1991 House Introduced Bill 4482
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I I I I I I I I I 1 I 1 I I I I I
I I WISCONSIN I A Summary of Cooperative Water Resources Investigations I U.S. Geological Survey and I Wisconsin Department of Natural Resources I I I I 1 I 1 I I I I I I 2000 USGS I science for a changing world I I I I I I I I I I I I I I I I I 1 I I I A SUMMARY OF COOPERATIVE WATER-RESOURCES INVESTIGATIONS U.S. GEOLOGICAL SURVEY Water Resources Division I 8505 Research Way Middleton, Wisconsin 53562 and I WISCONSIN DEPARTMENT OF NATURAL RESOURCES P.O. Box 7921 I Madison, Wisconsin 53707 I I I I I I I I i 2000 i I I I I I I I I I I I I I I I I I 1 I A Summary of Cooperative Water-Resources Investigations « U.S. Geological Survey and Wisconsin Department of Natural Resources .- "V-._.-;; , - 2000 The cooperative program of water-resources investigations between the U.S. Geological Survey and the Wisconsin Department of Natural Resources began as a continuation of cooperative programs with the various State agencies which were merged to form the Wisconsin Department of Natural Resources. These investigations involve various aspects of research, resource evaluations, and water-quantity- and water- quality-monitoring activities. This is a brief summary report of the activities and plans for the cooperative projects during the July 1999 through June 2000 fiscal year. Each project summary includes a brief description of the objectives, approach, and progress during the 2000 fiscal year, and plans for the 2001 fiscal year. -
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. -
Department of Natural Resources
DEPARTMENT OF NATURAL RESOURCES LAW ENFORCEMENT DIVISION SPECIAL LOCAL WATERCRAFT CONTROLS (By authority conferred on the department of natural resources by sections 80113 and 80121 of 1994 PA 451, MCL 324.80113 and MCL 324.80121) Regulation No. 0, General provisions. R 281.700.1 Definitions. Rule 1. The words and phrases defined in Act No. 303 of the Public Acts of 1967, being SS281.1001 to 281.1199 of the Michigan Compiled Laws, have the same meaning when used in the rules prescribing special local watercraft controls, whether such rules were promulgated before or after this rule becomes effective. History: 1979 AC. R 281.700.2 "Airboat" defined. Rule 2. As used in these rules, "airboat" means a vessel or contrivance, other than a conventional seaplane, helicopter, or autogiro, that makes use of motor-powered propeller, air vane, or other aerostatic force to support or propel, or both to support and propel, the vessel on or over the surface of the water. History: 1979 AC. R 281.700.3 High-speed boating and water skiing prohibited; time. Rule 3. (1) On the waters of this state where special local watercraft controls have been established prohibiting high-speed boating and water skiing from 6:30 p.m. to 10:00 a.m. of the following day, the hours shall be 7:30 p.m. to 11:00 a.m. of the following day when and where eastern daylight saving time is in effect. (2) "Daylight saving time" means the advancing of the standard time by 1 hour, commencing at 2 o'clock antemeridian on the second Sunday of March of each year and ending at 2 o'clock antemeridian on the first Sunday of November of each year in conformity with the federal uniform time act of 1966, as amended by the energy policy act of 2005. -
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. -
MAPPING and CHARACTERIZING a RELICT LACUSTRINE DELTA in CENTRAL LOWER MICHIGAN by Christopher B. Connallon a THESIS Submitted T
MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of Geography – Master of Science 2015 ABSTRACT MAPPING AND CHARACTERIZING A RELICT LACUSTRINE DELTA IN CENTRAL LOWER MICHIGAN By Christopher B. Connallon This research focuses on, mapping and characterizing the Chippewa River delta - a sandy, relict delta of Glacial Lake Saginaw in central Lower Michigan. The delta was first identified in a GIS, using digital soil data, as the sandy soils of the delta stand in contrast to the loamier soils of the lake plain. I determined the textural properties of the delta sediment from 142 parent material samples at ≈1.5 m depth. The data were analyzed in a GIS to identify textural trends across the delta. Data from 3276 water well logs across the delta, and from 185 sites within two-storied soils on the delta margin, were used to estimate the thickness of delta sands and to refine the delta's boundary. The delta heads near Mount Pleasant, expanding east, onto the Lake Saginaw plain. It is ≈18 km wide and ≈38 km long and comprised almost entirely of sandy sediment. As expected, delta sands generally thin away from the head, where sediments are ≈4-7m thick. In the eastern, lower portion of the delta, sediments are considerably thinner (≈<1-2m). The texturally coarsest parts of the delta are generally coincident with former shorezones. The thick, upper delta portion is generally coincident with the relict shorelines of Lakes Saginaw and Arkona (≈17.1k to ≈ 16k years BP), whereas most of the thin, distal, lower delta is generally associated with Lake Warren (≈15k years BP). -
Rapid Wetland Assessment for Michigan: Section 1 Biological
RAPID WETLAND ASSESSMENT FOR MICHIGAN SECTION 1: BIOLOGICAL FRAMEWORK Prepared by: Dennis A. Albert, Paul Adamus, David Campbell, John Christy, Joshua G. Cohen, Theadore Cook, Helen Enander, Linda Hardison, Michael A. Kost, Katie Mitchell, Jennifer Sackinger, and Bradford S. Slaughter Of: Michigan Natural Features Inventory Oregon State University, and Adamus Resource Assessment, Inc. For: Michigan Department of Transportation September 2008 Report Number 2008-06 Cover image taken by: D. Albert Table of Contents 1.0 Introduction................................................................................................................................................. 1 2.0 Literature Review........................................................................................................................................ 1 3.0 Field Sampling ............................................................................................................................................ 2 4.0 Plant Community Classification and Distribution Map Development ........................................................ 4 5.0 Quantitative Metrics for Wetland Quality, Function, and Value ................................................................. 5 6.0 Hydrologic Metric - Relationship to Plant Communities and Species ........................................................ 5 7.0 Characteristic Plant Species for Each Wetland Type ................................................................................ 10 8.0 Photos and Diagrams of Plant -
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 -
Great Lakes Region, USA
Spatial variation in till texture and clay mineralogy across the Saginaw Lobe terrain, Great Lakes region, USA Department of Geography, Environment and Spatial Sciences, Randall J. Schaetzl, Chris Baish, Jarrod Knauff, Thomas Bilintoh, East Lansing, Michigan, USA Dan Wanyama, Kevin McKeehan, and Michelle Church Abstract STUDY AREA SAMPLE DISTRIBUTION Great Lakes region We present a spatial/mapping approach to the study of the glacial history of the Saginaw lobe of the Laurentide Ice Sheet. The Saginaw Lobe flowed into southern Michigan, USA, forming modern-day Saginaw Bay and leaving behind a series of small moraines in down- ice locations. Upon its retreat – and likely also during its advance – a large proglacial lake (Glacial Lake Saginaw) formed in the northeastern margins of the “Saginaw terrain”. The Saginaw lobe advanced to the southwest, out of this lake basin and onto thinly mantled, sandstone and shale bedrock. Although the Late Pleistocene deglacial chronology of this lobe has been generally assumed for decades, few numerical ages exist that could help constrain a better defined timeline. Indeed, as luminescence ages slowly emerge for terrain of the Saginaw Lobe and nearby areas, it seems clear that the lobe retreated from the region considerably earlier than is generally assumed, adding to the potential for large areas of ponded water in proglacial settings, all of which are as yet unmapped. In this project, we sampled tills on uplands across the terrain of the Saginaw Lobe, avoiding outwash plains. In all, we obtained 334 samples of calcareous till, by bucket auger. Sample locations were sited generally uniformly across >20,000 km2. -
Ellsworth American COUNTY Dunham’S Hotel
Sbfcntfennmt*. Rsed, of Kllsworth, and Mrs. Annie 'Itjfnrtiacmmis. _ v- LOCAL AFFAIRS. Powers, of Bangor. Mrs. Higgins had friends in Ellsworth who NEW AI1VKUTIM M ENT* THIS WEEK. many regret C. 0. RURRILL & deeply to hear of her death. She visited SON, state assessor**’ notice. here about two *■* I‘s ('omtnissiiiu of fi-h and fisheries—Sealed years ago. ^ 1 proposals. The Mutual Life Insurance Co., of New Hancork lmll— M urrDon ( omeily « «>. m j of m qenekal INSURANCE Robert It H" in. < *<ut *\ culture *»ale- York, *, |Kent, of this city, j AGENTS, I’anook Is a speciafagent, has paid through Mr. Hi him Bank Bldg., ELLSWORTH, ME. Tyler, Fogg A « •»—Municipal bonds. Kent the policy of |15,0CK) on the life of ^ Rockland, My the late W. it. Blaisdell, of Franklin. ARSOL«JT.F*v 'piJRE Rockland Cumin* rc’.al < *•!!* ;<■. WE REPRESENT THE This is one of the largest policies of life \ A '•:iimri)1 '* > in«u1 me v; paid in this vicinity. Makes the food more de'icious and v 'v '. sew Most Kciiiihle Home ami Foreign Coni pan it's. Curtis Novelty < <>— Agent wanted George W. Davis, of Boston, formerly J'■■//> a ih/r V'i/h ! ■■■■■■■BHanannaHDunaniaaBHBaMHManiir^nMnnnnHr «ommJ9 L Safi )J. of this a brother of 10. Davis, t'nvijmt Far othrr focal news see pages •/, .7 and S. city, Henry lias purchased the Tontine house at Miss Mari* *i of Auburndaln, In sums to Hu it on real c.si ate and Morgan, Unitarian noinc. improved Brunswick. The Tontine is a popular re- of the engine had passed over the boy’s Conference at MON KY TO LOAN J is the guest of Miss Mabel —--- collateral.- .. -
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. -
Pere Marquette River System Drains an Area of Approximately 740 Square Miles
5 I. THE WATERSHED AND STUDY AREA A. General Characteristics 1. The Watershed. Located in portions of Lake, Mason, Newaygo and Oceana counties, the Pere Marquette River system drains an area of approximately 740 square miles. Roughly 53 percent of the watershed is in Lake County. The mainstream starts at the confluence of the Middle Branch and Little South Branch, known as the "Forks" and flows in a westerly direction for approximately 67 miles to its mouth at Pere Marquette Lake, just south of the City of Ludington. 2. The Study Area. The area of study included the entire mainstream from its mouth at Pere Marquette Lake, its four major tributaries, the Baldwin River, Little South Branch, Big South Branch and the Middle Branch, as well as the numerous smaller tributaries which make up the system. B. Physiography and Soils The topography of the watershed is rolling to flat. The eastern portion of the basin is characterized by its hilly nature, with the western portion generally being more broad and flat. Like other watersheds in the area, the effects of glaciation are evident. Rolling, hilly moraines, flat outwash plains, kettle and oxbow lakes, eskers, drumlins, and kames can all be found in the watershed. The majority of the watershed is dry sand plains and rolling sandy hills. These well-drained droughty soils make them generally unsuitable for agriculture, and hence, are in pine - scrub oak forests. Poorly drained muck and peat soils are fairly common along the lower portion of the mainstream and the headwaters of the Big South Branch, some of which serve as agricultural drains.