Land Type Associations of the Hiawatha National Forest
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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. -
National Forests in Michigan
OriqiMI from Digitized by Go gle UNIVERSITY OF MICHIGAN NATIONAL FORESTS IN MICHIGAN UNITED STATES DEPARTMENT OF AGRICULTURE FOREST SERVICE NORTH CENTRAL REGION • MILWAUKEE, WIS. ON THE COVER. —Great Conglomerate Falls on the Black River. p-3e«M ERRATA Page Line 5 3 97,000,000 should be 45,000,000. 7 4 Porcupine should not be listed vvilh fur bearers. 17 7 Si.o'jld read "the red pine by its ClUoLC"G Cf t»Vj". 44 2-3 Should read "4 rniies east of Munising". UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1941 sEr^ •*«$• . AU TRAIN FALLS ON THE HIAWATHA NATIONAL FOREST. Drama of Michigan Forests DRAMA of the forests of Michigan has been written in several acts THEeach with its colorful pageantry. The action has concerned the magni ficent woodlands of the redman, the rapid depletion of those forests in the last century, and their slow but sure rebuilding in the present. The elusive "northwest passage" to China, Indian furs and Indian souls, iron and land and copper brought the white men to Michigan. In 1621, only 1 year after the Pilgrims landed at Plymouth Rock, young Etienne Brule, protege of Champlain, reached Lake Superior and was disappointed to find its waters fresh. Thirteen years later, Jean Nicolet, another protege of the French governor of Canada, entered the unknown Lake Michigan through the Straits of Mackinac. Though he never found the longed-for route to the Orient, Nicolet did initiate the French fur trade with the Indians in this territory. Heroic followers of Brule and Nicolet were the Jesuit fathers Jogues and Raymbault, who preached to the Ojibwas in 1641 at Sault Ste. -
Stories in Sand
Above: Cliffs along the trail east of Miners Castle Stories in Sand Sandstone cliffs-ochre, tan, and brown with layers of Moving ice ground volcanic and sedimentary rock from Twelvemile Beach are horn coral from an ancient sea, white and green-tower 50 to 200 feet above the water. previous eras into rubble and slowly enlarged river valleys polished granite and quartz rounded like eggs, and Vast, blue Lake Superior glistens against a cloud-streaked into the wide basins that would become the Great Lakes. disk-shaped fragments of the Jacobsville sandstone. sky. Deep forests of emerald, black, and gold open onto small lakes and waterfalls. The images are like a painter's The last glacier began retreating about 10,000 years ago. Colorful Cliffs The name Pictured Rocks comes from the work. A palette of nature's colors, textures, and shapes Over time its meltwater formed powerful rivers and streaks of mineral stain decorating the face of the cliffs. sets the scene at Pictured Rocks National Lakeshore. scattered rubble onto outwash plains and into crevasses. The streaks occur when groundwater oozes out of cracks. Water scooped out the basins and channels that harbor The dripping water contains iron, manganese, limonite, This place of beauty was authorized as the first national wetlands in the park today. Eventually, as the weight of copper, and other minerals that leave behind a colorful lakeshore in 1966 to preserve the shoreline, beaches, the glacier lessened, the land rose and exposed bedrock stain as the water trickles down a cliff face. cliffs, and dunes and to provide an extraordinary place to lake erosion. -
United States Department of the Interior
United States Department of the Interior FISH AND WILDLIFE SERVICE East Lansing Field Office (ES) 2651 Coolidge Road, Suite 101 IN REPLY REFER TO: East Lansing, Michigan 48823-6316 May 1, 2015 Leslie Auriermno, Forest Supervisor Huron-Manistee National Forests 1755 South Mitchell St. Cadillac, MI 49601-8533 Re: Fonnal Section 7 Consultation on the Huron-Manistee National Forests' Ongoing and Planned Actions- Log# 1O-R3-ELF0-03 Dear Ms. Amiemmo: This letter transmits the U.S. Fish and Wildlife Service's Biological Opinion for the Huron Manistee National Forests' (HMNF) ongoing and planned actions in accordance with Section 7 of the Endangered Species Act (Act) of 1973, as amended (16 U.S .C. 1531 et seq.). The HMNF detennined that the proposed actions were "Likely to Adversely Affect" the norihern long-eared bat (Myotis septentrionalis). We base the enclosed Opinion on information provided in several documents, including your northern long-eared project matrix and Biological Assessment, the Programmatic Biological Assessment and Opinion for the HMNF's Land and Resource Management Plan, and our April 1, 2015, Conference Opinion. Other sources ofinfonnation include previous telephone conversations, e-mails and meetings. A complete administrative record of this consultation is on file at our East Lansing Field Office. After reviewing the current status of northern long-eared bat, the environmental baseline for the action area, the effects of the proposed action, and the cumulative effects, it is our biological opinion that the action, as proposed, is not likely to jeopardize the continued existence of northern long-eared bat With respect to ESA compliance, all aspects of the project description are binding. -
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 ................................................. -
Emmet Cheboygan Lake Michigan Lake Superior Lake
Superior Region - East RoadRoad andand TrailTrail BicyclingBicycling GuideGuide ) X M Whitefish Twp Park !! ! Whitefish Point Vermillion _ !! Twomile Weatherhogs reek Lk. ns C Lk. Lake Superior Crisp Point ) Brow Browns Marsh Lakes d R Lk. t Be in tsy McMullan Lakes o Ri v P e r h 11 s i CR 412 f e t T Hawkins i hree h M Lk. W i l e Shelldrake Dam 9 Little Lake Harbor C r Betsy e State Forest Campground e River Little!! _¬ k X ! ! ! ! ! ! ! ! ! ! Lk. ! ! ! ! ! ! ! ! ! ! ! ! Bodi Lake 9 9 ! ! Andrus Lake ! ! ! Andrus ! X ! Bear Lk. X ! ! ! ! ! State Forest Campground Lk. Mouth of Two Hearted River ! Ile Parisienne ! ! ! Culhane State Forest Campground ! ! !! 9 !! !! Bodi Lk. ! Lk. State Forest Campground! X ! ! ! ! ! s ! X ! Bet y ! ! ! R ! Culhane! Lake ! ! ! i ! ! ! ! !! ! ! ! ! ! v ! !! ! !! ! !! ! ! ! !! ! ! 9 e ! ! ! ! ! ! ! State Forest Campground r !! ! ! ! ! ! Lake Superior ! Shelldrake ! r ! ! Randolph Muskallonge Lake State Park e Muskrat ! ! ! ! ! 9 ! v ! ! ! i ! ! ! ! ! ! ! ! ! ! ! 9 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! State Forest Campground! ! ! ! ! ! R ! ! ! ! ! ! ! ! ! ! r ! ! Lk. ! ! ! ! e ! ! ! ! ! ! ! ! ! !! !iv ! ! ! ! d Lakes ! ! ! ! ! ! R ! ! ) ! ! ! ! ! ! ! ! ! e ! r ! ! ! ! ! ! !! ! ! ! ! !e! ! !! ! t ! Section k ! ! ! ! ! ! ! ! ! c ! ! ! ! !! ! ! u ! ! ! ! r ! S ! ! ! ! ! d ! ! ! ! ! ! a S ! ! ! Deer! Park ! X n ! ! ! ! ! ! ! i ! ! ! ! ! ! ! ! ! ! ! l ! ! ! e ! ! B Mud ! ! ! u ! ! ! X ! ! ! ! ! ! ! ! Woodland Park ! ! H !! GRAND MARAISc ! ! Four Lk. ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! o ! ! ! k ! ! ! ! ! ! ! -
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 -
Biodiversity of Michigan's Great Lakes Islands
FILE COPY DO NOT REMOVE Biodiversity of Michigan’s Great Lakes Islands Knowledge, Threats and Protection Judith D. Soule Conservation Research Biologist April 5, 1993 Report for: Land and Water Management Division (CZM Contract 14C-309-3) Prepared by: Michigan Natural Features Inventory Stevens T. Mason Building P.O. Box 30028 Lansing, MI 48909 (517) 3734552 1993-10 F A report of the Michigan Department of Natural Resources pursuant to National Oceanic and Atmospheric Administration Award No. 309-3 BIODWERSITY OF MICHIGAN’S GREAT LAKES ISLANDS Knowledge, Threats and Protection by Judith D. Soule Conservation Research Biologist Prepared by Michigan Natural Features Inventory Fifth floor, Mason Building P.O. Box 30023 Lansing, Michigan 48909 April 5, 1993 for Michigan Department of Natural Resources Land and Water Management Division Coastal Zone Management Program Contract # 14C-309-3 CL] = CD C] t2 CL] C] CL] CD = C = CZJ C] C] C] C] C] C] .TABLE Of CONThNTS TABLE OF CONTENTS I EXECUTIVE SUMMARY iii INTRODUCTION 1 HISTORY AND PHYSICAL RESOURCES 4 Geology and post-glacial history 4 Size, isolation, and climate 6 Human history 7 BIODWERSITY OF THE ISLANDS 8 Rare animals 8 Waterfowl values 8 Other birds and fish 9 Unique plants 10 Shoreline natural communities 10 Threatened, endangered, and exemplary natural features 10 OVERVIEW OF RESEARCH ON MICHIGAN’S GREAT LAKES ISLANDS 13 Island research values 13 Examples of biological research on islands 13 Moose 13 Wolves 14 Deer 14 Colonial nesting waterbirds 14 Island biogeography studies 15 Predator-prey -
The National Forests of Michigan, Federal Payments to States
The National Forests of Michigan Federal Payments to States The Eastern Region of the U.S. Forest Service The Federal Government reimburses States that contain National Forest System Lands in several ways. The 25 Percent Payments. The first county payment or revenue is the “25 Percent Fund payment.” The 25 Percent Fund payment is based on gross National Forest receipts within a National Forest and is allocated to counties by the proportion of the total National Forest acreage within each county in the particular National Forest. Secure Rural Schools. The Secure Rural Schools (SRS) program is an alternative to 25 Percent Payments. This program allows counties to elect the manner in which their payment is calculated. A county may choose to continue to receive the 25-percent payments based on a 7-year rolling average of receipts from national forests located in the State. Counties may elect to receive the Full Payment option, in which Title I dollars are allocated to roads and schools while Title II and III funds are spent on work completed on or that benefit National Forest System lands. The PILT Payment. Payments in Lieu of Taxes (PILT) are Federal payments to local governments that help offset losses in property taxes due to nontaxable Federal lands within their boundaries. The key law that implements the payment is Public Law 94-565. The Law recognizes that the inability of local government to collect property taxes on Federally-owned land can create a financial impact. Mineral Royalties. The third major Federal program that funds States and counties involves mineral royalties generated on Federal lands. -
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. -
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