Saginaw River/Bay Fish & Wildlife Habitat BUI Removal Documentation
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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. -
DEQ RRD BULLETIN Tittabawassee/Saginaw River
MICHIGAN DEPARTMENT OF ENVIRONMENTAL QUALITY John Engler, Governor • Russell J. Harding, Director INTERNET: www.michigan.gov/deq DEQ ENVIRONMENTAL RESPONSE DIVISION INFORMATION BULLETIN TITTABAWASSEE/SAGINAW RIVER FLOOD PLAIN Environmental Assessment Initiative Midland, Saginaw counties February 2002 INTRODUCTION PHASE I ENVIRONMENTAL ASSESSMENT Flood Plain Soil This is the first in a series of bulletins to inform area communities about progress, future plans, meeting Historical flow data indicates that during the spring dates, and other activities regarding the and fall months it is common for the flow of water Tittabawassee/Saginaw River Flood Plain Dioxin within the Tittabawassee River to increase to a Environmental Assessment Initiative. What follows level that causes the river to expand onto its flood is an overview of the Department of Environmental plain. During these high flow periods it is possible Quality (DEQ) efforts to identify flood plain areas that sediments, and dioxins that have come to be where dioxin and dioxin-related compounds located in the sediments, are transported from the (hereinafter referred to collectively as “dioxin”) river bottom, or other unidentified source areas, could pose public health or environmental concern. and deposited onto the flood plain. Please refer to the accompanying document entitled “Dioxins Fact Sheet” for a more detailed From December 2000 through July 2001, DEQ account of public health and environmental issues Environmental Response Division (ERD) staff associated with dioxin compounds. A map collected soil samples from the Tittabawassee identifying the environmental assessment area is River flood plain at three locations: 1) at property also included. near the headwaters of the Saginaw River, 2) at property located near the end of Arthur Street in As always, DEQ staff is available to help clarify Saginaw Township, and 3) along the northern issues or address concerns you may have on any perimeter of the Shiawassee National Wildlife aspect of the environmental assessment initiative. -
U.S. Fish and Wildlife Service
U.S. Fish and Wildlife Service Alpena FWCO - Detroit River Substation Fisheries Evaluation of the Frankenmuth Rock Ramp in Frankenmuth, MI Final Report - October 2019 U.S. Fish and Wildlife Service Alpena FWCO – Detroit River Substation 9311 Groh Road Grosse Ile, MI 48138 Paige Wigren, Justin Chiotti, Joe Leonardi, and James Boase Suggested Citation: Wigren, P.L., J.A. Chiotti, J.M. Leonardi, and J.C. Boase. 2019. Alpena FWCO – Detroit River Substation Fisheries Evaluation of the Frankenmuth Rock Ramp in Frankenmuth, MI. U.S. Fish and Wildlife Service, Alpena Fish and Wildlife Conservation Office – Waterford Substation, Waterford, MI, 22 pp. On the cover: Staff from the Alpena Fish and Wildlife Conservation Office – Detroit River Substation holding the only northern pike that was recaptured upstream of the rock ramp; a tagged walleye; a small flathead catfish; a net full of tagged fish ready to be released downstream; four tagged white suckers recaptured upstream and boat crew conducting an electrofishing transect. 3 Summary Since the construction of the rock ramp, 17 fish species not previously detected upstream have been captured. These species include eight freshwater drum, eleven walleye, two gizzard shad, eight flathead catfish and two round goby. Over the past three years 2,604 fish have been tagged downstream of the rock ramp. Twenty-nine of these fish were recaptured upstream during boat electrofishing assessments or by anglers. Based on the mean monthly discharge of the Cass River during April and May, the data suggests that white and redhorse suckers can move past the rock ramp during normal discharge years. -
Flint River Flood Mitigation Alternatives Saginaw County, Michigan
Draft Environmental Assessment Flint River Flood Mitigation Alternatives Saginaw County, Michigan Flint River Erosion Control Board FEMA-DR-1346-MI, HMGP Project No. A1346.53 April 2006 U.S. Department of Homeland Security FEMA Region V 536 South Clark Street, Sixth Floor Chicago, IL 60605 This document was prepared by URS Group, Inc. 200 Orchard Ridge Drive, Suite 101 Gaithersburg, MD 20878 Contract No. EMW-2000-CO-0246, Task Order No. 138. Job No. 15292488.00100 TABLE OF CONTENTS List of Acronyms ........................................................................................................................................ iii Section 1 ONE Introduction........................................................................................................................ 1 1.1 Project Authority..........................................................................................1 1.2 Project Location and Setting........................................................................1 1.3 Purpose and Need ........................................................................................2 Section 2 TWO Alternative Analysis .......................................................................................................... 3 2.1 Alternative 1 – No Action Alternative.........................................................3 2.2 Alternative 2 – Dike Reconstruction and Reservoir Construction (Proposed Action) ........................................................................................3 2.2.1 Project Segment -
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. -
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 -
SAGINAW BAY Multiple Stressors Summary Report
NOAA Technical Memorandum GLERL-160 SAGINAW BAY Multiple Stressors Summary Report Craig Stow1 and Tomas Hook2, Editors Project Team: Dmitry Beletsky Michael D. Kaplowitz Raisa Beletsky William Keiper Ashley Burtner Peter J. Lavrentyev James H. Bredin Frank Lupi Joann Cavaletto David F. Millie Yoonkyung Cha Nancy Morehead Carlo De Marchi Thomas F. Nalepa Joseph V. DePinto Tammy J. Newcomb Julianne Dyble Danna Palladino Dave Fanslow Scott D. Peacor Steve Francoeur Steven A. Pothoven Duane Gossiaux Todd Redder Nathan Hawley Michelle Selzer Chansheng He Henry A. Vanderploeg Thomas H. Johengen Ed Verhamme Donna R. Kashian Kim Winslow 1NOAA, Great Lakes Environmental Research Laboratory, Ann Arbor, MI 48108 2Purdue University, W. Lafayette, IN 47907 September 2013 ATMOSPH ND ER A I C C I A N D UNITED STATES NATIONAL OCEANIC AND A M E I C N O I S L T DEPARTMENT OF COMMERCE ATMOSPHERIC ADMINISTRATION A R N A T O I I O T N A N U E .S Penny Pritzker C Kathy Sullivan .D R E E PA M RT OM MENT OF C Secretary Acting, Under Secretary for Oceans & Atmosphere NOAA Administrator NOTICE Mention of a commercial company or product does not constitute an endorsement by the NOAA. Use of information from this publication concerning proprietary products or the tests of such products for publicity or advertising purposes is not authorized. This is GLERL Contribution No. 1684. This publication is available as a PDF file and can be downloaded from GLERL’s web site: www.glerl.noaa.gov. Hard copies can be requested from GLERL Information Services, 4840 S. -
Saginaw Bay Watershed Conservation Partnership
SAGINAW BAY WATERSHED CONSERVATION PARTNERSHIP Regional Conservation Partnership Program Michigan’s Saginaw Bay watershed he Regional Conservation Partnership Program Why Saginaw Bay? (RCPP) is being implemented by the United The Saginaw Bay watershed is the largest in the state of TStates Department of Agriculture (USDA) under Michigan, spanning 5.5 million acres and 22 counties. the 2014 Farm Bill. The RCPP makes $1.2 billion in The ecological health of Saginaw Bay and its tributaries federal funding available over 10 years to address critical is critically important to not only Lake Huron, but the conservation concerns across the country. Already, the entire Great Lakes ecosystem, supporting a diversity of Saginaw Bay Watershed Conservation Partnership, fish, migratory birds and other wildlife. It has the largest co-led by The Nature Conservancy and the Michigan concentration of coastal wetlands in the Lake Huron Agri-Business Association, is earning national attention Basin and serves as Lake Huron’s most important source and is considered by the USDA, U.S. Secretary of for several fish species, including walleye, and is home to Agriculture Tom Vilsack and others as an innovative way some of Michigan’s most productive farmland. With to address water quality resource concerns. The Saginaw agricultural use covering 45 percent of the watershed’s Bay Watershed Conservation Partnership will provide a land area, it is crucial that we understand how to total investment of $20 million, including $8 million in properly manage this land to balance agronomic and direct financial assistance and $12 million in technical environmental needs. assistance, to growers in the watershed to implement conservation practices intended to improve water quality for both people and nature. -
Senate Enrolled Bill
Act No. 353 Public Acts of 1996 Approved by the Governor July 1, 1996 Filed with the Secretary of State July 1, 1996 STATE OF MICHIGAN 88TH LEGISLATURE REGULAR SESSION OF 1996 Introduced by Senators McManus, Gast, Steil, Geake, Rogers, Bennett and Schuette ENROLLED SENATE BILL No. 979 AN ACT to make appropriations for the department of natural resources and the department of environmental quality for the fiscal year ending September 30,1996; to provide for the acquisition of land and development rights; to provide for certain work projects; to provide for the development of public recreation facilities; to provide for the powers and duties of certain state agencies and officials; and to provide for the expenditure of appropriations. The People of the State of Michigan enact: Sec. 1. There is appropriated for the department of natural resources to supplement former appropriations for the fiscal year ending September 30, 1996, the sum of $20,714,100.00 for land acquisition and grants and $5,688,800.00 for public recreation facility development and grants as provided in section 35 of article IX of the state constitution of 1963 and part 19 (natural resources trust fund) of the natural resources and environmental protection act, Act No. 451 of the Public Acts of 1994, being sections 324.1901 to 324.1910 of the Michigan Compiled Laws, from the following funds: For Fiscal Year Ending Sept. 30, 1996 GROSS APPROPRIATIONS............................................................................................................ $ 26,402,900 Appropriated from: Special revenue funds: Michigan natural resources trust fund.............................................................................................. $ 26,402,900 State general fund/general purpose................................................................................................... $ 0 DEPARTMENT OF NATURAL RESOURCES A. -
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. -
Advances in Agricultural Drainage
2 Shiawassee Conservation District Annual Report • Sunday, February 18, 2018 Shiawassee Conservation District Annual Report • Sunday, February 18, 2018 3 Controlled drainage, or drainage water management, Advances in uses a control structure to manage the level of water above the tile line. The control structure is placed close Agricultural Drainage to the outlet and water levels are controlled by adding Drainage has been part of U.S. agriculture since co- or removing “stop logs” or by the use of flow valves. lonial times, but it expanded to a broad scale when A field is typically divided into “drainage management Europeans settled the Midwest. At that time, large zones,” each managed by one control structure. Ideally, proportions of Michigan were swampland unsuited for the field should be flat (generally less than 0.5 percent normal cultivation. Most of the drainage occurred in slope) so that one structure can manage the water table the late 1800s and early 1900s. within 1 to 2 feet for as many acres as possible. If drain- The purpose of drainage is to remove excess water age laterals are installed on the contour, the practice and lower the water table. This creates a well-aerated could be used with greater slopes, but flatter fields re- environment for roots and soil organisms. Drainage al- quire fewer overall structures and allow each structure lows earlier warming of soil in the spring, and earlier to manage a larger area. traffic on fields. Installation of drainage tiles can have Drainage water management can be helpful for keep- a rapid and large return on the capital investment, by ing nutrients in the field by limiting runoff of subsur- substantially improving productivity.