Saskatchewan Regional Newcomer Gateways Updated September 2011 Meadow Lake Big River Candle Lake St. Walburg Spiritwood Prince Nipawin Lloydminster wo Albert Carrot River Lashburn Shellbrook Birch Hills Maidstone L Melfort Hudson Bay Blaine Lake Kinistino Cut Knife North Duck ef Lake Wakaw Tisdale Unity Battleford Rosthern Cudworth Naicam Macklin Macklin Wilkie Humboldt Kelvington BiggarB Asquith Saskatoonn Watson Wadena N LuselandL Delisle Preeceville Allan Lanigan Foam Lake Dundurn Wynyard Canora Watrous Kindersley Rosetown Outlook Davidson Alsask Ituna Yorkton Legend Elrose Southey Cupar Regional FortAppelle Qu’Appelle Melville Newcomer Lumsden Esterhazy Indian Head Gateways Swift oo Herbert Caronport a Current Grenfell Communities Pense Regina Served Gull Lake Moose Moosomin Milestone Kipling (not all listed) Gravelbourg Jaw Maple Creek Wawota Routes Ponteix Weyburn Shaunavon Assiniboia Radwille Carlyle Oxbow Coronachc Regway Estevan Southeast Regional College 255 Spruce Drive Estevan Estevan SK S4A 2V6 Phone: (306) 637-4920 Southeast Newcomer Services Fax: (306) 634-8060 Email: [email protected] Website: www.southeastnewcomer.com Alameda Gainsborough Minton Alida Gladmar North Portal Antler Glen Ewen North Weyburn Arcola Goodwater Oungre Beaubier Griffin Oxbow Bellegarde Halbrite Radville Benson Hazelwood Redvers Bienfait Heward Roche Percee Cannington Lake Kennedy Storthoaks Carievale Kenosee Lake Stoughton Carlyle Kipling Torquay Carnduff Kisbey Tribune Coalfields Lake Alma Trossachs Creelman Lampman Walpole Estevan -
Mannville Group of Saskatchewan
Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan. -
View of Valley and Ridge Structures from ?:R Stop IX
GIJIDEBOOJ< TECTONICS AND. CAMBRIAN·ORDO'IICIAN STRATIGRAPHY CENTRAL APPALACHIANS OF PENNSYLVANIA. Pifftbutgh Geological Society with the Appalachian Geological Society Septembet, 1963 TECTONICS AND CAMBRIAN -ORDOVICIAN STRATIGRAPHY in the CENTRAL APPALACHIANS OF PENNSYLVANIA FIELD CONFERENCE SPONSORS Pittsburgh Geological Society Appalachian Geological Society September 19, 20, 21, 1963 CONTENTS Page Introduction 1 Acknowledgments 2 Cambro-Ordovician Stratigraphy of Central and South-Central 3 Pennsylvania by W. R. Wagner Fold Patterns and Continuous Deformation Mechanisms of the 13 Central Pennsylvania Folded Appalachians by R. P. Nickelsen Road Log 1st day: Bedford to State College 31 2nd day: State College to Hagerstown 65 3rd day: Hagerstown to Bedford 11.5 ILLUSTRATIONS Page Wagner paper: Figure 1. Stratigraphic cross-section of Upper-Cambrian 4 in central and south-central Pennsylvania Figure 2. Stratigraphic section of St.Paul-Beekmantown 6 rocks in central Pennsylvania and nearby Maryland Nickelsen paper: Figure 1. Geologic map of Pennsylvania 15 Figure 2. Structural lithic units and Size-Orders of folds 18 in central Pennsylvania Figure 3. Camera lucida sketches of cleavage and folds 23 Figure 4. Schematic drawing of rotational movements in 27 flexure folds Road Log: Figure 1. Route of Field Trip 30 Figure 2. Stratigraphic column for route of Field Trip 34 Figure 3. Cross-section of Martin, Miller and Rankey wells- 41 Stops I and II Figure 4. Map and cross-sections in sinking Valley area- 55 Stop III Figure 5. Panorama view of Valley and Ridge structures from ?:r Stop IX Figure 6. Camera lucida sketch of sedimentary features in ?6 contorted shale - Stop X Figure 7- Cleavage and bedding relationship at Stop XI ?9 Figure 8. -
Spring Runoff Highway Map.Pdf
NUNAVUT TERRITORY MANITOBA NORTHWEST TERRITORIES 2007 SPRING RUNOFF POTENTIAL Waterloo Lake (Northernmost Settlement) Camsell Portage .3 999 White Lake Dam AND Uranium City 11 10 962 19 AFFECTEDIR 229 Fond du Lac HIGHWAYS Fond-du-Lac IR 227 Fond du Lac IR 225 IR 228 Fond du Lac Black Lake IR 224 IR 233 Fond du Lac Black Lake Stony Rapids IR 226 Stony Lake Black Lake 905 IR 232 17 IR 231 Fond du Lac Black Lake Fond du Lac ATHABASCA SAND DUNES PROVINCIAL WILDERNESS PARK BELOW NORMAL 905 Cluff Lake Mine 905 Midwest Mine Eagle Point Mine Points North Landing McClean Lake Mine 33 Rabbit Lake Mine IR 220 Hatchet Lake 7 995 3 3 NEAR Wollaston Lake Cigar Lake Mine 52 NORMAL Wollaston Lake Landing 160 McArthur River Mine 955 905 S e m 38 c h u k IR 192G English River Cree Lake Key Lake Mine Descharme Lake 2 Kinoosao T 74 994 r a i l CLEARWATER RIVER PROVINCIAL PARK 85 955 75 IR 222 La Loche 914 La Loche West La Loche Turnor Lake IR 193B 905 10 Birch Narrows 5 Black Point 6 IR 221 33 909 La Loche Southend IR 200 Peter 221 Ballantyne Cree Garson Lake 49 956 4 30 Bear Creek 22 Whitesand Dam IR 193A 102 155 Birch Narrows Brabant Lake IR 223 La Loche ABOVE 60 Landing Michel 20 CANAM IR 192D HIGHWAY Dillon IR 192C IR 194 English River Dipper Lake 110 IR 193 Buffalo English River McLennan Lake 6 Birch Narrows Patuanak NORMAL River Dene Buffalo Narrows Primeau LakeIR 192B St.George's Hill 3 IR 192F English River English River IR 192A English River 11 Elak Dase 102 925 Laonil Lake / Seabee Mine 53 11 33 6 IR 219 Lac la Ronge 92 Missinipe Grandmother’s -
PALEOZOIC STRATIGRAPHIC COLUMN of Central Pennsylvania
PALEOZOIC STRATIGRAPHIC COLUMN of Central Pennsylvania _____________________________________________________________________*Ridge Makers System & Series Formation and Members General Description Llewellyn Formation Cycles of conglomerate or sandstone; underclay coal, shale Pnn. L & N 2000’+ Pottsville Formation* Cycles of conglomerate or sandstone; underclay coal, shale L & M 1400’ Mauch Chunk Grayish red and gray shale M 5000’ Miss. Pocono* Mount Carbon Gray to buff, medium grained, cross-bedded sandstone 1600’ 940’ Beckville Gray to buff, medium grained, cross-bedded sandstone Lower 225’ Spechty Kopf Gray, fine and medium grained sandstone conglomerate 435’ near middle and base Catskill Duncannon Asymmetric, upward-fining fluvial cycles, basal nonred, locally 7250’ 2000’ conglomeratic sandstone is overlain by grayish red sandstone and siltstones Sherman Creek Interbedded grayish red claystone and fine grained, cross- 2400’ bedded sandstone Upper Irish Valley Interbedded, grayish red and olive gray sandstone, siltstone, 2850’ shale, overlain upward-fining cyclic deposits of gray sandstone and red siltstone Trimmers Rock Medium gray siltstone and shale, with fine grained sandstone in 2000’ upper part; graded bedding common Harrell Olive and medium light gray shale 200’ Mahantango Sherman Ridge* Olive gray, fossiliferous, claystone with interbedded fine 1600’ 600’ sandstones which coarsen upward Montebello Olive gray, medium grained, locally conglomeratic, fossiliferous 600’ sandstone, interbedded with siltstone and claystone in upward- -
PARCS UPDATE #108 Nov
1 Editorial Introducti PARCS UPDATE #108 Nov. 28/2019 All about our Community Members RV of Greig Lake DISTRICT of LAKELAND OH of Little Fishing Lake RM of MERVIN OH of Evergreen Acres OH of Powm Beach AcresOH of Turtle Lake South OH of Kopp’s Kove BayOH of Horseshoe Bay OH of Crystal Bay Sunset RV of Chitek Lake RV of Candle Lake OH of Evergreen Brightsand RV of Tobin Lake OH of Parkland Beach OH of Indian Point Golden OH of Sunset View Beach SandsOH of Turtle Lake Lodge OH of Mowry Beach RM OF HOODOO OH of Cudsaskwa OH of Little RM of MEOTA RV of Aquadeo OH of Balone Beach Swan River OH of Maymont Beach RV of Cochin RV of Wakaw Lake OH of Pelican Point POWL OH of Lakeview Beach RV of Leslie Beach OH of North Shore Fishing Lake RV of Chorney Beach OH of Ottman – Murray Beach RV of Shields OH of RV pf Manitou Beach RV of Thode Crystal Lake OH of Burgis OH of McPheat Park Beach OH of Sorenson’s Beach RV of Kannata Valley Sandy Shores Subdivision RV of Coteau Beach OH of North Colesdale Park RV of Sunset Cove RV of Mistusinne RV of Glen Harbour RV of Sask Beach OH of Hitchcock Bay RV of Island View OH of Pasqua Lake RV of Alice Beach OH of Taylor Beach RV of Melville Beach RV of Etter’s Beach RV of Beaver Flat RV of District of Katepwa RV of Bird’s Point Lumsden RV of West End Beach RV of South Lake PARCS bylaws divide the province into four regions for the purpose of electing 4 regional directors to the PARCS board. -
A Note on Petroleum Occurrences in the Kindersley District, Southwestern Saskatchewan
A Note on Petroleum Occurrences in the Kindersley District, Southwestern Saskatchewan J E. Christopher I Christopher, J.E. ( 1999): A nolc on petroleum occurrences in the Kindersley district, southwestern Saskatchewan: in Summary of Investigations 1999. Volume I. Saskatchewan Geological Survey. Sask. Energy Mines, Misc. Rep. 99-4.1. 1. Introduction shows in the context of the Success Formation within the general detrital basin on the Mississippian erosion There are few regions in Saskatchewan that offer as surface. many petroleum exploration options as the Kindersley di strict. It is productive in: I) natural gas from the Upper Cretaceous Judith River Formation, 2) petroleum and natural gas from the Lower 2. Lithology Cretaceous Viking and Mannville formations, 3) The Kindersley district is areally delineated by the petroleum from the Jura-Cretaceous Success distribution of deposits that infill and blanket the Formation, and 4) Mississippian Bakken formations. erosion surface on the Mississippian Madison Oil shows are widespread in the Mannville, Success, Formation. These deposits are described regionally by Bakken, and Upper Devonian Birdbear formations. Maycock (1967) and detailed by White (1969) for the This note examines the general setting of these oil Hoosier Oilfield. Maycock ( 1967, p 18) noted the presence of two lithologic types: "cherty breccio-conglomerates" as in the core from the Imperial Warrior l0-29-27-25W3 well (depth: 923.5 to 938.8 m), and ''whitish sandstones", unlike those of the overlying Mannville, cored in the Tidewater Plato Crown 9-22-24- l 9W3 well (depth: 831 .5 to 857.4 m). Core data from the Success Formation are relatively scattered, but representative well cuttings are available from most wells in the district. -
State of Lake Diefenbaker Report
State of Lake Diefenbaker Prepared for: Consultation Meeting on May 30, 2012. Document was edited and revised on October 19, 2012 Executive Summary The purpose of this report is to provide the stakeholders with some context of the South Saskatchewan River project, the management issues associated with the operation of the Gardiner and Qu’Appelle River Dams, and the health of Lake Diefenbaker and the Lake Diefenbaker Watershed. This report summarizes the management activities associated with the operation of the South Saskatchewan River Project and the potential outcomes related to these management activities. Information within this report provides a basis for evaluating the management objectives and setting priorities for the operation of the Project. Table 1 outlines the various reservoir management activities and the resulting consequences of these activities. The South Saskatchewan River Project, of which Lake Diefenbaker and the Gardiner and Qu’Appelle River Dams are the primary components, is a critical water resource for the province of Saskatchewan. The South Saskatchewan River Project is currently owned and managed by the Water Security Agency of Saskatchewan for multiple services, including irrigation, municipal and industrial water supply, hydroelectric power generation, recreation, aquatic and wildlife habitat, and downstream flood control. The services provided by the Project are fundamental to the province’s economic, social and environmental well being. Lake Diefenbaker construction started after an agreement between the province of Saskatchewan and the Government of Canada, which was signed in 1958. The initial purpose of the project was to form a reservoir that could provide source water to irrigate approximately 200,000 hectares of farmland in central Saskatchewan and the Qu’Appelle Valley. -
Xsec A-A Sht1of2 Layout FINAL V
U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 3425 U.S. GEOLOGICAL SURVEY (SHEET 1 OF 2) Explanatory pamphlet accompanies map A Ontario Allegheny Lowlands Plateau province province SEVERNE WATKINS-BEAVER LODI POINT FIRTREE DAMS ALPINE VAN ETTEN ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE ANTICLINE GLENORA SYNCLINE UNNAMED COHOCTON CORBETT POINT ENFIELD CAYUTA SYNCLINE SYNCLINE SYNCLINE SYNCLINE SYNCLINE Bend in section Bend in section Bend in section New York W SE Oatka Genesee NW SE Canisteo NW SW Pennsylvania Black Creek River Canaseraga River Tuscarora Creek Creek Creek FEET MILES 0 10 20 30 40 50 60 70 80 90 3,000 1 2 3 4 5 6 William Duchscherer, Jr. E.F. Blair and Associates NYS Natural Gas Company E.F. Blair and Associates Bowdoin Storage Service Inc. NYS Natural Gas Company No. 1 J. Klotzbach No. 1 L. Tyler No. 1 Albert McClurg No. 1 Arthur N. Kennedy No. 1 Hubbard No. 1 Robert Olin API No. 31-037-05117 API No. 31-037-04593 API No. 31-051-04552 API No. 31-051-04630 API No. 31-101-21496 API No. 31-101-03924 Genesee Co., New York Genesee Co., New York Livingston Co., New York Livingston Co., New York Steuben Co., New York Steuben Co., New York Perrysburg Formation Dunkirk Dunkirk Shale Shale 2,000 Member Wiscoy Sandstone Member Java Perrysburg West River Shale, Nunda Wiscoy Sandstone Member Formation Formation Genundewa Sandstone Member unnamed Pipe Creek 0 Pipe Creek shale member Limestone, Penn Member Shale Member Shale Member Perrysburg Yan Shale, and rmation Formation 0 Dun West River Shale, Java Fo kirk -
MG 259 - Keith Ewart Photograph Collection
MG 259 - Keith Ewart Photograph Collection Dates: 1885-2009 (inclusive), 1977-2009 (predominant). Extent: ~7000 photographs, 125 glass plates, 322 postcards. Biography: Keith Ewart was born on 9 September 1931, and was raised and schooled in Weyburn, Sk. He trained as a psychiatric nurse and spent most of his working career in Moose Jaw. He has lived in Saskatoon since 1989. A photographer by vocation, in 1975 Ewart began taking images of buildings in Saskatchewan. He has published two volumes of his photographic documentation of railway stations and railway buildings. He passed away in 2011. Scope and content: This collection includes images Keith Ewart has taken of structural landmarks, particularly in Saskatchewan, as well as glass plates from a Moose Jaw photographer ca. 1915-1920. The collection also contains some images that were not taken by Ewart, but were collected by him. Arrangement: This fonds was received inn groups of smaller accessions which have been kept in their original groupings. They are organized as such: Pg. 2001-092: Schools/Churches/Railway Buildings/Moose Jaw portraits. 2 2003-128: Court Houses, Town Halls, Banks, Businesses, Houses. / Bridges, Barns 36 2004-118: Canadian National and Pacific Railway Stations 49 2005-119: Rail stations in British Columbia. Manitoba Alberta 55 2006-112: Ontario, Quebec, Maritimes and USA train stations. 62 2007-100: Rail station photos, various 69 2008-096: Railway station postcards and photos (images by others) 80 2009-103: Elevators photos of Saskatchewan and Manitoba. 87 2010-105: Elevators in Saskatchewan and Alberta. 111 Related collections include the Joanne Abrahamson collection (MG 244); the Hans Dommasch fonds (MG 172); the photographic series in the Saskatchewan Wheat Pool fonds (MG 247); and the Community Progress Competitions in the Walter Murray fonds, (MG 1). -
Lake Diefenbaker Tourism Destination Area Plan
Lake Diefenbaker Tourism Destination Area Plan Lake Diefenbaker Tourism Destination Area Plan “A tourism destination area is a geographic area in which attractions, businesses, residents and regulatory authorities work together to deliver distinctive, high quality services and experiences, capable of attracting and holding significant numbers of visitors, from both within and outside the province.” Lake Diefenbaker Tourism Destination Area Plan Letter of Transmittal July 16, 2008 Dr. Lynda Haverstock, President and Chief Executive Officer, Tourism Saskatchewan, 1922 Park Street, Regina, Saskatchewan Dear Dr. Haverstock: We are pleased to submit the Lake Diefenbaker Tourism Destination Area Plan. The plan identifies tourism development issues and opportunities, and recommends specific strategies and actions to deal with them. The Tourism Planning Committee included a number of local stakeholders and representatives of tourism associations. In addition, public meetings held at Riverhurst, Elbow, Davidson, Kyle, Demaine, Outlook, and the Whitecap Dakota First Nation gave residents an opportunity to provide input in developing the plan. We would appreciate you forwarding copies of the plan to the Ministry of Tourism, Parks, Culture, and Sport, the Ministry of the Environment, the Ministry of Highways and Infrastructure, the Ministry of Enterprise and Innovation, and the Ministry of Municipal Affairs. The plan includes recommendations that pertain to these Ministries. We appreciate the assistance provided by Tourism Saskatchewan throughout the planning process, and we look forward to implementation of the plan. Sincerely, The Lake Diefenbaker Tourism Destination Area Planning Committee I Lake Diefenbaker Tourism Destination Area Plan PLANNING COMMITTEE Jim Tucker Russ McPherson General Manager - Mid Sask CFDC/ER Project Manager – WaterWolf M.L. -
Description of the Bessemer and Vandiver
DESCRIPTION OF THE BESSEMER AND VANDIVER INTRODUCTION the west of the Appalachian Plateaus are the Interior Low mentary, including limestone, dolomite, conglomerate, sand LOCATION AND EXTENT OF THE AREA Plateaus, which are included in the Interior Plains by the stone, and shale, which have been greatly disturbed by folding United States Geological Survey but which in the opinion of and faulting, as hereinafter described. The Bessemer and Vandiver quadrangles, which are called some, including the writer, should be included in the Appala in this folio the Bessemer-Vandiver area, are in Jefferson and chian Highlands. SUBDIVISIONS IN ALABAMA Shelby counties in the north-central part of Alabama. (See The boundary between the Piedmont and Blue Ridge Gahaba Ridges. Although the province is in general a fig. 1.) The area is bounded by parallels 33° 15' and 33° provinces is the east foot of the Blue Ridge and the foot of valley, there are within it many high ridges that extend the high but irregular eastern scarp of the mountains of west parallel to its general direction, of which Red Mountain is a ern North Carolina and northern Georgia which form the good example. These ridges are generally grouped along the southern extension of the Blue Ridge. The boundary between west side of the valley from New York to Alabama. In Ala the Blue Ridge and Appalachian Valley provinces is the west bama the ridge section includes all the valley west of the east foot of the Blue Ridge of Virginia and of the high mountains margin of the Coosa coal field and of a line in continuation of of eastern Tennessee.