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Natural Ground-Water Quality in Michigan, 1974-87
NATURAL GROUND-WATER QUALITY IN MICHIGAN, 1974-87 By T. Ray Cumnings U.S. GEOLOGICAL SURVEY Open-File Report 89-259 Prepared in cooperation with the MICHIGAN DEPARTMENT OF NATURAL RESOURCES GEOLOGICAL SURVEY DIVISION Lansing, Michigan July 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can write to: be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Section 6520 Mercantile Way, Suite 5 Federal Center, Building 810 Lansing, Michigan 48911 Box 25425 Denver, Colorado 80225 CONTENTS Page Abstract l Introduction 1 Purpose and scope 2 Methods of investigation 2 General water-quality conditions 3 Areal variations in water quality 12 Relation of water quality to geologic source 17 Relation of water quality to mineral associations 25 Conclusions 28 Selected references 30 Definition of terms 32 Appendix: Median values of chemical and physical characteristics of water from geologic sources 33 ill ILLUSTRATIONS Page Figure 1. Relation of dissolved-solids concentration to chemical characteristics of water 6 2. Relation of specific conductance to dissolved-solids concentration of water 7 3. Areal variation of dissolved solids in water 13 4. Areal variation of ammonia and hardness of water 14 5. Areal variation of total recoverable lead and total recoverable mercury in water- 15 6. Areal variation of total recoverable iron and total recoverable copper in water 16 7. Relation of depth of well to dissolved-solids concentration 18 8. Chemical characteristics of water from glacial deposit s 20 9. -
Table of Contents Figures
GEOLOGICAL SURVEY DIVISION STATE OF MICHIGAN BULLETIN #7 James J. Blanchard, Governor DEPARTMENT OF NATURAL RESOURCES SUBSURFACE STRATIGRAPHY OF CAMBRIAN David F. Hales, Director ROCKS IN THE SOUTHERN PENINSULA OF NATURAL RESOURCES COMMISSION MICHIGAN: MICHIGAN BASIN Raymond Poupore, Chairman by Thomas J. Anderson Marlene J. Fluharty RANDALL L MILSTEIN Gordon E. Guyer MICHIGAN DEPARTMENT OF NATURAL Kerry Kammer RESOURCES Ellwood A. Mattson O. Stewart Myers GEOLOGICAL SURVEY DIVISION R. Thomas Segall State Geologist and Chief Edited by Tyrone J. Black LANSING, MICHIGAN 1989 Published by authority of State of Michigan CL '48 s.321.6. Available from Information Services Center, Michigan Department of Natural Resources, P. O. Box 30028, Lansing, Michigan 48909. On deposit in public libraries, state libraries, and university libraries in Michigan and other selected localities. TABLE OF CONTENTS Introduction ........................................................................2 Previous Work....................................................................2 Stratigraphy........................................................................4 Lake Superior Group......................................................5 Mt. Simon Sandstone .............................................. 5 Munising Formation........................................................5 Eau Claire Member.................................................. 5 Dresbach (Galesville) Member................................ 5 Franconia Member ................................................. -
Summary of Hydrogelogic Conditions by County for the State of Michigan. Apple, B.A., and H.W. Reeves 2007. U.S. Geological Surve
In cooperation with the State of Michigan, Department of Environmental Quality Summary of Hydrogeologic Conditions by County for the State of Michigan Open-File Report 2007-1236 U.S. Department of the Interior U.S. Geological Survey Summary of Hydrogeologic Conditions by County for the State of Michigan By Beth A. Apple and Howard W. Reeves In cooperation with the State of Michigan, Department of Environmental Quality Open-File Report 2007-1236 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation Beth, A. Apple and Howard W. Reeves, 2007, Summary of Hydrogeologic Conditions by County for the State of Michi- gan. U.S. Geological Survey Open-File Report 2007-1236, 78 p. Cover photographs Clockwise from upper left: Photograph of Pretty Lake by Gary Huffman. Photograph of a river in winter by Dan Wydra. Photographs of Lake Michigan and the Looking Glass River by Sharon Baltusis. iii Contents Abstract ...........................................................................................................................................................1 -
Paleozoic Stratigraphic Nomenclature for Wisconsin (Wisconsin
UNIVERSITY EXTENSION The University of Wisconsin Geological and Natural History Survey Information Circular Number 8 Paleozoic Stratigraphic Nomenclature For Wisconsin By Meredith E. Ostrom"'" INTRODUCTION The Paleozoic stratigraphic nomenclature shown in the Oronto a Precambrian age and selected the basal contact column is a part of a broad program of the Wisconsin at the top of the uppermost volcanic bed. It is now known Geological and Natural History Survey to re-examine the that the Oronto is unconformable with older rocks in some Paleozoic rocks of Wisconsin and is a response to the needs areas as for example at Fond du Lac, Minnesota, where of geologists, hydrologists and the mineral industry. The the Outer Conglomerate and Nonesuch Shale are missing column was preceded by studies of pre-Cincinnatian cyclical and the younger Freda Sandstone rests on the Thompson sedimentation in the upper Mississippi valley area (Ostrom, Slate (Raasch, 1950; Goldich et ai, 1961). An unconformity 1964), Cambro-Ordovician stratigraphy of southwestern at the upper contact in the Upper Peninsula of Michigan Wisconsin (Ostrom, 1965) and Cambrian stratigraphy in has been postulated by Hamblin (1961) and in northwestern western Wisconsin (Ostrom, 1966). Wisconsin wlle're Atwater and Clement (1935) describe un A major problem of correlation is the tracing of outcrop conformities between flat-lying quartz sandstone (either formations into the subsurface. Outcrop definitions of Mt. Simon, Bayfield, or Hinckley) and older westward formations based chiefly on paleontology can rarely, if dipping Keweenawan volcanics and arkosic sandstone. ever, be extended into the subsurface of Wisconsin because From the above data it would appear that arkosic fossils are usually scarce or absent and their fragments cari rocks of the Oronto Group are unconformable with both seldom be recognized in drill cuttings. -
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. -
An Inventory of Trilobites from National Park Service Areas
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna. -
Geoscientific Review of the Sedimentary Sequence in Southern Ontario
July 2004 NWMO BACKGROUND PAPERS 6. TECHNICAL METHODS 6-12 LONG-TERM USED NUCLEAR FUEL WASTE MANAGEMENT - GEOSCIENTIFIC REVIEW OF THE SEDIMENTARY SEQUENCE IN SOUTHERN ONTARIO Martin Mazurek Rock-Water Interaction, Institute of Geological Sciences, University of Bern, Switzerland NWMO Background Papers NWMO has commissioned a series of background papers which present concepts and contextual information about the state of our knowledge on important topics related to the management of radioactive waste. The intent of these background papers is to provide input to defining possible approaches for the long-term management of used nuclear fuel and to contribute to an informed dialogue with the public and other stakeholders. The papers currently available are posted on NWMO’s web site. Additional papers may be commissioned. The topics of the background papers can be classified under the following broad headings: 1. Guiding Concepts – describe key concepts which can help guide an informed dialogue with the public and other stakeholders on the topic of radioactive waste management. They include perspectives on risk, security, the precautionary approach, adaptive management, traditional knowledge and sustainable development. 2. Social and Ethical Dimensions - provide perspectives on the social and ethical dimensions of radioactive waste management. They include background papers prepared for roundtable discussions. 3. Health and Safety – provide information on the status of relevant research, technologies, standards and procedures to reduce radiation and security risk associated with radioactive waste management. 4. Science and Environment – provide information on the current status of relevant research on ecosystem processes and environmental management issues. They include descriptions of the current efforts, as well as the status of research into our understanding of the biosphere and geosphere. -
Bedrock Maps
1987 BEDROCK GEOLOGY OF MICHIGAN BEDROCK GEOLOGY OF EASTERN UPPER PENINSULA MACKINAC BRECCIA BOIS BLANC FORMATION GARDEN ISLAND FORMATION BASS ISLAND GROUP SALINA GROUP SAINT IGNACE DOLOMITE POINT AUX CHENES SHALE ENGADINE GROUP MANISTIQUE GROUP BURNT BLUFF GROUP KEWEENAW CABOT HEAD SHALE MANITOULIN DOLOMITE QUEENSTON SHALE BIG HILL DOLOMITE HOUGHTON STONINGTON FORMATION UTICA SHALE MEMBER COLLINGWOOD SHALE MEMBER TRENTON GROUP BLACK RIVER GROUP ONTONAGON BARAGA PRAIRIE DU CHIEN GROUP TREMPEALEAU FORMATION MUNISING FORMATION GOGEBIC LU CE MARQUETTE ALGER CHIPPEWA IRON MACKINAC SCHOOLC RAF T DELT A DICKIN SON BEDROCK GEOLOGY OF WESTERN UPPER PENINSULA MACKINAC BRECCIA JACOBSVILLE SANDSTONE EMMET MENOMINEE FREDA SANDSTONE CHEBOYGAN NONESUCH FORMATION PRESQUE ISLE COPPER HARBOR CONGLOMERATE OAK BLUFF FORMATION CHAR LEVOIX PORTAGE LAKE VOLCANICS MONTMORENCY SIEMENS CREEK FORMATION ANT RIM ALPENA INTRUSIVE OTSEGO QUINNESEC FORMATION LEELANAU PAINT RIVER GROUP RIVERTON IRON FORMATION BIJIKI IRON FORMATION GRAND TR AVERSE ALCONA KALKASKA CRAW FOR D OSCOD A NEGAUNEE IRON FORMATION BENZIE IRONWOOD IRON FORMATION DUNN CREEK FORMATION BADWATER GREENSTONE MICHIGAMME FORMATION MANISTEE WEXFORD MISSAUKEE ROSCOMMON OGEMAW IOSCO GOODRICH QUARTZITE HEMLOCK FORMATION BEDROCK GEOLOGY OF ARENAC MENOMINEE & CHOCOLAY GROUPS LOWER PENINSULA EMPEROR VULCANIC COMPLEX MASON LAKE OSCEOLA CLARE GLADWIN SIAMO SLATE & AJIBIK QUARTZITE RED BEDS HURON PALMS FORMATION GRAND RIVER FORMATION CHOCOLAY GROUP SAGINAW FORMATION BAY RANDVILLE DOLOMITE BAYPORT LIMESTONE MICHIGAN -
Report of Investigation 15 SUBSURFACE GEOLOGY of BARRY COUNTY, MICHIGAN
Geological Survey Ordovician System .......................................................10 Report of Investigation 15 Cincinnatian Series...................................................10 Trenton Group ..........................................................10 SUBSURFACE GEOLOGY OF BARRY COUNTY, Black River Group ....................................................10 MICHIGAN St. Peter Sandstone .................................................11 by Prairie du Chien Group.............................................11 Richard T. Lilienthal Cambrian System.........................................................11 Illustrations by Author Trempealeau Formation ...........................................11 Lansing Munising Formation ..................................................12 1974 STRUCTURAL GEOLOGY .............................................12 POROUS INTERVALS....................................................12 Contents REFERENCES AND FURTHER READING ...................16 FOREWORD......................................................................2 ABSTRACT .......................................................................2 Illustrations INTRODUCTION ...............................................................3 GEOLOGIC SETTING.......................................................3 Figures MINERAL RESOURCES...................................................3 Index map ...................................................................................2 Surface Minerals ............................................................3 -
The Cambrian Sandstones of Northern Michigan
General Features .......................................................12 Interpretation..............................................................15 Lenticular Sandstone Facies ................................. 15 General Features .......................................................15 Sedimentary Structures..............................................15 Bedding..................................................................15 Channel Structures ................................................15 Cross-Bedding .......................................................16 Other Structures.....................................................18 Interpretation..............................................................18 Massive Sandstone Facies.................................... 19 General Features .......................................................19 Sedimentary Structures..............................................19 Bedding..................................................................19 Ripple Marks ..........................................................19 Interpretation..............................................................19 Frontispiece. The Munising formation exposed in the cliffs of Pictured Rocks. Red Siltstone Facies.............................................. 19 The Pre-Jacobsville Erosional Surface ........................20 STATE OF MICHIGAN Paleogeography ...........................................................21 DEPARTMENT OF CONSERVATION Location of the Source Area................................. -
Impact Origin of the Calvin 28 Cryptoexplosive Disturbance, Cass
Contents Acknowledgements .........................................................2 Introduction......................................................................3 Method of Study...............................................................4 Geologic Setting ..............................................................5 Stratigraphy......................................................................6 Lake Superior Group......................................................6 Munising Formation ................................................. 6 Trempealeau Formation .......................................... 7 Prairie du Chien Group ..................................................7 St. Peter Sandstone ................................................ 8 Black River Group ..........................................................8 Trenton Group................................................................8 Richmond Group ............................................................8 Utica Shale .............................................................. 8 Cataract Group...............................................................9 Structural Characteristics...............................................9 Rim Zone........................................................................9 Annular Depression......................................................10 Central Uplift.................................................................10 Microbreccia.................................................................10 Shock-Metamorphic -
Bedrock Geology of Michigan
BEDROCK GEOLOGY OF MICHIGAN PLV CHC BEDROCK GEOLOGY OF THE EASTERN UPPER PENNINSULA MAC MACKINAC BRECCIA BBF BOIS BLANC FORMATION GIF GARDEN ISLAND FORMATION BIG BASS ISLAND GROUP SAL CHC SALINA GROUP SID SAINT IGNACE DOLOMITE PLV PAC POINT AUX CHENES SHALE ENG ENGADINE GROUP MQG MANISTIQUE GROUP BBG BURNT BLUFF GROUP NSF CHS CABOT HEAD SHALE MND MANITOULIN DOLOMITE CHC QUS QUEENSTON SHALE FSS BHD BIG HILL DOLOMITE STF AGR STONINGTON FORMATION BBF NSF USM CHC JAC UTICA SHALE MEMBER NSF CSM COLLINGWOOD SHALE MEMBER OBF AVS JAC TRN FSS AGR TRENTON GROUP MUN MGF BRG BLACK RIVER GROUP TMP SCF EVC MGF PDC PRAIRIE DU CHIEN GROUP IIF PDC SAQ CHO NIF BRG TMP PAF NIF TREMPEALEAU FORMATION AGR SCF CSM TRN JAC MGF GDQ JAC MUN USM MUNISING FORMATION AMF AVS MCG BRG AGR NIF AGR BIF STF AGR BHD HEM QUS AGR MGF MND CHS AGR INT BHD MCG BBG BDG DCF BBG BEDROCK GEOLOGY OF THE AVS ENG QUS WESTERN UPPER PENNINSULA PRG RAD MND RAD AVS BBG CHS QUF MQG MAC MACKINAC BRECCIA MQG CG RIF M TMP PAC ENG JAC JACOBSVILLE SANDSTONE BDG CHO FSS FREDA SANDSTONE MAC AGR SID NSF NONESUCH FORMATION SAL ENG GIF CHC COPPER HARBOR CONGLOMERATE MGF BBF INT OBF OAK BLUFF FORMATION BBG BBF DRG BBF PLV PORTAGE LAKE VOLCANICS DRG SCF SIEMENS CREEK FORMATION QUF MQG BLS BBG ENG INT INTRUSIVE QUF QUINNESEC FORMATION MUN TRG DDL PRG PAINT RIVER GROUP RIF RIVERTON IRON FORMATION BIF BIJIKI IRON FORMATION ANT CWT ANT NIF NEGAUNEE IRON FORMATION BER IIF IRONWOOD IRON FORMATION BE DCF DUNN CREEK FORMATION R BED BDG BADWATER GREENSTONE ELL MGF MICHIGAMME FORMATION GDQ GOODRICH QUARTZITE