Mackinac County

Total Page:16

File Type:pdf, Size:1020Kb

Mackinac County MACKINAC COUNTY S o y C h r t o u Rock r u BETTY B DORGANS w C t d 8 Mile R D n 6 mlet h o i C d t H o y G r e e Island LANDING 4 CROSSING B u N a Y o d Rd R R R 4 e 8 Mile e y 4 1 k t R k d n 2 ix d t S 14 7 r i Advance n p n 17 d i m Unknow d o e a F u 5 C 123 t e T 7 x k d y O l a o s e i R i R 1 Ibo Rd 1 r r e r Sugar d C M o d Island R a e d R 4 p y f e D c E e S l e n N e i 4 C r a R E R o Y d R L 221 e v a i l 7 R h d A i w x d N i C n S a e w r d g d p e n s u d p 5 a c o r R a r t e B U d d T Island in t g G i e e a n r i g l R R n i o R a d e e R r Rd d o C C o e d d 9 Mile e c 4 r r g k P r h d a L M e n M t h R v B W R R e s e 2 r R C R O s n p N s l k n RACO ea l e u l 28 o ROSEDALE n i R C C d 1 y C l i ree a e le Rd e k a U d e v i 9 Mi e o S y r S a re e d i n g C R R Seney k t ek N e r h C Shingle Bay o U e i u C s R D r e U essea S Sugar B d e F s h k c n c i MCPHEES R L n o e f a a r s t P x h B y e d ut a k 3 So i r k i f u R e t o 0 n h a O t t 1 3 R r R d r r A h l R LANDING 3 M le 7 7 s i T o 1 E d 0 M n i 1 C w a S t U i w e a o s a kn ECKERMAN t R R r v k C o n I Twp r C B U i s Superior e e Island h d d e b Mile Rd r d d Mile Rd 10 e a S f 10 o e i r r q l n s k i W c h n d C u F 3 Columbus u T l McMillan Twp ens M g C g a h r t E a h r 5 Mo reek R n E T 9 H H q m REXFORD c e i u a DAFTER n R W r a l k 5 o M r v Twp Y m r h m L e e C p e i e Twp F s e STRONGS d i Dafter Twp H ty Road 462 East R t d e a Coun P n e e S n e r e v o v o s l d C i R m s n d T o Twp h R t Chippewa l p R C r e NEWBERRY U o e R a n A K i e r 11 Mile R s e P d p v n e k a t S l e e t e e k d n r a d d SEEWHY t A 2 i B C l a a R v B N n L y S v o 11 Mile Rd I i n i d k n HULBERT e s l r o o i r t STRONGS l C s R R v k LENCEL l C G ECKERMAN C e R s l r u l e r u d e i r DOLLARVILLE a e G e e a p e U r r S d r d e k k H Twp e a d CORNERS k a h r e a C Y r W s HOMESTEAD a CORNER R i n b e n r e h a R W Co d e s S C u i n 1 t ty k t e W C O R Hulbert B u M 28 o nty Road 466 s R ra ch r C T a Cou n w C k 2 d AN r 43 9 ADI h 4 A o N N C o e A 6 3 T c ION a h A M C L u RAIL r 3 l n c LAKETON WAY P B Mile Rd N 12 CANADIAN NATIONA N L RAILWAY e 5 r T P i 53 p n 36 Rd e a SOO i e l Usfs 3 12 Mile Rd h NATALIE n e y Twp e k r Lockhart Rd a t Sage C o r T R s U R oad MC MILLAN i HULBERT R d f rest R 3352 B MC CARRON u v o R DONAHER e JUNCTION d r l F d P B r s e era d R 7 d o h F e Fe h h U t F l t 1 O CORNERS k t s r S u u o r 4 g T o Hen A r T o S 5 r C o n S d e S e c d d d Mile R 1 p 13 1 a il o e s a a N 28 Island R 8 R s r D R t 4 p n o d t a Poo i 13 Mile R r 3 r r S R E o e s 3 C m a R k R S d i C e d D C o ou nty t Roa d c 1 d 4 Chicken r a n 57 d d d Hulbert d y a C a 4 t k r c u a L C R DONALDSON n i o e l R n e s M a Islands r r C n o Basnau Rd 4 u ty n d o Lake r u o e R C C R U 1 e o n n e a R O o ad 402 e Ro B County k a W d Bruce Road 454 o 5 County k W y o o r c d d o C d L a C t e 3 R e y U L d s a S t v 4 N r l O R n s i t T R Rd f i i e O s e s l 0 i r s d n R u a e l s P f M r 8 k T H y s s S A E I x k u ounty Road 43 o WATSON’S U h 75 4 t C 8 H u a Twp Soo Twp o MC LEODS l s o e l Kinross Twp iv 1 o e 3 n f C a F R n Arbutus Truck Trl n y o 6 R CORNER k OAK G C u C S r d C h ROBERTS CORNER s i East d St. 0 u v c MC MILLAN r c o r e S n l d I C yl i v e 8 l es R d R d n i i d e te e R S i rs C T RIDGE 15 Mil A e v r re e h K d a CORNER 28 k ek r o BARBEAU C P v P a h e m i R r Lake h d R n 5 e K CORNER R R r e a d R e T d R t n r c ile R M r y k p 15 H T Joseph B R g h d s k 3 d s r t s k u y e i R o t C l o l c C o n 1 v 6 B s o o r n e o C m d u e 8 r n a e A N S e Neebish Island o r e R y D c h 1 o E d r R f e c I Island e k s e e 3 S 9 k d r a R s S k v c h CARPENTER s O n 9 S i s e e o d 436 t d c a f o i h 3 n R Count 3 y R M y o e a R t d s d 45 u i ile R n R 8 r o S c 16 M LANDING D Lakefield u 9 d e l U o North v r J c D o k i e Allen Rd D 3 C a C e r h y e R ie Riv T g r e KINROSS d 1 r t S r r 1 o o o 6 M 9 C e nd k ile Rd a D d c u 3 g o 9 e n Manistique 2 t S gtra Rd R F R a u w Ploe n 5 s S e l 4 r S a H i 5 4 r ge B o u i T t r b 0 C Pentland Twp y y h C r s x Twp 4 i d D o k t r d F c h e s d e Lake o e H e u 4 n R k o n r R c e g n a l r Cr l a e R d k a e e i r R C lac k e e C o o u n r B o v t n e e a o d B ig h t C e e i w a a o t a w S y c R k d o r R s ile R a M R 17 d County Road 98 e r n o m C a y m R i t y o W B r w y nt N T r 4 t Q r t o s d e K t d y KINCHELOE t d Tone Rd i R 6 n r u u TONE m m d t n R k s v i N th o Kallio Rd 7 R n u i n a n u d e o 17 Mile R u C 80 R a u B P o y n s o u o u R e g r 7 t o n HELMER E i r L C e 7 C C l B d a r i t e R t r o C l n t b a o l s 4 C e y c k e n k e v r C I Cre c M i o a r d r e C u C R r h n u r a e C u n u e e s P o MARKS d k d e P c o o d v 129 C County Road 468 k i n R R i n g r n d n C i e e R Allard R MUNUSCONG d y R i e t h P R ve H r T n 18 Mile Rd T e i Hem i Aho Rd d u n loc i k C v d h reek 18 Mile R R o e r Turner Rd e c Pine Filler Rd r C R Q d e R d e d d n 123 on t n L i R COUNTY a v n R UCE S L u 7 FIBRON r e r e 3 1 t d a r o unty Road 447 B 3 n Co H d River s r e h o R JUNCTION a n i e r h o T h R P s r t t y s l c re i ile Rd o W M a u ra l F Main St 19 l n Fede Y d l Roa R d o ty 4 A k KINAC COUNTY a Lumpson Creek n 0 W W Desmareaux Creek e e MAC u e r S IL R Cr d Crane Rd o A Rudyard Z ck d B C R Moon la L n Upper B t d A RUDYARD R o s N d Manistique 334 R O rl e Road 3 Rd I d Island t T t l es s T R For 117 e n ore d A tilla Rd Ketola Rd W L l F n Munuscong Lus ra N e s e k y e d d re d a N r e i R C Twp K Lake d r F t i I v A r u Wilw cu ek I a in is R e i u 0 Mile Rd Island Tr B r l D 2 R He u a nd l d rie Rive u ck ind l t C A ile Rd p KELDEN m r T 0 M R r Br l i N 2 S an r u r c B o s h T Q l u d e ruck T sc A il o r l l o i C d S K e l re l N a r C ek r R i B nk r o r Two Tree h y u T r R k t t T D o D d S k c e a c n M s C c Shingle Bay d e u o Trout Lake Twp S a R R u a Island H r Brown Rd m 38 DRYBURG e Sandtown Rd g n Curtis Rd T 33 r n n p t ea C i R d r i u i B e r d a l s T o ek s k d r r R r u t c i g s u c o c e FIBRE a d k r o a o e c n F 21 Mile Rd s i Tr l t n M a r e B d l r s g w R e d i ile R ed n 21 M Raber Bay d d d R d e y v d i F Wilwin Rd e Germfask B i s a v v R G R R A d R e M C a i e l r Main St o D H k n y o n R e n e l e y Flet y l FIBRON c R g y a he r r r a C C C n r h L r r d e a e r ahn Rd a d n H r t e e y k rairie Rd i Steamboat a e P k k e e d r v R QUARRY G a d a Twp W R H R F CURTIS n k NADIAN NATIONAL RAILWAY 2 r CA r P R G d W r o 2 W y n R a u e e c Island r t DICK p a k M r d S J o n o i c t z M v i l a S d l f d R e Wards R t 48 e L Pilot e o W d STIRLINGVILLE C TROUT r u Trout Lake Rd Teets Rd Pine c o R n R R n y l Trout Lake Rd R f T d Portage Q e n d o d a d e r t Island LAKE t k C d n a u R n k SPURR Island s M S d R c r c B H Rd o R Kelvey d o Mc d H e n r k k Gull e a e i t e r i R s h d R p r r e e k R T D b R r b g D n c c i l W o s c r s D e ile Rd e r 23 M i e trom b n S l i g ree Island y C r e C k r Twp h r G b i n D f r F y u d Fisher Rd ll n L e o e r h M u v Mile Rd f i 23 P e e C e i r k d d e r k o l le R d Y 23 Mi C o a d A S u R l t v v h Kovar Rd W h e o l L a e I i E n i l A e k l a R d b R o L R l i S b P A L R r N C e R a n n S n TIO r y a A C u L ry R Rd R t r n e N r d Vertz s D e e Camp A Rd N t R b e k a IA s le Litt l g t Twin D a l h k e R Garfield Twp B m e k A w k s ea d c N r C D n A g c d e O e C e re e B e P a k T u S e d K C South a W i l o T Ah Rd e d R l H r r d L a d r t Island u v c Rd B o a Gogomain k B c d r s S R y r k R n Manistique F e y r T CAFFEY u a r r C a r l c y Line Rd e Town n n r e h J e e r Mile Rd u PICKFORD d f G Lake v e C b f i EWA COUNTY M P R e HIP r n C D a o M a e d R k C l u a REXTON d r g C GARNET g e r e o n rk R d p d e a d i d k k z g e r O u C e C M B e R R r R a R orton C C d Usfs 3323 l s Sa e d r Park R c Rd N e ile e e 25 M n r C C e 3 l a k l e o d i d Stru Ca NTY i v b ffe MACKINAC COU 2 Blair Rd R e l le y T n d r d 1 i L u M J M i C c g d d a N d k S a C eiffer Rd d We 3 h R s r ke T P R g t Bra e 7 n r c 8 R ch l a R G e o e R k R ck Trl R k ogo Hudson u h 2 n r d e T 2 m Lak s r r ain fin r i Y aw d R R r c i C a v o o p OZARK T h v e e i r s t B n a t lay Rd r h s C Rd o e i GILCHRIST y d k R i w e Raski Rd g Brot d T herton Rd l r s T o r d y R l F e i F n k F a i Y r v i T u n R e Rd l Hendricks Mil t 26 a r A l R Twp H a a o l C o e d n n r n Rd s Criderma n N g r Rd y l e Taylor r R Taylor Rd r d C le l n T d k d L e e r b T T l re e re C m i G e e k o r a e il e R k a R C G r M e e o M U n e h r C P e t r T a k k N r r y le u e a C e e k Twp F u h c r a t MILLECOQUINS a c m i k 6 C i T a s i r d l East r t r T d q B w 1 o O S p C l e e r.
Recommended publications
  • The Lake Michigan Natural Division Characteristics
    The Lake Michigan Natural Division Characteristics Lake Michigan is a dynamic deepwater oligotrophic ecosystem that supports a diverse mix of native and non-native species. Although the watershed, wetlands, and tributaries that drain into the open waters are comprised of a wide variety of habitat types critical to supporting its diverse biological community this section will focus on the open water component of this system. Watershed, wetland, and tributaries issues will be addressed in the Northeastern Morainal Natural Division section. Species diversity, as well as their abundance and distribution, are influenced by a combination of biotic and abiotic factors that define a variety of open water habitat types. Key abiotic factors are depth, temperature, currents, and substrate. Biotic activities, such as increased water clarity associated with zebra mussel filtering activity, also are critical components. Nearshore areas support a diverse fish fauna in which yellow perch, rockbass and smallmouth bass are the more commonly found species in Illinois waters. Largemouth bass, rockbass, and yellow perch are commonly found within boat harbors. A predator-prey complex consisting of five salmonid species and primarily alewives populate the pelagic zone while bloater chubs, sculpin species, and burbot populate the deepwater benthic zone. Challenges Invasive species, substrate loss, and changes in current flow patterns are factors that affect open water habitat. Construction of revetments, groins, and landfills has significantly altered the Illinois shoreline resulting in an immeasurable loss of spawning and nursery habitat. Sea lampreys and alewives were significant factors leading to the demise of lake trout and other native species by the early 1960s.
    [Show full text]
  • AN OVERVIEW of the GEOLOGY of the GREAT LAKES BASIN by Theodore J
    AN OVERVIEW OF THE GEOLOGY OF THE GREAT LAKES BASIN by Theodore J. Bornhorst 2016 This document may be cited as: Bornhorst, T. J., 2016, An overview of the geology of the Great Lakes basin: A. E. Seaman Mineral Museum, Web Publication 1, 8p. This is version 1 of A. E. Seaman Mineral Museum Web Publication 1 which was only internally reviewed for technical accuracy. The Great Lakes Basin The Great Lakes basin, as defined by watersheds that drain into the Great Lakes (Figure 1), includes about 85 % of North America’s and 20 % of the world’s surface fresh water, a total of about 5,500 cubic miles (23,000 cubic km) of water (1). The basin covers about 94,000 square miles (240,000 square km) including about 10 % of the U.S. population and 30 % of the Canadian population (1). Lake Michigan is the only Great Lake entirely within the United States. The State of Michigan lies at the heart of the Great Lakes basin. Together the Great Lakes are the single largest surface fresh water body on Earth and have an important physical and cultural role in North America. Figure 1: The Great Lakes states and Canadian Provinces and the Great Lakes watershed (brown) (after 1). 1 Precambrian Bedrock Geology The bedrock geology of the Great Lakes basin can be subdivided into rocks of Precambrian and Phanerozoic (Figure 2). The Precambrian of the Great Lakes basin is the result of three major episodes with each followed by a long period of erosion (2, 3). Figure 2: Generalized Precambrian bedrock geologic map of the Great Lakes basin.
    [Show full text]
  • Line 5 Straits of Mackinac Summary When Michigan Was Granted
    Line 5 Straits of Mackinac Summary When Michigan was granted statehood on January 26, 1837, Michigan also acquired ownership of the Great Lakes' bottomlands under the equal footing doctrine.1 However before Michigan could become a state, the United States first had to acquire title from us (Ottawa and Chippewa bands) because Anglo-American law acknowledged that we owned legal title as the aboriginal occupants of the territory we occupied. But when we agreed to cede legal title to the United States in the March 28, 1836 Treaty of Washington ("1836 Treaty", 7 Stat. 491), we reserved fishing, hunting and gathering rights. Therefore, Michigan's ownership of both the lands and Great Lakes waters within the cession area of the 1836 Treaty was burdened with preexisting trust obligations with respect to our treaty-reserved resources. First, the public trust doctrine imposes a duty (trust responsibility) upon Michigan to protect the public trust in the resources dependent upon the quality of the Great Lakes water.2 In addition, Art. IV, § 52 of Michigan's Constitution says "conservation…of the natural resources of the state are hereby declared to be of paramount public concern…" and then mandates the legislature to "provide for the protection of the air, water and other natural resources from 3 pollution, impairment and destruction." 1 The State of Michigan acquired title to these bottomlands in its sovereign capacity upon admission to the Union and holds them in trust for the benefit of the people of Michigan. Illinois Central Railroad Co. v. Illinois, 146 U.S. 387, 434-35 (1892); Nedtweg v.
    [Show full text]
  • 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
    [Show full text]
  • Beaver-Island.Pdf
    -J Anishinaabemowin language: George Trudeau Kchi Miigwetch to additional resource language translators: Ron Wakegijig, Wikwemikong Unceded Indian Reserve Eleanore Rivers, Wikwemikong Unceded Indian Reserve Wilfred (Willy) Trudeau, Wikwemikong Unceded Indian Reserve Language of Ojibwe and Odawa dialect found on Manitoulin Island Ontario, Canada. Story excerpts from the Elders of the Grand Traverse Band of Ottawa & Chippewa Indians Drawings by Mark Russell Maps by Pauline Barber Front Cover by James McCaan English translation of tape by Pauline Barber Interviews performed by Brian Corbiere, Pauline Barber and assistance from Carrie Leaureaux & Sammie McClellan-Dyal Video camera operators: Charles Nestell, Brian Corbiere, Pauline Barber and assistance from Carrie Leaureaux & Sammie McClellan-Dyal This book was made possible by the Department of Health and Human Services, Administration for Native Americans, and a match by the Grand Traverse Band of Ottawa & Chippewa Indians. The initial grant team consisted of Carrie Leaureaux, Sammie McClellan-Dyal, Brian Corbiere and Eva Petoskey. r Table of CoiA.teiA.ts Acknowledgements i Map of Beaver Island in relation to Lake Michigan Map of Beaver Island 1 Art Lewis 2 Mary Boulton 5 Pat Wabanimkee 7 Ring of stones 9 Cecelia Boomer Drawing of Rabbit snare ,...10 Ernest Gablow 11 Carolyn Ramey 12 Irene Mitchell 14 Jim Mitchell 15 Helen Paul 16 Gindaaswinan—Island words 17 Vowel-Consonant Syllable Chart 18 References 18 r Beaver Island is located about 30 miles from Charlevoix, Michigan, off the coast of Lake Michigan. Beaver Island is about 15 miles long and 6 miles wide. Gull Island, High Island, Trout Island, Whiskey Island, Garden Island and Hog Island surround Beaver Island, but Beaver Island is the largest of this group of islands.
    [Show full text]
  • FINAL GEOLOGIC REPORT Emerged
    although the conditions of extreme chaos anticipated were not encountered. Geological exploration has established the solidarity of bedrock underlying the Straits of Mackinac and its adequacy to support the comparatively modest loads that will be imposed by the structure. D. B. STEINMAN, CONSULTING ENGINEER MACKINAC BRIDGE Some 300-400 million years ago in early to mid- Devonian time, the land mass in the area of the Straits FINAL GEOLOGIC REPORT emerged. This pseudo-uplift, due to the retreat of the Devonian sea, quickened ground water movement and Jack C. Rosenau thereby, leaching of the salt beds of the Salina Resident Geologist Formation of the Silurian Period. As a result of the April 20, 1956 leaching, two important geological formations came into being: (1) the brine water worked its way into the Michigan Basin and deposited the upper salt beds of the Introduction Detroit River Formation, and (2) the solution of large quantities of rock salt left great voids or cavernous areas The Straits of Mackinac is a 70-mile connecting link with an overlying rock mass of shales, limestones, between Lakes Michigan and Huron; its width at the site dolomites, cherts, sandy shales and gypsum or of the Mackinac Bridge is 4 miles and its depth is known anhydrite. These deposits are the Salina (Pointe Aux to be at least 290 feet below lake level (578.5’ USLS, Chenes) and Bass Island (St. Ignace) Formations of the MLWD). The greatest depth to rock is more than 350 Silurian age and the Garden Island, Bois Blanc and feet and is located about mid-stream.
    [Show full text]
  • 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.
    [Show full text]
  • Wisconsin's Door Peninsula and Its Geomorphology
    WISCONSIN'S DOOR PENINSULA AND ITS GEOMORPHOLOGY Howard De II er AGS Collection, UW-Mllwaukee and Paul Stoelting University of Wisconsin-La Crosse The Door Peninsula of Wisconsin is one of the premier tourist regions of the American r~iddle West. According to a recent geography of Wisconsin (Vogeler et al 1986,8) , the region is best known for its picturesque sea­ scape, New England-style architecture, fish boils, and cherry orchards. Among geomorphologists, however, the region is known for the great variety of land­ form types and for the complex and changing geomorphological processes which have operated in the peninsula. Towering bluffs, sand dunes, lake terraces, abandoned beach ridges, swampy lowlands, and drumlin fields are only some of the many types of landforms to be found in the peninsula. Indeed, the region can be viewed as a unique geomorphological laboratory and an excellent example for classroom study. In this short paper an attempt is made to describe and analyze some of the more prominent landform features of the peninsula and the processes which have influenced their formation. LOCATION AND GENERAL CHARACTERISTICS The Door Peninsula, located In northeastern Wisconsin. is part of the Eastern Ridges and Lowlands province of the state. The peninsula extends in a northeasterly direction into Lake Michigan to separate Green Bay on the west from the main body of Lake Michigan on the east. The peninsula is approximately 64 miles long and about 26 miles wide on its southern end, between the mouth of the Fox River and the city of Kewaunee on Lake Michigan (Map I).
    [Show full text]
  • 2019 State of the Great Lakes Report Michigan
    MICHIGAN State of the Great Lakes 2019 REPORT 2019 STATE OF THE GREAT LAKES REPORT Page 1 Contents Governor Whitmer’s Message: Collaboration is Key ............................................................... 3 EGLE Director Clark’s Message: New Advocates for the Great Lakes Community ................. 4 New Standards Ensure Safe Drinking Water in the 21st Century ............................................ 5 Public Trust Doctrine and Water Withdrawals Aim to Protect the Great Lakes ........................ 8 High Water Levels Put State on Alert to Help Property Owners and Municipalities .................11 Asian Carp Threat from Chicago Area Looms Over Health of Lakes and Aquatic Life ............ 13 EGLE Collaborates on Research into Harmful Algal Blooms and Response Measures .......... 15 Initiatives Foster Stewardship, Raise Water Literacy for All Ages.......................................... 18 Michigan Communities Empowered to Take Action for Great Lakes Protection ...................... 22 EGLE Strengthens Michigan’s Sister State Relationship With Japan’s Shiga Prefecture ....... 24 Soo Locks Project Finally Underway with 2027 Target Date for Opening............................... 25 Great Lakes Cruises Make Bigger Waves in State’s Travel Industry ............................................. 26 MICHIGAN.GOV/EGLE | 800-662-9278 Prepared by the Michigan Department of Environment, Great Lakes, and Energy on behalf of the Office of the Governor (July 2020) 2019 STATE OF THE GREAT LAKES REPORT Page 2 Collaboration is Key hroughout the Great Lakes region, the health of our communities and the strength of our T economies depend on protecting our shared waters. The Great Lakes region encompasses 84 percent of the country’s fresh surface water, represents a thriving, $6 trillion regional economy supporting more than 51 million jobs, and supplies the drinking water for more than 48 million people.
    [Show full text]
  • Reptile and Amphibian Monitoring and Assessment on the Beaver Island Archipelago
    Reptile and Amphibian Monitoring and Assessment on the Beaver Island Archipelago November 2015 Prepared for: Conservation Resource Alliance Bayview Professional Centre 10850 Traverse Highway, Suite 1111 Traverse City MI 49684 Prepared by: Herpetological Resource and Management, LLC P.O. Box 110 Chelsea, MI 48118 www.HerpRMan.com (313) 268-6189 Suggested Citation: Herpetological Resource and Management. 2015. Reptile and Amphibian Community Assessment and Evaluation for the Beaver Island Archipelago. Herpetological Resource and Management. Chelsea, MI. 170 pp. Table of Contents Acknowledgements .......................................................................................................................... 2 Executive Summary .......................................................................................................................... 3 Site Locations and Descriptions ................................................................................................... 6 Beaver Island .................................................................................................................................... 7 Garden Island ................................................................................................................................ 16 Trout Island .................................................................................................................................... 16 Whiskey Island ..............................................................................................................................
    [Show full text]
  • Thunder Bay National Marine Sanctuary
    THUNDER BAY NATIONAL MARINE SANCTUARY 2006 state of the sanctuary report National Oceanic National Marine Sanctuary Program and Atmospheric The National Marine Sanctuary Program (NMSP) serves as the trustee for a system of 14 marine Administration protected areas, encompassing more than 150,000 square miles of ocean and Great Lakes waters from Washington State to the Florida Keys, and from Lake Huron to American Samoa. The National U.S. Secretary of Commerce Carlos M. Gutierrez Oceanic and Atmospheric Administration’s (NOAA) National Ocean Service (NOS) manages the national marine sanctuaries through the authority of the National Marine Sanctuaries Act of 1972. Under Secretary of Commerce for Oceans and Atmosphere Conrad C. Lautenbacher, Jr. Our marine sanctuaries contain deep ocean gardens, coastal coral reefs, whale migration corridors, Vice Admiral, U.S. Navy (Ret.) deep-sea canyons, and historically-significant shipwrecks and other underwater archaeological sites. They range in size from one-quarter square mile in Fagatele Bay, American Samoa, to more than Assistant Administrator for Ocean Services and Coastal 134,000 square miles at the Northwestern Hawaiian Islands Marine National Monument, the largest Zone Management marine protected area in the world. John H. Dunnigan The NMSP fosters public awareness of marine resources and maritime heritage through scientific National Marine research, monitoring, exploration, education, and outreach, and works cooperatively with its many Sanctuary Program partners and the public to protect and manage sanctuaries. The NMSP is a world leader in effective marine management, protecting living marine creatures, environmental quality, and maritime heritage Director Daniel J. Basta resources while maintaining recreational and commercial activities that are sustainable and compatible with long-term preservation.
    [Show full text]
  • Northern Michigan's
    Northern MIchigan’s 2010 Report Bass Lake Birch Lake Deer Lake Huffman Lake Larks Lake Long Lake Marion Lake GNoweland Lakem Silver Lake Susan LLake ThumbaLake Twikn Lake Wildewood Lakes What would Michigan be without water? One might as well to protect lakes throughout Northern Michigan. Projects ask what the Sahara would be without sand or the Himalayas carried out on these lakes have ranged from lake-wide without mountains. Michigan is defined by water and, aquatic plant surveys to individual shoreline property in fact, the definition of Michigan in some Native American restoration projects. Details about recent projects involving languages literally means water, “big lake” to be precise. the Gem Lakes are included in this report. Water formed Michigan, frozen water that is, thousands of We hope you find the information presented in this report feet thick. A series of glaciers advanced and retreated across both interesting and insightful. If you have any questions, Michigan over the course of millions of years, creating the comments, or concerns, please contact Tip of the Mitt present-day landscape of rolling hills and broad plains; Watershed Council at (231) 347-1181 or visit our website at dotted with lakes, crisscrossed with rivers, and surrounded www.watershedcouncil.org. by freshwater seas. Glacial scouring and huge ice chunks that were left behind formed thousands of lakes across the landscape, lakes of all shapes and sizes, each unique: each beautiful and special in its own way. Many people live in or travel through Northern Michigan because of these lakes and the character they lend to the region.
    [Show full text]