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Zenas King (1818-1892) was a 19th century bridge builder whose iron bridges received wide acceptance throughout the country. He developed his tubular bowstring bridge in 1859, patented the design in 1861, renewed the patent in 1867, and founded King Iron Bridge & Manufacturing Company in 1871. Based on an arch’s inherent strength, King’s design used less raw materials than wooden bridges and the square tubes were simple to fabricate and ship for on-site assembly. His Cleveland-based company soon built so many patent bowstrings across Ohio that it set a design standard. (Continued on other side)
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On July 18, 1907, Dr. Lee deForest broadcast the first ship-to-shore radio message from the steam yacht Thelma. The communication provided quick, accurate race results of the Annual Inter-Lakes Yachting Association (I-LYA) Regatta. Frank E. Butler, a Monroeville, Ohio, native and assistant to deForest, was stationed in the pavilion at Fox’s Dock (known today as The Jet Express Dock) and received the radio transmission. The creation of the vacuum tube by deForest permitted the rapid development of radio and eventually television. The inventor disliked the existing term “wireless,” and chose a new moniker — “radio.” On this site wireless-transmission radio broadcasting was born.
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The Independent Order of Odd Fellows (IOOF) traces its origins to mid-18th-century England, where it served as a mutual benefit society for traveling workmen. Odd Fellowship moved to the United States in 1819; the first Ohio lodge was established in 1830, and the Canfield Lodge was instituted in 1850. The charter members of this lodge were E.J. Estep, John G. Kyle, James Powers, W. M. Prentice, and William W. Whittlesey. Many of the early members of this lodge were businessmen, lawyers, physicians, and tradesmen. Lodge 155 remains one of the oldest active lodges in northeastern Ohio. (continued on other side)
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The Exaltation/Elevation of the Holy Cross Church served both Byzantine Greek and Russian Orthodox Catholic congregations from 1915 to 1967. As Slovak migrants found work in the Cambridge coal fields of Guernsey and Noble Counties, they dreamed of a place to worship surrounded by the religious rites and iconography of their homeland. On January 26, 1914, Daniel Varhola, John Fetkovich, John Demko, Stephen Varhola, and Mike Zeleznik (trustees of the “Greek Catholic Church, which is united forever with the Holy Catholic Apostolic Church”) purchased land on a hill overlooking Belle Valley. The two-sided cornerstone, inscribed in Russian and Slovak, was blessed November 15, 1915. For over 50 years, the church anchored the Eastern European immigrants living in Belle Valley to the ethnic identity and traditions of their homeland. (Continued on other side)
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Two Deputy U.S. General Land Office Surveyors traversed Goll Woods: Benjamin Hough in 1815 and Captain James Riley in 1821. Hough (1772-1819) established the Michigan Meridian in 1815 and was county and state office holder in Ohio. Riley’s life was more tumultuous. Riley (1777-1840) captained the merchant ship Commerce, which wrecked off the Saharan coast in 1815. Riley and crew were enslaved for four months until ransomed by British diplomat William Willshire. In 1817, Riley published a famous account of his time in North Africa, and, in 1819, was appointed a surveyor by Surveyor General Edward Tiffin. Moving to Northwest Ohio, Riley named the village he founded in 1822, Willshire, for his deliverer. Riley returned to New York in 1826 and to the sea, where he died. Riley’s book went through more than twenty editions by 1860 and Abraham Lincoln credited the account as one that influenced him deeply.
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Urbana University was established by the Swedenborgian Church in 1850. Bailey Hall (1853), named after Francis Bailey (1735-1815), was designed by W. Russell West, architect of the Statehouse of Ohio. Bailey was an American Revolutionary War hero, official printer of the Continental Congress and printer of The Freeman’s Journal or the North American Intelligencer. He also printed The True Christian Religion papers. John (Johnny Appleseed) Chapman (1774-1845) distributed The True Christian Religion papers along with his famous apple trees throughout Ohio as a missionary for the Swedenborgian Church. Barclay Hall (1883) was named after Hester Barclay, a ward of Francis Bailey. It was Hester Barclay’s brother-in-law, John Young, who converted Chapman to the Swedenborg faith. Francis Bailey and Hester Barclay were the first male and female Swedenborgian converts in North America. Both Bailey and Barclay halls appear on the National Register of Historic Places.
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The Dayton and Michigan Railroad provided the single most important impetus to the growth and development of Wapakoneta. Although Wapakoneta had been platted in 1833, at the time of incorporation (1848), “the town was still without any material improvement worth the name of enterprise, save in the erection of residences and opening of small retail stores and shops.” On March 15, 1854, in its first ordinance, the village council of Wapakoneta voted unanimously to grant a right-of-way to the Dayton and Michigan Railroad Company to construct a railroad line through the community. The financial backers of the railroad ran short of funds during construction, and planned to end the line at Sidney, but local leaders raised $70,000 to ensure its extension. (Continued on other side)
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Hemlock Falls is located nearby. Two small streams cascade down the face of the massive sandstone cliff in the shade of tall hemlock trees. One of the falls drops about 60 feet and the other about 100 feet. The rock is Black Hand Sandstone deposited in the deltas along the great salt-water sea during the Mississippian Period about 350 million years ago. The cliffs were created later and were produced by erosion along the side of the valley of the ancient pre-glacial Groveport River. One large slump block, which has separated from the rock wall by weathering, may be the largest in Ohio. Plants more typical of the Appalachian Plateau and rare to Richland County can be found in this area. The ecosystem is typical of that found at the past edge of a glacier.