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Public Groundwater Supplies in Carroll County. Bulletin 60, Which Is Divided by County Into Separate Publications, Supersedes Bulletin 40 and Its Supplements 1 and 2
??UL-60(28)/79 ??TIN 60-28 ?? OF ILLINOIS ILLINOIS INSTITUTE OF NATURAL RESOURCES Public Groundwater Supplies in Carroll County by Dorothy M. Woller and Ellis W. Sanderson ILLINOIS STATE WATER SURVEY URBANA 1979 PUBLIC GROUNDWATER SUPPLIES IN CARROLL COUNTY by Dorothy M. Woller and Ellis W. Sanderson Introduction This publication presents all available information on production wells used for public groundwater supplies in Carroll County. Bulletin 60, which is divided by county into separate publications, supersedes Bulletin 40 and its Supplements 1 and 2. The definition of public water supply as contained in the Environmental Protection Act of 1970 was used to determine those water systems and wells to be included. Systems and wells described furnish water for drinking or general domestic use in: 1) incorporated municipalities; 2) unincorporated communities where 10 or more separate lots or prop• erties are being served or are intended to be served; 3) state-owned parks and memorials; and 4) state-owned educational, charitable, or penal institutions. This report includes separate descriptions for groundwater supplies of 7 municipalities and 1 state park in Carroll County. These are preceded by brief summaries of the ground• water geology of the county and the development of groundwater sources for public use. An explanation of the format used in the descriptions is also given. Acknowledgments. This report was prepared under the general direction of Dr. William C. Ackermann, Chief of the Illinois State Water Survey, and Richard J. Schicht, Head of the Hydrology Section. Special thanks are given to R. T. Sasman, Hydrologist, who checked all of the data and reviewed the manuscript. -
Introduction to Geological Process in Illinois Glacial
INTRODUCTION TO GEOLOGICAL PROCESS IN ILLINOIS GLACIAL PROCESSES AND LANDSCAPES GLACIERS A glacier is a flowing mass of ice. This simple definition covers many possibilities. Glaciers are large, but they can range in size from continent covering (like that occupying Antarctica) to barely covering the head of a mountain valley (like those found in the Grand Tetons and Glacier National Park). No glaciers are found in Illinois; however, they had a profound effect shaping our landscape. More on glaciers: http://www.physicalgeography.net/fundamentals/10ad.html Formation and Movement of Glacial Ice When placed under the appropriate conditions of pressure and temperature, ice will flow. In a glacier, this occurs when the ice is at least 20-50 meters (60 to 150 feet) thick. The buildup results from the accumulation of snow over the course of many years and requires that at least some of each winter’s snowfall does not melt over the following summer. The portion of the glacier where there is a net accumulation of ice and snow from year to year is called the zone of accumulation. The normal rate of glacial movement is a few feet per day, although some glaciers can surge at tens of feet per day. The ice moves by flowing and basal slip. Flow occurs through “plastic deformation” in which the solid ice deforms without melting or breaking. Plastic deformation is much like the slow flow of Silly Putty and can only occur when the ice is under pressure from above. The accumulation of meltwater underneath the glacier can act as a lubricant which allows the ice to slide on its base. -
Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H. -
Fiscal Year 2005
THE CENTER FOR STATE POLICY AND LEADERSHIP 2005 ANNUAL REPORT UNIVERSITY of ILLINOIS at SPRINGFIELD THE CENTER FOR STATE POLICY AND LEADERSHIP Our Mission he UIS Center for State Policy and Leadership, T located in the Illinois state capital, emphasizes policy and state governance. The Center identifies and addresses public policy issues at all levels of government, promotes governmental effectiveness, fosters leadership development, engages in citizen education, and contributes to the dialogue on matters of significant public concern. Working in partnership with government, local communities, citizens, and the nonprofit sector, the Center contributes to the core missions of the University of Illinois at Springfield by mobilizing the expertise of its faculty, staff, students, and media units to carry out research and dissemination, professional development and training, civic engagement, technical assistance, and public service activities. Our Vision he UIS Center for State Policy and Leadership T will be an independent and nationally recognized resource for scholars and Illinois policy-makers, opinion leaders, and citizens. The Center will be known for its high-quality, nonpartisan public policy research, innovative leadership and training programs, and timely and thought-provoking educational forums, publications, media productions, and public radio broadcasts. The Center will take an active role in the development of ethical, competent, and engaged students, faculty, staff, and community and government leaders by providing intern, civic engagement, and professional development opportunities, in-person and through the use of multi-media and on-line technologies. Produced by Center Publications/Illinois Issues. Peggy Boyer Long, director; Amy Karhliker, editor; Diana L.C. Nelson, art director. The University of Illinois at Springfield is an affirmative action/equal opportunity institution. -
Indiana Glaciers.PM6
How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago. -
Quarrernary GEOLOGY of MINNESOTA and PARTS of ADJACENT STATES
UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman ,Wilbur, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director P~ofessional Paper 161 . QUArrERNARY GEOLOGY OF MINNESOTA AND PARTS OF ADJACENT STATES BY FRANK LEVERETT WITH CONTRIBUTIONS BY FREDERICK w. SARDE;30N Investigations made in cooperation with the MINNESOTA GEOLOGICAL SURVEY UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1932 ·For sale by the Superintendent of Documents, Washington, D. C. CONTENTS Page Page Abstract ________________________________________ _ 1 Wisconsin red drift-Continued. Introduction _____________________________________ _ 1 Weak moraines, etc.-Continued. Scope of field work ____________________________ _ 1 Beroun moraine _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 47 Earlier reports ________________________________ _ .2 Location__________ _ __ ____ _ _ __ ___ ______ 47 Glacial gathering grounds and ice lobes _________ _ 3 Topography___________________________ 47 Outline of the Pleistocene series of glacial deposits_ 3 Constitution of the drift in relation to rock The oldest or Nebraskan drift ______________ _ 5 outcrops____________________________ 48 Aftonian soil and Nebraskan gumbotiL ______ _ 5 Striae _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 48 Kansan drift _____________________________ _ 5 Ground moraine inside of Beroun moraine_ 48 Yarmouth beds and Kansan gumbotiL ______ _ 5 Mille Lacs morainic system_____________________ 48 Pre-Illinoian loess (Loveland loess) __________ _ 6 Location__________________________________ -
Trip F the PINNACLE HILLS and the MENDON KAME AREA: CONTRASTING MORAINAL DEPOSITS by Robert A
F-1 Trip F THE PINNACLE HILLS AND THE MENDON KAME AREA: CONTRASTING MORAINAL DEPOSITS by Robert A. Sanders Department of Geosciences Monroe Community College INTRODUCTION The Pinnacle Hills, fortunately, were voluminously described with many excellent photographs by Fairchild, (1923). In 1973 the Range still stands as a conspicuous east-west ridge extending from the town of Brighton, at about Hillside Avenue, four miles to the Genesee River at the University of Rochester campus, referred to as Oak Hill. But, for over thirty years the Range was butchered for sand and gravel, which was both a crime and blessing from the geological point of view (plates I-VI). First, it destroyed the original land form shapes which were subsequently covered with man-made structures drawing the shade on its original beauty. Secondly, it allowed study of its structure by a man with a brilliantly analytical mind, Herman L. Fair child. It is an excellent example of morainal deposition at an ice front in a state of dynamic equilibrium, except for minor fluctuations. The Mendon Kame area on the other hand, represents the result of a block of stagnant ice, probably detached and draped over drumlins and drumloidal hills, melting away with tunnels, crevasses, and per foration deposits spilling or squirting their included debris over a more or less square area leaving topographically high kames and esker F-2 segments with many kettles and a large central area of impounded drainage. There appears to be several wave-cut levels at around the + 700 1 Lake Dana level, (Fairchild, 1923). The author in no way pretends to be a Pleistocene expert, but an attempt is made to give a few possible interpretations of the many diverse forms found in the Mendon Kames area. -
4. Results & Analysis
T h e M i d d l e s e x N a t u r a l H e r i t a g e S t u d y on the nature of the soil overlaying the relatively 4. Results & Analysis impermeable clay layer. In general, flat homogeneous areas have experienced the greatest loss of woodlands due to their high agricultural value. This chapter provides a general summary of County trends Kame Moraines, Peat and Muck, Beveled Till Plains and based on the MNHS and LSWS field surveys and on spatial Beaches or Shore Cliffs are uncommon physiographic types analysis of the woodland patches in Middlesex County. in Middlesex, yet a relatively large proportion of these areas are covered in woodlands (Table 4). Peat and Muck soils, which occur on valley bottoms, are too saturated to farm unless drained and are generally used for cash crops. 4.1 WOODLAND PHYSIOGRAPHY Remnant wetlands tend to be irregularly shaped and account for a high proportion of the area in these bottom lands. Table 4 is a comparison between the area of physiographic Woodlands in riparian landscapes tend to be long and types in Middlesex County and the area covered by continuous, but irregularly shaped. The strong relief of woodlands for each physiographic type. Although Kame Moraines, Shore Cliffs and Beveled Till Plains are Undrumlinized Till Plains, Till Moraines and Clay Plains not easy to farm and therefore more of these areas are are common physiographic types in Middlesex County wooded. Sandy soils found in Sand Plains, Spillways and (Table 4), only a relatively small proportion of these areas Kame Moraines are dominated by relatively large forest are covered in woodlands. -
Policy Profile Vol
NORTHERN ILLINOIS UNIVERSITY | CENTER FOR GOVERNMENTAL STUDIES Policy Profile Vol. 20, No. 1 Dixon, Illinois: A Northern Illinois Community Aggressively Preparing for a Rapidly Changing Economic and Cultural Environment Prepared by Danny Langloss and Norman Walzer1 Dixon, Illinois, is a medium size rural What Issues Face Dixon and Other Small Communities? community in northwestern Illinois. With a population of 15,135, it has been, and hopes to Rural communities are being hurt by: continue to be, an active regional hub serving 1. Competition from foreign businesses where as a residence for people who work locally or labor costs are lower; in surrounding communities. To achieve this 2. Relatively poor access to broadband which, in goal, Dixon has used – with considerable success turn, is essential to an information — a planning/development model that other economy; and communities might wish to employ, not only 3. The widening divergence in wage rates to protect themselves from existing and future between urban and rural areas that lures economic and technology changes but, even more secondary school graduates with skills in importantly, to prosper from such changes. advanced technology to larger cities with better employment opportunities, aggravating the The need to do so is critical for many rural difficulties rural employers have in finding communities – especially those located within qualified workers. commuting distance from larger cities. In recent years, small rural communities with economies The challenges for rural communities are relying heavily on agricultural and manufacturing further complicated by indications that mid-size activities have performed less well than larger and larger communities will continue to outperform urban and metropolitan areas where businesses smaller, manufacturing-based communities. -
A Guide to the Geology of the Quincy North Area
557 IL6gui 1980-D uide to the geology of the Quincy North area David L Reinertsen Commemorating the 50th Field Trip Season and the Survey's 75th year. Cross section of one of the larger sinkholes exposed along the west siJe of State Route 336 at Stop 2. Printed by authority of the State of Illinois/1980/500 copies 'L L 'NO | STATE GEOLOGICAL l SURVEY | f 3 3051 00006 8142 , A guide to the geology of the Quincy North area In 1930 the Geological Survey was 25 years old and the new Educational Extension Section was conducting its first field trips. Dr. M. M. Leighton, the Survey's third Chief, had created the section and its program "...to cooperate with the science teachers of the state and furnish them information regarding geology, such as will be helpful in their teaching of earth history and the development of life.' Part of the Section's work was to start a series of six annual "earth history field trips." More than 250 teachers and laymen attended the first year's trips near Dun- dee, La Salle-Starved Rock, Charleston- Mattoon-Eff i ngham , Harri sburg-Shawneetown Quincy, and Rock Island. In its 50 years (except for the war years 1942 to 1945), Ed. Extension has conducted more than 290 field trips. In 1979, 367 people from all walks of life attended the Survey's four field trips. 0m, ~x~w* 4 <#P\* -M* mmm-"* s U / • '« '-^L^<*-^ Teachers on the Quincy field trip, October 4, 1930, assemble in a quarry. Figure 1. -
Attachment J-Historic Trails
ATTACHMENT J: HISTORIC TRAILS Jo Daviess County is littered with remnants of historic trails and roads. The earliest were the result of Native Americans following herds of large game animals. As trade networks and cultural centers developed among early cultures, trails branched out. The Galena area became a hub for some indigenous tribes because of the lead trade. As early as 6,000-7,000 years ago pieces of lead from the Tri-States were being traded throughout the Midwest and beyond. These pieces, traced by chemical analysis at archaeological sites throughout the mid-continent, show an advanced trading network at an early date. Galena (Latin for lead sulfide) was used for charms and for body paint. The first Europeans followed the trails of the native tribes. Waterways provided the most convenient routes for explorers and fur traders. Prairie du Chien was an important fur trading center beginning in the 1600s. The French also became interested in minerals and by 1690 had accessed the Galena Mines by way of the Mississippi and Fever (now Galena) Rivers. Overland routes were also important, particularly when the lead trade came under the control of the American government. The issuance of the first leases for mining were made in 1822, only four years after Illinois became a state. The excitement generated led to the first major mineral rush in U. S. history. The lead region represented the far fringes of the frontier in the 1820s. There was no settlement in northern Illinois, only the southern part, and the only town of note was St. -
Guide to the Geology of the Galena Area
5 (^$UiAA>*>M C 3 Guide to the Geology of the Galena Area Jo Daviess County, Illinois Lafayette County, Wisconsin David L. Reinertsen Field Trip Guidebook 1992B May 16, 1992 Department of Energy and Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY LIBRARY. Cover photos by D. L. Reinertsen Clockwise from upper left: Silurian dolomite cap on Scales Mound, early crevice mine south of Galena near the Mississippi River, and downtown Galena as viewed from the old Galena High School. Geological Science Field Trips The Educational Extension Unit of the Illinois State Geological Survey (ISGS) conducts four free tours each year to acquaint the public with the rocks, mineral resources, and landscapes of various regions of the state and the geological processes that have led to their origin. Each trip is an all-day excursion through one or more Illinois counties. Frequent stops are made to explore interesting phenomena, explain the processes that shape our environment, discuss principles of earth science, and collect rocks and fossils. People of all ages and interests are welcome. The trips are especially helpful to teachers who prepare earth science units. Grade school students are welcome, but each must be accompanied by a parent or guardian. High school science classes should be supervised by at least one adult for each ten students. A list of guidebooks of earlier field trips for planning class tours and private outings may be obtained by contacting the Educational Extension Unit, Illinois State Geological Survey, Natural Resources Building, 615 East Peabody Drive, Champaign, IL 61820. Telephone: (217) 244- 2407 or 333-7372.