Valley Railway (Oregon)
   HOME
*



picture info

Valley Railway (Oregon)
The Valley Railway was a shortline railroad which operated between the city of Cleveland and small town of Zoarville in the state of Ohio in the United States. The railroad was founded in 1871, but the first segment of track did not open until 1880 and the line was not completed until 1884. The Baltimore and Ohio Railroad (B&O) obtained a controlling interest in the Valley Railway in 1890. The railroad went bankrupt in 1895, at which time it was reorganized as The Cleveland Terminal and Valley Railroad Company (CT&V). The B&O took over operation of the CT&V in 1909, and the company was merged with the B&O in 1915. Traffic on the road declined significantly after the 1920s. CSX, the B&O's successor, abandoned a third of the line in 1984. This portion was acquired by the National Park Service in 1987, and the Cuyahoga Valley Scenic Railroad operates on it seasonally. CSX sold about of track south of Canton to the Wheeling and Lake Erie Railway in 1992, and the track between A ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Baltimore And Ohio Railroad
The Baltimore and Ohio Railroad was the first common carrier railroad and the oldest railroad in the United States, with its first section opening in 1830. Merchants from Baltimore, which had benefited to some extent from the construction of the National Road early in the century, wanted to do business with settlers crossing the Appalachian Mountains. The railroad faced competition from several existing and proposed enterprises, including the Albany-Schenectady Turnpike, built in 1797, the Erie Canal, which opened in 1825, and the Chesapeake and Ohio Canal. At first, the B&O was located entirely in the state of Maryland; its original line extending from the port of Baltimore west to Sandy Hook, Maryland, opened in 1834. There it connected with Harper's Ferry, first by boat, then by the Wager Bridge, across the Potomac River into Virginia, and also with the navigable Shenandoah River. Because of competition with the C&O Canal for trade with coal fields in western Maryland, t ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Stark County, Ohio
Stark County is a county located in the U.S. state of Ohio. As of the 2020 census, the population was 374,853. Its county seat is Canton. The county was created in 1808 and organized the next year. It is named for John Stark, an officer in the American Revolutionary War. Stark County is included in the Canton-Massillon, OH Metropolitan Statistical Area, which is also included in the Cleveland-Akron-Canton, OH Combined Statistical Area. History Stark County was named in honor of American Revolutionary War General John Stark. John Stark (August 28, 1728 – May 8, 1822) was a general who served in the American Continental Army during the American Revolutionary War. He became widely known as the "Hero of Bennington" for his exemplary service at the Battle of Bennington in 1777. In the 1760s and 1770s Moravian missionaries from Pennsylvania came to preach the gospel to the native people, and also to lead and resettle already converted native people migrating away from whites e ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Valley Railway Co Stock Certificate 1880
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  



MORE