DOCSLIB.ORG

Kootenay Lake

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

-•l-7sK?ti •~ •JrM- A 1* '".*>i\ .** !:CE FIVE CENTS Nelson, British Columbia, Saturday, Nov, 20,. 1897- WHOLE NUMBER 378. although the smoke was stifling they kept and calcining furnaces will not be blown at their work. At one time it looked as GENERMi LOCAL NEWS; in until the new ones are completed. IS I Wk though the hotel was doomed, lhe side THE M8T CLEAN-UP. At the mines everything has been wall and the cornice burst into flames working smoothly and a vast amount of but the men went to work with renewed EVENTS OF INTEREST IN AND ore has been taken out. \ Tho Jbinsare 'A REPORT THAT HAS A FLAVOR vigor and succeeded iu extinguishing PRODUCT OF IHE FERN MINE FOR full,and taken in connection ^ith'jthe ENTIRE KOOTENAY COUNTRY AROUND NELSON. ; OF KLONDYKE. them before they had got beyoud con­ THIRTY-EIGHT DAYS. custom ore on hand, there is a sufficient TRAIN SERVICE CHANGED. trol. The fact that the wood used in the > quantity to keep the big furnace'going construction was unseasoned wast greatly I." without interruption. A new Ingersoll in favor of the fireman. Mayor Houston, Brief Mention «r Happen fugs lu -the air compressor lias just been takeu to the Six r««t Lead «f Decomposed 4)nurl/ That Close Connection* Will Bfi Made at all Dr. Arthur. George, Bigelow, Barrister Ulsli-lct During tlie Fast Front or Over $10,000.—Ore Value* mine to assist in. the development work Give* Assays or &!,'<i'i roints anil the Time Creally McDonald, J. A. Gilker, W..F. Traves, J. Seven Days. Steadily Increasing. -Cyanide and will have a tendency to largely in­ In Cold. - Shortened. A. Turner and a host ot other business Process to he Added, crease the output. and professional. men were amongst the The first dividend of the Hall Mines, workers and worked like beavers.' When B." AVilson of- Sandon is in :the city. on the ordinary shares, is unofficially an­ A''Hnd of marvelous richness has it was seeD that the men were able to Commencing tomorrow a change in •a . On Monday Inst Mr. F. G. Innes and nounced to be nine per cent, and will be been- made in the Summit mine on control the flames in the hotel building A. T. Garland of Kaslo is a guest at thc entire time system of the Cana­ J. A. Veatch brought to Nelson from the i declared within a few days or weeks. Wild Horse creek near the Elise and a g'reatcbeer arose from the crowd of on at the Phair. > -,i That tbe announcement will be made dian Pacific railway in WestKootenay Fern mine on Morning mountain five the; owners, the Lindulade brothers, lookers. B. E; King of Sandon was.in Nelson will go into effect, the object being to bricks of gold bullion aa the result ot the before the first of the year is beyond tbe think- they have something that will The Broken Hill Mining Co's. building give a better service and do away; with last Tuesday. • , f Irat mill run of the mine. The bricks question of a doubt. yield as heavily as a Klondyke pro­ began to show signs of. igniting and the exasperating delays "and "stop overs." E. H. Thomlinson of Spokane is -We deposited in the Bank of Montreal The lead furnace is nearly ready for perty. The mine* was bonded by a steam and smoke from the sides led many The new system shortens the time all ! fcpd the value placed at 811,325. operation, and although a quantity of member of the Fern company on the to believe'that the ilames would* burst registered at thePhair. along the line and the completion of [r. Innes furnished the following re­ custom ore for it is on band, the proba­ strength of an IS inch cropping which forth at any minute. A bucket brigade T. AV. Jenkins, of London.'Englaud, the Slocan-branch will put Nelson lit ot the 38 days' run to November 13: bilities ore that it will not blow in' until assayed.about $100 Ln gold to the ton. was formed and the sides were kept sat­ was a visitor to Nelson during the within a fewhburs' travel to all Slocan lflion shipped, $11,325; bullion on after ore has commenced to have been The. dip of tho vein was about; 45 urated with water. One mau by the name week. 3d, $670; concentrates shipped, 20 received over the Slocan Lake bruueh. of points. "'-..- > ' > • '.' -* of Burns did some noble work aiid was degrees and a. shaft was started some Thomas Noonnn of-Toronto is a visi- . jte; net smelter returns,.$1,500; six tons the G. P. K. Under this order of things On "the Rossland division trainswill distance up the hill, to tap ib. After scotched nnd half frozsu at the same in­ tor to Nelson and is. stopping at the concentrates on hand,' $350r total it will be the middle of next month be­ leave Nelson at 0:30 p. m. and arrive sinking this shaft to a depth of about stant. He was drenched with the cold Phair. ' ...'.;". ''.'... fillet of the mill, $13,915; ore shipped, fore the fires are started. at Uossland at 11 p. m. daily. , They 40- i'oet and spending, in all, in the water from the'ereek' and his clothiDg 'tons; net returns, $1,200; making a will leave. Rossland at 6 p'. mi. and ar­ neighborhood ol! $5030, the bond was was singed by the fire. McArthur & Mc­ B. C. Silver of Montreal! is registered Ul of the mine and mill for the 38 days MUST GO TO TRIAL.; rive in.Nelson at 10:30 p.m. .Thus it thrown up. - Donald at one time thought that nothing at the Phair. lie bas golden opinions . will be seen that the service for busi­ ^$15,145. The total number of tons -The Liudblade brothers-took up the could save the building und sttirted to of the Kootenay. /' ' ; Contest Over the Keservoir Site Can Not Be ness men has been much improved, illed was 965, or an average of 25.4 tons work where it had been left otf and move out their stock of furniture. People No meeting ofthe city, council was - Settled ©ut of Court. allowing travelers to either city a full |er day. The segregation of values re­ after* sinking about five I'eet more in occupying the upper floor hurridly moved held. Wednesday night mi account of - The outlook is that the dispute over day iii" which to transact'tlieir busi­ ive red is as follows: The first five days, the.shaft, ran across a six foot lead of their possessions to a place of safety. a quorum failing to appear. The the land occupied by the city reservoir ness. Close .connections will lie made Iv tons per day, making 150 tons at $8 decomposed white quartz which gave The sidewalk between the burning build­ meeting was adjourned until Monday. and flume will not be settled out ot with the main line. Columbia river er ton, $1,200; succeeding 10 days,' 25 an assay , of §2700 in gold to the ton. ing and the Broken Hill block waa cut court It was thought at one time that steamers will leave Arrowhead at 10 Barrister J. A.' Aiknian. has been_ Mis per day, 250 tons at $9 per ton, Th'e'first test was by panning, two or down and pulled away by the means of. the matter could be amicably adjusted a. m, Nakusp at 1 p. ni; and arrive:in' acting as deputy registrar of the su­ ^',250: the next 10 days, 24 tons per day, three chunks being crushed and pauned ropes so that full attention could bt» by Mr. Joshua Davies for the,Nelson Robson at 8:30 p. m„ making connec­ preme court this week, during the ab­ HO tons at $14 per ton, $3,360; the next out.'-.The result was a run of gold given to keeping the side of the buildings Gity Land and Improvement company tions with the trains that arrive in : sence" of Mr. Simpkins, who has been days, 25 .tons per day, 325 tons at extending for four inches , over the saturated with water. At oue time the and the city council, but the ideas of the Nelson at 10:30 p. in. and Rossland at enjoying his honeymoon. ; ?1.85, $7,135. Tbe average duty per bottom of the, pan and, ccmUining fire got some headway in the basement gentlemen differ so widely that there ap­ 11 p. in., .People leaving Vancouver at lump in 24 hours .was' 2.54 tous. Tbe between 40 and 50 cents iii value. The of Hume's hotel buildiug. but. at'ler a , "VV. J. Diskson has concluded a sale pears to be no hope of a settlement by 2 p. m. 011 any day.may arrive,.in Nel­ i:v>rage free gold per ton milled was owners' at once put'a force of twelve hard fight it. was subdued., of 200 lots injAdditioir A to an English ,"' this means. Mr. Davies has instructed son at 10;30 p. in.. of the second day. |<2.43. The average value of coucen- meri: to work drifting-both ways on . When the laundry building collapsed syndicate, The lots ase being held for his attorney to push the matter to a'con­ The lay-over, at Revelstoke from 9:15 ites per ton milled was $2.02. The es.
Recommended publications
  • Vegetation and Fire at the Last Glacial Maximum in Tropical South America

    Vegetation and Fire at the Last Glacial Maximum in Tropical South America

    Past Climate Variability in South America and Surrounding Regions Developments in Paleoenvironmental Research VOLUME 14 Aims and Scope: Paleoenvironmental research continues to enjoy tremendous interest and progress in the scientific community. The overall aims and scope of the Developments in Paleoenvironmental Research book series is to capture this excitement and doc- ument these developments. Volumes related to any aspect of paleoenvironmental research, encompassing any time period, are within the scope of the series. For example, relevant topics include studies focused on terrestrial, peatland, lacustrine, riverine, estuarine, and marine systems, ice cores, cave deposits, palynology, iso- topes, geochemistry, sedimentology, paleontology, etc. Methodological and taxo- nomic volumes relevant to paleoenvironmental research are also encouraged. The series will include edited volumes on a particular subject, geographic region, or time period, conference and workshop proceedings, as well as monographs. Prospective authors and/or editors should consult the series editor for more details. The series editor also welcomes any comments or suggestions for future volumes. EDITOR AND BOARD OF ADVISORS Series Editor: John P. Smol, Queen’s University, Canada Advisory Board: Keith Alverson, Intergovernmental Oceanographic Commission (IOC), UNESCO, France H. John B. Birks, University of Bergen and Bjerknes Centre for Climate Research, Norway Raymond S. Bradley, University of Massachusetts, USA Glen M. MacDonald, University of California, USA For futher
  • Southern Accent July 1953 - September 1954

    Southern Accent July 1953 - September 1954

    Southern Adventist University KnowledgeExchange@Southern Southern Accent - Student Newspaper University Archives & Publications 1953 Southern Accent July 1953 - September 1954 Southern Missionary College Follow this and additional works at: https://knowledge.e.southern.edu/southern_accent Recommended Citation Southern Missionary College, "Southern Accent July 1953 - September 1954" (1953). Southern Accent - Student Newspaper. 33. https://knowledge.e.southern.edu/southern_accent/33 This Book is brought to you for free and open access by the University Archives & Publications at KnowledgeExchange@Southern. It has been accepted for inclusion in Southern Accent - Student Newspaper by an authorized administrator of KnowledgeExchange@Southern. For more information, please contact [email protected]. SOUTHERN msmm college UBRMV THE OUTH^^ ACCENT Souchern Missionary^ollege, Collegedale, Tennessee, July 3. 1953 o lleven SMC Graduates Ordained Young Men Ordained to M^ Kennedy Supervises Varied Gospel Ministry f. at Five Iprog am of Summer Activities Southern Union Camp Meetings fcht chapel scat Wednesday e c n ng br ngs these comn ents for once tadi week we ha\e chapel Many % r cd ch-ipel progran s ha e been '> p anned bj Dr R chard Hammill of the college rfOMffliililiins ! Thursday udenb and it d(-r e\en ng at the ball field br ngs torth to bu Id up cred cheers as a runner si des the hon e or as the umpire calls 6tr kc Three Student o^ram Comm ... and h ult) al ke mansh p of Profc share the thr II of a hon e run V d) hi\e out! ned Come th me
  • Indiana Glaciers.PM6

    Indiana Glaciers.PM6

    How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago.
  • Chapter 1. Natural History

    Chapter 1. Natural History

    CHAPTER 1. NATURAL HISTORY CHAPTER 1. NATURAL HISTORY —THE WILDERNESS THAT GREETED THE FIRST SETTLERS The land one sees today traveling through northern Ohio took gone. Thus, some 14,000 years ago as the last glacier receded millions of years to form. We can see evidence of tropical sea into the Lake Erie basin, the first Native Americans arrived and reefs on the Lake Erie Islands and deep ocean sediments here in began to utilize the natural resources that these natural processes the cliffs of the Black River. Ohio was just south of the equator had produced. at that time, some 350 million years ago, and over the millennia The natural history of Sheffield encompasses all those natural has migrated northward to its present position. Mountain features and processes of the environment that greeted the Native building to the east eventually raised the sea floor from under Americans, and later the pioneers, when they first arrived in the waves and erosion by streams, and later glacial ice, began Sheffield. To be sure, the landscape was a magnificent wilderness to sculpture the land. At the same time plants and animals were to the settlers, but it needed to be “tamed” in order to support evolving and began to populate the new land once the ice was the newcomers. Ice formation on the shale bluff of the Black River north of Garfield Bridge (2005). 1 BICENTENNIAL HISTORY OF SHEFFIELD TOPOGRAPHY Regional Physiography The topography of an area is the configuration of the land Physiography refers to the physical features or landforms of surface, including its relief [vertical differences in elevation of a region.
  • St. Louis River Natural Area to the DULUTH NATURAL AREAS PROGRAM DATE: 3/7/19

    St. Louis River Natural Area to the DULUTH NATURAL AREAS PROGRAM DATE: 3/7/19

    NOMINATION OF THE St. Louis River Natural Area TO THE DULUTH NATURAL AREAS PROGRAM DATE: 3/7/19 Nominated by: City of Duluth Parks & Recreation Division This report was produced by the Minnesota Land Trust under contract to the City of Duluth and funded by U.S. Environmental Protection Agency Great Lakes Restoration Initiative grant number GL00E02202. Many organizations and individuals participated in a variety of ways as collaborators to the report. St. Louis River Natural Area Nomination DRAFT 3/7/19 Table of Contents Executive Summary ..................................................................................................................... iii Introduction ................................................................................................................................1 Eligibility ......................................................................................................................................2 − Land Ownership ......................................................................................................................... 2 − Scientific Criteria ........................................................................................................................ 3 References ................................................................................................................................. 10 Figures .......................................................................................................................................12 Appendices ................................................................................................................................36
  • The Evolution of Crayfishes of the Genus Orconectes Section Limosus (Crustacea: Decopoda)

    The Evolution of Crayfishes of the Genus Orconectes Section Limosus (Crustacea: Decopoda)

    THE OHIO JOURNAL OF SCIENCE Vol. 62 MARCH, 1962 No. 2 THE EVOLUTION OF CRAYFISHES OF THE GENUS ORCONECTES SECTION LIMOSUS (CRUSTACEA: DECOPODA) RENDELL RHOADES Department of Zoology and Entomology, The Ohio State University, Columbus 10 The earliest described crayfish species now included in the Section limosus of the Genus Orconectes was described by Samuel Constantine Rafinesque (1817: 42). He reported the species, which he named Astacus limosus, "in the muddy banks of the Delaware, near Philadelphia." How ironical it now seems, that when Rafinesque located at Transylvania three years later and traveled to Henderson, Kentucky, to visit a fellow naturalist, John J. Audubon, he could have collected from the streams of western Kentucky a crayfish that he might have identified as the species he had described from the Delaware. We now know that these streams of the knobstone and pennyroyal uplands are the home of parent stock of this group. Moreover, this parental population on the Cumberland Plateau is now separated from Rafinesque's Orconectes limosus of the Atlantic drainage by more than 500 miles of mountainous terrain. Even Rafinesque, with his flair for accuracy and vivid imagination, would have been taxed to explain this wide separation had he known it. A decade after the death of Rafinesque, Dr. W. T. Craige received a blind crayfish from Mammoth Cave. An announcement of the new crayfish, identi- fied as "Astacus bartonii (?)" appeared in the Proceedings of the Academy of Natural Science of Philadelphia (1842: 174-175). Within two years the impact of Dr. Craige's announcement was evidenced by numerous popular articles both here and abroad.
  • Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES

    Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES

    UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman ,Wilbur, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director P~ofessional Paper 161 . QUArrERNARY GEOLOGY OF MINNESOTA AND PARTS OF ADJACENT STATES BY FRANK LEVERETT WITH CONTRIBUTIONS BY FREDERICK w. SARDE;30N Investigations made in cooperation with the MINNESOTA GEOLOGICAL SURVEY UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1932 ·For sale by the Superintendent of Documents, Washington, D. C. CONTENTS Page Page Abstract ________________________________________ _ 1 Wisconsin red drift-Continued. Introduction _____________________________________ _ 1 Weak moraines, etc.-Continued. Scope of field work ____________________________ _ 1 Beroun moraine _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 47 Earlier reports ________________________________ _ .2 Location__________ _ __ ____ _ _ __ ___ ______ 47 Glacial gathering grounds and ice lobes _________ _ 3 Topography___________________________ 47 Outline of the Pleistocene series of glacial deposits_ 3 Constitution of the drift in relation to rock The oldest or Nebraskan drift ______________ _ 5 outcrops____________________________ 48 Aftonian soil and Nebraskan gumbotiL ______ _ 5 Striae _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 48 Kansan drift _____________________________ _ 5 Ground moraine inside of Beroun moraine_ 48 Yarmouth beds and Kansan gumbotiL ______ _ 5 Mille Lacs morainic system_____________________ 48 Pre-Illinoian loess (Loveland loess) __________ _ 6 Location__________________________________
  • Table of Contents. Letter of Transmittal. Officers 1910

    Table of Contents. Letter of Transmittal. Officers 1910

    TWELFTH REPORT OFFICERS 1910-1911. OF President, F. G. NOVY, Ann Arbor. THE MICHIGAN ACADEMY OF SCIENCE Secretary-Treasurer, GEO. D. SHAFER, East Lansing. Librarian, A. G. RUTHVEN, Ann Arbor. CONTAINING AN ACCOUNT OF THE ANNUAL MEETING VICE-PRESIDENTS. HELD AT Agriculture, CHARLES E. MARSHALL, East Lansing. Geography and Geology, W. H. SHERZER, Ypsilanti. ANN ARBOR, MARCH 31, APRIL 1 AND 2, 1910. Zoology, A. S. PEARSE, Ann Arbor. Botany, C. H. KAUFFMAN, Ann Arbor. PREPARED UNDER THE DIRECTION OF THE Sanitary and Medical Science, GUY KIEFER, Detroit. COUNCIL Economics, H. S. SMALLEY, Ann Arbor. BY PAST-PRESIDENTS. GEO. D. SHAFER DR. W. J. BEAL, East Lansing. Professor W. H. SHERZER, Ypsilanti. BRYANT WALKER, ESQ. Detroit. BY AUTHORITY Professor V. M. SPALDING, Tucson, Arizona. LANSING, MICHIGAN DR. HENRY B. BAKER, Holland. WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Professor JACOB REIGHARD, Ann Arbor. 1910 Professor CHARLES E. BARR, Albion. Professor V. C. VAUGHAN, Ann Arbor. Professor F. C. NEWCOMBE, Ann Arbor. TABLE OF CONTENTS. DR. A. C. LANE, Tuft's College, Mass. Professor W. B. BARROWS, East Lansing. DR. J. B. POLLOCK, Ann Arbor. Letter of Transmittal .......................................................... 1 Professor M. H. W. JEFFERSON, Ypsilanti. DR. CHARLES E. MARSHALL, East Lansing. Officers for 1910-1911. ..................................................... 1 Professor FRANK LEVERETT, Ann Arbor. Life of William Smith Sayer. .............................................. 1 COUNCIL. Life of Charles Fay Wheeler.............................................. 2 The Council is composed of the above named officers Papers published in this report: and all Resident Past-Presidents. President's Address—Outline of the History of the Great Lakes, Frank Leverett.......................................... 3 On the Glacial Origin of the Huronian Rocks of WILLIAM SMITH SAYER.
  • Petition to List US Populations of Lake Sturgeon (Acipenser Fulvescens)

    Petition to List US Populations of Lake Sturgeon (Acipenser Fulvescens)

    Petition to List U.S. Populations of Lake Sturgeon (Acipenser fulvescens) as Endangered or Threatened under the Endangered Species Act May 14, 2018 NOTICE OF PETITION Submitted to U.S. Fish and Wildlife Service on May 14, 2018: Gary Frazer, USFWS Assistant Director, [email protected] Charles Traxler, Assistant Regional Director, Region 3, [email protected] Georgia Parham, Endangered Species, Region 3, [email protected] Mike Oetker, Deputy Regional Director, Region 4, [email protected] Allan Brown, Assistant Regional Director, Region 4, [email protected] Wendi Weber, Regional Director, Region 5, [email protected] Deborah Rocque, Deputy Regional Director, Region 5, [email protected] Noreen Walsh, Regional Director, Region 6, [email protected] Matt Hogan, Deputy Regional Director, Region 6, [email protected] Petitioner Center for Biological Diversity formally requests that the U.S. Fish and Wildlife Service (“USFWS”) list the lake sturgeon (Acipenser fulvescens) in the United States as a threatened species under the federal Endangered Species Act (“ESA”), 16 U.S.C. §§1531-1544. Alternatively, the Center requests that the USFWS define and list distinct population segments of lake sturgeon in the U.S. as threatened or endangered. Lake sturgeon populations in Minnesota, Lake Superior, Missouri River, Ohio River, Arkansas-White River and lower Mississippi River may warrant endangered status. Lake sturgeon populations in Lake Michigan and the upper Mississippi River basin may warrant threatened status. Lake sturgeon in the central and eastern Great Lakes (Lake Huron, Lake Erie, Lake Ontario and the St. Lawrence River basin) seem to be part of a larger population that is more widespread.
  • Mcmillan, Tyler 1999.Tif

    Mcmillan, Tyler 1999.Tif

    oPTrxd MY:'IORIPLL~BRPR~ TI~C ''fi-P,E ~'h'ivf~s~~y '185 S ,/ ~PJ.DF:'IE Senior Thesis Geology of The Ohio State University, Columbus Campus BY Tyler D. McMillan 1999 Submitted as partial fulfillment of The requirements for the degree of Bachelor of Science in Geological Sciences At The Ohio State University, Spring Quarter, 1999 Approved by: Dr. Garry McKenzie Table of Contents Page INTRODUCTION 1 Purpose of the Study i Location, Topography, and Geology 1 GEOLOGY AND GEOLOGIC HISTORY OF FRANKLIN COUNTY Quaternary Kansan (Pre- Illinoian) Glaciation Illinoian Glaciation Wisconsinan Glaciation Paleozoic Geologic History Columbus Limestone Delaware Formation Ohio and Olentangy Shale UNCONSLIDATED MATERIALS OF OSU CAMPUS Glacial and Post-glacial Deposits Soils of the OSU Campus CsB Crosby-Urban land complex CrB Crosby silt loam KO Kokomo silty clay loam Ut Udenthents-Urban land complex CfB Celina-Urban land comlex MnC Miamian-Urban land complex ErnB Eldean-Urban land complex Rs Ross silt loam Uw Urban land-Genesee complex Ux Urban land-Ockley complex Uv Urban land-Celina complex HYDROGEOLOGY OF THE OSU CAMPUS Groundwater in the Consolidated Rocks Groundwater in Surficial Aquifers STRATIGRAPHY OF THE SURFICIAL DEPOSITS OF THE OSU CAMPUS 23 CONCLUSION 30 List of Figures Page Figure I Physiographic diagram of Ohio (from Schmidt and Goldthwait, 1950) Figure 2 Bedrock geologic map and cross section of Ohio (Ohio Geological Survey, 1995) Figure 3 Glacial deposits map of Ohio (Ohio Geological Survey, 1997) 5 Figure 4 Bedrock topography and flow
  • Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba

    Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba

    Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province
  • Weekly Update #7 – February 21, 2020

    Weekly Update #7 – February 21, 2020

    Water Level & Flow Update for the Lower Nelson River Weekly Update # 7 February 21, 2020 Lower Nelson River (Split Lake to Hudson Bay) Water up and impoundment has not started at Keeyask (planned to begin in February). Flows on the Nelson River are high as heavy Fall rainfall in the southern parts of the watershed flows north on its way to Hudson Bay - this will continue all winter. Hydro system flows to Split Lake and the Lower Nelson River come from 2 sources – Lake Winnipeg (LW) outflows through Kelsey generating station (at 3115 cms or 110,000 cfs) and Churchill River Diversion (CRD), through Notigi control structure (960 cms or 33,900 cfs)-see map. These combined flows (of 4,075 cms or 143,900 cfs) have been relatively constant since early December. The Nelson’s flow downstream of Keeyask is 4,480 cms ( or 158,200 cfs) (measured at As of February 19, Lower Nelson River lake and Limestone GS). forebay levels are: • Split Lake 168.35 m (or 552.3 ft) Nelson River flow depends on Lake Winnipeg Water level: • Clark Lake 167.94 m (or 551.0 ft ) Lake Winnipeg outflows are largely controlled by the • Gull Lake 156.17 m (or 512.4 ft ) Jenpeg Generating Station (upstream of Kelsey Jenpeg• Stephens Lake 139.76 m (or 458.5 ft) Generating Station). These flows are maximized every • Long Spruce forebay 110.90 m (or 361.2 ft ) winter to allow as much water as possible to flow out of • Limestone forebay 85.07 m (or 279.1 ft) Lake Winnipeg to fuel generating stations on the Nelson River to meet heating demands by Manitobans.