/! I .'■/ ^^^^^U^ c^ Cj!n^a/2M^ HISTORY OF MIAMI COUNTY INDIANA A Narrative Account of Its Historical Progress, Its People and Its Principal Interests Edited by MR. ARTHUR L. BODURTHA ADVISORY EDITORS Mr. H. p. Loveland Mr. James W. Hurst Hon. Chas. A. Cole Mr. Alfred E. Zeiirixg VOLUME I ILLUSTRATED THE LEWIS PUBLISHING COMPANY CHICAGO AND NEW YORK 1914 THE KE'Af YORK PUBLIC LIBRARY ^, LENOX AND N rOUNDATlONE 1319 L PREFACE Eighty years liave passed since Miami county was organized under the provisions of an a^t of the Indiana legislature. To note accurately and make a record of the principal events of those eighty years is the purpose of this work. Although this history ni;iy luit iill the proverbial •'long felt want,"' the editor and publisluMs desire to state that no effort has been spared to make it both authentic and comprehensive. The division of the subject matter into topics and the arrangement of chapters is, we believe, the best that could be made and will prove of great convenience to the reader. The chapter on the City of Peru was written under the immediate supervision of Hon. Charles A. Cole, i whose long residence in the city and close identification with municipal .,^, ati'airs render him peculiarly qualified for tlie task. In the preparation ' of the chapter on the Bench and Bar acknowledgement is due to li. P. T .\I issionaries — The Catholics — Methodists — Presbyterians — ]5ai'Tists — German Baptists or Dunkards — Christians or Dis- ciples — New Lights — United Brethren — Friends or Quakers — Episcopal Church — Lutherans — Congregationalists — Seventh Day Adventists — The Church of God — Universalists — Brief Histories of the Various Congregations and Theik Houses of Worship 344 CHAPTER XVIII CHARITIES AND CEMETERIES Overseers of the Poor in Early Days — -Custom of Farming Out Paupers — Its Disadvantages — Miami County's First Poor House — Present County Asylum — Old Folks' and Orphan Children's Home — Dukes iMbmorial Hospital — Wabash Railway Hospital X CONTENTS — Country Graveyards by Townships — Odd Fellows' Cemetery AT Macy — Mount Hope Cemetery at Peru 370 CHAPTER XIX MISCELLANEOUS HISTORY First Flag in JIiami County — Lawlessness — A Vigilance Committee — Petition to President Polk — Early Prices and "Wages — The Stranger's CtRavb — Trading Wives — Queer Real Estate — Some Prominent People — Political Meetings — Temperance — Disas- trous Fires — A Stormy Summer — Historic Floods 3S3 CHAPTER XX SOCIETIES AND FRATERNITIES Agricultural Societies and Fair Associations — Social and Literary Clubs — Miscellaneous Societies — Detective Association — Amboy Civic and Industrial Club — -Masonic Fraternity — Independent Order op Odd Fellows — Knights of Pythias — Grand Army of the Republic — Benevolent and Protective Order of Elks — Im- proved Order op Red Men — Otheb Fraternal Orders — CatSolic Societies — Daughters of the Revollttion — Young Men's Chris- tian Association .- 409 CHAPTER XXI STATISTICAL REVIEW Increase in Population and We^vlth — Chronology — Events Le.\d- ing up to the Organization of and Connected with the History' of the County — Official Roster — A Complete List of County Officers from 1834 to 1914 429 INDEX Aaron, Jacob, 7'-iii Aaron X. Dukes Memorial Hospital. 374 Aboriginal inhabitants, 15 Agrii'iiltiire, 272 Af;ricultural societies ami fair ass(icia tions, 409 Alspacli, Abner J., 697 Altnian, Snnford 10., 459 Allen Township, location, 110; area, 110; first actual white settler, 110; first entry of land, 111; organized. 111; first white child born, 112; first school in, 112; schools, 112; earliest indus- tries, 112; first churches, 112; ceme- teries, 376 Aniboy, ISO Amboy Bank, 271 Amboy Gas and Oil Company, 2S0 Ancient Order of Hibernians, 420 ^ Andrews, Claude Y., 50;i Andrews, Ellis H., 524 An extraordinary "swap," 391 Anson, ISl Area of the county, 1 Arniitagc, .John t', 582 Associate .iudges, 320, 323 Atkinson, Hattie I., 751 Atkinson, Orie C, 751 Augur, William 11., .522 Bailey, Walter C, 549 Bair, George, 591 Bair, .lames S., 591 Baker, Lewis, 49S Baldwin, Charles P., 728 Baldwin. .John A., 724 Baldwin, Verne E., 720 Balsbaugh, Walter, 681 Banking institutions, 268 Bappert, Michael, 489 Baptists, 355 Battleground Memorial Association, 84 Battle of the Mississinewa, 82 Battle of Tippecanoe, 81 Bar Association, 328 Bargerhnflf, Benjiimin F., 777 Barnhisel, Noah B., 694 Barron. John C, 742 Bear storv, 95 Bearss, A'lbert C, 512 Bearss, D.aniel R., 158, 511 Bearss, Frank W., 519 Bench and bar, 310 Benevolent and Protective Order of lOlks, 424 Bennett 's Switch, 181 Eerger, Aaron S., 788 Berger, Henry, 787 Betzner, Anna M. K.. 574 Bet7ner Brothers, 526 Betzner, Louis F., 526 Betzner, Louis, 72S "Big Reserve," 121, 386 Binkerd, .James P.. 624 Birmingham, 181 Black. Charles H., 016 Blackburn, Daniel F., 723 Blair, James, 463 Blair, James J„ 802' Blair, Lvdia M., 404 Bodurtha, Arthur L.. 104. 830 Bond Family. 651 Bond, Charles, 068 Bond, lona, 6.53 Bond, .Jesse, 667 Bond, Walter S., 653 Bonded delit of the county, 267 Boone, .John, 678 Boone. William G., 400 Booth. John, 800 Bouslog, Rawley H., 815 Bowlanil, T)avid A., 680 Bread line, showing work of the .Vsso- eiated Charities at time of great flood in March. 1913 (view), 373 Broadway in the sixties (view), 104 Brower, Isaiah C. 609 Brownell, 182 Brownell, Charles H.. 469 Hundy, Wni. F., 717 Munker Hill, 142, 182 Hunker Hill Light Guards, 238 Burke, Michael, 5S4 Husaco, 184 Musby, Thomas M., 784 XI INDEX Butlev Township, loi-atioii, 11."; pic- turesque scenery, 114; first white man, 115; first settlers, 115; early indus- tries. 116; first white child liorn in, 117; organized, 117; first school, 117; schools, 117; railroads, 118; cemeteries, 377 Butler, Frank C, 555 Butt, Douglas M., 514 Butt, Elias, 472 Butt, Heury K., 692 Butt, Samuel W., 691 Canal era, 242 Capital, 85 Carl. Omer l'., 657 Carter, Charles, 718 Carter, Phineas B., 749 Cary, 184 Casper, Jacob, 619 Catholics, 344 Catholic societies, 426 Cemeteries, 376 Chamberlain, George R.. 506 Charities, 370 Charters, Charles M., 532 Charters. David, 531 Charters, Samuel M., 532 Charters. William J., 531 Chesapeake & Ohio Railroad, 118, 128, 131, 139, 151, 258 Chicago, Indiana & Kastern Railroad, 258" Chili, 145, 184 ' ' Chipanue War, ' ' 205 Christians or Disciples, 360 Christian Scientists, 369 Chronology, 430 Church history, 344 Church of God, 368 Church of the Brethren. 358 Circuit judges, 322 Citizens' Bank of Macy. 271 Citizens Gas and Pi].e Line ('iinii)an\, 280 Citi7ens' National Bank of Pern. 269 City of Peru, 153 City Park, 172 Civil War, 206 Clark, Eugene M., 634 Clark, Gen. George Rogers, 71 Clay Township, location, 118; last in the county to be settled, 118; first white man, 118; settlers, 118; first election, 119; early industries. 119; first school, 120; schools, 120; railroads, 120 Cleland, A. P., 740 "Cliffs," 114 Cole, Albert, 159, 774 Cole, Charles A., 827 Cole, James O., 775 Cole, Richard H.. 797 Concrete bridge over Wabash River, Peru (view), 268 Condo, Daniel W., 559 Conflicting claims of English and French, 70 Congregationalists, 367 Congressional school fund. 292 Conn, Milo P., 658 Conner, Joseph R., 750 Conradt, Godlove, 487 Converse, 185 Cory, Charles E., 787 Costin, Jlichael P., 570 Coucher. James M., 690 Country doctor, 332 County line wedding, 130 County poor asylum, 370 County seat, 153 County seminaries, 294 County superintendents, 297 Courter, 188 Courthouse. 100 Courthouse fire, 313 Court of Common Pleas, 321 Courts, 310 Cox. Jabe?. T., 813 Craig, Jasper J., 693 Creeks, 2 Crop statistics, 273 Crouder, William F., 040 Crnme. Pliny M., 524 Cunningham, Jacob A., 622 • Daughters of the Revolution, 427 Davis. John C 507 Davis, John H., 770 Davis, John W., 733 Davis, Wm. Edward, 767 Deedsville, 14S. 188 Deer Creek Township, location, 121; earliest settlers, 121 ; early industries, 122; first school in, 123; schools, 123; railroads, 123; first churches, 123; cemeteries, 377 Denuith, William, 739 Denver, 188 Denver College, 296 DeWald, John L., 761 Dice, John H., 649 Dingman, Peter, 476 Disastrous fires, 395 Distribution of school funds, 297 Dnan, Alva, 721 Douglass, Milton, 808 Douglass, Seymour A., 809 Doyle, 189 Drainage, 2lil Dukes. Aaron N., 494 Dukes, Elberf J., 495 Dunkards, 358 Dunn. Timotliy E., 578 INDEX Eagle, Ilpiiry A., 566 Earliest niaiuifai'tories in Miami County, 275 Early atturneys, 324 Early explorers, 86 Early exiilorations in the New World, 67 Early militia system, 204 Early prices and wages, 389 Farly trailiers, 293 EdMcatioiial development, 291 Edwards, Kicliard A., 563 Eel River Ifoad, 257 ElliLger, R. P., 328 Eighth Infantry, 210 Eitliith jtidieial district, 311 Eighty seventh Infantry, 221 Eikenlierry. B. F., 544 Eikenlierry, George, 613 Fikenberry, Levi I., 613 Eikenlierry, William M., 804 Elp'trie lighting plant. 170 Electric lines, 261 Eleventh Infantrv, 210 Ellis, E. A., 707 Engel, Henry, 593 Episcopal Chtirch, 364 Erie Township, location, 123; smallest in county, 123: area, 123; settlers, 124; early industries, 125; churches, 125: railroads. 125; schools, 125; cemeteries, 378 Estimated value of all the school property in the county, 296 Everts, Gustavus, 311 Falk, .Fulius, 539 Falk, Mos.s, 538 Farmers' State Bank of Bunker Hill, 271 Farmers' Bank of Converse, 271 Farmers ' Bank of Denver, 272 Father liarlin, 344 Father Rivet. 291 Faust, Joseph A., 520 Fidler, .lohn H., 470 Fifth street looking east from Broadway, boats landing on courthouse lawn (view), 403 Fifty-first Infantry, 219 Finance and industry, 267 Fires, 395 Fire Department of Peru, 166 First county .iail, 106 First courts. 312 First election for county ofTicers, 100 First exclusive high school luiilding, 296 First flag in Miami County, 383 First gas well, 12 First great flood of Miami County, 399 First highways, 241 First .jurors, 99 First missionaries, 344 First National Bank of Peru, 268 Fiist physician in Miami County, 333 I'iist printing press in Miami County, 299 First railroad in the United States, 253 First regular school, 291 First session of the circuit court, 311 First settlers, 88 I'irst telejihone exchange, 279 First train to arrive at Peru, 259 Fisher Family, 599 Fisher, Frank, 590 Fisher, Henry, 600 Fisher, Isaac, G53 Fisher, Joseph, 597 Fisher, Otto L., 462 Fisher, Peter, 599 Fife, Charles F., 603 Five Corners. 190 Floods, 399 Florence, 190 Foote, Carter, 520 Foote, Charles, 520 Foote. Jesse, 520 Formation of the first two civil town- ships, 109 ' ' I'ort Wayne, ' ' 76 Fort Wayne & Northern Indiana Traction Company, 139, 262 Fortieth Infantry, 218 Forty-sixth Infantry, 219 Founder of the City of Peru, 156 Fourteenth Battery, 232 Fraternal Order of Eagles, 425 Fraternities, 416 French and Indian War, 70 French claims, 67 Friends or Quakers, 363 Frontier doctor, 331 Fulwiler, James B., 159, 441 Fulwiler, Louis B., 442 Funeral oration over Francis Godfrey, 36 Gahs, Charles V., 771 Gallahan, Albert Q., 581 Gallahan, Schu.vler W., 820 Garritson, Margaret, 738 Garritson, Read S., 738 Gas works, 169 Geology of county, 3 German Baptists or Dunkards, 358 German Evangelical Association, 366 Germann, Gustave A., 454 Gerhart, Frederick, 713 Gilead, 138, 190 Ginney, Timothy M.. 669 Glassburn, Alfred, 704 Godfrov, Francis. 33, 36, 164 Godfro'y, Gabriel, 39 Godfroy, Gabriel (portrait), 39 Godfrov, Jacques. 33 Graft Familv. 614 Graft. Lerov. 615 Graham. John A., 299, 828 XIV INDEX Graham, Ira, 673 Grand Army of the Republic, 423 Grandview, 191 Graves, Clement, 778 Great flood of March, 1913, 401 Green, Burton, 748 Grimes. Harrison, 551 Grimes, Louise il., 552 Grimes, William. 551 Griswold, Edward H.. 548 Guendling, John H., 553 Gnstin, William H.. 6.S2 Gwinn, Elmer E., 581 Gysin, J. Frank. 490 Haag, Charles C, 776 Haas, Homer C, 547 Hacklev. Frederick S., 796 Hackle'y, Lavant E., 796 Hall, Clarence N., 544 Hall, Hal L., 812 Hall, Joseph, 803 _ _ Harmar, General, 76 Harris, Charles C, 760 jlarrison, Benton. 586 Harrison, Reuben C, 586 Harrison. General William H., 77 Harrison Township, location, 126; set- tlers, 126; organized, 127; first churches, 127; early industries, 127: first school, 127; schools, 127; rail- roads, 128; cemeteries, 378 Harter, Daniel, 523 Harter, Delliert D.. 523 Hattery, James E., 762 Helm, Charles J., 484 Helm, John H., 483 Henton, Dr. Benjamin, 333 Hensler, Moses D., 771 Herrell. Absalom, 765 Herrell, Beeeher, 641 Hiner, John, 479 Hiner, John M.. 479 Historic floods. 399 Hite. John C, 496 Hockman, Solomon, 644 Hoffman, Lorenzo. 792 Holman, Joseph, 153 Holman, Omer. 827 Holman Purchase, 153 Home Toleiihone Company, 282 Hood, John T., 596 Hood, Martha A., 597 Hood, William N., 156, 826 Hoover, Newton, 641 Hooversburg. 191 Horan, Michael, 445 "Hospital Hill," 375 Hostetler. Frank, 783 Howes. John Q. A., 659 Hughes. Charles R., 561 Hurst. Hurd J., 504 Hurst. James W., 826 hidings. Richanl S.. 665 Improved Order of Red Men, 425 Improvement and Park Association, 17"J Increase in population, 429 Increase in wealth, 430 Independent Order of Foresters, 426 Independent Order of Odd Fellows, 419 Indians. 20 Indian chiefs. 28 Indian traders. 86 Indian treaties, 41 Indian villages, 23, 25 Indiana admitteil to Union, 85 "Indiana Ap]iian Way,"' 249 Indiana Legion. 234 Indiana Manufacturing Company, 277 Indiana medical registration law. 342 Indiana National Guard. 238 Indiana Union Traction Company. 139, 142 Indinnapolis, 85 Indianapolis Northern Traction Com- pany, 262 Indianajiolis. Peru & Chicago Railroad, 255 Industries outside Peru. 288 Internal improvements, 241 Irwin, David, 580 Irwin. David & Co., 580 Isler, Frank F., 637 Itinerant Methodist ministers, 346 Jackson. Marshall. 656 Jackson Township, location, 128; area, 128; settlers. 129; organized, 129; first election, 130; county line wedding, 130; churches. 130; schools, 131; rail- roads, 131; cemeteries, 378 Jefl'erson Township, established. 132; area, 132; location, 132; first to be settled by white men, 132; settlers, 132; early industries. 133; first death, 134; first regular school house, 134; schools. 134; railroads. 135; first churches, 135; cemeteries, 378 Jenkins, Benjamin F., 677 Judges, 311 Kagv. Vites E., 535 Kalbfleisch, A. H.. 530 Kendall, Alvin, 805 Kepner. Amos A., 716 Kercher, Charles H., 683 Kessler, Ira A., 745 Keyes, Isaac, 568 Keves, Thomas, 568 Keyes, Thomas A.. 568 King. Daniel. 560 King. Noah W.. 810 Knauff, Henry, 760 Knights of Columbus. 426 Knights of the Maccabees. 426 Knights of Pythias, 422 INDEX XV KiHJX, .I(jlin. "Ill Kottennaii, Tiuiiiaii, 759 Kraiis, Miltou, S13 KriMitzer, John J.. 446 Kurt?, Andrew J., 7.'il Ladies of the Maccabees, 4l'() La Fontaine, Francis, 32 Lake Krie & Westarn Railroad, 123, 135, 139, 142, 148, 254 Landrnin, Caswell 11., 710 Larimer. James, S06 Lavengood, Jacob S., 675 Lawyers, 323 Laving cornerstone of new courthouse, iOo Leedv, George E., 747 Leouda, 192 Lewis, Henry, 607 Licensed physicians of Miami County, 342 Litigation regarding new courthouse, 102 Little Turtle, 28, 78 List of county officers, 433 List of old-time doctors, 340 Liston, Dr. James T., 333 Live stock, 274 Location, 1 Location of seat of .iustice, 98 Lockridge, Brenton W., 583 T-ockridge, Earle B., 5S4 Lockwood, George Browning, 306 Long. Abigail, 567 Long, Charles M., 566 Long, Charles W., 606 Long, .lames A., 662 Long, Michael F., 485 Long, William H., 654 Loree, 192 Loveland, Ebenezer P.. 450 Loveland, Hood P., 452 Loveland, Tfobert J., 453 Loyal Order of Moose, 426 Lucas, William L., 676 Lutheran parochial school 298 Lutherans, 365 Lutz, William C, 763 Lynch, Otho R., 795 Macy, 113, 193 Macy Fair Association, 410 Macv, Oliver H. P., 129 Malott. Richard, 674 Malsbury, Laughlin O'N., 602 Jfanufacturing, 275 Manufacturing statistics of Peru, 2S4 Masonic Fraternity, 416 Maus Family, 612 Mans, .losiah, 613 Mayors of Peru, 177 McCaffrev, Hugh, 817 McCarthy, John S., 540 McCaitliV, Jud R., 504 Mi-Conuell, Clarke 11., 647 ilcCoimell Family, 647 McConnell, William E., 648 Mcllanicls, William, 807 MrKlhenv. Kranklin K., 468 McLirawsville, 12S, 192 McGregor, William A., 162 McKillip, David, 757 Meilical jirofession, 331 ^lelcher. Solomon A., 577 Meiinonites, 35!) Mercer, William S., 305 Methodists, 345 Mexico. 194 Mexico and Denver Railroad, 135 Miamis, 20 Miami, 195 Miami chiefs, 28 Miami Club, 415 Miami County Agricultural Association, 411 Miami County Agricultural Society, 409 Miami County Bank, 271 Miami County Bar Association, 328 Miami County Courthouse (view), 101 Miami County Driving Park and Agri- cultural Society, 410 .Miami County Jail (view), 107 Miami County Medical Society, 341 "Miami County Sentinel." 299 Miami County Workingmen's Institute. 306 Mianiisport, 15.'i Miller, Edward H., 493 Miller, Edward L., 819 Miller Family, 491 Miller, George C, 473 Miller, G. Lee. 486 :\riller, J, H., 536 Miller, James T., 491 Miller, John. 274 Miller, John C, 460 Miller, John L., 703 Miller, John W., 492 Miller, Joseph E., 595 Miller. Levi, .536 Miller, Philij), 605 Miller, Robert, 460 Miller, W. P., 822 Mills, Eugene. 742 Mills. Josejih S., 648 Militia companies, 238 Military history, 204 Minute men, 224 Mitchell, Elmer E., 576 Miscellaneous enlistments, 233 Miscellaneous facts regarding Peru, 177 Miscellaneous history, 383 Miscellaneous societies, 415 Missionaries, 86 Mississinewa battle ground as a nation.il park, 83 XVl INDEX Mississinewa river, 2, 114 Model court houses, 106 Monday Xight Literary Club. 413 Mound Builders, 15 ilouuds of the United States, 17 Mowlray. William E., 328. 780 Muniaugh, Jesse, 645 Murden, George L., 589 !Murden. Jesse L., 589 iS'ash, Benoma. 517 Nash, Jessie F., 518 iSational Tile Company, 147 Natural gas era, 7, 145, 279 Natural gas of the county, 11 Nead. 196 Nelp. Louis, 515 Nelson, Susan, killing of, 317 Newell, Jay W., 682 New court house, 101 New jail, 106 New Light Christians, 243 New Lights, 361 Newman FamUy. 532 Newman, Medford Kyle, 533 Newman, Samuel Irvin, 601 Newspapers, 182 Niconza, 196 Ninth street bridge, Anderson, flood of 1913 (view), 331 Nineteenth Infantry, 291 Ninetieth Infantry^ 222 Ninety-ninth Infantry, 222 North Anderson Driving Park Associa- tion. 262 North Broadway, Peru, March 25, 1913. Elks home on the right. Masonic tem- ple behind street car (view), 401 North Grove, 128, 197 Northwest Territory, 29 Northwest Territory divided. 30 Nyberg Automobile Works. 150 Oakdale, 166 Oakdale Improvement Compauv, 166, 283 Official roster, 433 Oil field, 285 Oil first struck, 286 Oldest banking house in Miami county, 268 Old court house (view), 104 ' ' Old Folks ' and Orphan Children 's Home," 372 Old Holman residence (view), 155 Old tow-path on the Wabash & Erie Canal (view), 247 Old Sentinel office, southwest corner of Main and Broadway, 1867 (view). 300 Old Settlers ' Afsociations, 411 "Old Squirrelly." 140 Old Strawtown road, 241 On the Eel River near Chili (view), 252 One Hundred Days' Men, 228 One Hundred and Ninth Infantry, 224 One Hundred and Twenty-seventh In- fantry, 226 One hundred and Twenty-eighth In- fantry, 227 One Hundred and Thirtieth Infantry, 228 One Hundred and Thirty-fourth Infantry, 228 One Hundred and Thirty-eighth In- fantry, 228 One Hundred and Thirty-ninth Infantry, 229 One Hundred and Forty-second Infantry, 229 One Hundred and Fiftv-first Infantrv, 230 One Hundred and Fifty-fifth Infantry. 231 Order of the World, 426 Organization of county, 96 Other newspapers, 304 Overman. Thomas C, 709 Panhandle Railroad 120. 128, 131. 142, 256 Parent-Teacher Club, 414 Parkhurst, John W., 527 Passage. Dr. Henry V., 334 Pathfinders, 426 Patten, John C, 685 Patten. Lucinda, 685 Paw Paw, 197 Pennsylvania Lines, 256 People's Oil and Gas Company, 13 Peoria. 118, 198 Perry Township, location, 135; area, 135; settler. 136; early births and deaths, 137; early industries, 138; first churches, 138; first school house, 138; schools, 138; railroads, 138; cemeteries, 379 Perrysburg, 198 Peru Township, location, 138; organized, 139; area, 139; railroads, 139; first school, 139; schools, 139; cemeteries. 379 Peru, county seat, 153 ; early settlers, 154; founder of, 156; pioneers, 156: laid out. 157; named, 160; first build- ing on original plat, 160; incorporated as a town, 160; first town election. 162; first mayor, 162; .early town records, 162; incorporated as a city, 163; addition to, 164; fire depart- ment. 166; first paid fire depart- ment, 167; water works, 167; gas works, 169; first electric lights. 170; parks, 172; municipal im]>roven'ents, 173; postoffice, 174; finances, 175; police force. 177; public school build- INDEX xvii ings, 177; population, 177; mayors, 177; miscellaneous facts regarding. 177; first train to arrive in, 2n9; banks, 268; first foundry in, 27o ; manufactories, 275; railroad shops. 275; first telephone exchange. 279; natural gas companies, 280; manufac- turing statistics. 284; first oil wells. 28fi; schools, 295; newspapers, 299; pul'lic library, .SOG; clubs, 412 Peru & Detroit Railroad, 257 Peru A: Iniliana|)olis Kailroad Company. 254 Peru Associated Charities, 372 Peru Basket Factory, 278 "Peru Blues." 204" Peru Canning Company, 282 Pern Chatau<|ua Literary and Scientific Circle, 412 Peru Choral I'nion. 415 Peru Collegiate Institute, 295 Peru Commercial Club, 171. 284 Peru Country Club. 414 Pern Daily Chronicle. SO.'? Peru Drama League. 413 Peru Driving Park and Fair Associa- tion, 410 Peru Evening Journal. .302 Peru Forester, 299 Peru Gazette, 299 Peru Gazette-Peru Democrat. 299 Peru Gravs, 238 Peru Herald, 299 Peru High School (view), 29M Peru Light and Power Company, 17(1 Peru Literary Club, 413 Peru Lyceum", 306, 409 Pern Morning Journal, 303 Peru Mothers' Club. 414 Peru Musical Association, 415 Peru Natural Gas and Fuel Company, 12, 279 Peru Observer. 299 Peru Public Library (view), 307 Peru Ke.iding Club." 412 Peru Repubb.an, 302 Peru Trust Comnany, 269 Peru Woolen Mills. 275 Peru Y. M. C. A. (view), 428 Peters. John B., 753 Petition to the president, 386 Pettysville. 198 Phel'ps. Albert J., 695 Phelps. Caroline C. 701 Phelps. Frank C, 611 Phel|)s. George B.. 764 Phelps. Hal C, 5.34 Phelps, Thomas W., 701 I'hilapv, .lohn B., 576 Phillcliaum, William L.. 448 Philomathean Chautauqua Circle. 415 Physical features, 1 I'hysicians, 331 Pierceburg, 199 "Pillared Rocks," 4, 114 Pioneer amusements, 94 Pioneer life and customs. 89 Pioneer school house, 292 Pipe Creek Township, location, 139; area, 139; first white settlers, 140; early industries, 141 ; first churches, 141; first school, 141; schools, 142; railroads, 142; cemeteries, 381 Place, Willard B.. (>m Plotner. Harlen E., 663 Political meetings, 393 Pontiae, 70 Pontine 's war, 71 Population, 429 Po]nilation of Peru, 177 Portraits, Gabriel Godfrey, 40 PostoHice, Peru, 174 Postoflices in Miami county, 203 Pottawatoniis, 24 Presbyterians, 352 Press," the, 298 Probate court, 321 Progressive Brethren, 358 Prominent law cases, 329 Prosecuting attorneys, 323 I'ublie buildings, 100 Public finances, 267 Public libraries, 306 Puterbaugh, Eli, 573 Puterbaugh, Moses, 573 Queer real estate, 392 Quinn, Robert H., 734 Baber, Samuel, 587 Raber, Solomon D., 587 Railroad era, 253 Ramsey, Albion S., 655 Ray burn. James W., 769 Ream, Fdward B., 516 Ream. Fred S., 516 Reasoner, Ethan T., 818 Regular Array and Navy, 239 Report of the state bureau of inspection, 285 Resler, Joseph L., 768 Reyburn, William M., 823 Reynolds, George W., 466 Reynolds, Mary A., 466 Rhein, William L., 618 Rhodes. David E., 575 Rhodes. Thomas J., .594 Richardville. Jean Baptiste, 23, 29, 153 Richer, John, 628 Richer. Joseph, 629 Richland Township, location, 142; area, 142; first actual .settler, 143; settlers, 143; early industries, 143; first churches, 144; first school house, 144; XVIU INDEX schools, 145; railroads, 145; ceme- teries, 381 Riiienour, David, 569 Kidenour David C, 570 Ridgeview, 199 Rivers, 1 River navigation, 242 Roberts, Frederick M., 661 Robins, Ezekiel V., 758 Roll of honor, 234 Rose, Henry, 670 Roval Arcanum, 426 Rimnells' mill, 122 Rutherford, Dr. C. F., 334 Runyan, Britton L., 478 Runyan, Richard B., 478 St. Charles Catholic school, 298 St. Clair, General Arthur, 76 Saudifur, Noah A., 699 Santa Fe, 118, 199 Scene on the Mississinewa (view), 114 Schedule of treaty grants, 47 Scheriuerhorn, Mrs. E. L., 63 See. Sylvanus, 744 Seidner, Alvin, 754 Seitner. Ira, 684 Seitner, Reuben, 684 Senger, Fred W., 554 Settlement, 86 Seventh Day Adventists, 367 Seventeenth Infantry, 212 Seventy-third Infantry, 220 Shanks, Stephen S., 311 Sharp, Charles, 706 Sharp, Samuel M., 704 She-po-con-ah, 33, 56 Shinn, Edward D., 627 Shirk Family, 541 Shirk, Elbert W., 543 Shirk, Joseph H., 543 Shively, LeRoy A., 818 Shirk, Milton, 542 Shrock, Joseph, 462 Shrock, Stella, 463 Simons, Charles E., 660 Simons, William, 660 Sims, William, 638 Sixteenth Infantry, 211 Sloeum, Frances, 52 Slocum monument, 65 Smith, George, 618 Smith, James H., 690 Smith, John W., 689 Smith, J. J., 708 Smith, Marshall, 702 Smith, Marshall, 821 Smith, S. S., 687 Snowberger, Levi, 756 Snow Hill, 199 Social and Literary Clubs, 412 Social organization of the Indian tribes, 32 Societies and fraternities, 409 Sollitt, Elmer A., 578 SoUitt, John B., 578 Sollitt, Raliih V., 578 Some prominent citizens, 392 Sommer, John H., 634 South Peru, 200 Spanish-American War, 235 Spanish claims, 68 Spaulding, Frank, 802 Speck, Julius T., 665 Spooner, Jared, 334, 535 Spooner, John P., 536 Springer, Eli J., 671 Sproal, SOas J., 698 Starkey, James E., 743 Statistical Review, 429 Steamboat navigation on the Wabash 250 Stevens, Carleton C, 517 Stevens, Jesse T., 517 Stineman, Peter C, 679 Stitt, David, 711 Stitt, Leonard G., 768 Stockdale, 200 Stock raising industry, 274 Stormy summer, 398 Story of Frances Slocum, 52 Stowman, Walter W., 528 Stranger 's grave, the, 390 Street Scene in Macy (view), 193 Stringtown, 201 Struble, Phillip, 466 Stutesnian, Frank M., 481 Stutesman, James M., 481 Sullivan, Florence, 790 Sullivan, Theodore J., 501 Sutton, Ebenezer H., 755 Sutton, Eddie B., 756 Sutton, William A., 623 Swafiford, John W., 616 "Swamp angelK," 149 Swigert, Joel, 621 Swindler, Jorden, 592 Table showing number of miles of pub lie ditch in each township, 265 Tecuuiseh, 79 Temperance, 394 Teter, Jacob F., 715 The Swings, 88 Theobald, Jacob, 502 The Old Mexico Mill (view), 144 The Pillared Rocks (view), 5 The Prophet, 80 "The White Rose of Miami," 63 Thirteenth Infantry, 208 Thirty-fourth Infantry, 215 Thirty-ninth Infantry, 216 Tile drains, 266 Tillett, Joseph N., 443 "Tomahawk Right," 95 Tiimbaugh, George W., 696 INDEX Tuiiiov, John, 45(i Towns :iii(l villages, 179 Towns that aiv ami have lieen, 179 Tdwiisliip history, 109 Trading posts, 87 Treaties, 41 Treaty of Greenville. 77 Trilie of Ben Hur, 42(i Trip]ieer, Benjamin, 598 Trip|ieer, Claude, ti20 Tudor, Averv P.. 779 Twelfth Infantry, 210 Twentieth Infantry, :;13 Twenty-ninth Infantry, 214 I'nger, .John F., 811 Union City, 201 Union Township, location, 145; area, 14.5; settlers, 146; early industries, 147; lirst election, 147; first churches, 148; first "school house, 14S; schools, 14.S; railroads. 148; cemeteries, 382 United Brethren. 362 U. 8. Postoffiee, Peru (view), 175 Union Traction Company, 151 Universalists. 368 Urliaria. 201 Value of taxable property, 430 Vaii.lalia Railroad, 145 Vandalia Kailroad System, 135 Views — The Pillared Rocks, 5; Miami County Court House, 101; Old Court House, 102; Miami County .Tail, 107; Scene on the Mississinewa, 114; The Old Mexico Mill, 144; Old Holman Residence, 155; Broadway in the Six- ties, 164; Water Works Pumping Sta- tion, 168; U. S. Postoflice, Peru, 175; Street Scene in ilacy, 193; Old Tow- Path on the Wabash & Erie Canal, 247; On the Eel River Near Chili, 252; Concrete Bridge Over Wabash River, Peru, 268; Peru High School, 293; Old Sentinel Otfice, Southwest Corner of Main and Broadway, 1867, 300; Peru Public Library, 307"; Bread Line, Showing Work of the Asso- ciated Charities at Time of Great Flood, March, 1913, 373; North Broadway, Peru, March 25, 1913. Elks Home on the Right. Masonic Temple Behind Street Car. 401 ; Fifth Street Looking East from Broadway, Boats Landing on Court House Lawn, 403; Peru Y. M. C. A., 428 Vigilance committee, 384 Vincennes, 69 Volpert, John W., 630 Wabash river, 1, 250 W.abash river bridge case. 314 Wabash River Traction Company, 261 Wabash Railway Rniplo.yes Hospital, 375 Wabash Railroad. 125, "l09, 256 Wabash & Kv\c Canal, 96, 247 Wabash, St. Louis & Pacific Railroad Company, 256 Wabash \'alley Trust Company, 270 Wagoner, 201 Wagoner, William H., 511 Waisner, Albert M., 764 Waisner, Solomon, 737 Waite, Joseph II., 789 Wallace, Beniamin E., 785 Waltz, John 'C, 766 War of 1812, 81 War with Mexico, 205 Ward, Albert, 546 Ward, Beverly E., 772 Ward. Charles J., 571 Ward, Frank E., 686 Ward, Dr. J. O., 343 Ward, James O., 773 Washington Township, location, 148; area, 148; settlers, 149; organized, 150; early churches, 150; schools, 150; pioneer teachers, 150; early industries, 151; railroads, 151; cemeteries, 382 Waters, Frank, 643 Water works, 167 Water works pumping station (view), 168 Wauiiecong, 120, 202 Way, George L., 545 Wayne, Gen. Anthony, 76 Welch, Berne, 565 West, Elijah, 510 West. Harry E., 510 Wetherow, Edd B., 793 Wheatville, 202 Wilkinson, Jacob, 311 Will of Francis Godfroy, 36 William Smith's school, 295 Willson, Edward L., 732 Wilson, George F., 464 Wilson, John B., 475 Wininger, Michael B., 722 Winona Intenirban Railway, 138, 145, 263 Winona Tnterurban Railway Company, 139 Wolf, Levi B., 636 Wooleytown, 202 Xenia Gas and Oil Company, 12 Xenia Gas and Pipe Line Company, 280 Xenia Union Agricultural Society, 409 Yarian, Wilson, 714 Years, George M., 798 Younce, William W., 626 Young Men's Christian Association, 427 XX INDEX Z&rtman, Benjamin F., 610 Zartman, William F., 610 Zehring, Alfred E., 829 Zehring, Alonzo M., 646 Zehring, Benjamin F., 730 Zehring, Josiah, 741 Zimmerman, William H., 651 Zook, Aaron G., 824 History of Miami County CHAPTER I PHYSICAL FEATURES, GEOLOGY, ETC. Miami County — Location and Boundaries — Lines of Survey — Rivers AND Creeks — Underlying Rocks op the Upper Silurian and Devonian Periods — Quarries and Lime-kilns — -Along the Missis- sinewa — Bog Iron Ore — The Glacial Epoch — The Wabash River — Moraines — The Glacial Drift — Economic Geology — Clay's — Sand — Gravel — Natural Gas .and Oil — Primitive Forests and Their Destruction. Miami county is situated north and east of tlie center of the state. It is bounded on the north by Pulton county; on the east by Wabash and (irniit counties; on the soutli by Howard, and on the west by Cass and l''ulton counties. The forty-lirst parallel of latitude crosses the northein part, about two miles south of the northern boundary, and the elKhty-sixth meridian of longitude lies four miles west of the eastern bounihiry. The main l)ody of the county is in the form of a parallelo- gram, twelve miles from east to west and thirty miles from north to sontli. Measured by the lines of tlic official survey, the northern bound- ary is the line separating Congi-essional townsliips 29 and 30, and the soutliern boundary is the line separating townships 24 and 25. A strip two miles wide along the western l)order of the county lies in range 3, east, tlien comes all of range 4 and four miles of range 5, east. At the soutlieast corner of this parallelogram lies the civil township of Jackson, which extends four miles farther east than the main portion of the county. The total area of the county is 384 square miles. Flowing westward through the center of the county is the Wabash river, wiiicli separates the townships of Erie and Peru on the north from Butler, Wasliington and Pipe Creek on the south. Farther north is the Eel river, which flows in a southwesterly direction across the county 1 2 HISTORY OF MIAMI COUNTY throiigli the townships of Richland and Jefferson. The ]\Iississinewa river crosses the eastern border about the middle of Butler township and flows northwest, emptying into the Wabash a short distance above the city of Peru. The first white people to locate along this river pro- nounced the name " JIassissineway, " which it is said corresponded closely to the Indian pronunciation. The Indian name is "'Na-mah- chis-sin-wa, " and means "much fall in the water," which indicates in a general way the character of the stream. Big Pipe creek flows across the county in a northwesterly direction, touching every township south of the Wabash river except Deer Creek, and leaves the county in .section 11, township 26, range 3, where it enters Cass county. Its principal tributaries are Nigger, Walnut, Honey and Turkey creeks. The Nigger rises in Harrison township, near North Grove, and empties into Pipe creek in the northeast corner of Clay township. Walnut creek rises in section 21, in Harrison township, and flows northward until it discharges its waters into Pipe creek near the northeast corner of the same township. Honey creek is formed in the southeastern part of Harrison township by the east and west forks, then flows northward past Amboy and empties into Pipe creek in section 11, Jackson township. Turkey creek flows northward through the eastern part of Jackson township and finally empties into Pipe creek near the eastern line of section 18, township 25, range 6, east. Little Pipe creek has its source in Butler town-ship, about halfway between Big Pipe creek and the ]\Iississinewa river. Its general course is toward the northwest, through the townships of Butler and Wash- ington, until it joins the Wabash river near the lower part of the city of Peru. Through the townships of Harrison, Clay and Deer Creek, in the southwestern part of the county, Deer Creek flows in a westerly direction, crossing the western boundary line into Ca.ss county three miles north of the southwest corner of Miami. Farther south is South Deer creek, and near the village of Miami the Middle Fork empties into the main stream. North of the Wabash river the principal creeks are Flowers, Weesau (also written Wesaw), and Washoni's. The Big and Little Weesau creeks drain a large part of Union township and unite near the north- west corner of the old Weesau reservation, whence the main stream flows southward until it empties into the Eel river a little below the town of Denver. Flowers and Washoni's creeks both empty into the Eel river near Chili, the former just above and the latter immediately below the town. These streams, with a number of smaller ones, provide a natural system of drainage, which has been supplemented by a number HISTORY OF MIAMI COUNTY 3 of ditches, so tluit practically all the land iu iliaiui county lias thus been brought under cultivation and the soil rendered more productive. In geoldgical formation, Miami county belongs to the Upper Silurian era, with traces of the Devonian in the western part. The former is represented by the Waterlime and Niagara groups and the latter by from thirty to thirty-tive feet of Coi'uifurous limestones. The surface of the county consists almost entirely of glacial depo.sits — clay, sand and gravel — varying in depth from a few feet to 300 feet or more, and the few rock exposures are at points where the glacial drift has been washed away by the action of the streams. In 1872, E. T. Cox, then state geologist, made a report upon the rocks of Miami county, in which he says: "The rocks which were seen, and probably all the rock exposures of the county, are of upper Silurian age and seem to be equivalent to the silico-magnesia limestone mentioned in the description of Cass county, and the overlying limestones; the first mentioned beds much more argillaceous than in Cass couutj- — in some places becoming a magnesia argillite. ... The highest seam exposed is a limestone eiiuivalcnt to tile rock band at Delphi, in Carroll county. A light brown colored magnesian limestone, which, from false bedding, is often seen with strata dipping at every angle almost to a perpendicular. . . . This bed was formerly burned for lime at Dukes" t^uarry, adjoining Peru, the county town, but the kiln is not now in use. It is crowded with skeletonized fossils, yet still retaining a sufficient modicum of animal matter to prevent the lime from fully slackening in the short time usually allowed for that purpose by workmen. Hence, this lime is not suited for plasterers' use, unless the mortar is permitted to i-emain in damp vats for several months before being spread upon the walls of the houses. This is too slow a process for our fast age, yet the Roman architect, who built for ages, would use only mortar which had been prepared for a year or more before it would be needed by the artificer." At Dukes' (juarry a surface opening was made into the beds of the "silico-magnesia" limestone mentioned by Cox, but the stone was not suitable foi- building purposes. The beds of light brown colored lime- stone, referred to in the report, are generally local and of small extent. About a mile north of Dukes' quarry, on the farm of E. H. Shirk, an outcrop was formerly worked, and it is probat)le that the stone exists through the entire intervening area between the exposure on the Shirk farm and Dukes' quarry. In the lower beds along the Wabash river, at Lyde's quarry, two and a half miles west of Peru, Cox found a deposit "distinctly laminated, the seams being filled with clayey matter and pyrites." Upon examina- 4 HISTORY OF MIAMI COUNTY tion he decided that this stone might be used for foundations, oi- where protected from the weather, but upon exposure the clay and' pyrite matter would decompose and the stone become "shelly." Similar beds of stone have been developed at Trippier's quarries, two miles east of Peru, on the south side of the Wabash river, and at Wallick's mill on Little Pipe creek, near the Lake Erie & Western Railroad. State Geologist Thompson, in his survey of 1888, classifies the rock exposures at these quarries as Niagara limestone. Concerning the lime burned at Trippier's, Cox said: "It is similar if not equal to the Delphi lime, slakes perfectly, works 'cool,' bears transportation well, makes a strong and almost hydraulic cement, and deserves a more extended market." Near the mouth of the Mississinewa river there are extensive beds of Niagara limestone suitable for building purposes, the outcrop show- ing for over a mile. On the same stream, three miles east of Peru, are the "Pillared Rocks," interesting alike to the scientist and the lover of beautiful and romantic scenery. At this point the river is arrested in its northerly course by a solid wall of "cherty, silico-magnesia lime- stone" and makes a rather abrupt turn to the westward. The action of the rushing water against a stone wall composed of different textures, has caused an unequal disintegration of the rocks, carving them into pillars, rounded buttresses, alcoves, grottoes and overhanging shelves of beautiful and fantastic shapes. Cox says that in 1872 the summit of the bluff was covered with cedars. The "Pillared Rocks," with their celebrated picnic ground, form one of the beauty spots of Miami count}'. Locally, these rocks are known as the "Seven Pillars," but are often confused in name, by persons unfamiliar with them, with "The Cliffs" farther up the river. Farther up the Mississinewa there is a precipice on the north side of the stream — part of the elevation known as "The Cliffs" — and at this point Cox took the only section in IMiami county in his survey of 1872. That section was as follows : Sandy soil, 4 feet ; white glass and grit stone, 10 feet ; porous lime rock, 18 feet; cherty, laminated argillaceous limestone, to river, 35 feet; total, 67 feet. Concerning the porous limestone here Cox says: "Blocks of large size may be obtained, and the unexplored beds, if found sufficientl.v compact, will prove valuable for quarry purposes, as well as for 'burn- ing.' " At the time Cox made his survey he found that some fine, square blocks of stone had been taken from Thomas' (quarry, in the pool of the mill dam at Peoria. This stone was quarried at the water's edge, below the cherty stratum of the silico-magnesia division, but owing to HISTORY UF MIAMI COUNTY 5 its location was difficult to obtain, so that the quarry could never be operated at a profit, though the geologist pronounced it the best stoue he had seen in the county. The stone for the pilaster coping in the ('atholic church at Peru was taken from a quarry near Brouillette's, on the Mississinewa river above Peoria, and lias stood exposure to the weather well. In appearance it is of a modest, neutral tint, that contrasts harmoniously with the red brick walls, and resembles the Delphos limestone, of Ohio. This effect has since been destroyed by covering the church walls with stucco work. The I'lLi.ARED Rocks Cox's prediction tiial the porous liiiifslonc along the Mississinewa would ■prove valuable for (|uarry purposes, as well as for burning," has not hem rcali/ed, and the reason is explained by Thompson in his report on .Miami county in 1888. He found the Niagara limestones of the Mississinewa to be dolomitic, "hard and sub-crystalline in structure, only fit for foundation work or flagging, and difficult to work." Says he: "The Niagara limestones of Miami county do not possess the properties of valuable building stone, although they may be profitably used for foundations, or other rough work. The Waterlime rocks near Peru, however, are much better even for the roughest work, conse(|Uently 6 HISTORY OF MIAMI COUNTY there have been no special efforts made to develop a quarrying industry along the Mississinewa river. For the manufacture of lime the Niagara limestones furnish excellent material at many points along the Wabash and Mississinewa rivers, and several parties have made profitable use of the advantages afforded." The Waterlime rocks are exposed along the Wabash river for a distance of about half a mile above the Lake Erie & Western Railroad bridge, and again about a mile west of Peru. Among the quarries opened in these outcrops perhaps the most important were the O'Donnell, Brownell and Kissell cjuarries, in the order named as one descends the river. The ledges or layers range from three to sixteen inches in thick- ness and maj^ be quarried in any desirable dimensions. The stone is a hydraulic limestone, of fine texture, bluish in color, and is well adapted to foundation work, bridge abutments, etc., the thin layers being exten- sively used for flagging. The only rocks of the Devonian formation that are exposed in the county are along Pipe creek from the vicinity of Bunker Hill to the county line. North of Bunker Hill, on Big Pipe creek, for a distance of about three-fourths of a mile are almost continuous exposures of Cornif- erous limestone, the larger proportion of which is a bluish gray lime- stone, somewhat crystalline in structure, much of it being well adapted to rough masonry, such as foundations, bridge abutments and similar work. As a rule the Corniferous limestones of iliami county are too cherty and silicious to make good lime, though there are a few localities where fairly good lime has been burned from the gray, fossiliferous limestones that overlie the cherty deposits. In the northern part of the county bog iron ore is found in con- siderable quantities at several places. Furnaces were operated along the Eel river in early days and an excellent quality of iron was pro- duced. The collection of the ore was attended by rather heavy expense, however, and with the introduction of improved transportation facilities the Eel river furnaces were abandoned, owing to their inability to compete with mines more favorably situated. All over the county there are traces of iron in combination with the soil and also filtered into the limestone rocks. When these rocks become disintegrated and mixed with the glacial drift a soil is formed that is not exceeded in fertility any- where in the state. (See State Geologist's Report for 1888, p. 177.) Probably no phenomena have proven more perplexing to students of geology than those which brought about the destruction of vast beds of rock and the distribution of their fragmentary remains over large areas of territory far from their original location. For illustration: The large bowlders found in all parts of Indiana, commonly called HISTORY OF MIAMI COUNTY 7 ''nignrerlifads. " are of a grranitoid charactpr. belonging to beds tliat are nowhere represented in the state, and must have come from some phiee beyond lier boi'ders. \'ai'ious tlieories have been advanced to aecount for tliese eondilions, the most prominent of whieh. and the one most generally aeeejited by scientists, is the Glacial theory-. The Glacial epoch, or Pleistocene ])eriod of geologic time, sometimes called the "lee Age." comprises the earliest part of the Qiiai"ternary period. During the latter jjart of the Tertiary period, preceding, there was a gratlnal lowering of temperature throughout what is now termed the north temperate zone, until the entire surface of the earth in that region was covered with large liodies of ice called glaciers.' These glaciers were formed by pci'iddical oi' intermittent snows. During the periods between these I'alls of snow, that whieh Jiad already fallen became so compressed by its own weight that the entire mass was in time converted into one .solid body. The pressure upon the yielding mass of snow imparted motion to the trlaciei-, which carried with it rocks, soil and other mineral matter. As it moved forward the grinding and equalizing work of the glacier ultinuitely wi'ought great changes in the topography and meteorological conditions of the earth. Not only were the mountain peaks in the path of the glacier woin down and the general leveling of the earth's. surface brought about, but also vast quantities of earth and sand were carried forward by the streams of wjiter formed by the melting of the ice and deposited in the ocean. In this way shores of the continent were pushed forward iluring a period of several centuries and the superficial area of the land was materially increased. As a general rule, the course of the North American glaciers was toward the south. One of them extended over Canada and the north- eastern part of the United States, reaching from the Atlantic ocean on the east to the slopes of the Rocky mountains on the west, and covering the entire basin of the Great Lakes. When the ice melted, the rocks and other debris carried along by the glacier were left to form what is known as the glacial drift, also called till, bowlder clay and older diluvium. As the glacier glided slowly along — probably not more than one foot per day — the bowlders and other hard ininerals at the bottom, pressed downward by the gigantic mass above, left marks or scratches on the lied rock, and from these marks or stris the geologist has been able to determine with reasonal)le aceuracj- the course of the glacier by noting the direction of the striic. Concerning the course of the glacier in this state. State Geologist Thompson, in his report for 1888, says: "In Indiana the general direction of the glacial movement was a little west of south. There are localities in the state where the striae or sand 8 HISTORY OF MIAMI COUNTY marks on the ice-ground rocks run from east to west, and in almost every other horizontal direction ; but by careful study these are found to be merely local exceptions to the general rule. . . . The glacial deposits of Indiana by their conformation, by the materials found in their mass and by the stria- underlying them, have come into the state from a direction almost north and south." The accumulation of earth and stone carried by the glacier was sometimes heaped up along the margin, where it formed a ridge or deposit called a lateral moraine. When two glaciers came together, the deposit formed at the point of conjunction is called a medial moraine. The nearly level deposit under the body of the glacier is known as the ground moraine and the ridge formed at the farthest point reached by the glacier is the terminal moraine. The valley of the Ohio river was the terminus of the glacier that once covered Miami county and the channel of that stream owes its origin to the melting of the ice and the flow of water which always underlies the bed of a glacier. As the melting process w^ent on, the terminal margin withdrew to the north- ward, and wherever there remained undestroyed rock barriers or dams they gave direction to the waters of the terminal moraine. In this way the course of the Wabash river was determined, or modified, centuries before Columbus discovered the New World. To quote again from Thompson : "From Wabash to Delphi the Wabash up-lifl (called the Wabash Arch) has determined the course of the Wabash river, just as it also determined the form of the drift mass immediately south of it. The river itself is runuiug along the general line of a wide fracture or system of fissures in the Niagara rocks from Wabash to Logansport. At the latter place it has cut through a spur of the Devonian formation, and at Delphi it curves around the ba.se of a curious conical up-lift of the Niagara limestone. To my mind it is plain that the river simply follows the example of the ice current which went before it plowing out the great furrow which we call the Wabash valley. At present evidence is wanting to prove any theory as to what particular part of the glacial age was devoted to the work of channeling out a groove for Indiana's greatest river, but it would appear that this must have been the first result of the glacier's contact with the low but compact and stubborn knobs of the Wabash Arch. Subsequently, as the ice field grew in weight and power it arose and surmounted this barrier, grinding away its conical peaks and tearing out of its hollows in many places the non- conformable Devonian and Carboniferous rocks." In some portions of North America the lateral moraines rise to a height of five hundred or even one thousand feet. The terminal moraine HISTORY OF :\riAMI COUNTY 9 in uortherii Indiana that marks the southern boundary of the Great Lake basin contains several mounds that are from 150 to 200 feet in height, and "the existence of a grand moraine lying across central Indiana has been fully demonstrated." Along the line of this great moraine the contoui- of tile drift mass is found to be comparatively regular, the glacial matter having been more uniformly deposited. In this territiiry lies Jlianii eouiity. where there is al)undant evidence of glacial action, though great local changes have taken place in the surface of the drift mass since it was first deposited. Upon the retreat of the ice the whole drift area was left bare and desolate, accompanied by an arctic teinpei-ature and without either animal or plant life. Rain and wind were active forces in leveling or modifying the surface during the period that elapsed before the northward migration of plant life began to clothe it with a garment of resistance and render it habitable. How long that period may have been geologists can only conjecture. It was by this method that the surface of iliami county was formed. Concerning the depth of the drift in Sliami county, Thompson says: "South of the Wabash river the drift varies in depth from nothing to one hundred feet or more, though it is only along the streams where it has been carried away by the water that it is wholly wanting. At Bunker Hill, gas well No. 1, it is 58 feet thick; at Xenia (Converse) it is 50 feet thick, while at Amboy, midway between the two points, it is 35 feet thick. The alluvial matter in the Wabash river bottom varies from 5 to 50 feet in thickness. In gas well No. 2, at Peru, it is 10 feet thick; in well No. 1, Northside, it is 36 feet thick, while at the Bearss gas well. No. 4, bored on the high lands two miles north of Peru, the drift is 324 feet thick. It is quite likely that the maximum thickness of the drift north of the Wabash river in iliami county will approximate four hundred feet, even if it does not exceed that ilepth." At widely distant places in the glacial iltil't of the United States have been found the remains of prehistoric animals of the IMiocene period, but which l)ecame extinct in the Pleistocene, or lee Age. The most common of these remains are the bones of the mastodon — so-called from the shape of its teeth — an animal closely allied to the elephant of modern times. Several times in making excavations in Miami county, a few bones of this great monster of a past era have been found, but it was not until the fall of 1904 that a complete skeleton was unearthed. Some men engaged in digging a ditch about twelve miles north of Peru, found a few bones, which were given to Pred Kite, a taxidermist of Denver. Jlr. Fite employed some helpers and continued digging in the locality until the entire skeleton, with the exception of a few minor bones, was found. He then spent some time in cleaning and articulating 10 HISTORY OF MIAMI COUNTY tlie parts of the skeleton, supi)l.viii£r the place of the missing bones with wooden substitutes, and in the spring of 1905 his mounted skeleton was finished. It stood nine feet high and measured eighteen feet in length, the tusks being nine feet long. In hauling the bones from the place where they were found to his laboratory two \vagous were used, the entire collection weighing over a ton. It was not long after he had the skeleton mounted until ]Mr. Fite received several offers for it. He finally sold it to a museum in Detroit, Michigan, for .$500. The principal elements that go to make up the drift formation in Indiana are silica, alumina, lime and iron. Silica is found principally in the clays, sands and bowlders; alumina in the clays and bowlders; lime in the clays, marls, chalk and the peat-like bog deposits, and the iron is abundant in the swamps in the form of bog ore, or in the gravel dei^osits. In Miami county some of the drift deposits are of economic or commercial importance. Some years ago John E. ililliron, of Denver, began a systematic study of the county's mineral resources, especially the clay deposits. At several points near Denver he found clay suitable for a good article of pottery, and clays adapted to the manufacture of tile or brick may be found in nearly all parts of the county. ]\Ir. Milliron also found an ochreous kind of i-lay, of fine texture and strongly impregnated with iron, that makes a good quality of mineral paint when ground and mixed with oil. Paint made from this clay has been used at Denver and has been found to possess durability, and it is believed that a profitable industry might be built uji in lis manufacture. Four miles northwest of Denver, on Weesau creek, there is an extensive deposit of clay that burns to a light cream color, stands fire w'ell, does not warp to any great extent during the burning process, and could no doubt be utilized to advantage in the manufacture of brick, tile and pottery. (See State Geologist's Report for 1888, p. 176.) Sand in abundance is found along all the creeks and rivers of the county, and in lenticular beds at various places in the drift. A large portion of the iliami county sand is valuable for building purposes and there are deposits that are well adapted for the grinding of glass or for molders' use, but these deposits have not been developed along those lines. ^lost of the sand used in the Indiana glass factories comes from distant points, much of it from outside of the state, and there is no question that the development of some of these beds would prove of great convenience to the glass manufacturer, as well as a source of profit to the owner of the sand-pits. In his report for the year 1905, State Geologist Blatchley devoted considerable attention to the road-building materials of the various counties of the state. He found gnod gravel alnindant near ]\Iaey and HISTORY OF :\IIAMI COUNTY 11 at some other points in the glacial till plain in the northwestern part of the countj-, though most of the gravel in other portions north of the Wabash river was found only along the streams. The south half of the county, also a till plain, has a sandy clay as the surfaeo soil, with a coarse ([uicksand in places that is used for road-building and makes a fairly good highway. The Wabash river bluffs, ranging from twenty- five to forty feet in height, contain very little gravel, being generally composed of clay, but there are good gravel deposits along some of the other streams in the southern part of the county, notably at Bunker Hill and Amboy. At the latter place the upper deposit of clay has been removed along Big Pipe creek and there are half a dozen or more good gravel pits. Blatchley also found small gravel deposits at several places in the moraine south of the Wabash. From the information at his com- mand he expressed the opinion that it would not be necessary to haul gravel more than three miles — probably not that far — anywhere in the county for the construction of roads. Notwithstanding the statements of the state geologist, in the report above referred to, it is a well known fact that practically all of the Wabash river valley — that is, the river bottom and the bluffs which bound it on either side — is underlaid with gravel. These deposits are the most extensive, the most important, the most easily accessible and the most valuable in the county. In all other portions of the county, the deposits are scattered, less valuable, more expensive to develop and more difficult to render available for use. In the southern part of the county much of the gravel used on the roads is pumped from the bed of Pipe creek, or from other beds below the water level. It is of very inferior quality as compared with the Wabash valley gravel. No account of the geology of the county would be complete without some mention of natural gas and oil, both of which have been found within tlic county limits. Natural gas is described as "a member of the paraffin series (hydrocarbons), a combination of carbon and hydro- gen, about sixty per cent, as heavy as air and highly inflammable." It is composed of marsh gas, or methane, the gas fields in Ohio and Indiana having been formed by the decomijosition of animal matter, while the Pennsylvania field is composed of decaying vegetation. The decom- position, or chemical change, that generated the gas is believed to have taken place at a comparatively low temperature within the porous rocks of the Lower Silurian formation, the Trenton limestone especially serving as a reservoir for the aeeummulated gas. It is quite probable that natural gas was first used in connection with the Delphic oracles, about 1,000 B. C, and it has been used for centuries by the Chinese in the evaporation of salt water. It was first 12 HISTORY OF .MIAMI COUNTY used ill the United States in 1821, when a well one and a half inelies in diameter and twenty-seven feet deep was drilled near a "gas spring"" at Fredonia, New York, and the gas was iised for lighting the streets of the town. In 1838 the presence of gas was observed at Findlay. Ohio, and about three years later it was found in a well at Charleston, West Virginia. While developing the oil fields of Pennsylvania, in 1860, the gas was used vinder the boilers instead of coal, but the first systematic use of it as a fuel was at Erie, Penns.vlvania, in 1868. Prior to 1884 little was known of the Trenton limestone, except from the outcrops in Canada and a few places in the United States. In that year gas was struck at Findlay, Ohio, in the Trenton limestone, which marked the beginning of an era of great prosperity for that city and led to prospecting in Indiana. On March 14, 1886, the first gas well in Indiana "blew in" at Portland, Jay county, where the gas was also found in the Trenton formation. The people of Miami county were among the first in the state to undertake an active search for natural gas. Soon after the discovery of gas at Portland, the idea became prevalent that gas could be found almost anywhere in paying (|uantities by drilling down to the Trenton limestone, and prospecting became general throughout the central part of the state. The Peru Natural Gas and Fuel Company was incorporated on October 25, 1886, "for the purpose of prospecting for natural gas, coal, coal oil, or any other valuable mineral." The first gas well was drilled in the northern part of the city of Peru, at an altitude of 657 feet above the sea level. The following is the record of the strata passed through in drilling: Alluvium — river drift, 36 feet ; Niagara limestone, 385 feet ; Hudson river and Utiea shales, 454 feet ; Trenton limestone. 30 feet ; total depth, 905 feet. In this well a small quantity of petroleum was found at a depth of 880 feet, or five feet after the drill first entered the Trenton rock. At 900 feet a strong vein of salt water was struck, but no gas was found. A second well was drilled just south of the city of Peru, but with no better results. The third well was on the Y'onee farm, about seven miles southeast of Peru, and well No. 4 was on the Bear.ss farm, about three miles north of the city. Here the drill went to a depth of 1,041 feet, penetrating the Trenton limestone for thirty-one feet, but without find- ing gas. Xenia (now Converse) was the first point in Miami county to secure gas. The Xenia Gas and Oil Company was incorporated on January 4, 1887, and the first successful gas well in the county was drilled the HISTORY OF MIAm COUNTY 13 folliiwiiif^ suimiicr. The record below illustrates the eharacter of the strata throuy;h whieh the drill passed : Soil. 4 feet; gravel, 46 feet; waterlime, 31 feet; Niagara limestone, 238 feet; Hudson river and Utica shales, 587 feet; Trenton limestone, 31 feet : total depth, 937 feet. Tiie altitude at the surface of the well was 815 feet and the Trenton rock was first struck at ninety-one feet below the sea level. A strong vein of water was struek in the Niagara limestone, but it was cased off and the drilling proceeded. Soon after piercing the Trenton i-ock water was reached, and this had the effect of weakening the flow of gas, so that the well was never a heavy producer. The second well at Xeuia was a strong one, yielding a suflicient quantity of gas to supply the entire town. Several strong wells were also found at Aralioy and in the immediate vicinity. At Bunker Hill tlie drill went down to a depth of 1,004 feet, or 12 feet into the Trenton limestone, where salt water was struck. This water raised in the bore of the well to within twenty feet of the surface and caused the drillers to suspend operations. The People's Oil and Gas Company, of Peru, was organized by approximately one hundred citizens in the spring of 1897, but was not incorporated at the time. The fii-st well was bored on the B. E. Wallace farm, just east of the ^lississinewa river. It proved to be a "dry hole," but the members of the company did not lose hope and a second well was drilled in the northwestern part of Peru, on a tliree-cornered tract of land belonging to A. N. Dukes. Trenton rock was struck at a depth of 855 feet and on July 19, 1897, the well was yielding about twelve barrels of oil daily. The company was then incorporated, the well was tubed and pumped and the output was thus increased to 120 barrels daily. 'I' wo other wells in the same locality yielded 150 and 175 barrels, respect ively. By the close of the year over two hundred wells had been drilled. A more complete account of the development of the oil and gas fields of the county will be found in the chapter on "Finance and Industries.'" When the Hrst white men raiiie U> what is now Miami county they found the surface covered with a heavy growth (jf tindjer. The great forests contained many beautiful .specimens of walmit, poplar, various varieties of oak, ash, maple, hickory and other valuable trees, and there were likewise a number of less important species, including sycamore, beech, locust, mulberry, wild cherry, elm and willow. At that time the soil was of more value for cultivation than the timber. Consequently many trees were cut down and burned that, if they were standing today, would be worth more than the land upon which they grew. Then no tliought of a timber famine ever entered the minds of the pioneers. 14 HISTORY OF MIAMI COUNTY Far away to the westward stretched the boundless forest and to the frontiersman it seemed, if he gave it a thought, that there would be timber enough to supply the wants of the people for generations to come. The ax, the fire-brand and the saw-mill have done their deadly work so well that now, though less than a century has passed, the con- servation of American forests is an engrossing subject. Possibly much of the timber might have been saved, but would the people of the present day act differently under the same conditions? Probably not. CHAPTER II ABORIGINAL INHABITANTS The Mound Builders — Theories Regardixg Their Antiquity — Thomas' DmsiON of the United States into Districts — Ch.uj- acteristics of Each District — Pew Relics in Miami County — The Indians— How Distributed in 1492 — The "Six Nations" The ^liAMi Tribe^Habits and Customs — Their Domain — Vil- lages IN the Wabash Valley— The Pottawatomi — Character and Traditions — Villages — Policies in Dealing with the Indians. Before the white man, the Indian ; before tlie Indian, who? The (iiies- tion is more easily asked than answered. When the first Europeans came to this country they found here a peculiar race of copper-colored people, to whom they gave the name of "Indians," but after a time some stu- dents of archaeology came to the conclusion that this race had its prede- cessors. Who were they? The archaeologist has given them the name of "Mound Builders," on account of the great number of mounds or earthworks they erected, and which constitute the only data from whidi to write their history. During the last century a great deal of dis- cussion concerning the character and fate of the Mound Builders has been indulged in by antiquarians and archaeologists, but the qu(;stioii seems to be no nearer a positive settlement than when it first came up for consideration. In 1812 the American Antiquarian Society was or- ganized and during the years immediately following made some inves- tigations of the prehistoric relics left by the primitive inhabitants. But the first work of consequence on American archaeology — "Ancient Mon- uments of the Jlississippi Valley" — compiled by E. G. Squier and E. II. Davis, did not make its appearance until in 1847. The authors, who had made an exhaustive study of the mounds and earthworks in the section indicated, advanced the theory that the jMound Builders were a very ancient race and that they were in no way related to the Indians found here when the continent was discovered by Columbus. Allen Lapham, who in 1855 wrote a treatise on the "Antiquities of Wisconsin," also held to the great age and separate race theory. In fact, most of the earl>- writers on the subject have supported this 15 16 HISTORY OP MIAMI COUNTY hypothesis, and some have gone so far as to arrange the period of human occupancy of the Mississippi valley into four distinct epochs, viz: 1. The :\Iound Builders; 2. The Villagers; 3. The Fishermen; 4. The In- dians. This somewhat fanciful theory presupposes four separate races or peoples and is not sustained by any positive evidence. Other writers have contended that the early American aborigines were descendants of the lost tribes of Israel and efforts have been made to substantiate such an assertion. With regard to the :\Iound Builders. Baldwin, in his ■'Ancient America," says: "They were un(iuestionably American aborigines and not immigrants from another continent. That appears to me the most reasonable .sug- gestion which assumes that the :\Iouud Builders came originally from Mexico and Central America. It explains many facts connected with their remains. In the Great Valley their most populous settlements were at the .south. Coming from Alexico and Central Ainerica, they would begin tlieir settlements on the Gulf Coast, and afterward advance grad- ually up the river to the Ohio Valley. It seems evident that they came by this route, and their reuuiins show that their only connection with the coast was at the south. Their settlements did not reach the coast at any other point." On the other hand, McLean says; "From time immemorial, there has been immigration into :\Iexico from the North. One type after another has followed. In some cases different branches of the same family have successively followed one another. Before the Christian era the Nahoa immigration from the North made its appearance. They were the founders of the stone works in Northern Jlexico. Certain eminent scientists have held that the Nahoas belonged to the race that made the mounds of the Ohio and Mississippi valleys. Following this people came the Toltecs, and with them the light begins to dawn upon ancient Mexican migration. They were cultivated and constituted a liranch of the Nahoa family. . . .In the light of modern discovery and scientific investiga- tion, we are able to follow the Mound Builders. We first found them in Ohio, engaged in tilling the soil and developing a civilization peculiar to themselves. Driven from their homes, they sought an asylum in the South, and from there they wandered into Mexico, where we begin to learn something definite concerning them." Here is a fine illustration of "When doctors disagree." Two more widely diverse theories than those advanced by Baldwin and McLean can hardly be imagined, yet they show the vast amount of speculation indulged in by writers upon the subject. There is not, and never has been, a unity of opinion regarding the ]\Iound Builders. While the early writers classed them as a hypothetical people, supposed to have antedated HISTORY OP -MIAMI COUNTY 17 tlic Indian ti-il)t'.s \>y several cciiliii-ics as inlialiitants ol' tlic Oliio and Mississippi valleys, the iMouml Hnildrrs arc now regarded "as the ances- tors and representatives of the tribes foiiiul in tlie same region hy the Spanish. Frerieh and English pioneci-s. " Says Hrinton: "The period wiicn the Mound Builders tlourisiu'd has Ix'en differ- ently estiniatetl : but there is a growing tendency to reject the assump- tion of a very great anti(|uity. There is no good reason for assigning any of the remains in the Ohio valley an age antecedent to tiie Christian era, and the final destruction of their towns may well have been but a few generations before the discovery of the continent hy Columbus. Faint traditions of this event were still retained by the tribes who occu- pied the region at the advent of the whites. Indeed, some plausible attenii)ts have been made to identify their descendants with certain e.xisting tribes." In the early part of the sixteenth century De Soto and the French explorers found in the southern part of the present United States cer- tain ti'ibes who were mound builders, their structures differing; but slightly in character from those for which great antiquity is claimed. The culture of the !\lound Builders was distinctly Indian in character and the relics found in many of the so-called ancient mounds differ but little from those of known Indian origin. As these facts have been devel- oped in the course of investigation, archaeologists have generally come to accept the theory that the Mound Builders were nothing more than the ancestors of the Indians, and i)roliably not so very remote as for- merly believed. Cyrus Thomas, of the United States Bureau of Ethnology, who has made a careful study of the ancient earthworks of the country, divides the mounds of the Uniteil States into eight districts: I. The Wisconsin district, which embraces the southern half of Wis- consin, the northern portion of Illinois and the northeastern part of Iowa. This district is replete with effigy mounds — that is mounds hear- ing a resemblance to some beast or bird. These are believed to have been copied from some bird or aniuud that served as a totem for the tribe, though they may have been objects of veneration or worship. Effigy mounds are likewise found in some of the other districts, one of the most notable examples of this class being the "Great Serpent" mound, of Adams county, Ohio. This mound is located on a narrow- ridge, almost surrounded by three streams of water. It is in the form of a serpent and is 1,348 feet in length. The opened jaws measure sev- enty-five feet across and immediately in front of the mouth is a circidar or elliptical inclosure with a heap of stones in the center. The body of the serpent is from thirty to fifty feet wide and about eight feet in 18 HISTORY OF MIAMI COUNTY height at tlie highest part. The state of Ohio reeeiitly purchased the tract of groimd upon which this ancient work is located and converted it into a park, or reserve, in order to protect the mound from the ravages of the curiosity hunter. 2. The Upper Mississippi district, which includes northern and cen- tral Illinois, southeastern Iowa and northeastern Missouri. In this dis- trict the mounds are generally conical tumuli, located on the ridges of the uplands and possess very little that is of interest to the archaeologist. 3. The Ohio district, which covers the state of Ohio, the eastern part of the state of Indiana and the western part of West Virginia. Forti- fications and altar mounds constitute the distinguishing features of this district, though the ordinary conical tumuli are by no means absent. One of the largest known mounds of this character is the famous mound on Grave creek, West Virginia, which is about three hundred feet in diame- ter at the base and seventy feet high. In the state of Ohio alone about thirteen thousand mounds have been found and many of them explored. 4. The New York district, embracing western New York, the central lake region, and a small section of Pennsylvania. In western New York there are a number of inclosing walls or fortifications. 5. The Appalacliian district, which includes western North Carolina, eastern Tennessee, southwestern Virginia and southeastern Kentucky. In the mounds through this district have been found a large number of human skeletons, stone pipes, copper bracelets, mica plates and other relics unlike any found in the other districts. 6. This district includes the middle portion of Mississippi, south- eastern ilissouri. northern Arkansas, western Tennessee, western Ken- tucky, southern Illinois and the Wabash valley in Indiana. The distin- guishing feature of this district is the truncated and terraced pyramid mounds, which are found here in larger numbers than in any other part of the country. There are also some inclosures resembling fortifications, ditches or canals, and pottery and stone coffins have been found in several of tlie mounds that have been explored. Near Cahokia, Illinois, is a truncated pyramid five hundred by seven hundred feet at the base and ninety-seven feet in height. 7. The lower ilississippi district, which includes the southern half of Arkansas, the greater part of Louisiana and tlje southern portion of ]\Iississippi. It was in this district that De Soto and the French explorers above mentioned found, upon their early visits to the region, certain Indian tribes who were mound builders. The mounds here are chiefly of the simple, conical type and show no special characteristics. 8. The Gulf States district, which embraces the southeastern part of the United States. In this section the large, flat-topped pyramidal iiisTORV OF :\[rA:\ii county 19 iiiouiuls and iin-losiiiTs or furtilieatiuus are abundant. There are also a number of effigy mounds, the great eagle mound of Georgia being one of the finest exampli's of this class in the country. Concerning the structure and purpose of the mouuds, Brinton says: "The mounds or tumuli are of earth, or earth mingled with stones, and are of two general classes, the one with a circular base and conical in shape, the other with a rectangular base and a superstructure in the form of a tnuicated i)yramid. The former are generally found to con- tain human remains anil are, therefore, held to have been barrows or sepulchral monuments raised over the distinguished dead, or, in some instances, serving as the comnuinal place of interment for a gens or elan. The truncated pyramids, with their flat surfaces, w^ere evidently the sites for buildings, such as tem{)les or council houses, which, being con- structed of perishable uuitcrial, have disappeared." While much of the foregoing is not directly applicable to i\riami county, it shows the various theories concerning the aborigines who dwelt or roved about in this country long before the white man even knew of the existence of the continent. At various places in the Wabash valley ajid the valleys of its tributaries — the Sixth district in Thomas" division — there are numerous relies of Jlound Builders, even though iliami county is lacking in works of interest to the archaeological student. With regard to the archaeological reuuiins in iMiami county, State Geologist Thompson, in his report for 1888 (page 188), says: "The aberuiit him to vio- late its stipulations, and by this mean^ iu> won the confidence and esteem of the whites. General (ieorge Washington, while president of the Cnited States, presented him with a medal and a handsome sword, which were buried with him at Fort Wayne, where he died on July 14, 1812. He was buried by the white people with honors, a monument was erected over his grave, was Pe-she-wa 'the l.vnx), a name indicative of his char- acter — always alert and watchful for his own interests and the welfare of his tribe. Richardville (pronounced Roosheville) was not a full- blootl Miami. His father, a noted Fi-encb trader, .was Joseph Drouet de Richardville, a scion of a noble family of France, and there is a tra- dition that he was an officer in the French service in Canada before be- coming interested in^the fur trade. His brother was a trader at Vin- cennes, where some of his descendants still live, and who according to Meginnis have in their possession valuable documents "which trace their ancestry back to the year 1162." The mother of Chief Richardville was TahJvum-wali, daughter of the old chief Aguenackgue and a sister of Little Turtle. He was born at the Miami village of Kekionga (Fort Wayne) about the year 1761. His election to the chieftainship of the tribe was the result of a daring feat that for bravery is entitled to rank with the defense of the pass at Ther- uiopjlae or the heroic .sacrifice of .\rnold W'inkelricd. A white nuiii was captured by a war part\- of ilia mis and brought into the Indian camp on the Maumee river. Little Turtle's successor had not yet been chosen and, after a consultation of the head men. the uiifoi-tunate prisoner 30 HISTORY OF .MIAMI CorXTY was seuteuced to be buriu-d at the stake. Among the ]\Iiainis there were some who wanted to abandon this barbarous custom and one of these was Tah-kum-wah, the mother of Richardville. With her son she stood apart, sileuth- watching the preparations for the sacrifice of the prisoner, who, knowing that protestations were useless, resigned himself to his horrible fate. The stake was planted, the captive ))ound to it securely, the fagots piled around him, the bloodthirsty savages around him reveling in fiendish anticipation. When all was ready the torch was applied and the Indians "began tlu^ir awful dance of death." Then Richardville 's mother thrust a knife into his hand and bade him assert his claims to the chieftainship. Springing through the circle of frenzied dancers and kicking aside the blazing fagots, Richardville (juickly severed the cords that bound the prisoner and bore him beyond the cordon of flames. It would probably be a difficult matter to say which was the most aston- ished — the liberated captive or the Indians whose barbaric ceremony had been so rudely interrupted. Jleginnis says they were "by no means pleased at the loss of their prize, yet the young man. their favorite, for his daring conduct, was at once esteemed as a god by the crowd, aiul then became a chief of the first distinction and honor in the tribe." The story then continues to the effect that Richardville 's mother took charge of the man, placed him in a canoe, covered him with peltries and sent him down the ilaumee under the protection of friendly Indians. Some years later, while on his way to Washington, Richardville stopi)ed for a few hours in a town in Ohio and while there a stranger came up to him, gave him a warm greeting and declared himself to be the rescued prisoner. - The story of this dramatic incident, was related by the chief to Allen Hamilton, the Indian agent at Fort Wayne, and has since been repeated by several writers, all of whom describe Richardville as a young man at the time he did the daring deed that won for him the chieftainship of his tribe. The same authorities agree that he did not become chief until after the death of Little Turtle, in the summer of 1812. The story of the rescue may be true, but if Richardville was born in 1761 and did not succeed to the chieftainship until after the death of Little Turtle, he was therefore past fifty years of age when he became the principal chief, civil ruler and great lawgiver of the Miamis. There is abundant evidence, however, that for years prior to that time he had been one of the leading men of his tribe. He was more of a diplo- mat than a warrior, but he took part in the action that defeated General Harmar's army in October, 1790. He was one of the Miami representa- tTves in the council of Greenville, which resulted in the treaty of August 3, 1795 ; was one of the signers of the treaty of Fort Wayne, June 7. HISTORY OF MIAMI COUNTY 31 1803, ami nf the treaty oT (Irousi'laiid. Aii sum of his own money and luiilt a ratlirr ])re- tentious residence' on one of his I'esei-vations. Tlie "'Handbook" issued by the United States Bureau of Ktimology says: "His house on the bank of the St. Mary's, abdut four miles from Fort Wayne, was foi- many years known as the abode of hospitality."' For a mimher of years he conducted a lai-jre tradint; house at Fort Wayne, where he spent most of his time, but about 1836 he removed his trading post to Wabash and contiinied in linsincss there for some time, his wife and the younger mem- bi^rs of the family remaining at tiie houie on the St. Mary's. The follow- ing description of him is from the pen of Judge Horace P. Biddle, who was personally aei|uainted with the chief for several years preeedinij his death : '"In stature Richardville was about five feet ten inches, with broad shoulders, and weighed about 180 pounds. His personal appearance was attractive and he was graceful in carriage and manner. E.xemjit from any expression of levity, he is said to have 'preserved his dignity umlei- all circumstances.' His nose was Roman, his eyes were of a lightish blue and slightly protruding, his upper lip pressed firmly upon his teeth, and the under one slightly projecting. That he was an Indian half-breed there can be no doubt. His own statements and unvarying traditions conclusively prove that he inherited his position through his mother, by the laws of Indian descent, and contradict the theory that he was a ■•'renchman, who obtained the chieftainship by trickery or purchase. In appearance he was remarkable, in that his skin was neither red nor white, but both coloi's combined in his skin, which was mottled or spotted red and white.'' Richardville died at his home on the St. Mary's river on August 13, 1841. The next day he was buried by the Catholic church, the services being conducted by Father Clark, the priest from Peru, in the church of St. Augustine. His body was first interred where the cathedi'al of Fort Waj'ue was afterward erected, and when work on that building was commenced his remains were removed to the Catholic ceuieteis- south of the cit}-. His grave is marked by a marble monument placed there by his daughters. On the east side of the monument is the inscription: "Here rest the remains of Chief Richardville, principal chief of the .Miami tribe of Indians. He was born at Fort Wayne, about the year 1760. Died August 13, A. I). 1841," and on the west side: "This monument has been, erected l)v La Blonde, Sarah and Catherine, daughters of the deceased." 32 ■ HISTORY OF JIIAMI COUNTY Catherine, whose Indian name was Po-con-go-qua, became the wife of Francis La Fontaine (To-pe-ah), who was the last principal chief of the ^Miamis. Like his illustrious predecessor, he was the son of a Preuch- niau and his mother was a Jliami. His marriage to the daughter of Biehardville occurred when he was about twenty-one years of age, and but a short time before the old chief's death. In that short interval he took such interest in the welfare of the iliamis that he was unanimously selected as chief soon after the death of his father-in-law. La Fontaine is described as a "tall portly man, weighing about 350 pounds." His home was on two sections of land a short distance east of the city of Huntington. But his elevation to the position of chief came after the treaties of 1826 and 1838, which had taken from the Miamis their lands and humbled their pride, hence he had no opportunity to display liis (lualifieatioiis as a leader. He accompanied his people to their new reservation in Kansas, spent the winter there with them, and the follow- ing spring set out to return to his home in Indiana. On the way he was taken ill and died at Lafayette, Indiana. April 13, 1847. His remains were taken to Huntington and interred in the Catholic cemetery. With regard to the social and political organization of the Indian tribes, J. N. B. Hewitt, of the United States Bureau of Ethnology, says: ■'Among the Nortli American Indians a chief may be generally defined as a political officer whose distinctive functions are to execute the ascer- tained' will of a definite group of jjcrsons united by the possession of a common territory or range. . . . The clan or gens, the tribe and confederation present more complex forms of social and political organi- zation. The clan or gens embraces several such chieftaincies, and has a more highly developed internal political straeture with definite land l)oundaries. The tribe is constituted of several elans or gentes, and the confederation of several tribes. . . . There were in several com- munities, as the Iroquois and Greeks, civil and sub chiefs, chosen for jicrsonal merit, and permanent and temporary war chiefs." The social and political structure of the iliamis was very similar to that of the Iroquois and Creeks. The principal chief was the civil ruler and executive official of the tribe, and under him were the war chief and the chiefs of the clans or gentes. There is a tribal tradition that at an early date a chief named Osandiah, at the head of one division of the ]\liami tribe, left the Wabash country and established himself on the Big Miami river in Ohio. Some time afterward he visited President Wash- ington, who presented him with several tokens of regard. His popular- ity with the white man 's government awakened the jealousy of some of the other clans and Osandiah 's death followed in such a way as to give rise to the suspicion that he had been poisoned. HISTORY OF MIAMI COUNTY 33 His son Ataw-ataw then became chief aud upon his 'death was iu turn succeeded by his son Met-o-cin-yah (or Me-to-sin-ia), who led the clan back to Indiana, locating near the line between the present counties of Grant and Wabash. Of his ten children Me-shin-go-me-sia, the eldest son, became chief of the band upon the death of his father. He was born in what is now Wabash county, about the time of the Revolutionary war, according to Indian tradition, and lived until December, 1879. At the battle of the Mississinewa, December 18, 1812, he distinguished him- .self by his bravery and qualities as a leader, but at his death the band had become so decimated that the chiel'tainship perished. From this tradition it appears that at least some of the minor chiefs inherited their honors, though the known history of the tribe shows that L'liii'fs were frequently selected for their intellectual ability, or as a reward for the performance of some noteworthy action, as in the case of Richardville. In Little Turtle the functions of civil ruler and war chief were com- bined. After his death, when Richardville became the principal chief, the mantle of the war chief fell upon She-po-con-ah. later known as the Deaf i\lan, who was the husband of Frances Slocum, the white woman mentioned in another chapter. Shepoconah is described as a large, heavy set man and a great warrior until his hearing became affected. His headciuarters were at the Osage village, near the mouth of the Mississinewa river, until he retired from the chieftainship, when he went farther up the river and built a log house, where a settlement grew up that became known as "the Deaf Man's village." He died iu the early '30s and was buried on a knoll a few hundred yards from his dwelling. Graham, in his History of IMiami County, says that Shepo- conah i)artieipated iu the battle of Fort Wayne, August 20, 1794; the battle of Tippecanoe, November 7, 1811, and the battle of the Mississi- newa, December 18, 1812. In the last named engagement he was one of the leaders of the Indian forces against Colonel Campbel