The Influence of Rivers on the History of Indiana
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E.3-IDNR Roster of Navigable Waterways in Indiana
APPENDIX E.3 IDNR Roster of Navigable Waterways in Indiana Nonrule Policy Documents NATURAL RESOURCES COMMISSION Information Bulletin #3 July 1, 1992 SUBJECT: Roster of Indiana Waterways Declared Navigable I. NAVIGABILITY Property rights relative to Indiana waterways often are determined by whether the waterway is "navigable". Both common law and statutory law make distinctions founded upon whether a river, stream, embayment, or lake is navigable. A landmark decision in Indiana with respect to determining and applying navigability is State v. Kivett, 228 Ind. 629, 95 N.E.2d 148 (1950). The Indiana Supreme Court stated that the test for determining navigability is whether a waterway: was available and susceptible for navigation according to the general rules of river transportation at the time [1816] Indiana was admitted to the Union. It does not depend on whether it is now navigable. .The true test seems to be the capacity of the stream, rather than the manner or extent of use. And the mere fact that the presence of sandbars or driftwood or stone, or other objects, which at times render the stream unfit for transportation, does not destroy its actual capacity and susceptibility for that use. A modified standard for determining navigability applies to a body of water which is artificial. The test for a man-made reservoir, or a similar waterway which did not exist in 1816, is whether it is navigable in fact. Reed v. United States, 604 F. Supp. 1253 (1984). The court observed in Kivett that "whether the waters within the State under which the lands lie are navigable or non-navigable, is a federal" question and is "determined according to the law and usage recognized and applied in the federal courts, even though" the waterway may not be "capable of use for navigation in interstate or foreign commerce." Federal decisions applied to particular issues of navigability are useful precedents, regardless of whether the decisions originated in Indiana or another state. -
Total Maximum Daily Load (TMDL) for the Wabash River Watershed, Ohio
Appendix E Response to Comments WW-16J Re: Response to Public Comments - Comment Period ending March 27, 2004 Wabash River Watershed Total Maximum Daily Load (TMDL), Ohio Dear Sir/Madam: Thank you for your recent comments regarding the Draft Wabash River Total Maximum Daily Load (TMDL) document dated February 2004. The U.S. EPA has responded to your comments below. We first address the comments related to designated use and then address all remaining comments. In 1999, Ohio EPA completed a thorough examination of habitat and biological and chemical conditions in the Wabash River watershed. Ohio EPA found that Wabash River watershed’s Warmwater Habitat use designation was still appropriate. Consequently, we used the nutrient and sediment targets associated with the Warmwater Habitat use designation in this TMDL.1 Comments from: Ohio Department of Agriculture Comment: Page 23, the first sentence is a repeat of the last sentence at the bottom of page 22. Response: This typo does not exist in the PDF version of the report that was made available on U. S. EPA’s Web page. Comment: Page 23, the footnote "plans" should be "plants" Response: Comment addressed. 1The State expects to propose Water Quality Standards (WQS) rules changes based on the 1999 work study later this year. Their rule-making process includes an opportunity for public comment. The use designations and the 1999 study results for the areas upstream of the state line provide useful information that should be taken into consideration when recommending implementation strategies to restore the watershed. 2 Comment: Page 25, the footnote at the bottom of table 7-1 should be "from " instead of "form" Response: Comment addressed. -
Proceedings of the Indiana Academy of Science 1 15(2):79-81
2006. Proceedings of the Indiana Academy of Science 1 15(2):79-81 THE WABASH RIVER SYMPOSIUM Daryl R. Karns: Rivers Institute and Biology Department, Hanover College. Hanover, Indiana 47243 USA Mark Pyron: Department of Biology, Ball State University, Muncie, Indiana 47306 USA Thomas P. Simon: Division of Fishes, Aquatic Research Center, Indiana Biological Survey, 6440 Fairfax Road, Bloomington, Indiana 47401 USA Important in both the natural and cultural The population of the Wabash River basin, history of the region, the Wabash River is within the State of Indiana, included approx- considered The River of Indiana, and it is the imately 3.56 million people in 2000 (U.S. designated State River. From its origin in the Census Bureau, http://quickfacts.census.gov/ state of Ohio to its junction with the Ohio Riv- qfd/states/ 18000.html). This represents 58.9% er, the Wabash runs 765 km. From the dam in of the entire population of Indiana. The econ- Huntington, Indiana to its terminus at the omy of the basin is primarily agriculture: but River, Ohio the Wabash flows freely for 661 manufacturing is of significant importance. of its total length, the longest stretch of km Land use in the Wabash River is primarily ag- free-flowing river in the United States east of ricultural (66%); however, significant portions the Mississippi River (Fig. 1). Several papers in the southern watershed are comprised of in this issue of the Proceedings of the Indiana forest (15%), and urban land uses (13%) (Pur- Academy of Science are devoted to aspects of due University, http://pasture.ecn.purdue.edu/ the biodiversity, environment, and conserva- —jychoi/wcLhome/). -
Introducing Indiana-Past and Present
IndianaIntroducing PastPastPast ANDPresentPresent A book called a gazetteer was a main source of information about Indiana. Today, the Internet—including the Web site of the State of Indiana— provides a wealth of information. The Indiana Historian A Magazine Exploring Indiana History Physical features Physical features of the land Surficial have been a major factor in the growth and development of Indiana. topography The land of Indiana was affected by glacial ice at least three times Elevation key during the Pleistocene Epoch. The Illinoian glacial ice covered most of below 400 feet Indiana 220,000 years ago. The Wisconsinan glacial ice occurred 400-600 feet between 70,000 and 10,000 years ago. Most ice was gone from the area by 600-800 feet approximately 13,000 years ago, and 800-1000 feet the meltwater had begun the develop- ment of the Great Lakes. 1000-1200 feet The three maps at the top of these two pages provide three ways of above 1200 feet 2 presenting the physical makeup of the land. The chart at the bottom of page lowest point in Indiana, 320 feet 1 3 combines several types of studies to highest point in give an overview of the land and its 2 use and some of the unique and Indiana, 1257 feet unusual aspects of the state’s physical Source: Adapted from Indiana Geological Survey, Surficial To- features and resources. pography, <http:www.indiana. At the bottom of page 2 is a chart edu/~igs/maps/vtopo.html> of “normal” weather statistics. The first organized effort to collect daily weather data in Indiana began in Princeton, Gibson County in approxi- mately 1887. -
Indiana Michigan Power Company State of Indiana
I.U.R.C. NO. 18 ORIGINAL SHEET NO. 1 INDIANA MICHIGAN POWER COMPANY STATE OF INDIANA INDIANA MICHIGAN POWER COMPANY SCHEDULE OF TARIFFS AND TERMS AND CONDITIONS OF SERVICE GOVERNING SALE OF ELECTRICITY IN THE STATE OF INDIANA ISSUED BY EFFECTIVE FOR ELECTRIC SERVICE RENDERED TOBY L. THOMAS ON AND AFTER MARCH 11, 2020 PRESIDENT FORT WAYNE, INDIANA ISSUED UNDER AUTHORITY OF THE INDIANA UTILITY REGULATORY COMMISSION DATED MARCH 11, 2020 IN CAUSE NO. 45235 I.U.R.C. NO. 18 ORIGINAL SHEET NO. 2 INDIANA MICHIGAN POWER COMPANY STATE OF INDIANA LOCALITIES WHERE ELECTRIC SERVICE IS AVAILABLE LOCALITY COUNTY LOCALITY COUNTY Aboite Township Allen Decatur Adams Adams Township Allen Delaware Township Delaware Albany Randolph Dunkirk Jay Albion Noble Blackford Albion Township Noble Duck Creek Township Madison Alexandria Madison Allen Township Noble Eaton Delaware Anderson Township LaPorte Eel River Township Allen Elkhart Elkhart Baugo Township Elkhart Elwood Madison Bear Creek Township Jay Bear Creek Township Adams Fall Creek Township Henry Benton Township Elkhart Fairfield Township DeKalb Berne Adams Fairmount Grant Blountsville Henry Farmland Randolph Blue Creek Township Adams Fort Wayne Allen Boone Township Madison Fowlerton Grant Bryant Jay Franklin Township DeKalb Bryant Township Wells Franklin Township Grant Butler DeKalb Franklin Township Randolph Butler Township DeKalb French Township Adams Cedar Creek Township Allen Galena Township LaPorte Center Township Delaware Gas City Grant Center Township Grant Gaston Delaware Center Township LaPorte Geneva Adams Center Township Marshall German Township St. Joseph Centre Township St. Joseph Grabill Allen Chester Township Wells Grant Township DeKalb Chesterfield Madison Green Township Noble Churubusco Whitley Green Township Randolph Clay Township St. -
Centennial History of Indiana
Livre de Lyon Academic Works of Livre de Lyon Social, Humanity and Administrative Sciences 2019 Centennial History of Indiana Aleck Davis Follow this and additional works at: https://academicworks.livredelyon.com/soc_hum_ad_sci Part of the United States History Commons Recommended Citation Davis, Aleck, "Centennial History of Indiana" (2019). Social, Humanity and Administrative Sciences. 11. https://academicworks.livredelyon.com/soc_hum_ad_sci/11 This Book is brought to you for free and open access by Livre de Lyon, an international publisher specializing in academic books and journals. Browse more titles on Academic Works of Livre de Lyon, hosted on Digital Commons, an Elsevier platform. For more information, please contact [email protected]. This volume is Respectfully Dedicated to the Order of Hoosieroons and its First Grand High Potentate, May they suffer long, silently and patiently, THE AUTHOR. INTRODUCTION A half century ago, there was a crying need for Mrs. Winslow’s Soothing Syrup among the children of Indiana. To day, those of the children of ’66’ who have survived the tak- ing ways of malaria, the White Caps and the automobile, are engaged in the mad rush for wealth and too busy to spend weeks and months poring over, and wading through, the long drawn-out detailed, dry facts of history as here tofore doled out to Indiana readers; hence this little volume. It is designed to take the place of Mother Winslow’s concoction as the crying need of a busy public. This work is not intended to belittle the efforts of such historians as have gone before. They did the best they could. -
Hoosiers and the American Story Chapter 3
3 Pioneers and Politics “At this time was the expression first used ‘Root pig, or die.’ We rooted and lived and father said if we could only make a little and lay it out in land while land was only $1.25 an acre we would be making money fast.” — Andrew TenBrook, 1889 The pioneers who settled in Indiana had to work England states. Southerners tended to settle mostly in hard to feed, house, and clothe their families. Every- southern Indiana; the Mid-Atlantic people in central thing had to be built and made from scratch. They Indiana; the New Englanders in the northern regions. had to do as the pioneer Andrew TenBrook describes There were exceptions. Some New Englanders did above, “Root pig, or die.” This phrase, a common one settle in southern Indiana, for example. during the pioneer period, means one must work hard Pioneers filled up Indiana from south to north or suffer the consequences, and in the Indiana wilder- like a glass of water fills from bottom to top. The ness those consequences could be hunger. Luckily, the southerners came first, making homes along the frontier was a place of abundance, the land was rich, Ohio, Whitewater, and Wabash Rivers. By the 1820s the forests and rivers bountiful, and the pioneers people were moving to central Indiana, by the 1830s to knew how to gather nuts, plants, and fruits from the northern regions. The presence of Indians in the north forest; sow and reap crops; and profit when there and more difficult access delayed settlement there. -
Illinois Indiana
Comparing and Contrasting Illinois and Indiana Name: _________________________ Illinois Located in the Midwestern United States, Illinois is known as the Land of Lincoln because Abraham Lincoln made the state capital, Springfield, his home for many years before he was president. Illinois became America’s 21st state on December 3, 1818. It borders Michigan, Indiana, Iowa, Wisconsin, Missouri, and Kentucky. Its northeast coast borders Lake Michigan, making it one of the Great Lake states as well. Illinois is largely grasslands and prairies. The Mississippi River forms its eastern border and the Ohio River forms its southern border. Chicago is the largest city in Illinois and the third largest city in the entire country. It is nicknamed the “Windy City” because of the harsh winds that form off of Lake Michigan and streak through the city in winter. Chicago’s Sears Tower was once the tallest building in the world. With over 12.5 million people, Illinois is the nation’s sixth largest state by population. Its state bird, the cardinal, is also the state bird of six other states. Indiana Indiana became America’s 19th state on December 11, 1816. It is nicknamed the Hoosier State. The origin of the word “Hoosier” remains unknown, but today it refers to a citizen of Indiana and has been in use since as early as 1833. Indiana is located in the Midwestern United States and borders Michigan, Illinois, Ohio, and Kentucky. Its northwestern coast borders Lake Michigan, thus, making it one of the Great Lakes states as well. The Ohio River forms its southern border between it and Kentucky. -
Unconsolidated Aquifer Systems of Hancock County, Indiana
Unconsolidated Aquifer Systems of Hancock County, Indiana by Glenn E. Grove Division of Water, Resource Assessment Section November 2005 Three unconsolidated aquifer systems have been mapped in Hancock County: the New Castle Till; the White River and Tributaries Outwash Subsystem; and the New Castle Complex. All three systems comprise sediments deposited by, or resulting from, glaciers, glacial meltwaters, and post-glacial precipitation events. Boundaries of these aquifer systems are commonly gradational and individual aquifers may extend across aquifer system boundaries. However, a relatively distinct boundary occurs where the White River Outwash and Tributaries Subsystem abuts the relatively steep valley walls of the Big Blue River. Outside of the valley of the Big Blue River, nearly the entire county has more than 100 feet of unconsolidated materials overlying the bedrock. Unconsolidated deposits are especially thick in the eastern third of the county where the sediments are commonly greater than 200 feet and in places (north of Cumberland) greater than 300 feet thick. However, in the Big Blue River valley there are a few areas where the unconsolidated deposits are less than 50 feet in thickness. Most unconsolidated deposits contain some sand or gravel and only a few dry holes have been reported in Hancock County. All the aquifer systems are typically capable of supplying domestic wells. The New Castle Till Aquifer System and the New Castle Complex Aquifer System are, in most places, capable of producing high-capacity wells. There are areas in the New Castle Complex where sand and gravel deposits are of sufficient thickness and extent to constitute major ground-water resources capable of supplying large municipal, industrial, and irrigation needs. -
Surficial Geologic Map of the Evansville, Indiana, and Henderson, Kentucky, Area
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the U.S. GEOLOGICAL SURVEY SCIENTIFIC INVESTIGATIONS MAP 3069 INDIANA, KENTUCKY, AND ILLINOIS STATE GEOLOGICAL SURVEYS Pamphlet accompanies map 87°45'00" 87°37'30" 87°30'00" 87°22'30" ° ° 38 07'30" 38 07'30" CORRELATION OF MAP UNITS Qel Qlt Qlt Qlt af1 DIACHRONOUS GEOLOGIC-TIME UNITS SURFICIAL DEPOSITS UNITS af1 (EPISODES) Man-made depositsColluvial Alluvial depositsEolian Lacustrine Lacustrine- Outwash deposits deposits deposits deposits outwash transitional af1 af2 af3 deposits af1 Qel Qc Qal Qall Qas Qaf Qafp Qat Hudson Holocene Qlt Qel Qa Qot1o Qot1g 11.5 ka Qes Qltm QltQlot Qotp Qot1 Qel Qot2 Wisconsin Qel Sangamon 127 ka QUATERNARY Qlt af1 Illinois Older Pleistocene alluvial deposits af1 780 ka af1 Qel lower middle upper QTg 1,800 ka 1.8 Ma Qlt Qlt Qel af1 Pliocene TERTIARY af1 5.3 Ma af1 Qlt Qel Qel NOT MAPPED BEDROCK af1 Qlt Desmoinesian and PENNSYLVANIAN Pz Missourian NOT MAPPED Qa af1 af1 DESCRIPTION OF MAP UNITS wood collected from a trench, 14 ft deep, east of Evansville (see location on map, [Note: Munsell color designations of deposits appear in the format “brown (10YR 4/3)”, for UTM coordinates lat 37.99105°N., long 87.47139°W., WGS84 datum, Ron Qa Counts, KGS, written commun., 2008). An age of 33,100±590 radiocarbon years Qa example] SURFICIAL DEPOSITS B.P. (ISGS radiocarbon laboratory no. 3313) was obtained on wood from Indiana Qa Geological Survey auger hole 93-102 (Woodfield, 1998, p. 52), 52 ft deep in Qel Man-made deposits Qa deltaic-lacustrine sediments near Pigeon Creek (see symbol in north-central part of Qlt af1 Artificial fill, engineered (modern)—Unconsolidated silt and fine sand, crushed stone, map area). -
LENAPE VILLAGES of DELAWARE COUNTY By: Chris Flook
LENAPE VILLAGES OF DELAWARE COUNTY By: Chris Flook After the signing of the Treaty of Greenville in 1795, many bands of Lenape (Delaware) Native Americans found themselves without a place to live. During the previous 200 years, the Lenape had been pushed west from their ancestral homelands in what we now call the Hudson and Delaware river valleys first into the Pennsylvania Colony in the mid1700s and then into the Ohio Country around the time of the American Revolution. After the Revolution, many Natives living in what the new American government quickly carved out to be the Northwest Territory, were alarmed of the growing encroachment from white settlers. In response, numerous Native groups across the territory formed the pantribal Western Confederacy in an attempt to block white settlement and to retain Native territory. The Western Confederacy consisted of warriors from approximately forty different tribes, although in many cases, an entire tribe wasn’t involved, demonstrating the complexity and decentralized nature of Native American political alliances at this time. Several war chiefs led the Western Confederacy’s military efforts including the Miami chief Mihšihkinaahkwa (Little Turtle), the Shawnee chief Weyapiersenwah (Blue Jacket), the Ottawa chief Egushawa, and the Lenape chief Buckongahelas. The Western Confederacy delivered a series of stunning victories over American forces in 1790 and 1791 including the defeat of Colonel Hardin’s forces at the Battle of Heller’s Corner on October 19, 1790; Hartshorn’s Defeat on the following day; and the Battle of Pumpkin Fields on October 21. On November 4 1791, the forces of the territorial governor General Arthur St. -
DIRECTORY of FORT WAYNE PHOTOGRAPHERS 1843-1930 by John D
DIRECTORY OF FORT WAYNE PHOTOGRAPHERS 1843-1930 By John D. Beatty Aber, John F. 1875-1876. Photographs. He was born in Indiana about 1851 and was enumerated in Adams County in 1870. He was apparently in business briefly with Elisha Poston and listed his studio at the same address, 44 Calhoun, in 1875-76. He described himself at that time as a “solar photographer.” A subsequent directory lists him in Auburn, but by 1880 he was working as a salesman for a wholesale grocery store in Logansport.1 Allen, James O. 1883-1886. Photographs. He had a studio for a single year at 129 Broadway. After his death the studio was run by his wife, Rose Allen, until 1886.2 Andrews, Dexter Brimmer. 1850; 1864-65. Daguerreotypes and Photographs. He was born at Gorham, Ontario County, New York, on 18 July 1825. In 1850, he worked briefly as a daguerreian, occupying rooms above Mr. Smith’s store at corner of Columbia and Calhoun streets. His studio was later occupied by a Mr. and Mrs. Caldwell. In 1850, Andrews and wife Celestia were enumerated in Washington Township, Allen County. In 1860, he was in Perry Township, working as a millwright. He returned to Fort Wayne briefly and opened a gallery in partnership with Theodore Conklin in 1864-65, located at the west end of Columbia Street, but he apparently left by 1866 when Conklin was in business alone. He died at Huntertown, Indiana, on 12 April 1894.3 Aufrecht, Gustave. 1880-1881. Photographs. Born in Pennsylvania about 1856, he came to Fort Wayne in 1880 and established a studio briefly at 60 Calhoun Street.