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The river crossed the flood stage seven times in the 1990s. Since 2000, the river has crested above flood stage twice - at 54.42 feet on Feb 2, 2020, and at 56.86 feet on March 4, 2021.
The reference water levels are used on inland waterways to define a range of water levels allowing the full use of the waterway for navigation. [1] Ship passage can be limited by the water levels that are too low, when the fairway might become too shallow for large ("target", "design") ships, or too high, when it might become impossible for the target ships to pass under the bridges. [1]
The Auglaize River (Shawnee: Kathinakithiipi) [5] is a 113-mile-long (182 km) [1] tributary of the Maumee River in northwestern Ohio in the United States. It drains a primarily rural farming area in the watershed of Lake Erie. The name of the river was derived from the French term for it.
The Ottawa River (Shawnee: Koskothiipi [1]) is a tributary of the Auglaize River, approximately 50 miles (80 km) long, [2] in northwestern Ohio in the United States. The river is named for the Ottawa tribe of Native Americans who inhabited the area in the 18th century. [ 3 ]
The River Raisin Clean-Up is from 9 a.m. to noon Saturday in Monroe. Volunteers should meet in the Riverfront Parking Lot behind 116 W. Front St.
It is one of two rivers in northwestern Ohio that share the same name, along with the Ottawa River that is a tributary of the Auglaize River. The upper 4 miles (6 km) of the river in Michigan north of Sylvania, Ohio is called North Tenmile Creek on federal maps, [ 3 ] while another branch rising in Fulton County, Ohio , is called Tenmile Creek .
Henderson Bridge (Ohio River) CSX Transportation: Union Township and Henderson: 1932 Bi-State Vietnam Gold Star Bridges: US 41: Evansville and Henderson (crosses the river entirely within the state of Kentucky at this point) 1932, 1965
In hydrology, stage is the water level in a river or stream with respect to a chosen reference height. [ 1 ] [ 2 ] It is commonly measured in units of feet. Stage is important because direct measurements of river discharge are very difficult while water surface elevation measurements are comparatively easy.