An Updated Radiocarbon-Based Ice Margin Chronology for the Last Deglaciation of the North American Ice Sheet Complex

Total Page:16

File Type:pdf, Size:1020Kb

An Updated Radiocarbon-Based Ice Margin Chronology for the Last Deglaciation of the North American Ice Sheet Complex ORE Open Research Exeter TITLE An updated radiocarbon-based ice margin chronology for the last deglaciation of the North American Ice Sheet Complex AUTHORS Dalton, AS; Margold, M; Stokes, CR; et al. JOURNAL Quaternary Science Reviews DEPOSITED IN ORE 19 August 2020 This version available at http://hdl.handle.net/10871/122545 COPYRIGHT AND REUSE Open Research Exeter makes this work available in accordance with publisher policies. A NOTE ON VERSIONS The version presented here may differ from the published version. If citing, you are advised to consult the published version for pagination, volume/issue and date of publication AS Dalton et al. Feb 2020 – final version 1 An updated radiocarbon-based ice margin chronology for the last deglaciation of the 2 North American Ice Sheet Complex 3 4 April S. Daltona,b, Martin Margoldb, Chris R. Stokesa, Lev Tarasovc, Arthur S. Dyked,e, 5 Roberta S. Adamsf, Serge Allardg, Heather E. Arendsh, Nigel Atkinsoni, John Attigj, Peter J. 6 Barnettk, Robert Langdon Barnettl,m, Martin Battersonn, Pascal Bernatchezl, Harold W. Borns, 7 Jro, Andrew Breckenridgep, Jason P. Brinerq, Etienne Brouardr,s, Janet E. Campbellt, Anders 8 E. Carlsonu, John J. Claguev, B. Brandon Curryw, Robert-André Daigneaultx, Hugo Dubé- 9 Louberty,z, Don J. Easterbrookaa, David A. Franzibb, Hannah G. Friedrichh†, Svend Fundercc, 10 Michelle S. Gauthierdd, Angela S. Gowanee, Ken L. Harrisff, Bernard Hétul, Tom S. 11 Hooyergg†, Carrie E. Jenningshh, Mark D. Johnsonii, Alan E. Kehewjj, Samuel E. Kelleykk, 12 Daniel Kerrt, Edward L. Kingll, Kristian K. Kjeldsencc,mm, Alan R. Knaebleee, Patrick 13 Lajeunesser, Thomas R. Lakemannn, Michel Lamothes, Phillip Larsonoo, Martin Lavoier, 14 Henry M. Loopepp, Thomas V. Lowellqq, Barbara A. Lusardiee, Lorraine Manzff, Isabelle 15 McMartint, F. Chantel Nixonrr, Serge Occhiettix, Michael A. Parkhillss, David J. W. Piperll, 16 Antonius G. Pronktt, Pierre J. H. Richarduu, John C. Ridgevv, Martin Rossww, Martin Royz, 17 Allen Seamang, John Shawll, Rudolph R. Steaxx, James T. Telleryy, Woodrow B. Thompsonzz, 18 Harvey L. Thorleifsonee, Daniel J. Uttingaaa, Jean J. Veillettet, Brent C. Wardv, Thomas K. 19 Weddlezz, Herbert E. Wright, Jrhh† 20 Author affiliations 21 aDepartment of Geography, Durham University, Durham, United Kingdom 22 bDepartment of Physical Geography and Geoecology, Charles University, Prague, Czech 23 Republic Page 1 of 90 AS Dalton et al. Feb 2020 – final version 24 cDepartment of Physics and Physical Oceanography, Memorial University, St. John’s, 25 Newfoundland, Canada 26 dDepartment of Earth Sciences, Dalhousie University, Halifax, Nova Scotia, Canada 27 eDepartment of Anthropology, McGill University, Montreal, Quebec, Canada 28 fMadrone Environmental Services Ltd, Abbotsford, British Columbia, Canada 29 gNew Brunswick Department of Energy and Mines, Geological Surveys Branch, Fredericton, 30 New Brunswick, Canada 31 hDivision of Lands and Mineral, Minnesota Department of Natural Resources, St. Paul, 32 Minnesota, USA 33 iAlberta Geological Survey, Edmonton, Alberta, Canada 34 jWisconsin Geological and Natural History Survey, Madison, Wisconsin, USA 35 kHarquail School of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada 36 lDépartement de biologie, chimie et géographie & Centre for Northern Studies (CEN), 37 Université du Québec à Rimouski, Rimouski, Québec, Canada 38 mGeography, College of Life and Environmental Sciences, University of Exeter, Exeter, 39 United Kingdom 40 nGeological Survey of Newfoundland and Labrador, St. John’s, Newfoundland, Canada 41 oSchool of Earth and Climate Sciences, University of Maine, Orono, Maine, USA 42 pNatural Sciences Department, University of Wisconsin–Superior, Superior, Wisconsin, USA Page 2 of 90 AS Dalton et al. Feb 2020 – final version 43 qDepartment of Geology, University at Buffalo, Buffalo, New York, USA 44 rDépartement de géographie and Centre d'études nordiques, Université Laval, Québec, 45 Québec, Canada 46 sDépartement des sciences de la Terre et de l'atmosphère, Université du Québec à Montréal, 47 Montréal, Québec, Canada 48 tGeological Survey of Canada, Natural Resources Canada, Ottawa, Ontario, Canada 49 uCollege of Earth, Ocean, and Atmospheric Science, Oregon State University, Corvallis, 50 Oregon, USA 51 vDepartment of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada 52 wIllinois State Geological Survey, Prairie Research Institute, University of Illinois at Urbana- 53 Champaign, Champaign, Illinois, USA 54 xDépartement de géographie, Université du Québec à Montréal, Montréal, Québec, Canada 55 yMinistry of Energy and Natural Resources of Quebec, Val-d’Or, Quebec, Canada 56 zDépartement des Sciences de la Terre et de l'atmosphère, Centre de recherche GEOTOP, 57 Université du Québec à Montréal, Montréal, Québec, Canada 58 aaDepartment of Geology, Western Washington University, Bellingham, Washington, USA 59 bbCenter for Earth and Environmental Science, State University of New York Plattsburgh, 60 Plattsburgh, New York, USA 61 ccCentre for GeoGenetics, Natural History Museum of Denmark, Copenhagen, Denmark 62 ddManitoba Geological Survey, Winnipeg, Manitoba, Canada Page 3 of 90 AS Dalton et al. Feb 2020 – final version 63 eeMinnesota Geological Survey, University of Minnesota, St. Paul, Minnesota, USA 64 ffNorth Dakota Geological Survey, Bismarck, North Dakota, USA 65 ggDepartment of Geosciences, University of Wisconsin, Milwaukee, Wisconsin, USA 66 hhDepartment of Earth and Environmental Sciences, University of Minnesota, Twin Cities, 67 Minnesota, USA 68 iiDepartment of Earth Sciences, University of Gothenburg, Sweden 69 jjDepartment of Geological and Environmental Sciences, Western Michigan University, 70 Kalamazoo, Michigan, USA 71 kkSchool of Earth Sciences, University College Dublin, Dublin, Ireland 72 llNatural Resources Canada, Geological Survey of Canada (Atlantic), Bedford Institute of 73 Oceanography, Dartmouth, Nova Scotia, Canada 74 mmDepartment of Glaciology and Climate, Geological Survey of Denmark and Greenland 75 (GEUS), Copenhagen, Denmark 76 nnGeological Survey of Norway, Trondheim, Norway 77 ooSwenson College of Science and Engineering, University of Minnesota Duluth, Duluth, 78 Minnesota, USA 79 ppIndiana Geological and Water Survey, Indiana University, Bloomington, Indiana, USA 80 qqDepartment of Geology, University of Cincinnati, Cincinnati, Ohio, USA 81 rrDepartment of Geography, Norwegian University of Science and Technology, Trondheim, 82 Norway Page 4 of 90 AS Dalton et al. Feb 2020 – final version 83 ssNew Brunswick Department of Energy and Mines, Geological Surveys Branch, Bathurst, 84 New Brunswick, Canada 85 ttGeological Survey, Energy and Resource Development, Fredericton, New Brunswick, 86 Canada 87 uuDépartement de géographie, Université de Montréal, Montréal, Québec, Canada 88 vvDepartment of Earth and Ocean Sciences, Tufts University, Medford, Massachusetts, USA 89 wwCentre for Groundwater Research, University of Waterloo, Waterloo, Ontario, Canada 90 xxStea Surficial Geology Services, Halifax, Nova Scotia, Canada 91 yyDepartment of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, Canada 92 zzMaine Geological Survey, Augusta, Maine, USA 93 aaaAlberta Energy Regulator, Calgary, Alberta, Canada 94 †deceased 95 Keywords 96 Quaternary; glaciation; North America; ice margin chronology; radiocarbon 97 Abstract 98 The North American Ice Sheet Complex (NAISC; consisting of the Laurentide, 99 Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay in 100 the Northern Hemisphere during the Quaternary. Understanding its pattern of retreat 101 following the Last Glacial Maximum is critical for studying many facets of the Late 102 Quaternary, including ice sheet behaviour, the evolution of Holocene landscapes, sea level, Page 5 of 90 AS Dalton et al. Feb 2020 – final version 103 atmospheric circulation, and the peopling of the Americas. Currently, the most up-to-date and 104 authoritative margin chronology for the entire ice sheet complex is featured in two 105 publications (Geological Survey of Canada Open File 1574 [Dyke et al., 2003]; ‘Quaternary 106 Glaciations – Extent and Chronology, Part II’ [Dyke, 2004]). These often-cited datasets track 107 ice margin recession in 36 time slices spanning 18 ka to 1 ka (all ages in uncalibrated 108 radiocarbon years) using a combination of geomorphology, stratigraphy and radiocarbon 109 dating. However, by virtue of being over 15 years old, the ice margin chronology requires 110 updating to reflect new work and important revisions. This paper updates the aforementioned 111 36 ice margin maps to reflect new data from regional studies. We also update the original 112 radiocarbon dataset from the 2003/2004 papers with 1,541 new ages to reflect work up to and 113 including 2018. A major revision is made to the 18 ka ice margin, where Banks and Eglinton 114 islands (once considered to be glacial refugia) are now shown to be fully glaciated. Our 115 updated 18 ka ice sheet increased in areal extent from 17.81 to 18.37 million km2, which is an 116 increase of 3.1% in spatial coverage of the NAISC at that time. Elsewhere, we also 117 summarize, region-by-region, significant changes to the deglaciation sequence. This paper 118 integrates new information provided by regional experts and radiocarbon data into the 119 deglaciation sequence while maintaining consistency with the original ice margin positions of 120 Dyke et al. (2003) and Dyke (2004) where new information is
Recommended publications
  • Lexicon of Pleistocene Stratigraphic Units of Wisconsin
    Lexicon of Pleistocene Stratigraphic Units of Wisconsin ON ATI RM FO K CREE MILLER 0 20 40 mi Douglas Member 0 50 km Lake ? Crab Member EDITORS C O Kent M. Syverson P P Florence Member E R Lee Clayton F Wildcat A Lake ? L L Member Nashville Member John W. Attig M S r ik be a F m n O r e R e TRADE RIVER M a M A T b David M. Mickelson e I O N FM k Pokegama m a e L r Creek Mbr M n e M b f a e f lv m m i Sy e l M Prairie b C e in Farm r r sk er e o emb lv P Member M i S ill S L rr L e A M Middle F Edgar ER M Inlet HOLY HILL V F Mbr RI Member FM Bakerville MARATHON Liberty Grove M Member FM F r Member e E b m E e PIERCE N M Two Rivers Member FM Keene U re PIERCE A o nm Hersey Member W le FM G Member E Branch River Member Kinnickinnic K H HOLY HILL Member r B Chilton e FM O Kirby Lake b IG Mbr Boundaries Member m L F e L M A Y Formation T s S F r M e H d l Member H a I o V r L i c Explanation o L n M Area of sediment deposited F e m during last part of Wisconsin O b er Glaciation, between about R 35,000 and 11,000 years M A Ozaukee before present.
    [Show full text]
  • Champlain Valley (Why Are Clay Soils Where They Are?)
    Geomorphic history of the Champlain Valley (why are clay soils where they are?) part 1) How did landscape evolve and where do “clay” minerals come from? part 2) How were they deposited in Lake Vermont/ Champlain Sea? part 3) Can we predict the distribution of “clay” thickness? (…can we compare prediction with what people observe) 500,000,000 years Today ~500,000,000 years: Sediments of “Champlain Valley Sequence” deposited on shoreline of ancient ocean Monkton quartzite + Taconic Slates Limestones + Marbles ~460,000,000 years: Collision of island arc causes thrusting + metamorphism Champlain Thrust Fault Champlain Thrust: -Exposed at Snake Mtn + Mt. Philo -delineates boundary between “low” and “mid” grade metamorphic rocks -Marbles pf middlebury syncline folded along back of thrust -Topography of Addison County reflects erodibility of bedrock: T1: lower surface: “low grade” sedimentary rocks below thrust (e.g. shale) T2: upper surface: “mid grade” meta-sedimentary rocks above thrust (e.g. marble) Green Mountains= “high grade” metamorphic rocks (e.g. schist and gneiss) T1 T2 Green Mtn gneiss Geologic map of Addison County Taconics Part 2: How were clays deposited in Lake Vermont and the Champlain Sea? 500,000,000 years Today ~96,000 - 20,000 years (i.e. yesterday…): Champlain Valley sat below 1-3 km of ice Soils and clay minerals from previous inter-glacial cycles were stripped by advancing glaciers Rocks were ground into “clay size fraction” and trapped under ice retreating glacial ice withdrew from Champlain Valley between ~14-13 kyr Many depositional features in Champlain Valley record ice retreat -Layers of “basal till” deposited beneath ice sheets (coarse, angular, poorly sorted debris) -Meltwater streams flow between glacier and hillslopes -Sedimentary deposits accumulate, leaving ‘kame terraces’ when glacier retreats Lake Vermont had 2+ stages: Coveville: Ice dammed in So.
    [Show full text]
  • Constraints on Lake Agassiz Discharge Through the Late-Glacial Champlain Sea (St
    Quaternary Science Reviews xxx (2011) 1e10 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Constraints on Lake Agassiz discharge through the late-glacial Champlain Sea (St. Lawrence Lowlands, Canada) using salinity proxies and an estuarine circulation model Brandon Katz a, Raymond G. Najjar a,*, Thomas Cronin b, John Rayburn c, Michael E. Mann a a Department of Meteorology, 503 Walker Building, The Pennsylvania State University, University Park, PA 16802, USA b United States Geological Survey, 926A National Center, 12201 Sunrise Valley Drive, Reston, VA 20192, USA c Department of Geological Sciences, State University of New York at New Paltz, 1 Hawk Drive, New Paltz, NY 12561, USA article info abstract Article history: During the last deglaciation, abrupt freshwater discharge events from proglacial lakes in North America, Received 30 January 2011 such as glacial Lake Agassiz, are believed to have drained into the North Atlantic Ocean, causing large Received in revised form shifts in climate by weakening the formation of North Atlantic Deep Water and decreasing ocean heat 25 July 2011 transport to high northern latitudes. These discharges were caused by changes in lake drainage outlets, Accepted 5 August 2011 but the duration, magnitude and routing of discharge events, factors which govern the climatic response Available online xxx to freshwater forcing, are poorly known. Abrupt discharges, called floods, are typically assumed to last months to a year, whereas more gradual discharges, called routing events, occur over centuries. Here we Keywords: Champlain sea use estuarine modeling to evaluate freshwater discharge from Lake Agassiz and other North American Proglacial lakes proglacial lakes into the North Atlantic Ocean through the St.
    [Show full text]
  • 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.
    [Show full text]
  • Correlation of Wisconsin Glacial Events Between the Eastern Great Lakes and the St
    Document generated on 09/25/2021 8:21 p.m. Géographie physique et Quaternaire Correlation of Wisconsin glacial events between the Eastern Great Lakes and the St. Lawrence Lowlands Corrélation entre les événements glaciaires wisconsiniens de l’est des Grands Lacs et des basses terres du Saint-Laurent A. Dreimanis Troisième Colloque sur le Quaternaire du Québec : 1re partie Article abstract Volume 31, Number 1-2, 1977 The interrelationship of the Wisconsin glaciogenic events among the Upper St. Lawrence Lowland and the eastern Great Lakes, particularly the Lake Ontario URI: https://id.erudit.org/iderudit/1000053ar basin is controlled mainly by 3 factors: 1) presence or absence of a glacial dam DOI: https://doi.org/10.7202/1000053ar across the St. Lawrence Lowland; 2) isostatic lowering or rise of the outlet of Lake Ontario, related mainly to glacial loading or unloading in the Upper St. See table of contents Lawrence Lowland; 3) shifting in the regional direction of glacial movement through the Upper St. Lawrence Lowland, upglacier from it, and in the Lake Ontario basin. Changes in the above conditions result in detectable changes in lake levels, and in compositional changes of tills in the Lake Ontario basin. Publisher(s) Crosschecking of the above relationships supports the relative sequence Les Presses de l’Université de Montréal already proposed. However, the chronology of the events which are older than reliable finite 14C dates, may be reinterpreted by a comparison with oceanic stratigraphies. A possible re-interpretation of some late-glacial Late Wisconsin ISSN glacial fluctuations depends greatly upon the reliability of 14C dates on shells 0705-7199 (print) and correct interpretation of till-like deposits.
    [Show full text]
  • Geologic Resources Inventory Map Document for Indiana Dunes National Lakeshore
    U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Indiana Dunes National Lakeshore GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Indiana Dunes National Lakeshore indu_geology.pdf Version: 3/4/2014 I Indiana Dunes National Lakeshore Geologic Resources Inventory Map Document for Indiana Dunes National Lakeshore Table of Contents Geologic R.e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About the N..P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 2 GRI Digital .M...a..p.. .a..n..d.. .S..o..u..r.c..e.. .M...a..p.. .C..i.t.a..t.i.o..n............................................................................... 4 Map Unit Li.s..t.......................................................................................................................... 5 Map Unit De..s..c..r.i.p..t.i.o..n..s............................................................................................................. 7 Qlmm - Fille..d.. .a..n..d.. .m..o..d..i.f.i.e..d../.d..i.s..t.u..r.b..e..d.. .l.a..n..d.. .(.H..o..l.o..c..e..n..e..).................................................................................................. 7 Qlma1 - Ch.a..n..n..e..l. .a..n..d.. .f.l.o..o..d..p..l.a..in.. .(..H..o..l.o..c..e..n..e..)................................................................................................................. 7 Qlma2 - Ch.a..n..n..e..l. .a..n..d.. .f.l.o..o..d..p..l.a..in.
    [Show full text]
  • Behavior of the James Lobe, South Dakota During Termination I
    Behavior of the James Lobe, South Dakota during Termination I A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY in the Department of Geology of the McMicken College of Arts and Sciences by Stephanie L. Heath MSc., University of Maine BSc., University of Maine July 18, 2019 Dissertation Committee: Dr. Thomas V. Lowell Dr. Aaron Diefendorf Dr. Aaron Putnam Dr. Dylan Ward i ABSTRACT The Laurentide Ice Sheet was the largest ice sheet of the last glacial period that terminated in an extensive terrestrial margin. This dissertation aims to assess the possible linkages between the behavior of the southern Laurentide margin and sea surface temperature in the adjacent North Atlantic Ocean. Toward this end, a new chronology for the westernmost lobe of the Southern Laurentide is developed and compared to the existing paradigm of southern Laurentide behavior during the last glacial period. Heath et al., (2018) address the question of whether the terrestrial lobes of the southern Laurentide Ice Sheet margin advanced during periods of decreased sea surface temperature in the North Atlantic. This study establishes the pattern of asynchronous behavior between eastern and western sectors of the southern Laurentide margin and identifies a chronologic gap in the western sector. This is the first comprehensive review of the southern Laurentide margin since Denton and Hughes (1981) and Mickelson and Colgan (2003). The results of Heath et al., (2018) also revealed the lack of chronologic data from the Lobe, South Dakota, the westernmost lobe of the southern Laurentide margin.
    [Show full text]
  • Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 8-1977 Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan Norman A. Lovan Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Lovan, Norman A., "Analysis of an Interlobate Boundary in the Wisconsinan Drift of Kalamazoo County and Adjacent Areas in Southwestern Michigan" (1977). Master's Theses. 2207. https://scholarworks.wmich.edu/masters_theses/2207 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. ANALYSIS OF AN INTERLOBATE BOUNDARY IN THE WISCONSINAN DRIFT OF KALAMAZOO COUNTY AND ADJACENT AREAS IN SOUTHWESTERN MICHIGAN by Norman A. Lovan A Thesis Submitted to the Faculty of The Graduate College in partial fulfillment of the Degree of Master of Science Western Michigan University Kalamazoo, Michigan August 19 77 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ANALYSIS OF AN INTERLOBATE BOUNDARY IN THE WISCONSINAN DRIFT OF KALAMAZOO COUNTY AND ADJACENT AREAS IN SOUTHWESTERN MICHIGAN Norman A. Lovan, M.S. Western Michigan University, 1977 ABSTRACT A detailed investigation of selected textural and mineralogical aspects of tills in southwestern Michigan is used to define an interlobate boundary relationship be­ tween the Wisconsinan ice of the Lake Michigan and Saginaw lobes. Bedrock underlying the study area contributed lit­ tle to the bulk composition of the tills investigated.
    [Show full text]
  • New York State Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020
    Link to NYGS Publications New York State Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020 2018 Bird, B. C., Kehew, A. E., and Kozlowski, A. L., 2018, Glaciotectonic deformation along the Valparaiso Upland in southwest Michigan, in Kehew, A. E., and Curry, B. B., eds., Quaternary glaciation of the Great Lakes region–process, landforms, sediments, and chronology: Geological Society of America Special Paper 530, p. 139–161, doi: 10.1130/2018.2530(07). Feranec, R. S., and Kozlowski, A. L., 2018, Onset age of deglaciation following the Last Glacial Maximum in New York State based on radiocarbon ages of mammalian megafauna, in Kehew, A. E., and Curry, B. B., eds., Quaternary glaciation of the Great Lakes region–process, landforms, sediments, and chronology: Geological Society of America Special Paper 530, p. 179–189, doi: 10.1130/2017.2530(09). Kozlowski, A. L., Bird, B. C., Lowell, T. V., Smith, C. A., Feranec, R. S., and Graham, B. L., 2018, Minimum age of the Mapleton, Tully, and Labrador Hollow Moraines indicates correlation with the Port Huron Phase in central New York State, in Kehew, A. E., and Curry, B. B., eds., Quaternary glaciation of the Great Lakes region–process, landforms, sediments, and chronology: Geological Society of America Special Paper 530, p. 191–216, doi: 10.1130/2018.2530(10). Kozlowski, A. L., Bird, Brian, Mahan, S. A., Feranec, R. S., and Leone, James, 2018, Glacial geologic mapping in Cayuga County, New York–footprint to framework, in Thorleifson, L. H., ed., Geologic Mapping Forum 2018 abstracts: Minnesota Geological Survey Open-File Report 18-1, p.
    [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]
  • Trip I DEGLACIAL HISTORY of the LAKE CHAMPLAIN-LAKE GEORGE
    163 . Trip I DEGLACIAL HISTORY OF THE LAKE CHAMPLAIN-LAKE GEORGE LOWLAND by G. Gordon Connally Lafayette College Easton, Pennsylvania and Leslie A. Sirkin Adelphi University Garden City, New York GENERAL GEOMORPHOLOGY The Lake Champlain and Lake George Valleys are two separate physiographic units, situated in separate physiographic provinces (see Broughton, et al., 1966). The Champlain Valley lies in the St. Lawrence-Champlain Lowlands while the Lake George trough lies in the Adirondack Highlands. It is the continuous nature of the deglacial history of the two regions that links them together for this field trip. Indeed, the deglacial history of the regions begins at the north end of the Hudson-Mohawk Lowlands near Glens Falls, New York. Physiography The Champlain Valley lies between the Adirondack Mountains of New York on the west and the Green Mountains of Vermont on the east. Lake Champlain occupies most of the valley bottom and has a surface elevation of about 95 feet. The Great Chazy, Saranac, Ausable, and Bouquet Rivers enter the valley from the Adirondacks while the Mississquoi, Lamoille, and Winooski Rivers and Otter Creek enter from the Green Mountains. Figure 1 shows the general physiography and the field trip stops. According to Newland and Vaughan (1942) Lake George occupies a graben in the eastern Adirondacks. The'surface of Lake George is about 320 feet above sea level and it drains into Lake Cham­ plain via Ticonderoga Creek at its northern end. In general, Lake George marks the divide between southerly flowing Hudson River drainage and northerly flowing St. Lawrence River drainage. 164 Great Chazy Lamoille R.
    [Show full text]
  • Proceedings of the Indiana Academy Of
    The Tinley Moraine in Indiana 1 Allan F. Schneider, Indiana Geological Survey Abstract The Tinley Moraine, which was named in Illinois for a subsidiary ridge behind the main part of the Valparaiso Morainic System, has received little recognition as a discrete moraine in Indiana. Recent mapping sug- gests, however, that ice of the Lake Michigan Lobe probably did recede some unknown distance from its position along the Valparaiso Moraine and then readvanced to form the Tinley Moraine. The Tinley Moraine enters Indiana in west-central Lake County, and its main ridge can be traced for about 20 miles across Lake County and western Porter County. It is more readily recognized as a discrete moraine by ice-block depressions and drainage relations along its distal margin than by its height or good internal morphology. The crest of the Tinley ridge gradually decreases in elevation from 736 feet at the state line to about 700 feet at the eastern end of the segment, where the moraine be- comes obscure near a prominent gap in the Valparaiso Moraine. Here the terminal zone of the Tinley ice apparently curved northward through an arc of about 90 degrees and is represented by an upland till plain that was probably deposited with the ice front standing in a lake. Farther north- east the terminal zone of the ice possibly is marked by an undulating till belt that trends eastward through northeastern Porter County and northeastward through northwestern LaPorte County. This belt has long been considered to be part of the Lake Border Morainic System, which is, however, presumably younger than the Tinley Moraine.
    [Show full text]