WABASH RIVER
Wabash River
The Wabash River /ˈwɔːbæʃ/ (French: Ouabache) is a 503-mile-long (810 km)[2] river that drains most of the state of Indiana in the United States. It flows from the headwaters in Ohio, near the Indiana border, then southwest across northern Indiana turning south near the Illinois border, where the southern portion forms the Indiana-Illinois border before flowing into the Ohio River.
It is the largest northern tributary of the Ohio River and third largest overall, behind the Cumberland and Tennessee rivers. From the dam near Huntington, Indiana, to its terminus at the Ohio River, the Wabash flows freely for 411 miles (661 km). Its watershed drains most of Indiana. The Tippecanoe River, White River, Embarras River and Little Wabash River are major tributaries. The river's name comes from a Miami word meaning "water over white stones", as its bottom is white limestone, now obscured by mud.
The Wabash is the state river of Indiana, and subject of the state song "On the Banks of the Wabash, Far Away" by Paul Dresser. Two counties (in Indiana and Illinois); eight townships in Illinois, Indiana, and Ohio; one Illinois precinct, one city, one town, two colleges, one high school, one canal, one former class I railroad, several bridges and avenues are all named for the river itself while four US Navy warships are either named for the river or the numerous battles that took place on or near it.
The name Wabash is an English transliteration spelling of the French name for the river, Ouabache. French traders had adopted the Miami-Illinois word for the river, waapaahšiiki, meaning 'it shines white', 'pure white', or 'water over white stones', and attempted to spell it according to their own phonetic system.The Miami name expressed the clarity of the river in Huntington County, Indiana, where the river bottom is limestone.
As the Laurentide Ice Sheet began to retreat from present-day Northern Indiana and Northwest Ohio between 14,000 and 15,000 years ago, it receded into three distinct lobes. The eastern or Erie Lobe sat atop and behind the Fort Wayne Moraine. Meltwater from the glacier fed into two ice-marginal streams, which became the St. Joseph and St. Marys rivers. Their combined discharge was probably the primary source of water for the proglacial Wabash River system.
As the Erie Lobe of the glacier continued to retreat, its meltwater was temporarily trapped between the ice front to the east and the Fort Wayne Moraine to the west, and formed proglacial Lake Maumee, the ancestor of modern Lake Erie. Around 11,000 years ago the waters of Lake Maumee became deep enough that it breached a "sag" or weak spot in the Fort Wayne Moraine. This caused a catastrophic draining of the lake, which in turn scoured a 1 to 2 mi (1.6 to 3.2 km) wide valley known as the Wabash-Erie Channel or "sluiceway". The Little (Wabash) River flows through this channel. U.S. 24 traverses it between Fort Wayne and Huntington. The valley is the largest topographical feature in Allen County, Indiana.
When the ice melted completely from the region, new outlets for Lake Maumee's water opened up at elevations lower than the Wabash-Erie Channel. While the St. Joseph and St. Marys Rivers continued to flow through the channel, Lake Maumee no longer did. Now a low-lying, probably marshy bit of terrain lay in between.
It is not known for certain when, but at some point in the distant past the St. Joseph and St. Marys Rivers jumped their banks and flooded the marshy ground of the Fort Wayne Outlet. The discharge of this unusual flood was enough to cut across the outlet and come into contact with the headwaters of the Maumee River. Once this happened, the flood waters rushed to the east into the Maumee River, and their erosive force was enough that the new channel cut across the Fort Wayne Outlet into the Maumee River since it was at a lower elevation than that of the sluiceway. This meant that when the flood waters receded, the sluiceway was permanently abandoned by the two rivers. As a result of capturing them both, the Maumee was converted from a minor creek to a large river. Once again, river waters flowed through the Fort Wayne Outlet, but now they flowed eastward, toward Lake Erie, instead of westward.Following this event, the branch of the Wabash River that originates along the Wabash Moraine near Bluffton became the system's main course and source.
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