Lake Huron's Phosphorus Contributions
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Physical Limnology of Saginaw Bay, Lake Huron
PHYSICAL LIMNOLOGY OF SAGINAW BAY, LAKE HURON ALFRED M. BEETON U. S. Bureau of Commercial Fisheries Biological Laboratory Ann Arbor, Michigan STANFORD H. SMITH U. S. Bureau of Commercial Fisheries Biological Laboratory Ann Arbor, Michigan and FRANK H. HOOPER Institute for Fisheries Research Michigan Department of Conservation Ann Arbor, Michigan GREAT LAKES FISHERY COMMISSION 1451 GREEN ROAD ANN ARBOR, MICHIGAN SEPTEMBER, 1967 PHYSICAL LIMNOLOGY OF SAGINAW BAY, LAKE HURON1 Alfred M. Beeton, 2 Stanford H. Smith, and Frank F. Hooper3 ABSTRACT Water temperature and the distribution of various chemicals measured during surveys from June 7 to October 30, 1956, reflect a highly variable and rapidly changing circulation in Saginaw Bay, Lake Huron. The circula- tion is influenced strongly by local winds and by the stronger circulation of Lake Huron which frequently causes injections of lake water to the inner extremity of the bay. The circulation patterns determined at six times during 1956 reflect the general characteristics of a marine estuary of the northern hemisphere. The prevailing circulation was counterclockwise; the higher concentrations of solutes from the Saginaw River tended to flow and enter Lake Huron along the south shore; water from Lake Huron entered the northeast section of the bay and had a dominant influence on the water along the north shore of the bay. The concentrations of major ions varied little with depth, but a decrease from the inner bay toward Lake Huron reflected the dilution of Saginaw River water as it moved out of the bay. Concentrations in the outer bay were not much greater than in Lake Huronproper. -
The Huron River History Book
THE HURON RIVER Robert Wittersheim Over 15,000 years ago, the Huron River was born as a small stream draining the late Pleistocene landscape. Its original destination was Lake Maumee at present day Ypsilanti where a large delta was formed. As centuries passed, ceding lake levels allowed the Huron to meander over new land eventually settling into its present valley. Its 125 mile journey today begins at Big Lake near Pontiac and ends in Lake Erie. The Huron’s watershed, which includes 367 miles of tributaries, drains over 900 square miles of land. The total drop in elevation from source to mouth is nearly 300 feet. The Huron’s upper third is clear and fast, even supporting a modest trout fishery. The middle third passes through and around many lakes in Livingston and Washtenaw Counties. Eight dams impede much of the Huron’s lower third as it flows through populous areas it helped create. Over 47 miles of this river winds through publicly owned lands, a legacy from visionaries long since passed. White Lake White Lake Mary Johnson The Great Lakes which surround Michigan and the thousands of smaller lakes, hundreds of rivers, streams and ponds were formed as the glacier ice that covered the land nearly 14,000 years ago was melting. The waters filled the depressions in the earth. The glaciers deposited rock, gravel and soil that had been gathered in their movement. This activity sculpted the land creating our landscape. In section 28 of Springfield Township, Oakland County, a body of water names Big Lake by the area pioneers is the source of the Huron River. -
Lake Huron Scuba Diving
SOUTHERN LAKE ASSESSMENT SOUTHERN RECREATION PROFILE LAKE Scuba Diving: OPPORTUNITIES FOR LAKE HURON ASSESSMENT FINGER LAKES SCUBA LAKES FINGER The southern Lake Huron coast is a fantastic setting for outdoor exploration. Promoting the region’s natural assets can help build vibrant communities and support local economies. This series of fact sheets profiles different outdoor recreation activities that could appeal to residents and visitors of Michigan’s Thumb. We hope this information will help guide regional planning, business develop- ment and marketing efforts throughout the region. Here we focus on scuba diving – providing details on what is involved in the sport, who participates, and what is unique about diving in Lake Huron. WHY DIVE IN LAKE HURON? With wildlife, shipwrecks, clear water and nearshore dives, the waters of southern Lake Huron create a unique environment for scuba divers. Underwater life abounds, including colorful sunfish and unusual species like the longnose gar. The area offers a large collection of shipwrecks, and is home to two of Michigan’s 12 underwater preserves. Many of the wrecks are in close proximity to each other and are easily accessed by charter or private boat. The fresh water of Lake Huron helps to preserve the wrecks better than saltwater, and the lake’s clear water offers excellent visibility – often up to 50 feet! With many shipwrecks at different depths, the area offers dives for recreational as well as technical divers. How Popular is Scuba Diving? Who Scuba Dives? n Scuba diving in New York’s Great Lakes region stimulated more than $108 In 2010, 2.7 million Americans went scuba A snapshot of U.S. -
A Changing Lake Huron
A Changing Lake Huron The Lake Huron Food Web total phosphorus levels in the spring and summer. The source of food for all living things in Lake Huron are microscopic aquatic Total phosphorus declined by 50% plants called algae. Every other living from 1995 to 2003 (4 mg/L to 2 mg/l). organism in the lake must either eat live Levels have since increased slightly or dead algae directly or eat another and stabilized at approximately 2.5-3.0 organism that depends on algae. mg/L. The decline in nutrients means Although algae can reach nuisance levels that Lake Huron can support under certain conditions, it is essential less overall fish biomass than it did to the life of the lake. All aquatic animals before 2000 (Fig. 2). in the lake are connected to algae through a food web (Fig. 1). Lake Huron can support less Phosphorus overall fish biomass than it and Fish Biomass did before 2000. Phosphorus is an essential nutrient required for algae growth. The total weight of all living fish, termed the fish Food Web Trophic biomass, is positively related to total phosphorus, but other factors change Transfer Efficiency the amount of fish biomass that can A food web can be organized into be sustained (Fig. 2). These modifying trophic (energy) levels (Fig. 3, overleaf). Living factors include changes to food web algae and organic material are the first, or structure caused by invasions (e.g., lowest, trophic level (TL-1). Small animals, quagga mussels), habitat availability, like small zooplankton, quagga mussels, and water clarity, level of fishing, stocking, Diporeia consume algae and represent TL-2. -
Huron River Water Trail Trip Description 1 Hudson Mills Metropark
Huron River Water Trail Trip Description Hudson Mills Metropark (Mile 67) to Delhi Metropark (Mile 58.3) - 3.5 hours; 8.7 miles Launch at the Rapids View Picnic Area in Hudson Mills Metropark, near North Territorial Road. This trip provides easy access to both launch and take-out sites. Paddle through parkland and then into Dexter. TRIP DESCRIPTION: Excerpt from “Canoeing Michigan Rivers: A Comprehensive Guide to 45 Rivers” by Jerry Dennis and Craig Date provided with permission from Thunder Bay Press. Put in at Hudson Mills Metropark, where there is good access and parking just below Territorial Road [at the Rapids View Picnic Area]. Upstream, fair access and parking are found a Bell Road. [Note: Launching at Bell Road will take you past the Hudson Mills canoe campground and rapids where a portage is recommended.] The river here is 60-90 feet wide and alternates sections of slow water one to four feet deep with sections of very shallow riffles. Low water in summer will produce some bottom-bumping. Hudson Mills has been the site of a saw mill, grist mill, cider mill and plaster mill, the earliest dating back to 1827. Today, only the ruins of foundations and a short stretch of light rapids mark the spot just below Territorial Road Bridge where the mills were located. The rapids can be run down the chute at left center. Pumpkin- to bushel-size rocks create standing waves that could become fairly high during high water. If in doubt, portage on the left just beyond the bridge. Light riffles extend well into Hudson Mills Metropark, where there are several access sites and two overnight canoe campgrounds. -
Reduced Annualreport1972.Pdf
PROVINCE OF BRITISH COLUMBIA DEPARTMENT OF RECREATION AND CONSERVATION HON. ROBERT A. WILLIAMS, Minister LLOYD BROOKS, Deputy Minister REPORT OF THE Department of Recreation and Conservation containing the reports of the GENERAL ADMINISTRATION, FISH AND WILDLIFE BRANCH, PROVINCIAL PARKS BRANCH, BRITISH COLUMBIA PROVINCIAL MUSEUM, AND COMMERCIAL FISHERIES BRANCH Year Ended December 31 1972 Printed by K. M. MACDONALD, Printer to tbe Queen's Most Excellent Majesty in right of the Province of British Columbia. 1973 \ VICTORIA, B.C., February, 1973 To Colonel the Honourable JOHN R. NICHOLSON, P.C., O.B.E., Q.C., LLD., Lieutenant-Governor of the Province of British Columbia. MAY IT PLEASE YOUR HONOUR: Herewith I beg respectfully to submit the Annual Report of the Department of Recreation and Conservation for the year ended December 31, 1972. ROBERT A. WILLIAMS Minister of Recreation and Conservation 1_) VICTORIA, B.C., February, 1973 The Honourable Robert A. Williams, Minister of Recreation and Conservation. SIR: I have the honour to submit the Annual Report of the Department of Recreation and Conservation for the year ended December 31, 1972. LLOYD BROOKS Deputy Minister of Recreation and Conservation CONTENTS PAGE Introduction by the Deputy Minister of Recreation and Conservation_____________ 7 General Administration_________________________________________________ __ ___________ _____ 9 Fish and Wildlife Branch____________ ___________________ ________________________ _____________________ 13 Provincial Parks Branch________ ______________________________________________ -
Delhi Metropark
PARK MAP Park Entrance H udso GPS: 42º23’18.52”N 83º54’12.17”W n Mills M etropa te rk i s S s West HUR e c c River ON RIVER DR Trail to g A n Dexter i CHAMBERLIN RD h s Fi Hur HUR o r n R e Group iv D ON RIVER DR e r elh Camp i n Riv Me o tr r op u ar H Labyrinth k 1 3 2 NOR PARK ENTRANCE TH TERRIT GPS: 42º23’11.88”N 83º54’31.13”W ORIAL RD DEXTER-HURON METROPARK 6535 Huron River Drive, Dexter, MI 48130 (Administered through Hudson Mills Metropark) Rapids View 734-426-8211 • www.metroparks.com Service 23 Area MAP KEY PICNIC SHELTERS Outdoor Sports Small Boat Launch 1 West HUR Restroom Toll Booth 2 Central River Grove ON RIVER DR Oak ROADS AND TRAILS 3 East 2 Meadows Paved Road Paved Hike-Bike Trail Dirt Road Railroad Track Nature Trail FEET 0 250 500 750 1000 MILES 0 ¼ lls Met Y RD Y Mi ropa son rks ud H & on ur H r- W HUR te Activity Center ex E TER PINCKN TER D ON RIVER DR Hur X DE on Riv r 4 ive West er ron R Delhi HUR u H DELHI CT ON RIVER DR DELHI METROPARK 1 3902 East Delhi Road Ann Arbor, MI 48103 HUDSON MILLS (Administered through E DELHI RD Hudson Mills Metropark) East METROPARK 5 734-426-8211 Park Entrance Delhi 8801 North Territorial Road www.metroparks.com GPS: 42º19’55.99”N 83º48’37.65”W Pineview A Dexter, MI 48130 n GREGORY RD MAP KEY n 734-426-8211 A r www.metroparks.com Restrooms b RAILR o H OAD ST r u Small Boat Launch ro MAP KEY n R iv Camping er Boat Rental D Toll Booth Disc Golf e x t e r - Playground Outdoor Sports H u r o n Outdoor Sports & D e Paved Road Playground lh i FLEMMING RD M e Dirt Road Golf t r o p a r Railroad Track Restroom k s Small Boat Launch PICNIC SHELTERS FEET 0 250 500 750 1000 1 North Shelter Toll Booth MILES 0 ¼ Trail-head Waterslide WHITMORE Paved Roads LAKE 23 Dirt Roads N. -
PROGRESS REPORT NUMBER THREE Geology of Arenac County
STATE OF MICHIGAN Standish Structure........................................................14 PROGRESS REPORT NUMBER THREE Chapter - V OIL AND GAS PRODUCTION....................15 Geology of Arenac County Gas Production.............................................................15 by Oil Production...............................................................15 Gordon H. Pringle CONCLUSION.................................................................16 Assistant Petroleum Geologist Geological Survey Division Department of Conservation Plates May, 1937 Plate 1. Surface geology of Arenac County. ...........................2 Plate 2. Areal geology of Arenac County. ...............................3 Plate 3. Subsurface structural contour map of Arenac Contents County............................................................................12 Chapter I - INTRODUCTION............................................ 1 Plate 4. Structural contours drawn on the top of the Berea Formation. ......................................................................13 Chapter II - PHYSIOGRAPHY ......................................... 2 Plate 5. Geological cross-section along Line A-B..................13 Chapter III - AREAL GEOLOGY AND STRATIGRAPHY 3 Plate 6. Composite section along Lake Huron in Section 13, Areal Geology................................................................ 3 T.20N., R.7E. .................................................................14 Pennsylvanian System .................................................. 3 Saginaw -
History of the Lake St. Clair Fisheries Research Station, 1966 - 2003
DEPARTMENT OF NATURAL RESOURCES History of the Lake St. Clair Fisheries Research Station, 1966 - 2003 Mike Thomas, Research Biologist (retired) and Todd Wills, Area Station Manager Email: [email protected] Email: [email protected] The Lake St. Clair Great Lakes Station was constructed on a confined dredge disposal site at the mouth of the Clinton River and opened for business in 1974. In this photo, the Great Lakes Station (red roof) is visible in the background behind the lighter colored Macomb County Sheriff Marine Division Office. Lake St. Clair Fisheries Research Station Website: http://www.michigan.gov/dnr/0,4570,7-153-10364_52259_10951_11304---,00.html FISHERIES DIVISION LSCFRS History - 1 History of the Lake St. Clair Fisheries Research Station, 1966-2003 Preface: the other “old” guys at the station. It is my From 1992 to 2016, it was my privilege to hope that this “report” will be updated serve as a fisheries research biologist at the periodically by Station crew members who Lake St. Clair Fisheries Research Station have an interest in making sure that the (LSCFRS). During my time at the station, I past isn’t forgotten. – Mike Thomas learned that there was a rich history of fisheries research and assessment work The Beginning - 1966-1971: that was largely undocumented by the By 1960, Great Lakes fish populations and standard reports or scientific journal the fisheries they supported had been publications. This history, often referred to decimated by degraded habitat, invasive as “institutional memory”, existed mainly in species, and commercial overfishing. The the memories of station employees, in invasive alewife was overabundant and vessel logs, in old 35mm slides and prints, massive die-offs ruined Michigan beaches. -
Detroit River Group in the Michigan Basin
GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan. -
Suggested Parking and Access Points
Stockbridge Unadilla Putnam Township Township Township Border-to-Border Trail: 36 36 Overview and Phasing Stockbridge Unadilla Putnam STtoocwknbsrhidipge TUonwandsihllaip TPoPuwtinnnsahcmipkney D Township Township Township e Border-to-Border Trail: xt "The Huron River Greenway" Stockbridge n e o r t Border-to-Border Trail: m P s a Ypsilanti - Ann Arbor - Dexter - Lakelands Trail i 36 e Overview and Phasing n g h ke k 36 n La ckn a n o g t rs L Hamburg i Pa t e 36 y Overview and Phasing n v e r I r i 36 e "The Huron Waterloo Loop" Stockbridge Unadilla PPutinnacmkney y wb Township n L a Livingsto Str Township Township ToPwinnshcipkneD y Dexter - Chelsea - Stockbridge - Lakelands Trail Ingham e xt enaw "The Huron River Greenway" Stockbridge SUntaodillca kbridge n Putnam Washt D Border-to-Border Trail: e o Webster e r t Township m Township Township Jackson September 2019 - Prepared By: Washtenaw County Parks xt "The Huron River Greenway" P Stockbridge n s a Township Ypsilanti - Ann Arbor - Dexter - Lakelands Trail e i e o n g h k r t e m k a ckn n L 36 a Overview and Phasing P n o g L s s Hamburg a t r i 36 a t e Ypsilanti - Ann Arbor - Dexter - Lakelands Trail P i y e n n g v h k e r I ke ckn r i La e a "The Huron Waterloo Loop" 36 n y n o g t rs b L THoawmnbsuhrigp i a t e w n L ingsto 36 Pinckney P tra y Liv n v e S r I Pinckney r i e Dex"teTrh - eCh Helsuerao - nSt oWckabrtiedgrel o- oLa kLeolaondps "Trail y wb Township n L ingsto Ingham D a Liv Pinckney Recreation Str Washtenaw e Dexter - Chelsea - Stockbridge - Lakelands Trail D xt -
Lake Erie Metropark
PARK MAP LAKE ERIE 7 mile Hike-Bike Trail Connector METROPARK to Oakwoods 32481 West Jeerson Avenue S GIBRALTAR RD Brownstown, MI 48173 734-379-5020 Bro wn sto reek GOLF COURSE wn C 14786 Lee Road Battle of Brownstown Detroit River Brownstown, MI 48173 Monument 734-379-0048 MARINA WOODRUFF RD Wyman’s Canal 35001 Milleville Road Overlook Brownstown, MI 48173 BOAT, CANOE AND MAP KEY Eagle’s Way Overlook KAYAK LAUNCH Rental Shelter Hawthorn Outer Buoys Sanger’s Lagoon GPS: 42º04’43”N 83º11’27”W Thicket Overlook Restrooms Riley Creek Overlook Boat Softball Diamond House and Dock MARSHLANDS MUSEUM Basketball Court Tennis Court Volleyball Court PARK OFFICE Playground 734-379-5020 W JEFFERSON AVE JEFFERSON W Paved Hike-Bike Trail Lotus Beds PICNIC SHELTERS Toll A American Lotus Park Entrance A GPS: 42º04’14”N 83º12’36”W B Blue Heron Service C Cattail Area Sturgeon Bar B Island D Wood Duck GREAT WAVE AREA Wave Pool, Playground, E Muskrat HURON RIVER DR First Aid, Food Bar, and Sledding Hill C NATURE TRAILS Big Turtle Shortcut - ½ mile PLEASANT DR MCCANN RD Trapper’s Run - 1 mile Shore Fishing Cherry Island Trail - 1¼ miles Boardwalk D STREICHER RD E N COVE POINT PICNIC AREA Driving Range GOLF COURSE 734-379-0048 MARINA OFFICE Marina Point Observation GPS: 42º03’13.06”N 83º12’0.12”W Deck and Fishing Site W JEFFERSON AVE JEFFERSON W 734-379-5020 GPS: 42º03’12.67”N 83º11’33.04”W Service Area LEE RD MARINA Outer Buoys HEIDE RD Ice Fishing GPS: 42º03’12”N 83º11’02”W SOVEY MARLEY AVE ERIE DR MILLEVILLE RD MILLEVILLE Lake Erie H CAMPAU RD A R B I N