Portland Daily Press: February 22,1871

Total Page:16

File Type:pdf, Size:1020Kb

Portland Daily Press: February 22,1871 Xt/I JfVO »«««'»» in advance. The Portland Dally Press BONDS. 6Vei ’aJ _INSURANCE. BONDS. MISCELLANEOUS^ th«PUbUahed (SuTjay8e*oepted) b: ^ business DIRECTORY. Portland ANNUAL STATEMENT OP THE Publishing Co., SIX PER CENT. THE TREA81R1 DEPABTHENT, DAILY PRESS* 109 Wasiiijofon, Feb 4,1871. Advertising Agency At Exchange Portland. MUTUAL ATWELL & CO.. Street, LIFE INSURANCE 171* Middle v POBTLAN I>. Public nolice i9 hereby given, that bools will be ments inserted a COMPANY, in (tapers inE Terms:—Eight Dollars Tear In advance opened on thesixLh day of March next, in this coun- OF NEW YORK. mthe country at mi PublisbeCs toy*" Central Railroad try and in r.nrope, lor subscriptions to tbe National r^e's GOLD under tbe Act F. 8. President. Loan, approved July 14, 1870,entitled The Maine State Press WINSTON, H. A. Vies BONDS, **An Act to the WEDNESDAY, FEBRUARY 22,1871. NtCIBDV, President. authorize Ketuodmg ot the National Agricultural Implements A Seeds Free from Debt,’* a^d the Act in amendment Government Tax. OF thereoi, approved 8AWYElt ft WOODFORD, No. 119 Is published every Thursday Morning at CO., IOWA. January 20. 1871. Exchange St] Made $2.50 a year; if paid in advance, at $2.00 a January 1st, 18M, to the Commissioner of Maine. satwh<ch subscriptions mav bo ■ cultural DrparlMCHI. Lave DOW built anTbe^plac l «he made, year. and equipped. Id flrat-clas» [manner, names ot the author zed Agents'of ihe Gov- Auctioneer. ernment, wul be Portland and Railroad about announced hereafter, j he propos- C. W. HOLMES, No. 327 Anction ral 9I! r 1 horticulturists are ln- (AllCash.) eu loan CongreseSt. Sales Vii Rates of inch of space, ..$44,009,155.78, Ogdensbnrg comprises three classes ot name 1 v: Private Sales ",l3 s-ch nutters Advertising.—One Bonds, every Evening. during tbe day. u havacUnIi«l,“,.tt0 "leparimcut in constitutes a INVESTED AS 10 tbe nt hve bundrei mil »nd ob- lenetb of column, square.” FOLLOWS: 180 Miles ilona of ofno1!^8 a*?0UDt urs.tioo lorior ,h‘,h,n .xperieuce of Pa,able lu at the tervation, the geoer..! „ava, $1.50 per daily first week. 75 cents Railroad, co’n’ Pleasure ceuieut ol the cause. square Cash on band, Banks and Trust at ten from tbe date Agencies for Sewing Machines. three or Ip Companies, interest..... tom om ,1 which their St iS year* per week after; insertions, less, $1.00; First Bonds. completes entire line, with the ex- ihSlVl .na^tLaU"rhearing W. S. teriv in .m ot interest, payable quar- DYER, T9* Middle St, over H. H. Hay’s. All ate other day after first week, 50 iuK.'::::S Mortgage ot the Thebe 1047 patent continuing every »sD,daK?k18,0»'texceed*,one ception laying track on twenty-fit^ miles, kinds of* Maehines lor sale and to let. cUurua. cents. Repaving, which is thus The average assessed or already graded. They open the valuation of lam Half square, three insertions less, 75cents; %mteta,eSluck8’(itC08t>-.".’.v.v:."'::::::::It Principal and Interest week after. Balance due in Payable Bakers. lands in Maine in 1800 was $12.04 one week. $1.00; 50 cents per byAgenU,' course' or irausmission;.':::.':;: :.\V:.\V.\V::.V.V.V.'.V.V.7." ‘m.I&S 2 per acre.— one third additional. in First W. C.COBB, No. 12 Pearl Street. Special Notices, Gold. Through Line Across the State at ^ In 1800 in was $13.73. Under head of “Amusements,” $2.00 per “ annum!0’ Add Interest accrued, but not Ashes is fertilizer for week; three insertions oy less $1.50. due. ,42*2Svl» from north to south, and, by making a detour Boots and Shoes—Gents agood strawberries. square per Tfc* slight Custom Work. Advertisements inserted in the Maine undersigned bare nulhcriiy la alfov at one point, WALTER Prime corn delivered at the stores Premiums due bat Dot yet they give BERRY. No. 101 Middle Street. in south- (which has a reported..V.’.V.V ".V.7.V.'.V.' 7"'. 3*2*1 30 far aale iae o the United states, alter State Press” large circulation Deterred, and Bauds of the Portland and thirty years from the *atS ern Illinois is worth cents Quarierly, Semi-aDnual Premiums... 1 119.573 77 Dsrect ot t> eir t-rae, and 20 a bushel.; in every part ol the State) for $1.00 per square Present market value ol Bailraad nl Communication Between §(• Louie bearing interest, pay ib'e qiar- Stocks in excess ot cost.7.77777.77.! 17.7.7.7. 428,(124 00 Otdratkari Company teriy iu coi», at tbe rate or t*cr Booksellers and for first and 50 cents uud S'l. percent. per annum Stationers. The Commissioners appointed the Gov- insertion, per square for Ibe Tory law af 90 with ac- Paul. Sub crihers to the by price Lean will have i reference iu ihe HOYT. FOGO ft each subsequent insertion. Gross Dec. 78 foil-wing order, BREED, *2 Middle Street. ernors of thi3 and other States to Assets, 31st, 1870,.$44,609,155 crued interest in currency. Thi? line of Railroad will namely: investigate Address all communications to have very special advan- first Subscribers tor Increase equal amounts of each class the cattle disease, met in on the in net assets for 85 tages tor both local and thiough besides of Bonds. Albany 0th PORTLAND PUBLISHING CO. 1870,.$7,170,853 Tills road is business, Book-Binders. Dividend surplus to policy holders, over... 00 now completed to West Baldwin, such Second. y,00d,(Mi0 superior railroad connections as will secure to Subscribers for equal amounts ot honds inst. On a full comparison of notes among the Rece pis fjr premiums ami in 34 and trains are Pr'Dt''‘s policies, 1870.12,I69,7!7 running to that point, 33 miles hom it bearing mtere.i at ibe rate ot lour t nd a half ^No. Exchange Keceints for a large portion of the trade ot the per Street." were interest, ien*e, 2 477.7T2 68 Portland. B* carrying great cent, and Ol bouds interest at ibe Commissioners they unanimously of the Paid Claims yotd West Baldwin the road is graded North-west bearing raieot SMALL ft No. BUSINESS by death, and endowments matured,. 2j0l0 224 62 The live per cenc. SHACKEDKl>, 39 Plnm Street. CARDsT to Fryebnrg, Bit miles from and the rails opinion that the disease now Portland, Third. Subscribers lor five cent, prevailing As will be the per bends. seen, receipts for interest. &c., being over $400,000 more than its death claims and endow* will be laid to that point as early in tbe as Bonnet and Hat It I amoug the cattle was meor- in 1870. It spring IpST MORTGAGE When a subscription Is made the subscriber will cache easily prevented, provi- policies paid ts prohibited by its charier from investing in any but the safest securities, the weather will ry such as is permit. From Fryebnrg tils Tend be required to wo H. E. No. ded that here exhibited. It is low as will be seen, the largh-ht, not io say the safest, institution of deposit per cent, of rbe amount UNDERWOOD, 310* Congress Street. prompt sanitary and restrictive meas- JOHN 0. WINSHIP its kind IV ij under contract to thereof. 10 be accounted ior ibe the world.—I is average expenses being less than anv other company in the country. CoDway, N. H„ to which point oy Government ures were wben tbe bonds are adopted. The Having beeu Agent tor this gieat company lor more than ‘27 we are to lurnDh trains will ran in delivered; and Dayment may be following prescrip- at years, prepared facts, July, 1871. 7 Per made eieber <n Cabinet Furniture Attorney showing the immense advantages of in tuis and Ct. Gold Bonds com or iu bends ol ihe United Stales Manufacturers. tion for of Law, insuring invite any who detite on daily disinfection the cattle Company, information The road bas thus far been built and known a? THBO. yards the suidect to call oh us. equipped five-i went v bonds, at their value. JOHNSON ft CO.. No. 13* Union Street. Rooms which are issued Ihe par received the of the No. BAG Fluent Bloch, from cash subscriptions to tbe Capita] Stock; but to upon this road are limited, iu com received inpayment will be applied to ibe approval Commissioners. amount of it to Bartlett, N. and to to $16,000 per mile (wbl,e roads redemption live twenty bonds. Ten of 60 Corner of Congress and StB complete H., provide addi- many issue Ibe bonus will Carpenters and Builders pounds copperas, gallons of water Exchange from be remstered or Issued with coa- W. D. Little & Co. tional for $?0f000 to and are ottered and Agts., 491-2 St. equipment its increasing business, the $10,000,) at 90 and pon*, as msv b. d-sired bv subscribers. WHITNEY & MEANS. Pearl st, opposite the Park. one half gallon of 30 per cent, catholic POHTLAN’P, HIM.ja&lly Exchange accrued bouds Will Begi-tced Company bas issued bonds to tbe amount ot interest, in currency. be Issued ol the denoml mtlons of 150 total $800,- *100. il acid; expense twenty tive cents per bar- Heman A. Crane. Horace A. Crane. Geo. Jr. secured a The m$st experienced financiers that *500, OOu, *5,«00, aud *10.000; and cou unn Allen, II. II. 000, by mortgage ol its [entire property to agree First bonus ol Cement Drain and rel REMINGTON, Gen’l each den •minanou except the ia*t two Water’Pipe, lor the preparation.
Recommended publications
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Geology of Michigan and the Great Lakes
    35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed.
    [Show full text]
  • LAKES of the HURON BASIN: THEIR RECORD of RUNOFF from the LAURENTIDE ICE Sheetq[
    Quaterna~ ScienceReviews, Vol. 13, pp. 891-922, 1994. t Pergamon Copyright © 1995 Elsevier Science Ltd. Printed in Great Britain. All rights reserved. 0277-3791/94 $26.00 0277-3791 (94)00126-X LAKES OF THE HURON BASIN: THEIR RECORD OF RUNOFF FROM THE LAURENTIDE ICE SHEETq[ C.F. MICHAEL LEWIS,* THEODORE C. MOORE, JR,t~: DAVID K. REA, DAVID L. DETTMAN,$ ALISON M. SMITH§ and LARRY A. MAYERII *Geological Survey of Canada, Box 1006, Dartmouth, N.S., Canada B2 Y 4A2 tCenter for Great Lakes and Aquatic Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. ::Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. §Department of Geology, Kent State University, Kent, 0H44242, U.S.A. IIDepartment of Geomatics and Survey Engineering, University of New Brunswick, Fredericton, N.B., Canada E3B 5A3 Abstract--The 189'000 km2 Hur°n basin is central in the catchment area °f the present Q S R Lanrentian Great Lakes that now drain via the St. Lawrence River to the North Atlantic Ocean. During deglaciation from 21-7.5 ka BP, and owing to the interactions of ice margin positions, crustal rebound and regional topography, this basin was much more widely connected hydrologi- cally, draining by various routes to the Gulf of Mexico and Atlantic Ocean, and receiving over- ~ flows from lakes impounded north and west of the Great Lakes-Hudson Bay drainage divide. /~ Early ice-marginal lakes formed by impoundment between the Laurentide Ice Sheet and the southern margin of the basin during recessions to interstadial positions at 15.5 and 13.2 ka BE In ~ ~i each of these recessions, lake drainage was initially southward to the Mississippi River and Gulf of ~ Mexico.
    [Show full text]
  • Contents List of Illustrations
    STATE OF MICHIGAN Deltas..................................................................... 41 MICHIGAN GEOLOGICAL AND BIOLOGICAL SURVEY Distributaries.......................................................... 42 Lake deposits ........................................................ 42 Publication 12. Geological Series 9. CHAPTER IV. Physical Geography (Continued). .......44 GEOLOGICAL REPORT ON WAYNE COUNTY Surface drainage..........................................................44 BY Stream development ............................................. 44 W. H. SHERZER. Drainage systems.................................................. 45 Lakes, ponds, swamps and drains ........................ 54 PUBLISHED AS A PART OF THE ANNUAL REPORT OF THE Soils and subsoils. .......................................................55 BOARD OF GEOLOGICAL SURVEY FOR 1911. General characteristics.......................................... 55 LANSING, MICHIGAN Clay soils ............................................................... 55 WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS Sand and gravel soils ............................................ 56 1913 Loam...................................................................... 57 Silt.......................................................................... 58 Contents Muck ...................................................................... 58 Amelioration of soils .............................................. 59 CHAPTER I. Geographical and Historical CHAPTER V. Physical geography (Continued)..........61
    [Show full text]
  • Geoscenario Resources—Glaciers
    Geoscenario Resources—Glaciers: Geologist Task Now that you have explored as a team the general story of how glaciers shaped the midwestern and northeastern United States, it is time for each of you to dive into more specialized information. The geologist focuses on regional features shaped by glaciers and how they formed. Add helpful details to your notes for Geoscenario Team Questions. Then work together and combine all the information to successfully present your story of glaciers. Questions for the Geologist to Consider • What geological features in this region were formed by glaciers? • What is the geological story of how the features were formed? Information Over a period of 10,000 years (100,000–110,000 years ago), the temperature dropped about 17°C, and the most recent glacial period began (evidence from oxygen ratios and foraminifera data). Around 20,000–35,000 years ago, the Laurentide (or Wisconsin) Ice Sheet covered most of Canada and a large portion of the northern United States. The massive ice sheet scraped away layers of earth materials as it pushed southward. Geologists look for clues today that help them determine the path and rate of glacial movement. The Great Lakes A glacier pushing poorly sorted glacial till in front of it. The glacial till forms a fill basins that the glaciers carved. In other areas, moraine. © iStockphoto/cotesebastien exposed rock displays scrape marks created by advancing ice carrying rocks and debris, called glacial till. Piles of glacial till form landmarks like moraines. Even huge boulders can be carried by glaciers. When geologists spot a boulder in an unexpected place, called an erratic, they often suspect a glacier carried it there.
    [Show full text]
  • Congressional Record-Senate. 3861
    1886. CONGRESSIONAL RECORD-SENATE. 3861 By Mr. WHEELER: Petition of Margaret W. Roach, asking that her The scope of the investigation, as actually conducted by the com­ case, with evidence before the Southern Claims Commission, be referred mittee,· is stated in the majority report as follows: to the Court of Claims-to the Committee on War Claims. • Whenever our attention was called to anything which indicated the probable • By Mr. A. C. WHITE: Memorial of Grange No. 680, of Pennsylvania, employment of improper means to gain support, we followed the clews pre­ against the reduction oftariffon wool and other raw materials-to the sented on the theory t.llat we were not only authorized, but in duty bound, to pursue any matter that promised even remotely to show the ~se of such means Committee on Ways and Means. in connection with the election, because the discovery of one Important fact, al­ Also, memorial of the same, for the passage of bill to suppress the thoughhavingnoimmedia.tebearingup6nthechargeagai?-sttheperso~snam.ed manufacture and sale of all imitation dairy products--:-to the Committee in the resolution, might lead to the discovery of facts havmg such bearmg. And furthermore, and upon the same-theory, our i';lquiries'Yere ~ot confined on Agriculture. · to the technical rules of legal proof, but the committee availed 1tse1! c;>f any By Mr. MILO WHITE: Petition of citizens of Minnesota, for regu- source af information-admitted hearsay statements and even the opmions of lating imitation dairy products-to the same committee.. _ witnesses. By Mr. WILKf.NS: Petition of B.
    [Show full text]
  • Ohio Radiocarbon Report-Radiocarbon Ages From
    OHIO RADIOCARBON REPORT RADIOCARBON AGES FROM OHIO’S SURFICIAL MATERIAL by Melinda C. Higley & Tyler A. Norris Open-File Report 2020-1 Columbus 2020 DISCLAIMER The information contained herein has not been reviewed for technical accuracy and conformity with current Ohio Department of Natural Resources (ODNR), Division of Geological Survey standards for published or open-file materials. The ODNR Division of Geological Survey does not guarantee this information to be free from errors, omissions, or inaccuracies and disclaims any responsibility or liability for interpretations or decisions based thereon. GRAPHIC DESIGN & LAYOUT: Jeremy E. Gladden EDITING: Anthony J. Bresnen COVER IMAGE: Layers of organic-rich sands from proglacial lake deposits in an aggregate pit near Whitehouse, Ohio. RECOMMENDED CITATION: Higley, M.C., and Norris, T.A., 2020, Ohio Radiocarbon Report: Radiocarbon ages from Ohio surficial material: Columbus, Ohio Department of Natural Resources Division of Geological Survey Open-File Report 2020-1, 28 p. CONTENTS Abstract ............................................................................................. 1 Introduction ........................................................................................ 1 Radiocarbon dating ................................................................................ 1 Ohio’s glacial geology .............................................................................. 1 Previous work .................................................................................... 2
    [Show full text]
  • The Geologic Framework of the Ohio Area of Lake Erie
    U.S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY THE GEOLOGIC FRAMEWORK OF THE OHIO AREA OF LAKE ERIE BY J.A. FULLER 1, R.C. CIRCE2, AND R.N. OLDALE3 OPEN-FILE REPORT 95-220 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. lOhio Geological Survey, Sandusky, Ohio 44870 2 U.S. Geological Survey, Reston, Virginia 22092 3 U.S. Geological Survey, Woods Hole, Massachusetts 02543 CONTENTS INTRODUCTION................................................ 1 METHODS..................................................... 4 RESULTS..................................................... 5 ELEVATION OF THE BEDROCK SURFACE............................ 6 ELEVATION OF THE TOP OF THE GLACIALLY RELATED SEDIMENTS..... 7 THICKNESS OF THE GLACIALLY RELATED SEDIMENTS................ 9 THICKNESS OF THE POSTGLACIAL LAKE DEPOSITS.................. 10 DISCUSSION AND CONCLUSIONS .................................. 11 ACKNOWLEDGEMENTS ............................................ 12 REFERENCES .................................................. 13 LIST OF ILLUSTRATIONS Index map. Showing the location of track lines and profile shown on Figure 3. Figure 1. Bathymetric map showing locations of cores, boreholes, and bottom samples. Figure 2. Proglacial lake level phases and postglacial lake level recovery curves. Figure 3. Finger and boomer records with line interpretation. Figure 4. Generalized cross section of units. Figure 5. Map showing the elevation of the bedrock surface. Figure 6. Map showing the elevation of the top of the glacially related deposits. Figure 7. Isopach map of the glacially related sediments. Figure 8. Isopach map of the postglacial lake deposits. 11 THE GEOLOGIC FRAMEWORK OF THE OHIO AREA OF LAKE ERIE by J.A. FULLER, R.C. CIRCE, AND R.N. OLDALE INTRODUCTION In September of 1991, the Ohio Department of Natural Resources-Division of Geological survey began field work as part of a cooperative with the U.S.
    [Show full text]
  • Black Hi3tory
    DOCUMENT RESUME ID 176 9 3 SI 028 907 AUTHOR Jeukins, Edward p. Sd. TITLE American ElackiScientists and Inventors. INSTITUTION National Science Teachers Asscciation, WazhinIton, D.C. PUB DATE 75 NOTE 85p.; Not available in hard copy due to ccpyright restrictions AVAILABLE FROM' National Science Teachers Associaticn 1742 Connecticat Ave.. N.W., Washington, D.C. 20009 (Stock No. 471-14690; $2.50) EDRS PRICE MPO1 Plus Postage. PC Not Available-from EDRZ. DESCaIPTOgS Black Education; *Black Emplcyment; *BlackHi3tory; Blacki Leadership; Black Rcle; Blacks; Black Studies; . Innovation; *Inventions; Research; Science Education; *Science History; Scientific Personnel; Scientific Research; *Scientists; Technology ABSTRACT Presented are the stories of 12 notable black scientists and inventors. Each individual wasselected fox scientific and inventive excellence with theadded accounts of their excellence as citizens, family men,,andhumanitarian's. (Author/RE) ( *********************************************************************** Reproductions supplied by EDES are the best that canbe made from the original document. *****************************1***************************************** t "11. e' 1 AMERICAN BLACK SCIENTISTS AND INVENTORS , 0.41.0111! MR HOF :CHE ONO N L:1 ..1.77IYI {,f tt- IIP,Jc f.Ti()SFS k 'AWE k NATIONAL SCIENCE TEACHERS ASSOCIATION "11 AMERICAN BLACK SCIENTISTS AND INVENTORS EDWARD S. JENKINS EdD, Editor Associate Professor of Science Education and Director of Educational Opportunity Program State University of New York at Buffalo GOSSIE HAROLD HUDSON PhD Professor of History and Chairman, Division School Sciences Lincoln University Jefferson City. Missouri '0 W. SHERMAN JACKSON PhD Assistant Profe'Ssor of Constitutional History Miami University of Ohio EXYIE C. RYDER PhD Associate Professor of Science Education Southern University Oaton Rouge. Louisiana Cover design and mit sketches for the chapter hea.is by Kathy Nichols, atUdent at Southern University in ;Baton Rouge.
    [Show full text]
  • Ottawa National Wildlife Refuge Complex
    Hydrogeomorphic Evaluation of Ecosystem Restoration and Management Options for Ottawa National Wildlife Refuge Complex Prepared For: U. S. Fish and Wildlife Service Region 3 Bloomington, MN Greenbrier Wetland Services Report 16-02 Mickey E. Heitmeyer Cary M. Aloia Josh D. Eash Mary S. Gerlach September 2016 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION AND MANAGEMENT OPTIONS FOR OTTAWA NATIONAL WILDLIFE REFUGE COMPLEX Prepared For: U. S. Fish and Wildlife Service Region 3 Refuges and Wildlife Bloomington, MN 55437 and Ottawa National Wildlife Refuge 14000 West State Route 2 Oak Harbor, OH 43449 By: Mickey E. Heitmeyer Greenbrier Wetland Services Advance, MO 63730 Cary M. Aloia Wetland Dynamics Monte Vista, CO 81144 and Josh D. Eash Mary S. Gerlach U.S. Fish and Wildlife Service, Region 3 Water Resources Branch Bloomington, MN 55437 Greenbrier Wetland Services Report No. 16-02 September 2016 Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Route 2, Box 2735 Advance, MO 63730 www.GreenbrierWetland.com Publication No. 16-02 Suggested citation: Heitmeyer, M. E., C. M. Aloia, J. D. Eash, and M. S. Gerlach. Hydrogeomorphic evaluation of ecosystem restoration and management options for Ottawa National Wildlife Refuge Complex. Prepared for U. S. Fish and Wildlife Service, Region 3. Report No. 16-02. Blue Heron Conservation Design and Print- ing LLC, Bloomfield, MO. Photo credits: USFWS, https://www.flickr.com/photos/136805129@ N03/; Cary Aloia, GardnersGallery.com; Karen Kyle This publication printed on recycled paper by 2 Contents EXECUTIVE
    [Show full text]
  • Shoreline Sediment Problems
    PART 2 SHORELINE SEDIMENT PROBLEMS CHAPTER 5 GEOLOGIC HISTORY OF GREAT LAKES BEACHES Jack L. Hough Department of Geology University of Illinois Urbana, Illinois ABSTRACT The locations of the Great Lakes and many details of the lake bottom topography bear a distinct relationship to the bed rock structure. Normal stream erosion in pre-glacial time probably etched out the major topographic relief of the region, forming the major basins and even some of the present bays, in the weak rock belts. Glacial ice, advancing over the region in several stages, followed the lowlands but reshaped them and probably deepened most of them. The known lake history, beginning with the last retreat of the ice from the southern rims of the Michigan and £rie basins, involves a number of stages at different levels in each of the basins. These lakes discharged at various places at different times, because of readvancement or retreat of the glacial ice front and because of tilting of the earth's surface. The writer's summary of this history is illustrated by a series of sixteen maps. The practical importance of two extremely low lake stages is pointed out. These have affected foundation conditions in the vicinity of many river mouths. The newly established recency of some of the higher lake stages (Nipissing and Algoma), and the revision of the elevations attained by them, affect estimates of the intensity of beach action and they affect conclusions regarding the time of last discharge of water through the Chicago outlet. INTRODUCTION Many details of the geologic history of the Great Lakes are pertinent to the study of present day shore processes and to foundation problems along the lake shores.
    [Show full text]