Ca 1978 ISSS Tours 5+13E Report.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Ca 1978 ISSS Tours 5+13E Report.Pdf r ~-=- · - '" - __ .._. ,1'..,.-- .. ~..c-.;.... o:· -- .. •· ... ~:. -:_.. ~-· .. 11th CONGRESS INTERNATIONAL SOCIETY OF SOIL SCIENCE EDMONTON, CANADA JUNE, 1978 GUIDEBOOK FOR A TOUR TO OBSERVE SOIL LANDSCAPES AND CROPPING SYSTEMS IN CENTRAL AND SOUTHERN ALBERTA AND SOUTHWESTERN SASKATCHEWAN TOURS 5 AND 13 T. W. PETERS AGRICULTURE CANADA, SOIL SURVEY, EDMONTON, ALBERTA J.A. SHIELDS AGRICULTURE CANADA, SOIL RESEARCH INSTITUTE OF OTTAWA, ONTARIO J.G. ELLIS SASKATCHEWAN INSTITUTE OF PEDOLOGY, SASKATOON, SASKATCHEWAN GUIDEBOOK EDITORS D.F. ACTON AND L.S. CROSSON CONTRIBUTION OF SASKATCHEWAN INSTITUTE OF PEDOLOGY S.R.I. No. 652 SASKATOON, SASKATCHEWAN PREFACE The a geographical area of great interest. a resources, but sparsely popu­ better appreciate the scale, nature route and general relief across the western in Fig. P.l. les) in southern Alberta and soil zonat on ecting gradual anges ces from Edmonton southeast and t. It also witnesses the e evation on the anks the n climates, soils and landforms are rises and cropping practises. Tour lement the excursion itself by providing descri ve i areas traversed. The Guide is arranged in three section I or Plains of Canada, the daily log, ces. nying maps provide an informative tra ogue concerni landforms. Crop yields and management practices on di areas are discussed in relation to soil capability. are interspersed throughout log. Appendix A desc s, Appendix B contains meteorological data and Appendix C con on relating to crop yields and production costs. i i i 109' 108° 54° ALBERTA- SASKATCHEWAN 53' 52° 50° I 49° Selected City or Town 0 __ .J _______ 49' Overnight Stop cfu Tour Route . .. - 0 20 40 60 80 MILES t--·---,----1, -y 20 40 60 80 100 120 140 KILOMETRES 114' 113' 112' 111° 110' 109' 108° FIGURE P.l THE ROUTE AND GENERAL RELIEF MAP FOR TOURS 5 and 13 iv TABLE OF CONTENTS Page THE INTERIOR PLAINS Or CANADA .. .. .. .. .. ... .. .. .. .. ........ .. 1 Major Physiographic Regions of Canada ... ... ... .. .. .......... 2 The route . 4 Wisconsin Glaciation and Deposits in the Interior Plains ... 6 Bedrock Geology of the Interior Plains . .. ........ ......... .. 9 Physiographic Divisions of the Interior Plains .... .......... 11 Principal Rivers and Drainage Basins ... ................ ..... 13 Soil Temperature of the Interior Plains . .. ... .. .. .. 15 Soil Moisture of the Interior Plains . 18 Agro-climatic subregions of the Interior Plains ..... .... .. 18 Vegetation of the Interior Plains .. ...... .. ................. 20 Zonal soils of the Interior Plains ............... ~.... ...... 23 Main Types of Farming in the Interior Plains ................ 27 Canada Land Inventory of the Interior Plains ... ooo••o•••oo·. 30 Land Survey Systems in the Interior Plains ........ ······oo.. 32 LEGEND FOR DAILY TOUR ROUTE MAPS ............. o ·••o•o•••o····· •••• 38 DAY 1. CROPPING PRACTICES AND YIELDS OF BLACK AND DARK BROWN CHERNO- ZEMIC SOILS; EDMONTON TO DRUMHELLER ... o •••• •o o••o•· •• ••••• 44 Site l: Black Solodized Solonetz ....... 0 •••• o. 0 •••• o 0 ••••• 49 Solonetzic Soils ...... o •••••••••••••••••••• o ••• o ••••••••• o 50 Summerfallow ·········o···········o •• ooo•·······••o••oo•o• 53 000 00 0 Site 2: Orthic Dark Brown Chernozemic '' ' •••• ••••••• 55 Site 3: Rego Dark Brown Chernozemic ....... •o••········ 0 •• 56 DAY 2. SOILS AND AGRICULTURE OF THE DARK BROWN AND BROWN SOIL ZONES; DRUMHELLER TO BROOKS o ••••••• o •• o •••••••••• o •• o •••• o •••••• o 58 Production Costs . 0 ••••••• 0 •••••• 0 ••••• o0 0 •• 0 ••• 0 •••• o.... 58 Alberta Horticulture Research Centre .. ·····o·•·••o••oo•.. 62 DAY 3. BROWN CHERNOZEMIC AND SOLONETZIC SOILS AND THEIR AGRICULTURAL UTILIZATION; BROOKS TO MEDICINE HAT ................. o 0 ' •• 64 Dinosaur Park ....... o •••••••••••••••• o •••• o............... 64 Site 4: Brown Solodized Solonetz •o········ oo••·••oo•• 0 ••o 64 Site 5· Brown Solod . o •••• o •••• o ••••••• o ••••••• o ••• o....... 64 Developments of Ranching and Farming in Southeastern Alberta 67 DAY 4. DRYLAND SALINITY IN THE BROWN SOIL ZONE; MEDICINE HAT TO SWIFT CURRENT ..... o ••••• o ••••••••••• o o ••••••• o •• o ••••••••• o.... 70 Great Sand Hills ... o •••• o •••••• 0. o ••••••••••• o •••• o. 0.... 76. Site 6: Orthic Regosol -Saline Phase ..... o•······· ...... 79 Site 7: Orthic Brown Chernozemic ....... o.... ... 79 So i 1 Sa 1 in i ty o •••••••••• o ••••••••••••••••••••••••••• o • • • • • 7 9 Swift Current Research Station ······o· ····o•o•• o········· 83 v Page DAY 5. PRAIRIE TO PINE; SWIFT CURRENT TO MEDICINE HAT VIA THE CYPRESS HILLS . 85 Swift Current Loess . .. 85 Site 8: Orthic Brown to Dark Brown Chernozemic . ........... 88 Avena Community Pasture .................. -·.............. 90 General Description of the Cypress Hills Area .......... ... 92 Historic Fort Walsh ........... ..................... .. .. ... 95 DAY 6. BROWN AND DARK BROWN CHERNOZEMIC SOILS UNDER IRRIGATION AND DRYLAND AGRICULTURE; MEDICINE HAT TO LETHBRIDGE .... .. ..... 97 Site 9: Orthic Brown Chernozemic .... .............. ..... .. 100 Site 10: Rego Dark Brown Chernozemic-Carbonated Phase ..... 103 Site 11: Calcareous Dark Brown Chernozemic ... ........ ..... 103 Lethbridge Research Station ... ..... .......... .... .... .. .. 103 DAY 7. REST DAY . .. 104 DAY 8. LAND USE PANORAMA FROM THE PLAINS TO THE FOOTHILLS; LETHBRIDGE TO CALGARY . 107 Wind Erosion . 107 Chinook . 110 Buffalo Jump ............................. · .... · ...... · .. ·. 110 Site 12: Orthic Black Chernozemic .................. ~...... 112 DAY 9: BLACK CHERNOZEMIC AND SOLONETZIC SOILS, THEIR UTILIZATION AND AVERAGE CROP YIELDS; CALGARY TO EDMONTON ··············· .. 114 Site 13: Gleyed Eluviated Black Chernozemic .... ........ ... 119 Lacombe Research Station ........................ .. .. ..... 119 REFERENCES o 1>" 1> o 11 <> o o $II! II> fll 0 II 0 o .o o o" 0 <11 1> It" 1101 t1 <1 <t"' .. (i! 0 G" 1>" 'I 10 <>'" & 0 "'" "" e ill e I" 0 124 APPENDIX A. Field Description, Analyses, and Micromorphological Descriptions of Soil Sites ......................... 126 APPENDIX B. Meteorological Data 158 APPENDIX C. Crop Yields and Production Costs . 163 APPENDIX D. ·Format for Micromorphological Descriptions 170 vi LIST OF APPENDICES Page APPENDIX A. , ANALYSES, AND MICROMORPHOLOGICAL IL SI . ........... 126 Appendix A.l.l. is. and ogy onetzic so l 126 Appendix A.l.2. 1 Site 2 128 Appen x A. l. 3. ion, analysis, and cromorphology Che c soil at te 3 131 Appendix A.3.4. on, anal is, and cromorphology zed Solonetz soil at Site 4 134 Appendix A.3.5. eld ion analysis of a Brown Solod soil 5 (Brooks) .......................... 136 Appendix A.4.6. analysis of an Orthic Regosol seat Site 6 (Benallack Farm) . .. ... 138 Appendix A.4.7. ption and analysis of anOrthic Dark soil at Site 7 (Ben a 11 ack Farm). .. 140 Appendix A.5.8. eld ption, analysis, and micromorphology an ic Brown to Dark Brown soil at Site 8 (Girodat Farm) . .. .. .. .. .. .. .. .. .. .. 142 Appendix A.6.9. Fi d ption, analysis, and micromorphology of an Orthic Brown Chernozemic soil at Site 9 ( ). .. 145 Appendix A.6.10. on analysis of a Rego Dark Brown c soil-carbonated phase at Site 10 ) . 147 Appendix A. 6. 11. and analysis of a Calcareous Dark c 1 at Site 11 (Lethbridge) ..... 149 Appendix A.8.12. cromorpho logy c s l at te 12 152 Appendix A.9. 13. Field scri ion, analysis, and micromorphology of a.Gl El ated Black Chernozemic soil at Site 13 Lacombe) ........................ · · · · · · · · · · 155 vii Page APPENDIX B. METEOROLOGICAL DATA 158 Appendix B. 1 Meteorological data showing temperature, precipitation and days without frost for weather stations along the tour route, 1941-70: ............................... 158 Edmonton Cypress Hill Park Camrose Foremost Stettler Lethbridge Drumheller Claresholm Brooks Lyndon Gull Lake Skyline Medicine Hat Pekisko Swift Current Calgary Shaunavon Olds Eastend Lacombe APPENDIX C. CROP YIELDS AND PRODUCTION COSTS ................. ..... 163 Appendix C. 1. 1. Yields from different cropping practices on soil capability areas 20 and 3D in agroclimatic subregion 1, 1966-74 ....................................... 163 Appendix C. 1.2. Monthly precipitation at Camrose from April to October (1965-74) and crop yields on soil capability areas 20 and 30. 164 Appendix C. 1.3. Summerfallow costs for Warner District. .... .. .. .. 165 Appendix C.l.4. Monthly precipitation at Drumheller from April to October (1965-74) and crop yields on soil capability areas 1 and 2C . 166 Appendix C. 1,5. Average crop yields from different cropping practises on soil capability areas 1 and 2C, 1965-74. 167 Appendix C.2. 1. Cost of wheat production in the Hussar District. 168 Appendix C.4.1. Plant communities of the Great Sand Hills......... 169 APPENDIX D. FORMAT FOR MICROMORPHOLOGICAL DESCRIPTIONS ..... ...... 170 viii Page LIST OF TABLES Table 1.1 Average eld of eld crops under all management prac- ces on capabili areas 20 and 30, 1965-74 ........... 49 Table 1.2 Average crop elds occurring on capability areas 2M and 3M, 1965-74 52 Table 1.3 low costs in different soil-climatic subzones ... 55 Table 2.1 Average production costs for wheat in soil-climatic sub- zones along the tour route ............................ 61 Table 5.1 Climatic data for selected stations in southwest Saska­ 88 tchevJan 'It ill "' • 11 ., ,. <11 "' ., "' • • • ., ., t .. e "' ., " "' " " • ., ,. ., ., • e e ., ,. ., ., ., ~ • " ., .,. ., ,. "' ., .. Table 5.2 Average crop yields for Municipalities in the Shaunavon-Robsart area, 1964-73. 91 Table 8.1 Average crop yields for some
Recommended publications
  • Action Plan for Multiple Species at Risk in Southwestern Saskatchewan: South of the Divide
    PROPOSED Species at Risk Act Action Plan Series Action Plan for Multiple Species at Risk in Southwestern Saskatchewan: South of the Divide Black-footed Ferret Burrowing Owl Eastern Yellow-bellied Racer Greater Sage-Grouse Prairie Loggerhead Shrike Mormon Metalmark Mountain Plover Sprague’s Pipit Swift Fox 2016 Recommended citation: Environment and Climate Change Canada. 2016. Action Plan for Multiple Species at Risk in Southwestern Saskatchewan: South of the Divide [Proposed]. Species at Risk Act Action Plan Series. Environment and Climate Change Canada, Ottawa. xi + 127 pp. For copies of the action plan, or for additional information on species at risk, including the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) Status Reports, residence descriptions, recovery strategies, and other related recovery documents, please visit the Species at Risk (SAR) Public Registry1. Cover illustration: Landscape photo: South of the Divide, Jones Peak © Native Plant Society, C. Neufeld; Prairie Loggerhead Shrike © G. Romanchuck; Mormon Metalmark © R.L. Emmitt; Swift Fox © Environment and Climate Change Canada, G. Holroyd; Yellow-bellied Racer © Environment and Climate Change Canada, A.Didiuk Également disponible en français sous le titre « Plan d’action pour plusieurs espèces en péril dans le sud-ouest de la Saskatchewan – South of the Divide [Proposition] » © Her Majesty the Queen in Right of Canada, represented by the Minister of Environment and Climate Change, 2016. All rights reserved. ISBN Catalogue no. Content (excluding the illustrations) may be used without permission, with appropriate credit to the source. 1 http://www.registrelep-sararegistry.gc.ca Action Plan for Multiple Species in Southwestern Saskatchewan: South of the Divide 2016 Preface The federal, provincial, and territorial government signatories under the Accord for the Protection of Species at Risk (1996)2 agreed to establish complementary legislation and programs that provide for effective protection of species at risk throughout Canada.
    [Show full text]
  • East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
    East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig.
    [Show full text]
  • The North-West Rebellion 1885 Riel on Trial
    182-199 120820 11/1/04 2:57 PM Page 182 Chapter 13 The North-West Rebellion 1885 Riel on Trial It is the summer of 1885. The small courtroom The case against Riel is being heard by in Regina is jammed with reporters and curi- Judge Hugh Richardson and a jury of six ous spectators. Louis Riel is on trial. He is English-speaking men. The tiny courtroom is charged with treason for leading an armed sweltering in the heat of a prairie summer. For rebellion against the Queen and her Canadian days, Riel’s lawyers argue that he is insane government. If he is found guilty, the punish- and cannot tell right from wrong. Then it is ment could be death by hanging. Riel’s turn to speak. The photograph shows What has happened over the past 15 years Riel in the witness box telling his story. What to bring Louis Riel to this moment? This is the will he say in his own defence? Will the jury same Louis Riel who led the Red River decide he is innocent or guilty? All Canada is Resistance in 1869-70. This is the Riel who waiting to hear what the outcome of the trial was called the “Father of Manitoba.” He is will be! back in Canada. Reflecting/Predicting 1. Why do you think Louis Riel is back in Canada after fleeing to the United States following the Red River Resistance in 1870? 2. What do you think could have happened to bring Louis Riel to this trial? 3.
    [Show full text]
  • Physical Geography of the United States and Canada: a Land of Contrasts S
    Chapter 5 Guided Notes _________________________________________________________________________________________ NAME Physical Geography of the United States and Canada: A Land of Contrasts s North America’s vast and varied landscape and abundant resources have attracted immigrants and shaped the development of the United States and Canada. Section 1: Landforms and Resources The United States and Canada have vast lands and abundant resources. These two countries share many of the same landforms. Landscape Influenced Development U.S., Canada: former British colonies, most people speak English Strong economic and political ties with one another Vast Lands Canada second largest country in the world by area; U.S. third Together they cover one-eighth of the earth’s land surface Abundant Resources Landmass and natural resources attract immigrants to both countries U.S. and Canada have developed into global economic powers Many and Varied Landforms All major landforms are found in U.S. and Canada; The two countries share mountain chains and interior plains The Appalachian Highlands Appalachian Mountains run 1,600 miles from Newfoundland to Alabama; More than 400 million years old o include Green and Catskill mountains in the north; Blue Ridge and Great Smoky mountains in the south Erosion has created gentle slopes, peaks from 1,200–2,400 feet The Appalachian Trail is a scenic hiking path along the chain The Interior Lowlands Great Plains extend from Missouri River to Rocky Mountains; Interior Plains extend from Appalachians
    [Show full text]
  • Landforms and Resources
    Name _____________________________ Class _________________ Date __________________ Physical Geography of the United States and Canada Section 1 Landforms and Resources Terms and Names Appalachian Mountains major mountain chain in the eastern United States and Canada Great Plains largely treeless area in the interior lowlands Canadian Shield rocky, flat area that surrounds Hudson Bay Rocky Mountains mountain chain in the western United States and Canada Continental Divide line of the highest points in the Rockies that marks the separation between rivers flowing to the east and to the west Great Lakes five large lakes found in the central United States and Canada Mackenzie River Canada’s longest river Before You Read In the last chapter, you read about human geography–the way humans in general relate to their environment. In this section, you will learn about the physical features and resources of the United States and Canada. As You Read Use a graphic organizer to take notes about the landforms and resources of the United States and Canada. LANDSCAPE INFLUENCED The United States and Canada are rich DEVELOPMENT (Page 117) in natural resources. They have much How vast are these countries? fertile soil and water and many forests and The United States and Canada occupy the minerals. This geographic richness has central and northern four-fifths of the attracted immigrants from around the continent of North America. Culturally, the world for centuries. region is known as Anglo America. This is 1. What binds Canada and the United because both countries were colonies of States together? Great Britain at one time and because most of _______________________________ the people speak English.
    [Show full text]
  • Saskatchewan Intraprovincial Miles
    GREYHOUND CANADA PASSENGER FARE TARIFF AND SALES MANUAL GREYHOUND CANADA TRANSPORTATION ULC. SASKATCHEWAN INTRA-PROVINCIAL MILES The miles shown in Section 9 are to be used in connection with the Mileage Fare Tables in Section 6 of this Manual. If through miles between origin and destination are not published, miles will be constructed via the route traveled, using miles in Section 9. Section 9 is divided into 8 sections as follows: Section 9 Inter-Provincial Mileage Section 9ab Alberta Intra-Provincial Mileage Section 9bc British Columbia Intra-Provincial Mileage Section 9mb Manitoba Intra-Provincial Mileage Section9on Ontario Intra-Provincial Mileage Section 9pq Quebec Intra-Provincial Mileage Section 9sk Saskatchewan Intra-Provincial Mileage Section 9yt Yukon Territory Intra-Provincial Mileage NOTE: Always quote and sell the lowest applicable fare to the passenger. Please check Section 7 - PROMOTIONAL FARES and Section 8 – CITY SPECIFIC REDUCED FARES first, for any promotional or reduced fares in effect that might result in a lower fare for the passenger. If there are none, then determine the miles and apply miles to the appropriate fare table. Tuesday, July 02, 2013 Page 9sk.1 of 29 GREYHOUND CANADA PASSENGER FARE TARIFF AND SALES MANUAL GREYHOUND CANADA TRANSPORTATION ULC. SASKATCHEWAN INTRA-PROVINCIAL MILES City Prv Miles City Prv Miles City Prv Miles BETWEEN ABBEY SK AND BETWEEN ALIDA SK AND BETWEEN ANEROID SK AND LANCER SK 8 STORTHOAKS SK 10 EASTEND SK 82 SHACKLETON SK 8 BETWEEN ALLAN SK AND HAZENMORE SK 8 SWIFT CURRENT SK 62 BETHUNE
    [Show full text]
  • Shared with You Here
    Winged moccasins Winged Words by Margaret Complin I wish to thank the Editors 'Lohose en­ couragement made this booklet possible. perance, the first post of the Qu'Appelle of which any record appears to bt. available, was built in 1783 by a Nor'wester, Robert Grant. "There is eviden ce that the Hudson's Bay also had sent men from the Assiniboine to the Mis­ souri about this time," says Lawrence J. Burpee in "The Search for the ' 'Vestern Sea," but neither names nor dates are now extant." Brandon House on the Assiniboine, about seventeen m iles below the city of Brandon, was built by the Company in 1794. Two years later the post a t P ortage la P rairie (the site of La Verendrye's Fort la R eine) was est ablished. According to Dr. Bryce it was about 1799 that the Company took possession of the Assini­ boine district. The Swan River count ry, w hich later became one of the most important districts of the Northern Department of Rupert's Land, is associated with the name of Daniel Harmon, the Nor'west er, who arrived in the district in 1800. Harmon spent over three years a t Fort Alexandria and various post s in the district, and we learn from his journal that in 1804 he was at Lac la Peche (probably what we t oday call the Quill Lakes). On March 1st he w as at Last Mountain Lake, and by Sunday, 11th, had reached the banks of Cata buy se pu (the River that Calls).
    [Show full text]
  • Laurentide Ice Sheet Retreat Around 8000 Years Ago Occurred Over Western Quebec (700-900 Meters/Year)
    The retreat chronology of the Laurentide Ice Sheet during the last 10,000 years and implications for deglacial sea-level rise David Ullman University of Wisconsin-Madison, Department of Geoscience Author Profile Shortcut URL: https://serc.carleton.edu/59463 Location Continent: North America Country: Canada State/Province:Quebec, Labrador City/Town: UTM coordinates and datum: none Setting Climate Setting: Tectonic setting: Type: Chronology Show caption Show caption Show caption Description Much of the world's population is located along the coasts. In a world of changing climate, the rate of sea level rise will determine the ability of these communities to adapt to sea level rise. Perhaps the greatest uncertainty in sea level rise prediction has to do with amount of water melting off of Earth's major ice sheets. Recent decades have seen an accelerated loss of ice from Greenland and Antarctica. These bodies of ice may be prone to change more rapid than expected. Greenland and Antarctica contain enough frozen water, which, if melted could raise sea level by 70 m, but predictions on the rate at which this sea level rise could occur depend on scientists' understanding of the complex physics of ice flow (and on future climate scenarios). Paleoclimate researchers study past climates in hopes of developing a better understanding of our current and future climates. Similarly, understanding past ice sheets will aid in future prediction of ice sheet change. At the end of the Last Glacial Maximum, roughly 20,000 years ago, much of Earth in the northern hemisphere was covered in vast ice sheets.
    [Show full text]
  • Gazette Part I, March 26, 2021
    THIS ISSUE HAS NO PART III (REGULATIONS)/CE NUMÉRO NE THE SASKATCHEWAN GAZETTE, 26 mars 2021 793 CONTIENT PAS DE PARTIE III (RÈGLEMENTS) The Saskatchewan Gazette PUBLISHED WEEKLY BY AUTHORITY OF THE QUEEN’S PRINTER/PUBLIÉE CHAQUE SEMAINE SOUS L’AUTORITÉ DE L’IMPRIMEUR DE LA REINE PART I/PARTIE I Volume 117 REGINA, FRIDAY, MARCH 26, 2021/REGINA, vendredi 26 mars 2021 No. 12/nº 12 TABLE OF CONTENTS/TABLE DES MATIÈRES PART I/PARTIE I SPECIAL DAYS/JOURS SPÉCIAUX ................................................................................................................................................. 794 PROGRESS OF BILLS/RAPPORT SUR L’ÉTAT DES PROJETS DE LOI (First Session, Twenty-Ninth Legislative Assembly/Première session, 29e Assemblée législative) ................................................ 794 ACTS NOT YET IN FORCE/LOIS NON ENCORE EN VIGUEUR ............................................................................................... 795 ACTS IN FORCE ON ASSENT/LOIS ENTRANT EN VIGUEUR SUR SANCTION (First Session, Twenty-Ninth Legislative Assembly/Première session, 29e Assemblée législative) ................................................ 799 ACTS IN FORCE BY ORDER OF THE LIEUTENANT GOVERNOR IN COUNCIL/ LOIS EN VIGUEUR PAR DÉCRET DU LIEUTENANT-GOUVERNEUR EN CONSEIL (2020) ........................................ 799 ACTS IN FORCE BY ORDER OF THE LIEUTENANT GOVERNOR IN COUNCIL/ LOIS EN VIGUEUR PAR DÉCRET DU LIEUTENANT-GOUVERNEUR EN CONSEIL (2021) ........................................ 800 ACTS PROCLAIMED/LOIS PROCLAMÉES
    [Show full text]
  • Soil Ecoregions in Latin America 5
    Chapter 1 Soil EcoregionsSoil Ecoregions in Latin Latin America America Boris Volkoff Martial Bernoux INTRODUCTION Large soil units generally reflect bioclimatic environments (the concept of zonal soils). Soil maps thus represent summary documents that integrate all environmental factors involved. The characteristics of soils represent the environmental factors that control the dynamics of soil organic matter (SOM) and determine both their accumulation and degradation. Soil maps thus rep- resent a basis for quantitative studies on the accumulation processes of soil organic carbon (SOC) in soils in different spatial scales. From this point of view, however, and in particular if one is interested in general scales (large semicontinental regions), soil maps have several disadvantages. First, most soil maps take into account the intrinsic factors of the soils, thus the end results of the formation processes, rather than the processes themselves. These processes are the factors that are directly related to envi- ronmental conditions, whereas the characteristics of the soils can be inher- ited (paleosols and paleoalterations) and might no longer be in equilibrium with the present environment. Second, soils seldom are homogenous spatial entities. The soil cover is in reality a juxtaposition of several distinct soils that might differ to various degrees (from similar to highly contrasted), and might be either genetically linked or entirely disconnected. This spatial heterogeneity reflects the con- ditions in which the soils were formed and is expressed differently accord- ing to the substrates and the topography. The heterogeneity also depends on the duration of evolution of soils and the geomorphologic history, either re- gional or local, as well as on climatic gradients, which are particularly obvi- ous in mountain areas.
    [Show full text]
  • CTK-First-Nations Glimpse
    CARRY THE KETTLE NAKOTA FIRST NATION Historical and Current Traditional Land Use Study JIM TANNER, PhD., DAVID R. MILLER, PhD., TRACEY TANNER, M.A., AND PEGGY MARTIN MCGUIRE, PhD. On the cover Front Cover: Fort Walsh-1878: Grizzly Bear, Mosquito, Lean Man, Man Who Took the Coat, Is Not a Young Man, One Who Chops Wood, Little Mountain, and Long Lodge. Carry the Kettle Nakota First Nation Historical and Current Traditional Land Use Study Authors: Jim Tanner, PhD., David R. Miller, PhD., Tracey Tanner, M.A., and Peggy Martin McGuire, PhD. ISBN# 978-0-9696693-9-5 Published by: Nicomacian Press Copyright @ 2017 by Carry the Kettle Nakota First Nation This publication has been produced for informational and educational purposes only. It is part of the consultation and reconciliation process for Aboriginal and Treaty rights in Canada and is not for profit or other commercial purposes. No part of this book may be used or reproduced in any manner whatever without the written permission of the Carry the Kettle First Nation, except in the case of brief quotations embodied in reviews. Layout and design by Muse Design Inc., Calgary, Alberta. Printing by XL Print and Design, Saskatoon, Saskatchewan. Table of Contents Table of Contents 1 Table of Figures 3 Letter From Carry the Kettle First Nation Chief 4 Letter From Carry the Kettle First Nation Councillor Kurt Adams 5 Elder and Land User Interviewees 6 Preface 9 Introduction 11 PART 1: THE HISTORY CHAPTER 1: EARLY LAND USE OF THE NAKOTA PEOPLES 16 Creation Legend 16 Archaeological Evidence 18 Early
    [Show full text]
  • 1982 Report to the IJC Appendix B.Pdf
    L APPENDIX B TO THE L REPORT TO THE INTERNATIONAL JOINT COMMISSION L L ON L THE DIVISION OF THE WATERS OF THE \ ST. MARY AND MILK RIVERS L 1982 L L BY L D. A. DAVIS representing Canada L l L. \ L.. AND L I PHILIP COHEN I ~ representing the United States L L L L I I ii \, CONTENTS Station L Station Name Number Page St. Mary River at International Boundary 05AE027 1-2 L Lake Sherburne at Sherburne, Montana 05AE036 3 L St. Mary Canal at St. Mary Crossing near Babb, Montana 05AE029 4 Milk River at Western Crossing of International Boundary 11AA025 5 L Milk River at Milk River 11AAOOS 6 \ Milk River at Eastern Crossing of International Boundary 11AA031 7 L South Fork Milk River near Babb, Montana 11AA033 8 North Fork Milk River above St. Mary Canal near L Browning, Montana 11AA032 9 North Milk River near International Boundary 11AA001 10 L Lodge Creek below McRae Creek at International Boundary 11AB083 11 L Michele Reservoir near Elkwater 11AB091 12 Greasewood Reservoir near Elkwater 11AB092 13 L Massy Reservoir near Elkwater 11AB104 14 Bare Creek Reservoir near Elkwater 11AB094 15 il Cressday Reservoir near Cressday 11AB097 16 \ L Mitchell Reservoir near Elkwater 11AB099 17 Jaydot Reservoir near Jaydot 11AB098 18 L Middle Creek near Saskatchewan Boundary 11AB009 19 L Middle Creek Reservoir 11AB080 20 Middle Creek Reservoir Main Outlet 11AB113 21 L Middle Creek Reservoir Bedford Outlet 11AB114 22 Middle Creek Reservoir Flood Spillway 11AB115 23 L Middle Creek below Middle Creek Reservoir 11AB001 24 L 1 l- L iii Station L Station Name Number
    [Show full text]