Central Lake Michigan Coastal Ecological Landscape
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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. -
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. -
2. Blue Hills 2001
Figure 1. Major landscape regions and extent of glaciation in Wisconsin. The most recent ice sheet, the Laurentide, was centered in northern Canada and stretched eastward to the Atlantic Ocean, north to the Arctic Ocean, west to Montana, and southward into the upper Midwest. Six lobes of the Laurentide Ice Sheet entered Wisconsin. Scale 1:500,000 10 0 10 20 30 PERHAPS IT TAKES A PRACTICED EYE to appreciate the landscapes of Wisconsin. To some, MILES Wisconsin landscapes lack drama—there are no skyscraping mountains, no monu- 10 0 10 20 30 40 50 mental canyons. But to others, drama lies in the more subtle beauty of prairie and KILOMETERS savanna, of rocky hillsides and rolling agricultural fi elds, of hillocks and hollows. Wisconsin Transverse Mercator Projection The origin of these contrasting landscapes can be traced back to their geologic heritage. North American Datum 1983, 1991 adjustment Wisconsin can be divided into three major regions on the basis of this heritage (fi g. 1). The fi rst region, the Driftless Area, appears never to have been overrun by glaciers and 2001 represents one of the most rugged landscapes in the state. This region, in southwestern Wisconsin, contains a well developed drainage network of stream valleys and ridges that form branching, tree-like patterns on the map. A second region— the northern and eastern parts of the state—was most recently glaciated by lobes of the Laurentide Ice Sheet, which reached its maximum extent about 20,000 years ago. Myriad hills, ridges, plains, and lakes characterize this region. A third region includes the central to western and south-central parts of the state that were glaciated during advances of earlier ice sheets. -
Door County Here to Help Transportation Vehicle Purchase & Repair Loans
Rentals Group & Door-Tran: Options Door County Here to help Transportation Vehicle purchase & repair loans America’s Best Choice Rentals Half-price travel & gasoline Resource Guide - Young Automotive, Sturgeon Bay vouchers 920-743-9228 Volunteer transportation for Avis Rent-A-Car veterans and Door County - Super 8, Sturgeon Bay residents 920-743-7976 - Tailwind Flight Center Trip planning 920-746-9250 Information & referral Door County Trolley to get you - Customer tours, groups, parades, where you need to go! festivals, weddings This program is funded in part by the Federal Transit Administration 920-868-1100 (FTA) as authorized under 49 U.S.C. Section 5310 Mobility Options of Seniors and Individuals with Disabilities Program (CFDA 20.521) www.doorcountytrolley.com Door-Tran operates its programs and services without regard to race, color, and national origin in accordance with Title VI of the Door Peninsula Sales & Storage Civil Rights Act. Any person who believes she or he has been aggrieved by any unlawful discriminatory practice under Title VI - Vehicle, trailer, & snowmobile rentals may file a complaint with Door-Tran. 920-743-7297 Lamers Bus Lines - Wheelchair accessible - Small to large groups 800-236-1240 Sah’s Auto, Inc. 1009 Egg Harbor Road PO Box 181 - Vehicle rentals Sturgeon Bay, WI 54235-0181 920-743-1005 www.door-tran.org Email: [email protected] Sunshine House, Inc. Phone: 920-743-9999 - Wheelchair accessible Toll-free: 877-330-6333 - Group transportation 920-743-7943 Door-Tran Here to get you Volunteer Transportation -
Central Region Technical Attachment 91-23 an Excessive Lake
/Ws-oVT A-7f CRH SSD OCTOBER 1991 CENTRAL REGION TECHNICAL ATTACHMENT 91-23 AN EXCESSIVE LAKE-ENHANCED SNOWFALL EPISODE OVER NORTHEAST WISCONSIN ON DECEMBER 13-15, 1989 Eugene S. Brusky National Weather Service Office Green Bay, Wisconsin Thomas D. Helman National Weather Service Forecast Office Milwaukee, Wisconsin 1. Introduction During the late fall and early winter months, the well known lake effect snows frequently develop over portions of the western Great Lakes. Areas most susceptible to heavy lake snows are typically in Upper Michigan, along Lake Superior and along the eastern shoreline of Lake Michigan. These areas commonly experience a cold and dry northwesterly wind flow which gathers moisture from the lakes and deposits it in the form of snow. Orographic lifting, such as along the Gogebic Range in Upper Michigan, helps to enhance and localize the heaviest snowfall. Tn comparison, heavy lake effect snow along the western shores of Lake Michigan is not as common since the prevailing wind direction in the winter is northwest, and not a more favorable northeast. The purpose of this paper is to examine a heavy lake enhanced snowfall episode which occurred over northeast Wisconsin. During a 2-day period from December 13-15, 1989, up to 30 inches of snow fell over a portion of Wisconsin's Door Peninsula. This event was characterized by a snowband which initially formed over Lake Michigan and moved westward before becoming quasi-stationary over northeast Wisconsin. The snovband was then observed to rotate cyclonically over northeast Wisconsin in concert with a mid-level shear axis. It will be shown that the heavy snowfall was caused by a combination of lake induced mesoscale and synoptic scale weather features. -
Wisconsin's John Muir
Wisconsin’s John Muir An Exhibit Celebrating the Centennial of the National Park Service “Oh, that glorious Wisconsin wilderness! “Everything new and pure in the very prime of the spring when Nature’s pulses were beating highest and mysteriously keeping time with our own!” “Wilderness is a necessity... Mountain parks and reservations are useful not only as fountains of timber and irrigating rivers, but as fountains of life.” This exhibit was made possible through generous support from the estate of John Peters and the Follett Charitable Trust Muir in Wisconsin “When we first saw Fountain Lake Meadow, on a sultry evening, sprinkled with millions of lightning- bugs throbbing with light, the effect was so strange and beautiful that it seemed far too marvelous to be real.” John Muir (1838–1914) was one of America’s most important environmental thinkers and activists. He came to Wisconsin as a boy, grew up near Portage, and attended the University of Wisconsin. After decades of wandering in the mountains of California, he led the movement for national parks and helped create the Sierra Club. But for much of his life, Muir’s call to protect wild places fell on deaf ears. Muir studied science in Madison but quit in 1863 without a degree, “...leaving one University for another, the Wisconsin University for the University of the Wilderness.” Muir’s letter to the classmate who taught him botany at UW The Movement for National Parks Yosemite Valley “Everybody needs beauty as well as bread, places to play in and pray in, where Nature may heal and cheer and give strength to body and soul alike.” In 1872, Congress named Yellowstone the first national park. -
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 -
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. -
65Th Annual Tri-State Geological Field Conference 2-3 October 2004
65th Annual Tri-State Geological Field Conference 2-3 October 2004 Weis Earth Science Museum Menasha, Wisconsin The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago Joanne Kluessendorf & Donald G. Mikulic Organizers The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago 65th Annual Tri-State Geological Field Conference 2-3 October 2004 by Joanne Kluessendorf Weis Earth Science Museum, Menasha and Donald G. Mikulic Illinois State Geological Survey, Champaign With contributions by Bruce Brown, Wisconsin Geological & Natural History Survey, Stop 1 Tom Hooyer, Wisconsin Geological & Natural History Survey, Stops 2 & 5 William Mode, University of Wisconsin-Oshkosh, Stops 2 & 5 Maureen Muldoon, University of Wisconsin-Oshkosh, Stop 1 Weis Earth Science Museum University of Wisconsin-Fox Valley Menasha, Wisconsin WELCOME TO THE TH 65 ANNUAL TRI-STATE GEOLOGICAL FIELD CONFERENCE. The Tri-State Geological Field Conference was founded in 1933 as an informal geological field trip for professionals and students in Iowa, Illinois and Wisconsin. The first Tri-State examined the LaSalle Anticline in Illinois. Fifty-two geologists from the University of Chicago, University of Iowa, University of Illinois, Northwestern University, University of Wisconsin, Northern Illinois State Teachers College, Western Illinois Teachers College, and the Illinois State Geological Survey attended that trip (Anderson, 1980). The 1934 field conference was hosted by the University of Wisconsin and the 1935 by the University of Iowa, establishing the rotation between the three states. The 1947 Tri-State visited quarries at Hamilton Mound and High Cliff, two of the stops on this year’s field trip. -
April 20, 2017 Robert Kaplan Acting Regional Administrator U.S
State of Wisconsin DEPARTMENT OF NATURAL RESOURCES Scott Walker, Governor 101 S. Webster Street Cathy Stepp, Secretary Box 7921 Telephone 608-266-2621 Madison WI 53707-7921 Toll Free 1-888-936-7463 TTY Access via relay - 711 April 20, 2017 Robert Kaplan Acting Regional Administrator U.S. Environmental Protection Agency - Region 5 77 West Jackson Blvd. Chicago, IL 60604-3507 Subject: Supplemental Information for 2015 Ozone National Ambient Air Quality Standard (NAAQS) Area Designations Dear Mr. Kaplan: On October 1, 2015, the U.S. Environmental Protection Agency (EPA) revised both the primary and secondary ozone NAAQS. On September 21, 2016, in accordance with section 107(d)(1)(A) of the Clean Air Act (CAA), Governor Walker recommended that all counties in Wisconsin be designated as attainment for this standard. In support of the governor’s recommendation, the Wisconsin Department of Natural Resources (WDNR) is submitting the enclosed technical support document (TSD). EPA should consider this supporting information and ensure it is reflected in any modifications to the governor’s recommendation EPA elects to make in the “120 day” notifications that would occur prior to final designations. While the general concept of ozone formation and transport in the Lake Michigan basin has long been recognized, this TSD incorporates data from a variety of sources, some of which were unavailable until recently. This includes: Analysis of ozone data from the lakeshore and inland monitors operated by WDNR in both Sheboygan and Kenosha counties to help understand the lakeshore ozone gradient; Analysis of wind data when values above the 2015 ozone standard have been measured at shoreline monitors; Recent HYSPLIT and source apportionment modeling results; Photochemical modeling conducted by the Lake Michigan Air Directors Consortium (LADCO). -
Chapter 3, Historical and Cultural Resources
Door County Comprehensive and Farmland Preservation Plan 2035: Volume II, Resource Report CHAPTER 3: HISTORICAL AND CULTURAL RESOURCES 16 | Chapter 3: Historical and Cultural Resources Door County Comprehensive and Farmland Preservation Plan 2035: Volume II, Resource Report INTRODUCTION This chapter begins by briefly discussing Door County’s “community character,” which is intertwined with many of the county’s historical and cultural resources. It then provides a brief history of the county’s residents and its development, followed by an inventory of the historical resources in Door County. Included are discussion of the county’s historical associations; the area’s maritime history and maritime museums, lighthouses, and shipwrecks; general museums; archaeological sites; sites on the state and/or federal historic registries; and cemeteries. Finally, this chapter provides an inventory of cultural resources, such as cultural organizations, educational and cultural opportunities, visual and performing arts groups and venues, and festivals. COMMUNITY CHARACTER Community character is defined by a variety of sometimes intangible factors, including the people living in the area, the visual character of the area, and the quality of life and experiences offered to residents and visitors. Door County’s community character was ranked as either the county’s highest or second- highest asset during the public input exercises conducted at the county-wide visioning sessions held between 2006 and 2007. As is evidenced by the lists below of responses from residents at those visioning meetings, all aspects of community character – the people, the visual attributes, and the general quality of life as well as the county’s specific historical and cultural resources – define or exemplify life in Door County. -
TRS ED JD Final 06 29 2020
Job Announcement: Executive Director Location: Bailey’s Harbor, WI (www.ridgessanctuary.org) General Position Description: Executive Director The Executive Director is responsible for leading The Ridges Sanctuary, Inc. (TRS) in a manner that fulfills its mission of inspiring stewardship of natural areas through programs of education, outreach and research. The Executive Director provides leadership, strategic direction, fundrais- ing, human resource and financial management, and administration for TRS. The Executive Direc- tor oversees communications and inspires engagement with the membership, the public, and fed- eral, state, and local government agencies. The Executive Director is the senior staff person of TRS and is hired by and responsible to the Board of Directors. The President of the Board serves as primary liaison with the Executive Director. The Board evaluates performance of the Executive Di- rector in relation to the responsibilities of the position, and annual and long-term goals estab- lished by the Board. Compensation is set by the Board. About The Ridges Sanctuary Incorporated in 1937, the Ridges Sanctuary has grown thoughtfully and strategically from its original 30-acre parcel to over 1,600 acres in and around Bailey’s Harbor to insure the protection of some of the most biologically diverse areas of Wisconsin. The Ridges includes a LEED Certified Nature Center, an ADA accessible boardwalk, rustic trails, two fully restored historic Range Lights and a Family Discovery Trail. Our mission is to protect the Sanctuary and inspire stewardship of natural areas through programs of education, outreach and research. The Ridges is dedicated to protecting the distinctive topography for which it is named – a series of ridges and swales formed by the movement of Lake Michigan over 1,100 years.