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Between 1811 and 1834, the National Road was constructed, which passed near the Dillon region. The road connected central Ohio to the east coast, extending from Maryland to Illinois. The road passed through Zanesville, the town directly next to Dillon State Park. Furthermore, the road significantly boosted local economic activity as traffic ...
Swiss Chalet Revival architecture developed in the United States, emulating the original Swiss chalet style of Switzerland. [1] The style was popular in the U.S. in the early 20th century, approximately coinciding with the Arts and Crafts era. [1] [2] The Bomante House (1905) in Cleveland, Ohio, an example of Swiss Chalet Revival style.
The Miami Valley is the land area surrounding the Great Miami River in southwest Ohio, USA, and includes the Little Miami, Mad, and Stillwater rivers as well. Geographically, it includes Dayton, Springfield, Middletown, Hamilton, and other communities. The name is derived from the Miami Indians. [1]
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A typical chalet in the Swiss Alps. A chalet (pronounced / ˈ ʃ æ l eɪ / SHAL-ay in British English; in American English usually / ʃ æ ˈ l eɪ / shal-AY), also called Swiss chalet, is a type of building or house, typical of the Alpine region in Europe.
Most Swiss Amish are located in Indiana, but there are Swiss Amish settlements in other states, most notably in Michigan, New York, Missouri and Ohio. The largest Swiss Amish settlement is located in Adams County, Indiana , near Berne with a total Amish population of 8,595 people in 2017. [ 13 ]
The Ohio Valley is a sub region in Kentucky running 658 miles (1,059 km) long including parts of 25 counties and across five regions of the state. Over 45% of Kentucky's population live in counties that border the Ohio River , although those counties are only 16% of the state's land area.
Sugar Creek is a tributary of the Tuscarawas River in northeastern Ohio in the United States.It is 45 miles (72 km) long. Via the Tuscarawas, Muskingum, and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of 356 square miles (922 km 2) on glaciated and unglaciated portions of the Allegheny Plateau.
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