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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.
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 ...
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]
LAFAYETTE, Ind. — On Monday, Indiana Gov. Eric Holcomb announced that he had directed the Indiana Finance Authority to oversee the completion and validation of the INTERA water supply study that ...
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 .
The White River is an American two-forked river that flows through central and southern Indiana and is the main tributary to the Wabash River. Via the west fork, considered to be the main stem of the river by the U.S. Board on Geographic Names, [2] the White River is 362 miles (583 km) long. [3] Indiana's capital, Indianapolis, is located along ...
The valley then disappears under glacial sediments but can be tracked using water well yields and other means (Hansen, 1995). A total of seven tills have been identified within the Teays River Valley (Andrews, 2004). In portions of Ohio, the buried valley is up to 2 miles (3.2 km) wide and lies beneath 500 feet (150 m) of glacial sediments ...
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