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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. -
Ecological Regions of Minnesota: Level III and IV Maps and Descriptions Denis White March 2020
Ecological Regions of Minnesota: Level III and IV maps and descriptions Denis White March 2020 (Image NOAA, Landsat, Copernicus; Presentation Google Earth) A contribution to the corpus of materials created by James Omernik and colleagues on the Ecological Regions of the United States, North America, and South America The page size for this document is 9 inches horizontal by 12 inches vertical. Table of Contents Content Page 1. Introduction 1 2. Geographic patterns in Minnesota 1 Geographic location and notable features 1 Climate 1 Elevation and topographic form, and physiography 2 Geology 2 Soils 3 Presettlement vegetation 3 Land use and land cover 4 Lakes, rivers, and watersheds; water quality 4 Flora and fauna 4 3. Methods of geographic regionalization 5 4. Development of Level IV ecoregions 6 5. Descriptions of Level III and Level IV ecoregions 7 46. Northern Glaciated Plains 8 46e. Tewaukon/BigStone Stagnation Moraine 8 46k. Prairie Coteau 8 46l. Prairie Coteau Escarpment 8 46m. Big Sioux Basin 8 46o. Minnesota River Prairie 9 47. Western Corn Belt Plains 9 47a. Loess Prairies 9 47b. Des Moines Lobe 9 47c. Eastern Iowa and Minnesota Drift Plains 9 47g. Lower St. Croix and Vermillion Valleys 10 48. Lake Agassiz Plain 10 48a. Glacial Lake Agassiz Basin 10 48b. Beach Ridges and Sand Deltas 10 48d. Lake Agassiz Plains 10 49. Northern Minnesota Wetlands 11 49a. Peatlands 11 49b. Forested Lake Plains 11 50. Northern Lakes and Forests 11 50a. Lake Superior Clay Plain 12 50b. Minnesota/Wisconsin Upland Till Plain 12 50m. Mesabi Range 12 50n. Boundary Lakes and Hills 12 50o. -
Case Fil Copy
NASA TECHNICAL NASA TM X-3511 MEMORANDUM CO >< CASE FIL COPY REPORTS OF PLANETARY GEOLOGY PROGRAM, 1976-1977 Compiled by Raymond Arvidson and Russell Wahmann Office of Space Science NASA Headquarters NATIONAL AERONAUTICS AND SPACE ADMINISTRATION • WASHINGTON, D. C. • MAY 1977 1. Report No. 2. Government Accession No. 3. Recipient's Catalog No. TMX3511 4. Title and Subtitle 5. Report Date May 1977 6. Performing Organization Code REPORTS OF PLANETARY GEOLOGY PROGRAM, 1976-1977 SL 7. Author(s) 8. Performing Organization Report No. Compiled by Raymond Arvidson and Russell Wahmann 10. Work Unit No. 9. Performing Organization Name and Address Office of Space Science 11. Contract or Grant No. Lunar and Planetary Programs Planetary Geology Program 13. Type of Report and Period Covered 12. Sponsoring Agency Name and Address Technical Memorandum National Aeronautics and Space Administration 14. Sponsoring Agency Code Washington, D.C. 20546 15. Supplementary Notes 16. Abstract A compilation of abstracts of reports which summarizes work conducted by Principal Investigators. Full reports of these abstracts were presented to the annual meeting of Planetary Geology Principal Investigators and their associates at Washington University, St. Louis, Missouri, May 23-26, 1977. 17. Key Words (Suggested by Author(s)) 18. Distribution Statement Planetary geology Solar system evolution Unclassified—Unlimited Planetary geological mapping Instrument development 19. Security Qassif. (of this report) 20. Security Classif. (of this page) 21. No. of Pages 22. Price* Unclassified Unclassified 294 $9.25 * For sale by the National Technical Information Service, Springfield, Virginia 22161 FOREWORD This is a compilation of abstracts of reports from Principal Investigators of NASA's Office of Space Science, Division of Lunar and Planetary Programs Planetary Geology Program. -
Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES
UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman ,Wilbur, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director P~ofessional Paper 161 . QUArrERNARY GEOLOGY OF MINNESOTA AND PARTS OF ADJACENT STATES BY FRANK LEVERETT WITH CONTRIBUTIONS BY FREDERICK w. SARDE;30N Investigations made in cooperation with the MINNESOTA GEOLOGICAL SURVEY UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1932 ·For sale by the Superintendent of Documents, Washington, D. C. CONTENTS Page Page Abstract ________________________________________ _ 1 Wisconsin red drift-Continued. Introduction _____________________________________ _ 1 Weak moraines, etc.-Continued. Scope of field work ____________________________ _ 1 Beroun moraine _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 47 Earlier reports ________________________________ _ .2 Location__________ _ __ ____ _ _ __ ___ ______ 47 Glacial gathering grounds and ice lobes _________ _ 3 Topography___________________________ 47 Outline of the Pleistocene series of glacial deposits_ 3 Constitution of the drift in relation to rock The oldest or Nebraskan drift ______________ _ 5 outcrops____________________________ 48 Aftonian soil and Nebraskan gumbotiL ______ _ 5 Striae _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 48 Kansan drift _____________________________ _ 5 Ground moraine inside of Beroun moraine_ 48 Yarmouth beds and Kansan gumbotiL ______ _ 5 Mille Lacs morainic system_____________________ 48 Pre-Illinoian loess (Loveland loess) __________ _ 6 Location__________________________________ -
Minnesota Ground Water Bibliography
First Edition: May 1989 Second Edition: June 1990 MINNESOTA GROUND WATER BIBLIOGRAPHY By Dave Armstrong Revised by Toby McAdams First Edition: May 1989 Second Edition: June 1990 Original paper document scanned and converted to electronic format: 2004. MINNESOTA DEPARTMENT OF NATURAL RESOURCES Division of Waters St. Paul, MN ii Acknowledgements Many thanks for their willing help to Colleen Mlecoch and Char Feist, DNR librarians, and to the clerical and other library staff who assisted in the search for publications, to the Division of Waters groundwater unit staff members Jeanette Leete, Jay Frischman, Andrew Streitz, and Eric Mohring for their suggestions and patience and to Pat Bloomgren for review. Special thanks to Tami Brue, Chris Weller, and Penny Wheeler for scanning, typing, editing and word processing. iii iv PREFACE The primary objectives for this Bibliography were to provide both a localized reference to Ground Water Resource Publications, and a reference to the organizations, agencies and individuals in Minnesota who are currently publishing information on and related to ground water. The Bibliography is divided into two sections. Chapter I lists the publications of the United States Geological Survey (USGS) and the Minnesota Geological Survey (MGS). Publications which deal with a specific area are listed by area within the six DNR regions of Minnesota. These are followed by the listing of USGS and MGS publications of a general nature which deal with all of Minnesota. Chapter II contains publications from many organizations, individuals and journals. It is divided loosely into subject categories, and an index is provided at the end of the document to help locate additional subjects. -
Geologic Map of the Victoria Quadrangle (H02), Mercury
H01 - Borealis Geologic Map of the Victoria Quadrangle (H02), Mercury 60° Geologic Units Borea 65° Smooth plains material 1 1 2 3 4 1,5 sp H05 - Hokusai H04 - Raditladi H03 - Shakespeare H02 - Victoria Smooth and sparsely cratered planar surfaces confined to pools found within crater materials. Galluzzi V. , Guzzetta L. , Ferranti L. , Di Achille G. , Rothery D. A. , Palumbo P. 30° Apollonia Liguria Caduceata Aurora Smooth plains material–northern spn Smooth and sparsely cratered planar surfaces confined to the high-northern latitudes. 1 INAF, Istituto di Astrofisica e Planetologia Spaziali, Rome, Italy; 22.5° Intermediate plains material 2 H10 - Derain H09 - Eminescu H08 - Tolstoj H07 - Beethoven H06 - Kuiper imp DiSTAR, Università degli Studi di Napoli "Federico II", Naples, Italy; 0° Pieria Solitudo Criophori Phoethontas Solitudo Lycaonis Tricrena Smooth undulating to planar surfaces, more densely cratered than the smooth plains. 3 INAF, Osservatorio Astronomico di Teramo, Teramo, Italy; -22.5° Intercrater plains material 4 72° 144° 216° 288° icp 2 Department of Physical Sciences, The Open University, Milton Keynes, UK; ° Rough or gently rolling, densely cratered surfaces, encompassing also distal crater materials. 70 60 H14 - Debussy H13 - Neruda H12 - Michelangelo H11 - Discovery ° 5 3 270° 300° 330° 0° 30° spn Dipartimento di Scienze e Tecnologie, Università degli Studi di Napoli "Parthenope", Naples, Italy. Cyllene Solitudo Persephones Solitudo Promethei Solitudo Hermae -30° Trismegisti -65° 90° 270° Crater Materials icp H15 - Bach Australia Crater material–well preserved cfs -60° c3 180° Fresh craters with a sharp rim, textured ejecta blanket and pristine or sparsely cratered floor. 2 1:3,000,000 ° c2 80° 350 Crater material–degraded c2 spn M c3 Degraded craters with a subdued rim and a moderately cratered smooth to hummocky floor. -
Updates on Geologic Mapping of Kuiper (H06) Quadrangle
EPSC Abstracts Vol. 12, EPSC2018-721-1, 2018 European Planetary Science Congress 2018 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2018 Updates on geologic mapping of Kuiper (H06) quadrangle Lorenza Giacomini (1), Valentina Galluzzi (1), Cristian Carli (1), Matteo Massironi (2), Luigi Ferranti (3) and Pasquale Palumbo (4,1). (1) INAF, Istituto di Astrofisica e Planetologia Spaziali (IAPS), Rome, Italy ([email protected]); (2) Dipartimento di Geoscienze, Università degli Studi di Padova, Padua, Italy; (3) DISTAR, Università degli Studi di Napoli Federico II, Naples, Italy; (4) Dipartimento di Scienze & Tecnologie, Università degli Studi di Napoli ‘Parthenope’, Naples, Italy. 1. Introduction -C3 craters. They represent fresh craters with sharp rim and extended bright and rayed ejecta; Kuiper quadrangle is located at the equatorial zone of -C2 craters. Moderate degraded craters whose rim is Mercury and encompasses the area between eroded but clearly detectable. Extensive ejecta longitudes 288°E – 360°E and latitudes 22.5°N – blankets are still present; 22.5°S. The quadrangle was previously mapped for -C1 craters. Very degraded craters with an almost its most part by [2] that, using Mariner10 data, completely obliterated rim. Ejecta are very limited or produced a final 1:5M scale map of the area. In this absent. work we present the preliminary results of a more Different plain units were also identified and classified as: detailed geological map (1:3M scale) of the Kuiper - Intercrater plains. Densely cratered terrains, quadrangle that we compiled using the higher characterized by a rough surface texture. They resolution MESSENGER data. represent the more extended plains on the quadrangle; - Intermediate plains. -
SIMBIO-SYS: Scientific Cameras and Spectrometer for the Bepicolombo
Space Sci Rev (2020) 216:75 https://doi.org/10.1007/s11214-020-00704-8 SIMBIO-SYS: Scientific Cameras and Spectrometer for the BepiColombo Mission G. Cremonese1 · F. Capaccioni2 · M.T. Capria2 · A. Doressoundiram3 · P. Palumbo4 · M. Vincendon5 · M. Massironi6 · S. Debei7 · M. Zusi2 · F. Altieri2 · M. Amoroso8 · G. Aroldi9 · M. Baroni9 · A. Barucci3 · G. Bellucci2 · J. Benkhoff10 · S. Besse11 · C. Bettanini7 · M. Blecka12 · D. Borrelli9 · J.R. Brucato13 · C. Carli2 · V. Carlier5 · P. Cerroni2 · A. Cicchetti2 · L. Colangeli10 · M. Dami9 · V. Da Deppo14 · V. Della Corte2 · M.C. De Sanctis2 · S. Erard3 · F. Esposito 15 · D. Fantinel1 · L. Ferranti16 · F. Ferri7 · I. Ficai Veltroni9 · G. Filacchione2 · E. Flamini17 · G. Forlani18 · S. Fornasier3 · O. Forni19 · M. Fulchignoni20 · V. Galluzzi2 · K. Gwinner21 · W. Ip 22 · L. Jorda23 · Y. Langevin 5 · L. Lara24 · F. Leblanc 25 · C. Leyrat3 · Y. Li 26 · S. Marchi27 · L. Marinangeli28 · F. Marzari29 · E. Mazzotta Epifani30 · M. Mendillo31 · V. Mennella15 · R. Mugnuolo32 · K. Muinonen33,34 · G. Naletto29 · R. Noschese2 · E. Palomba2 · R. Paolinetti9 · D. Perna30 · G. Piccioni2 · R. Politi2 · F. Poulet 5 · R. Ragazzoni1 · C. Re1 · M. Rossi9 · A. Rotundi35 · G. Salemi36 · M. Sgavetti37 · E. Simioni1 · N. Thomas38 · L. Tommasi9 · A. Turella9 · T. Van Hoolst39 · L. Wilson40 · F. Zambon 2 · A. Aboudan7 · O. Barraud3 · N. Bott3 · P. Borin 1 · G. Colombatti7 · M. El Yazidi7 · S. Ferrari7 · J. Flahaut41 · L. Giacomini2 · L. Guzzetta2 · A. Lucchetti1 · E. Martellato4 · M. Pajola1 · A. Slemer14 · G. Tognon7 · D. Turrini2 Received: 12 December 2019 / Accepted: 6 June 2020 / Published online: 17 June 2020 © The Author(s) 2020 Abstract The SIMBIO-SYS (Spectrometer and Imaging for MPO BepiColombo Integrated Observatory SYStem) is a complex instrument suite part of the scientific payload of the Mer- cury Planetary Orbiter for the BepiColombo mission, the last of the cornerstone missions of the European Space Agency (ESA) Horizon + science program. -
Geologic History of Minnesota Rivers
GEOLOGIC HISTORY OF MINNESOTA RIVERS Minnesota Geological Survey Ed ucational Series - 7 Minnesota Geological Survey Priscilla C. Grew, Director Educational Series 7 GEOLOGIC HISTORY OF MINNESOTA RIVERS by H.E. Wright, Jr. Regents' Professor of Geology, Ecology, and Botany (Emeritus), University of Minnesota 'r J: \ I' , U " 1. L I!"> t) J' T II I ~ !oo J', t ' I' " I \ . University of Minnesota St. Paul, 1990 Cover: An early ponrayal of St. Anthony Falls on the Mississippi River In Minneapolis. The engraving of a drawing by Captain E. Eastman of Fan Snelling was first published In 1853; It Is here reproduced from the Second Final Report of the Geological and Natural History Survey of Minnesota, 1888. Several other early views of Minnesota rivers reproduced In this volume are from David Dale Owen's Report of a Geological Survey of Wisconsin, Iowa, and Minnesota; and Incidentally of a portion of Nebraska Territory, which was published In 1852 by Lippincott, Grambo & Company of Philadelphia. ISSN 0544-3083 1 The University of Minnesota is committed to the policy that all persons shall have equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age, veteran status, or sexual orientation. 1-' \ J. I,."l n 1 ~ r 1'11.1: I: I \ 1"" CONTENTS 1 .... INTRODUCTION 1. PREGLACIAL RIVERS 5 .... GLACIAL RIVERS 17 ... POSTGLACIAL RIVERS 19 . RIVER HISTORY AND FUTURE 20 . ... REFERENCES CITED iii GEOLOGIC HISTORY OF MINNESOTA RIVERS H.E. Wright, Jr. A GLANCE at a glacial map of the Great Lakes region (Fig. 1) reveals that all of Minnesota was glaciated at some time, and all but the southeastern and southwestern corners were covered by the last ice sheet, which culminated about 20,000 years ago. -
Hydrogeology of the Buffalo Aquifer, Clay and Wilkin Counties, West-Central Minnesota
HYDROGEOLOGY OF THE BUFFALO AQUIFER, CLAY AND WILKIN COUNTIES, WEST-CENTRAL MINNESOTA U. S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS 81-4 PREPARED IN COOPERATION WITH THE MINNESOTA DEPARTMENT OF NATURAL RESOURCES CLAY AND WILKIN COUNTIES CITIES OF MOORHEAD AND SABIN (200) WRi no. 81-4 50272-101_______________ REPORT DOCUMENTATION 1. REPORT NO. 3. Recipient's Accession No. PAGE 4. Title and Subtitle 5. Report Date HYDROGEOLOGY OF THE BUFFALO AQUIFER, CLAY AND February 1981 WILKIN COUNTIES, WEST-CENTRAL MINNESOTA 6. 7. Author(s) 8. Performing Organization Rept. No. Ronald J. Wolf 9. Performing Organization Name and Address 10. Project/Task/Work Unit No. U.S. Geological Survey Water Resources Division 11. Contract(C) or Grant(G) No. 702 Post Office Building (0 St. Paul, Minnesota 55101 (G) 12. Sponsoring Organization Name and Address 13. Type of Report & Period Covered U.S. Geological Survey Water Resources Division 702 Post Office Building 14. St. Paul, Minnesota 55101 __ ___ 15. Supplementary Notes Prepared in cooperation with the Minnesota Department of Natural Resources, Clay and Wilkin Counties, and the cities of Moorhead and Sabin 16. Abstract (Limit: 200 words) The Buffalo aquifer is the principal source of ground-water supplies in the Moorhead, Minnesota area. The aquifer is an elongate, narrow deposit of sand and gravel, which locally contains water under confined conditions. Although the Buffalo aquifer contains about 270 billion gallons of water in storage, only 120 billion gal lons could be withdrawn. Largest well yields occur along the deep trough in the center of the aquifer. Induced streambed infiltration may be possible in certain areas where the stream overlies the aquifer and where the intervening lake sediments are thin or absent. -
The Late Cenozoic Geology of West-Central Minnesota From
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 1977 The al te Cenozoic geology of west-central Minnesota from Moorhead to Park Rapids Roderic L. Perkins University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Perkins, Roderic L., "The al te Cenozoic geology of west-central Minnesota from Moorhead to Park Rapids" (1977). Theses and Dissertations. 225. https://commons.und.edu/theses/225 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. THE LATE CENOZOIC GEOLOGY OF WEST-CENTRAL MINNESOTA FROM MOORHEAD TO PARK RAPIDS . by Roderic L. Perkins Bachelor of Arts> State University of New York College. 1974 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degrea of Master of Arts GEOLOGY LIBRARY Grand Forks, North Dakota Universtty of North Dakota August 1977 " '' ' \ Thin thesis submitted by Roderic L. Perkins in partial fulfill ment of the requirements for the Degree of Master of Arts from the University of North Dakota is hereby approv~d by the Faculty Advisory Committee under whom the work has been done. ~l7.~Dean of the Graduate School ii Permission # THE LATE CENOZOIC GEOLOGY OF WEST-CENTRAL Title MINNESOTA FROM MOORHEAD TO PARK RAPIDS Department Geology Degree Master of Arts In presenting this thesis in partial fulfillment of the requirements for a graduate degree from the University of North Dakota, I agree that the Library of this University shall make it freely available for inspection. -
Relationship of Structural Geology of the Duluth Complex to Economic Mineralization
MINNESOTA DEPARTMENT OF NATURAL RESOURCES Division of Minerals Report 241-2 RELATIONSHIP OF STRUCTURAL GEOLOGY OF THE DULUTH COMPLEX TO ECONOMIC MINERALIZATION A Final Report to the Minnesota Department of Natural Resources and the Natural Resources Research Institute of the University of Minnesota Duluth by Timothy B. Holst, Eugene E. Mullenmeister, Val W. Chandler, John C. Green, and Paul w. Weiblen Funded by The Legislative Commission on Minnesota Resources The Natural Resources Research Institute TABLE OF CONTENTS I. Introduction I-1 II. Structural Analysis of the Northeast Mesabi Range II-1 III. Structural Analysis of the Dunka River Area III-1 IV. The Form of the Base of the Duluth Complex IV-1 v. Field Mapping V-1 VI. Geophysical Studies VI-1 VII. Discussion, Interpretation, Conclusions VII-1 VIII. Further Work VIII-1 References R-1 Maps: ~)Ire·,:,,,( Plate I: ~Geology of the Northeast Mesabi Range Plate II: Structure Contour Map on the Upper Contact of the Lower Slatey Member of the Biwabik Iron Formation in the Dunka Pit Area Plate III: Structure Contour Map of the Base of the Duluth Complex in the Minnamax Area Plate IV: Structure Contour Map on the Base of the Duluth Complex From the Dunka River Area to Hoyt Lakes Plate V: Structure Contour Map on the Base of the Duluth Complex in the Dunka River Area Plate VI: Structural Geology of the Dunka River Area Cross Sections: A: Minnamax Project Area B: Minnamax Project Area C: Minnamax Project Area D: Dunka River Area INTRODUCTION A series of mafic igneous rocks (both intrusive and extrusive), known from outcrop or inferred from geophysical data, forms an arc that runs from Kansas, through Iowa and Minnesota, through Lake Superior, and south through Michigan, perhaps into Ohio.