DOCSLIB.ORG

INGHAM COUNTY NEWS 10 Pages

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
INGHAM COUNTY NEWS 10 Pages Pages INGHAM COUNTY NEWS 10 Pages H)h. LIX MASON, MICH., THURSDAY, SEPTEMBER 6, 1917 NO. 36 MKS. MOLLIIO .SOUTT, WILCO.V UKUNION. Mrs. Nellie Scutt, wife of Tommy The seventh annual reunion of the Scutt, of Aurelius, who died a short GOME TO MASON'S BIG FREE STREET F1-- Wilcox family was held Thursday, time ago, passed away at the Sparrow August 30, at the Mason city park. hospital in Lansing, last Wednesday The day was spent in visiting and a HI M. E, afternoon, August 29, following an JURYMENS PICNIG-SOLDIER-SAILOR REONION basket dinner was served at noon, af­ operation for cancer, ter which Ice cream and cake were Mlt ANI> MKS. S. O. I'AltKFR MAR- .1, e V.WniOltCOOK TAIiKS OX Nellie Dletz was born December 14, SlilPT. II), 20, 21 Wllili HK lilCi HANIKLS-HAIJLKV UHUNION. served. Relatives were present from I'ltl'.SKN'l' WAIl. 1870, on the farm two miles north of DAVS IN COUNTY SKAT. Last Saturday September 1, about Dlmondale, Bay City and Battle lUr.n I'll'TY VKAK.S. Dlmondale, where she had lived, all 100 relatives met at the home of Mr. Creek. Mrs. Jessie Felton was elect­ I'olks At Home Duty Is To Keep her life. In the spring of IJllO she lOvcrytliiiiK Points To A Itiiiiiici' Fnir and Mrs, Samuel Boyce in Linden to ed president, Miss Ethel Gregg vice Phil McKunian Woman's Reliuf C^irin Up Spii'it Of Koys Now was married to Tommy Scutt of Aure­ Many lOxlilhits PfoinLsed And enjoy a reunion of the Daniels and president and Mrs. Maranda Hulse (iivu Reception In Honor of Coni- FightiiiK- lius. One daughter Margaret was .-OtMMl Time Assiiivd. Hadley families. After the dinner secretary and treasurer. The next nide und Mrs. Piirkur. born to them, who survives her moth­ hour, u pleasing program was given reunion will be held with Mr. and hip Iceop up the spirits of our er. Mrs, Scutt leaves a host of friends, All roads will lead to Mason, Mich­ and oflicers for the coming year elect­ Mrs. J. W. Mosher In Bay City, the An event of unusual Interest la :ii Francje," w.is one ot the state- who will miss her In their community. igan, Sept. 19, 20, 21. Mason's Free ed. Guests were present from Amery, last Thursday in August, 1918. Grand Army and Woman's Relief I iiiiulo by Dell C, Vaiulercook In Agricultural Street Fair is an assured Wis,, Ann Arbor, Mason, Fowlervllle, Corps circles, was the celebration ot ir talk at the M.' E. church Sun- success, attractions secured, exhibits Hamburg, Gregory, Tecumseh, Tip­ the Golden wedding anniversary ot • loniliiK. Mr, Vandorcook is the promised, liberal premiums offered. ton and Stockbrldge. Comrade S. C, Parker and wife at the or Mr. and Mrs, A. L. Vandorcook MENGE FIELD WEDS In fact every one has guaranteed their OLIVER GRIFFIN PASSES ' G. A, R, hall last Saturday evening. niii! of llio editors of the National support and co-operations except the Probably seventy-live members of the 1 riiilon of Y, M. C, A. in New weatherman—but he.has a habit ot two organizations, with "the invited K (lily. He has Ijoen on an in- ATUNTIC OITY GIRL AWAY THURSDAY MORNING guests of the familyi witnessed the- holding off 'till the last minute. SCHOOLS OPEN ceremony pQ.rformed by a former pas­ I on tour of tlio Y. M. C. A, work \vi ICIO MAI{|{|l':il AT ATLANTIC Col, Ives has been induced to act HAS LIVEh IN INOHAM COUNTY I mining camps In llie eastern FIFTY-NINE YEARS, tor of the Parkers, Rev, .1. If. Stewart (;ri'Y AuousT 22. as secretary and the Colonel Is letting of Portland, Michigan, ' I. II ()£ Llio United States and came no grass grow under his feet and is • irnni (ho Groat Lakes Training A pretty home wedding was solem­ ON TOESDAY M0RNIN6 Oliver Grlflln passed away last The hall itself was decorated in the ,• 10 ,ioin liis wife, who is visiting nized Wednesday, August 22, at the Thursday morning, August 30, at his iKillonal colors at one end. The sTiiiiKT FAiu omciins EXHOIVLMI'INT OF 22.5 IN THK Vollow Go'den Glow with fosloona ot 1 ,i)llior, Mrs. A. G, Bali, home of E, ,T, Smith, 28 North Texas HIGH SCHOOL. home in the nortliorii part of the city UK a Ijoy from this town his talk Ave., Atlantic City, N. ,T., when lleba Pros,—.Torome Waggoner at the age of 64. yollow und wliite crepe paper formed iiiuliiy aiM'rocialed hy tlio con- Gilbert, daughter of Mr. Christine G. Sec'v,—Col. L, H, Ives Two days previous, while in the llio (lecoralions for tlio front of the linn. Mr, Vandercook says More I'lvpocted To Heaiii .After Tlie hull, whore the bridal couple oC. Murlland, was unite'd in marriage to 'I'reas,—.1. E, Taylor Fall itush On Fiirm.s bay mow feeding slock, he fell-to the is no war spirit here when com- Lawrence Nortli Field, of East Lan­ basement, breaking several ribs and "lU'ly years" stood under a,eaiiopy of ,Su|iL'riiileu(lonls Is Over. yellow and white, fonuod of a white willi Ni'W York and otiior east- sing. Ivov. W- Bowen Uriioro of Col- Horses - 0, E. Boll being injured inlenially. It was nol iiids, lie has had the privilege purasol trimmed with Goldon Glow, liiigswood, N. J., ofllciatod, using tlio Cattle L. T. Lasenby and Tlie Mason public scliools opened lliouglit bis conrtllion was so serious, • ling many noted men from liur- iinprossivo old English service. but lie rapidly failed. Funeral ser­ 'I'ho liridal party enlGrod the luill lead Eugene Edgar ' 'i'uesday, Seplonibor 4, with an un­ hy the color boarcns, wlio wore fol­ Ak on l.iiis w!ir situation and luis Promptly at four o'clock, to the Slieep ,T. N. Thorburn vices wore held at llio homo Sunday, ' il many interesting facts from usually large onrolliiient. 'About 225 lowed by Ucv, Stewart, Mr, and Mrs. strains of tlie wedding march from Swine Carl .Tewelt are enrolled in the high school, tlie Soploniber 2, at two o'clock, liev, T. 111.' said if the war lasted Lohengren, rendered by Miss Frances W. Hughes ofriciallng, and interment •Towelt, and Mr. and Mrs, Baniaby, Poultry Mason E. Reynolds freshman class alone claiming 52. llion the bride and groom, wlio stood ,\'i?ai's, as Is tiio general belief, Mann'uni, the bridal party took (heir Grain, Fruit and It was found necessary to divide this was made in tlie Maple Grove ceme­ ,11 not think of ourselves as in- places beneath an arch of golden glow tery, l)enoath the canopy while a ceremony Vegetables.Mason U. D. Carriers class into two and three sections. prepared for such occasions, and as lais, Init as one large organiza- and while hydrangeas. About sev­ Baked Goods. .Mrs. C. W. Randall Mr, Grinin was the son of Mr. and or sfvt>ral organizations, doing Owing to the scarcity for farm lab­ nearly like the usual marriage cere­ enty-five guests were present, includ­ Embroidery. .Airs, M. E. Reynolds or, some were unable to attend at the Mrs. Itcsolvo Gridln, jMlchigan pio­ '•ry best to iielp out, ing Mr. and Mrs. F. II. Field and Mr. neers, deceased for some time. Ho mony as, possible, was perforn'ied. Concessions S, L, Marshall^ opening, but it is expected many more Mrs, Parker was gowned In while and . Vandercook tried to Impress and Mrs, S. E, Field ot this city. Af­ Sports "Jack" Symons* spent all of his life in Mason, with .• minds of all who had a loved will come as soon as they can be carried a cluster bouquet ot white ter a wedding luncheon, the couple spared from the farms. The usual the exception of five years In Califor­ ill the trenches or some who loft for Michigan, stopping at Phil­ nia. Ho assisted his father In farm­ asters. The groom wore the conven­ completing the details that go to work In science, nialhematics, 13ng- tional black. Members of the bridal I soon be leaving that it was adelphia, Pa., Ellzabethport, N, J,, make this Street Fair one to be long ing uiitil his death, and then cared 'Inty to help them keep up their lish, languages and history are offer­ party carried sprays of Golden Glow. and Niagara Falls, remembered. Mr. Ives can be found ed. for his own farm. Ho was married to ; in every way possible. It is Miss Delia Canahan and a daughter, As the ceremony closed, Ralph The bride was attired in white at the News ollice any day and can be A new form of study has been ar­ Adams sung "Oil Promise Me," after ilal to help them endure the braided georgette crepe and carried gotten on either phone. Nellie, was born to them. At the age hips and keep up good, strong ranged for this year/which will be of 12 years she was taken from the which the bride and groom of ilfty white roses. She was attended by Invitations are being sent out for very beneficial to the students. The summers received the congratula­ |i iRi', Any man, no matter how her sister. Miss Anna Murtlaiid, and the annual Jurymen's Picnic which Coldwater school and murdered, He 111? nuiy 1)0 fed and in what good class hour has been lengthened five was united in marriage to Miss Mamie tions of their many friends and Mr, Shirley E, Field of this city, will be held on the court house lawn minutes and a portion ot this 50- guests.
Load more

Recommended publications
  • MAPPING and CHARACTERIZING a RELICT LACUSTRINE DELTA in CENTRAL LOWER MICHIGAN by Christopher B. Connallon a THESIS Submitted T
    MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of Geography – Master of Science 2015 ABSTRACT MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon This research focuses on, mapping and characterizing the Chippewa River delta - a sandy, relict delta of Glacial Lake Saginaw in central Lower Michigan. The delta was first identified in a GIS, using digital soil data, as the sandy soils of the delta stand in contrast to the loamier soils of the lake plain. I determined the textural properties of the delta sediment from 142 parent material samples at ≈1.5 m depth. The data were analyzed in a GIS to identify textural trends across the delta. Data from 3276 water well logs across the delta, and from 185 sites within two-storied soils on the delta margin, were used to estimate the thickness of delta sands and to refine the delta's boundary. The delta heads near Mount Pleasant, expanding east, onto the Lake Saginaw plain. It is ≈18 km wide and ≈38 km long and comprised almost entirely of sandy sediment. As expected, delta sands generally thin away from the head, where sediments are ≈4-7m thick. In the eastern, lower portion of the delta, sediments are considerably thinner (≈<1-2m). The texturally coarsest parts of the delta are generally coincident with former shorezones. The thick, upper delta portion is generally coincident with the relict shorelines of Lakes Saginaw and Arkona (≈17.1k to ≈ 16k years BP), whereas most of the thin, distal, lower delta is generally associated with Lake Warren (≈15k years BP).
    [Show full text]
  • Great Lakes Region, USA
    Spatial variation in till texture and clay mineralogy across the Saginaw Lobe terrain, Great Lakes region, USA Department of Geography, Environment and Spatial Sciences, Randall J. Schaetzl, Chris Baish, Jarrod Knauff, Thomas Bilintoh, East Lansing, Michigan, USA Dan Wanyama, Kevin McKeehan, and Michelle Church Abstract STUDY AREA SAMPLE DISTRIBUTION Great Lakes region We present a spatial/mapping approach to the study of the glacial history of the Saginaw lobe of the Laurentide Ice Sheet. The Saginaw Lobe flowed into southern Michigan, USA, forming modern-day Saginaw Bay and leaving behind a series of small moraines in down- ice locations. Upon its retreat – and likely also during its advance – a large proglacial lake (Glacial Lake Saginaw) formed in the northeastern margins of the “Saginaw terrain”. The Saginaw lobe advanced to the southwest, out of this lake basin and onto thinly mantled, sandstone and shale bedrock. Although the Late Pleistocene deglacial chronology of this lobe has been generally assumed for decades, few numerical ages exist that could help constrain a better defined timeline. Indeed, as luminescence ages slowly emerge for terrain of the Saginaw Lobe and nearby areas, it seems clear that the lobe retreated from the region considerably earlier than is generally assumed, adding to the potential for large areas of ponded water in proglacial settings, all of which are as yet unmapped. In this project, we sampled tills on uplands across the terrain of the Saginaw Lobe, avoiding outwash plains. In all, we obtained 334 samples of calcareous till, by bucket auger. Sample locations were sited generally uniformly across >20,000 km2.
    [Show full text]
  • Ellsworth American COUNTY Dunham’S Hotel
    Sbfcntfennmt*. Rsed, of Kllsworth, and Mrs. Annie 'Itjfnrtiacmmis. _ v- LOCAL AFFAIRS. Powers, of Bangor. Mrs. Higgins had friends in Ellsworth who NEW AI1VKUTIM M ENT* THIS WEEK. many regret C. 0. RURRILL & deeply to hear of her death. She visited SON, state assessor**’ notice. here about two *■* I‘s ('omtnissiiiu of fi-h and fisheries—Sealed years ago. ^ 1 proposals. The Mutual Life Insurance Co., of New Hancork lmll— M urrDon ( omeily « «>. m j of m qenekal INSURANCE Robert It H" in. < *<ut *\ culture *»ale- York, *, |Kent, of this city, j AGENTS, I’anook Is a speciafagent, has paid through Mr. Hi him Bank Bldg., ELLSWORTH, ME. Tyler, Fogg A « •»—Municipal bonds. Kent the policy of |15,0CK) on the life of ^ Rockland, My the late W. it. Blaisdell, of Franklin. ARSOL«JT.F*v 'piJRE Rockland Cumin* rc’.al < *•!!* ;<■. WE REPRESENT THE This is one of the largest policies of life \ A '•:iimri)1 '* > in«u1 me v; paid in this vicinity. Makes the food more de'icious and v 'v '. sew Most Kciiiihle Home ami Foreign Coni pan it's. Curtis Novelty < <>— Agent wanted George W. Davis, of Boston, formerly J'■■//> a ih/r V'i/h ! ■■■■■■■BHanannaHDunaniaaBHBaMHManiir^nMnnnnHr «ommJ9 L Safi )J. of this a brother of 10. Davis, t'nvijmt Far othrr focal news see pages •/, .7 and S. city, Henry lias purchased the Tontine house at Miss Mari* *i of Auburndaln, In sums to Hu it on real c.si ate and Morgan, Unitarian noinc. improved Brunswick. The Tontine is a popular re- of the engine had passed over the boy’s Conference at MON KY TO LOAN J is the guest of Miss Mabel —--- collateral.- ..
    [Show full text]
  • The Clinton Independent,A^M HANDSOME Dtepiar of Pattern
    BOTCHER k PETNCITS OPENING of Fall and Winter Millinery Will Occur FRIDAY AND 8ATCRDAT. SEPTEMBER 27 and 28. T'HK iiu»l and new—I nor*In ^m HANDSOME dtepiar of Pattern (n Era1 1—i Fall aad Winter M Htl per feet g en -will a* *x- A Sthlted at <Mtr o—um Frt4«> •n mat now be mmintoeri and ftatepirar. Srpt *1 aad ». A —e- vitatlun to love— of art aad HOUCHIB * I»BTSCU Laeaiy- The Clinton Independent, UOUCHKB * PI VOL XXIX.—NO. #0 ST. JOHNS, MICH.. FRIDAY MORNING, SEPTEMBER 27. 18»5. WHOLE NO.—1510. New Advertisement*. — Mrs. Henry Mulder is confined to -Ninety-six tickets were sold at this —Official board meeting at M. E. This Wm* Only. Vtelt Oar *t»r* her home by sickuees. station for the excursion to Detroit laat church tomorrow evening. During the week of the Fair we will We extend to you a cordial invitation MercautHe Oo.— Dry Gnoda. Uromrtm aad Sunday. offer some special bargains to aash buy­ to visit (Mir store during the week of the Boots aad Shorn. —Geo. K. Horry, St. Johns, has been —Eugenie Fern in the latest society granted an increase of pension. —Judge Daboll will deliver an address dramas, at Seriven's Opera House all ers. Here are the inducements : fair—next week. Jokn HIckt-biT Oooda, Cloaks. Carpets. One gent ’s open faee gold filled watch Our trimmers are making ready a fine Wilson A Son—Clot i>ln«. —It i» reported that Earnest, son of at the Gratiot county fair, to-day .
    [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]
  • Glacial Lakes Around Michigan
    The Glacial Lakes around Michigan By William R. Farrand, University of Michigan Bulletin 4, revised 1988 Geological Survey Division Michigan Department of Environmental Quality Bulletin 4 - Glacial Lakes Around Michigan By William R. Farrand, University of Michigan, 1967 revised 1998 Illustrated by Kathline Clahassey, University of Michigan Published by Michigan Department of Environmental Quality. Geological Survey Division Contents Preface............................................................................................................................................ 3 Abstract........................................................................................................................................... 3 Introduction ..................................................................................................................................... 4 Was There A Glacier?..................................................................................................................... 4 Figure 1: The modem Great Lakes have a water surface area greater than 95,000 square miles, a total drainage area of about 295,000 square miles, and a shore line 8,300 miles long. ................................................................................................4 Figure 2: Features originating at a glacier front occur in a definite order. ...................................................................................5 Figure 3: Landforms of continental glaciation are unmistakable. Compare with figure 2 ............................................................5
    [Show full text]
  • A Thesis Entitled Chronology and Sedimentology of the Imlay
    A Thesis entitled Chronology and Sedimentology of the Imlay Channel, Lapeer County, Michigan by Jonathan Neil Luczak Submitted to the Graduate Faculty as partial fulfillment of the requirements for the Master of Science Degree in Geology ________________________________________ Dr. Timothy Fisher, Committee Chair ________________________________________ Dr. David Krantz, Committee Member ________________________________________ Dr. Donald Stierman, Committee Member ________________________________________ Dr. Cyndee Gruden, Interim Dean College of Graduate Studies The University of Toledo December 2018 Copyright 2018, Jonathan Neil Luczak This document is copyrighted material. Under copyright law, no parts of this document may be reproduced without the expressed permission of the author. An Abstract of Chronology and Sedimentology of the Imlay Channel, Lapeer County, Michigan by Jonathan Neil Luczak Submitted to the Graduate Faculty as partial fulfillment of the requirements for the Master of Science Degree in Geology The University of Toledo December 2018 The Imlay channel on the thumb of Michigan was one of two outlets for the Maumee stages (i.e. I–III or IV) of ancestral Lake Erie (ALE). The history and chronology of sediment within the channel is poorly understood, having been studied only sporadically over the last 100 years. Previous studies interpreted the floor of the channel to be the aerially exposed topographic divide near the intersection of Clear Lake and Van Dyke roads. However, geotechnical borings and water-well records along Clear Lake Road suggest that the bedrock sill that controlled drainage through the channel may be buried by more than 12 m of sediment that post-dates channel formation. A single radiocarbon age, i.e. ~16.7 calibrated ka BP, from ~6 km north of the Imlay channel was interpreted in most of the literature to mark the cessation of channel activity; an age from organic material found within colluvium replicates this age in this study.
    [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]
  • Geologic Framework and Glaciation of the Eastern Area Christopher L
    Boise State University ScholarWorks Anthropology Faculty Publications and Department of Anthropology Presentations 1-1-2006 Geologic Framework and Glaciation of the Eastern Area Christopher L. Hill Boise State University This document was originally published in Handbook of North American Indians. Geological Framework and Glaciation of the Eastern Area CHRISTOPHER L. HILL Late Pleistocene landscapes in glaciated eastern North In the Great Lakes region, the Wisconsin stage has been America included changing ice margins, fluctuating lake divided into a series of chronostratigraphic units (W.H. and sea levels, and deglaciated physical settings that were Johnson et al. 1997; Karrow, Driemanis, and Barnett inhabited by a variety of extinct (Rancholabrean) fauna. 2000). The Altonian substage dates to before 30,500 B.C. , The glaciated East of North America consists of the mid­ while the Farmdalian substage ranges in age from about continent from Hudson Bay to south of the Great Lakes 30,500 to 28,000 B.C. The Woodfordian substage ranges in and extends eastward to the Atlantic coast. Glaciers were age from about 28,000 to about 12,800 B.C.; it is associated present along the Atlantic coast from southern New York with extensive glacial activity and subsumes previously north to Labrador. used terminology such as Tazewell, Cary, and Mankato Some of this region appears to have been ice-free during (Willman and Frye 1970). The Twocreekan substage is parts of the Middle Wisconsin; the interstadial ice margin a short interval after the Woodfordian and before the around 33,400-29,400 B.C. may have been situated within the Greatlakean, generally ranging 12,800-11,800 B.C.
    [Show full text]
  • Irrigation Papers
    DEPARTMENT OF THE INTERIOR WATER-SUPPLY AND IRRIGATION PAPERS OP THE UNITED STATES GEOLOGICAL SURVEY No. SO WATER RESOURCES OF THE LOWER PENINSULA OF MICHIGAN. LANE WASHINGTON GOVERNMENT PRINTING OFFICE 1899 IRRIGATION REPORTS. The followhig list contains the titles and brief descriptions of the principal reports relating to water supply and irrigation, prepared by the United States Geological Survey since 1890: 1890. First Annual Report of the United States Irrigation Survey, 1890; octavo, 123 pp. Printed as Part II, Irrigation, of the Tenth Annual Report of the United States Geolog­ ical Survey, 1888-89i Contains a statement of the origin of the Irrigation Survey, a pre­ liminary report on the organization and prosecution of the survey of the arid lands for purposes of irrigation, and report of work done during 1890. 1891. Second Annual Report of the United States Irrigation Survey, 1891; octavo, 395 pp. Published as Part II, Irrigation, of the Eleventh Annual Report of the United States Geological Survey, 1889-90. Contains a description of the hydrography of the arid region and of the engineering operations carried on by the Irrigation Survey during 1890; also the statement of the Director of the Survey to the House Committee on Irrigation, and other papers, including a bibliography of irrigation literature. Illustrated by 29 plates and 4 figures. Third Annual Report of the United States Irrigation Survey, 1891; octavo, 576 pp. Printed as Part II of the Twelfth Annual Report of the United States Geological Sur­ vey, 1890-91. Contains " Report upon the location and survey of reservoir sitet during the fiscal year ended June 30, 1891," by A.
    [Show full text]
  • Lake Huron's Phosphorus Contributions to the St. Clair
    pubs.acs.org/est Article Lake Huron’s Phosphorus Contributions to the St. Clair−Detroit River Great Lakes Connecting Channel Donald Scavia,* Eric J. Anderson, Alice Dove, Brad Hill, Colleen M. Long, and Yu-Chen Wang Cite This: Environ. Sci. Technol. 2020, 54, 5550−5559 Read Online ACCESS Metrics & More Article Recommendations *sı Supporting Information ABSTRACT: The United States and Canada called for a 40% load reduction of total phosphorus from 2008 levels entering the western and central basins of Lake Erie to achieve a 6000 MTA target and help reduce its central basin hypoxia. The Detroit River is a significant source of total phosphorus to Lake Erie; it in turn has been reported to receive up to 58% of its load from Lake Huron when accounting for resuspended sediment loads previously unmonitored at the lake outlet. Key open questions are where does this additional load originate, what drives its variability, and how often does it occur. We used a hydrodynamic model, satellite images of resuspension events and ice cover, wave hindcasts, and continuous turbidity measurements at the outlet of Lake Huron to determine where in Lake Huron the undetected load originates and what drives its variability. We show that the additional sediment load, and likely phosphorus, is from wave-induced Lake Huron sediment resuspension, primarily within 30 km of the southeastern shore. When the flow is from southwest or down the center of the lake, the resuspended sediment is not detected at Canada’s sampling station at the head of the St. Clair River. ■ INTRODUCTION Canada and 83% of the urban land is in the United States.
    [Show full text]
  • A Fresh Look at the Sediments Within the Terraces And
    A FRESH LOOK AT THE SEDIMENTS WITHIN THE TERRACES AND CLIFFS THAT PARALLEL THE LAKE ERIE SHORE IN ERIE COUNTY, PENNSYLVANIA DAVID THOMAS and RAYMOND .BUYCE (Mercyhurst College) ... .. INTRODUCTION The lake plain adjoining the coastal bluffs of Lake Erie in Pennsylvania is comprised of two to three major southwest­ northeast trending terrace systems. They form a stair-step arrangement of very gently sloping terraces each bounded on the north by slightly to precipitously steeper escarpments or cliffs. The edges of these terraces have been referred to as "beach ridges" by several early workers (e.g. Leverett, 1892). Extensions of the terrace margins in Ohio and elsewhere are actually ridge-like although their beach origin has been questioned. Each relatively flat terrace level is reliably attributed to deposition associated with a corresponding lake level of a Pleistocene precursor to Lake Erie. It is still an open question whether the environment of deposition for any· particular terrace or part thereof can be justifiably ascribed to beach deposition or whether a braid-plain (sandar), delta, or some other setting might have been responsible. some of the early work relied heavily upon topographic expression to seek answers to the questions of origin but on this trip we will have the opportunity to look at two fine exposures within the terraces to see if the sedimentological evidence is more definitive. Exposed in the gravel pit at the first stop is the uppermost of the two terraces present along the southeastern part of the Harborcreek 7 1/2 minute quadrangle. The upper terrace is attributed to sediment deposition associated with Lake Whittlesey (elevation: 740 feet, age: 13,000 yr B.P.).
    [Show full text]