"Do Not Eat" Fish & "Avoid Foam" Advisories
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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 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 -
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). -
North Ridge Scenic Byway Geology
GUIDE TO THE NORTH RIDGE SCENIC BYWAY GEOLOGY LANDFORMS The North Ridge Scenic Byway corridor lies in the Erie Lake Plain landform of the Central Lowlands Physiographic Province of the United States (Fenneman 1938; Brockman 2002). The Lake Plain consists of wide expanses of level or nearly level land interrupted only by sandy ridges that are remnants of glacial-lake beaches and by river valleys carved into Paleozoic bedrock. With the exception of the sandy ridges, much of the Lake Plain in Avon and Sheffeld was a dense swamp forest prior to settlement. The North Ridge Scenic Byway follows the northernmost ancient beach ridge as it traverses Sheffeld and Avon at an elevation ranging from 675 to 690 feet above sea level, some 105 to 120 feet above modern Lake Erie. Topography of Sheffeld and Avon Townships as surveyed in 1901, showing North Ridge near the center of the map (courtesy of U.S. Geological Survey, Oberlin, Ohio Quadrangle 1903). 2 GEOLOGY FORMATION OF NORTH RIDGE Approximately 18,000 years ago, the last The chronology of lake stages in the Lake continental glacier blanketed northern Ohio as Erie basin relates a fascinating story of glacial it pushed down from the north to its maximum action, movements of the earth’s crust and southern thrust. The ice sheet reached as far erosion by waves to form the body of water south as Cincinnati, Ohio, then it began to we see today. The story begins nearly 15,000 melt back. As the glacier paused in its retreat, years ago as the last glacier [known as the piles of rock and clay debris [known as end Wisconsinan ice sheet] temporarily halted to moraines] were built up at the ice margins. -
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. -
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 -
2019 IL Fishing Information WEB DRAFT
Illinois 2021 REGULATION INFORMATION Effective: April 1, 2021 through March 31, 2022 Inside: • Current fishing regulations • Aquatic nuisance species • Places to fish • Illinois fish and your health • Current state records • Catchable trout program • Angler Alerts! • Free Fishing Days Division of Fisheries www.dnr.illinois.govFC1 www.ifishillinois.org Message from the Director Thank you for your interest in fishing in Illinois and for reviewing this 2021 edition of the Illinois Fishing Information guide. This booklet is an excellent resource for details on the best places to fish in Illinois, along with the rules and regulations in place for the 2021 season. During the last year, as we all dealt with the many challenges of the coronavirus pandemic, we saw an increase in interest in spending time outdoors in Illinois, including new and renewed interest in fishing. Our Division of Fisheries staff prepared this 2021 Illinois Fishing Information guide to provide an updated summary of statewide fishing regulations, as well as details on important site-specific regulations organized by the body of water or water area at which those regulations apply. On occasion, some site-specific regulations may be changed in emergency situations through the administrative rule process. In those cases, the changes are posted at the location where the rules apply, and online at www.ifishillinois.org. A reminder that the 2021 Illinois Free Fishing Days will be Friday, June 18 through Monday, June 21 – Father’s Day weekend – providing families and individuals a chance to go fishing even if they have not yet purchased an Illinois fishing license. The purchases of fishing licenses and equipment help fund our fisheries programs and ensure the future of fishing in Illinois. -
Late Glacial Origin of the Maumee Valley Terraces, Northwestern Ohio1
Late Glacial Origin of the Maumee Valley Terraces, Northwestern Ohio1 JACK A. KLOTZ2 AND JANE L. FORSYTH, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. Four major paired terraces and six short local terraces have been identified along the Maumee River valley between the Ohio-Indiana state line and Perrysburg in northwestern Ohio by detailed field mapping and study of gaging-station records, water-well logs, and soils data. From highest to lowest, the paired terraces have been named the Antwerp, Florida, Napoleon, and Grand Rapids terraces. The three higher terraces are correlated with Glacial Lakes Warren I and II, Lake Wayne, and Lake Grassmere, respectively, based on similarities in elevation of the lowest end of the terraces and the lake levels. The lowest of the four major terraces, the Grand Rapids Terrace, is rock-defended, controlled by outcrops of the Silurian Tymochtee Dolomite in its channel at Waterville. The short local terraces appear to be related to short-lived stages in the cutting of the Maumee Valley. Although some may correlate with one of the major terrace systems, such correlations remain tentative because of the isolation of these local terraces. OHIO J. SCI. 93 (5): 126-133, 1993 INTRODUCTION TABLE 1 The Maumee River is the largest river draining northwestern Ohio. It heads in Indiana, and is fed by Glacial Lakes in the Erie Basin. tributaries in Indiana, Michigan, and Ohio, creating a 2 drainage basin encompassing approximately 19,425 km Lake Elevation Outlet (7,500 mi2) (Cross and Weber 1959). The Maumee River flows across a broad, low lake plain formed by ice- dammed lakes in the Erie Basin during the retreat of the Modern Lake Erie 174 m (570 ft) Niagara Wisconsinan ice sheet (Leverett 1902; Leverett and Taylor Early Lake Erie 128 m (420 ft) Niagara 1915; Carman 1930; Forsyth 1966, 1970, 1973; Calkin and Feenstra 1985; Coakley and Lewis 1985; Eschman and Lundy 189 m (620 ft) east* Karrow 1985). -
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 -
Evidence of Sequence and Age of Ancestral Lake Erie Lake-Levels, Northwest Ohio
62 ANCESTRAL LAKE ERIE LEVELS VOL. 115 Evidence of Sequence and Age of Ancestral Lake Erie Lake-Levels, Northwest Ohio TIMOTHY G. FISHER, Department of Environmental Sciences, University of Toledo, OH, USA; JOSEPH D. BLOCKLAND, Department of Environmental Sciences, University of Toledo, OH, USA, North Dakota Geological Survey, Bismarck, ND, USA; BRAD ANDERSON, Department of Environmental Sciences, University of Toledo, OH, USA, Nyrstar Tennessee Mines, Gordonsville, TN, USA; DAVID E. KRANTZ, Department of Environmental Sciences, University of Toledo, OH, USA; DONALD J. STIERMAN, Department of Environmental Sciences, University of Toledo, OH, USA; RONALD GOBLE, Department of Earth and Atmospheric Sciences, University of Nebraska at Lincoln, Lincoln, NE, USA ABSTRACT. While the general scheme of the retreat of the Late Wisconsinan glacier from the ancestral Lake Erie basin is understood, the sequence and timing of those movements that caused lake-level changes are not well documented. Ground penetrating radar (GPR), electrical resistivity (ER), and optically stimulated luminescence (OSL) techniques were used to analyze beach and sand dune formations in the Wauseon area in northwest Ohio. The beaches showed no evidence of being flooded after deposition. Thirteen (13) new OSL ages revealed a short time of approximately 1000 years (16.9–15.9 ka) for formation of the Maumee, Arkona and Whittlesey shorelines. Evidence supporting the Ypsilanti lowstand in the ancestral Lake Erie basin was not observed within two sequences of glacial lacustrine sediments. The results of OSL dating of sand dunes indicate a period of older activity (~14–15 ka) and confirmation of previous work that documented activity during the Younger Dryas cold period (~13–11.5 ka). -
Geology of the Chicago Region
STATE OF ILLINOIS WILLIAM G. STRATTON, GoHntor DEPARTMENT OP REGISTRATION AND EDUCA'l'ION VERA M. BINKS, Dj,«UJr DIVISION OP THE STATE GEOLOG ICAL SURVEY M. M. LEIGHTON, Cbl;J URBANA B U L L E T I N N 0 . 65, P A 1t T I I GEOLOGY OF THE CHICAGO REGION PART II-IBEPLEISTOCENE BY J llARLBN BRETZ Pll.INTED BYUTHOlllTY A OF THE STATE O"l' lLLlNOlS URBANA, ILLINOIS 1955 STATE OF ILLINOIS WILLIAM G. STRATTON, Governor DEPARTMENT OF REGISTRATION AND EDUCATION VERA M. BINKS, Director DIVISION OF THE STATE GEOLOG IC AL SURVEY M. M. LEIGHTON, Chief URBANA B u L L E T I N N 0 . 65, p A RT I I GEOLOGY OF THE CHICAGO REGION PART II - THE PLEISTOCEN E BY J HARLEN BRETZ PRINTED BY AUTHORITY OF THE STATE OF ILLINOIS URBANA, ILLINOIS 1955 ORGANIZATION ST ATE OF ILLINOIS HON. WILLIAM G. STRATTON, Governor DEPARTMENT OF REGISTRATION AND EDUCATION HON. VERA M. BINKS, Director BOARD OF NATURAL RESOURC ES AND CONS ERVAT IO N HON. VERA M. BINKS, Chairman W. H. NEWHOUSE, PH.D., Geology ROGER ADAMS, PH.D., D.Sc., Chemistry R. H. ANDERSON, B.S., Engineering 0 A. E. EMERSO�. PH.D., Biology LEWIS H. TIFFANY, PH.D., Po.D., Forestry W. L. EVERITT, E.E., PH.D., Representing the President of the University of Illinois DELYTE W. MORRIS, PH.D. President of Southern Illinois University GEOLOGICAL SURVEY DIVIS IO N M. M. LEIGHTON, PH.D., Chief STATE GEOLOGICAL SURVEY DIVISION Natural Resources Building, Urbana M. M. LEIGHTON, PH.D., Chief Esm TOWNLEY, M.S., Geologist and Assistant to the Chief VELDA A. -
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.