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The Watersheds of Indiana consist of six distinct Indiana watershed regions that drain into five major bodies of water. In the above map, The largest area, shaded in green, drains into the Wabash River .
Created in 1837, the Indiana Geological and Water Survey (IGWS) is an official agency of the U.S. state of Indiana charged with geological research and the dissemination of information about the state's energy, mineral and water resources. [1] In 2017, the Indiana Geological Survey was renamed to the Indiana Geological and Water Survey. [2]
Clear Creek flows roughly in the west-south-westerly direction across the campus of Indiana University, passing in front of its major landmark, the Indiana Memorial Union. On campus, the creek was formerly known as the Jordan River , named so after David Starr Jordan , the seventh president of Indiana University and later the first president of ...
Map of the Patoka River highlighted within the Wabash River watershed. The Patoka River is a 167-mile-long (269 km) [1] tributary of the Wabash River in southwestern Indiana in the United States. It drains a largely rural area of forested bottomland and agricultural lands among the hills north of Evansville.
Several dye trace studies have shown that the drainage basin of Harrison Spring is, by Indiana standards, very large. Indian Creek is a major infeeder to the Harrison Springs drainage system as the entire summer flow of Indian Creek can disappear at the Sinks of Indian Creek and re-emerge at Harrison Springs in low-flow conditions, in about one hour.
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Richmond, Indiana is on the East Fork of the Whitewater River and is the most significant town in the river valley, containing most of the population of the valley. The West Fork of the river is paralleled by State Road 121 from Connersville to 5 miles (8 km) west of Brookville, thence by U.S. Route 52 to the Ohio River.
The water flow was sufficiently substantial in the 19th century to support a mill located below the falls; but the flow is less consistent now, and the falls are frequently quiet. This is due to the conversion of woodlands and grasslands to intensive mechanized farming and the diversion of natural water flows to impoundments used to provide ...