Available Data

Available Data

Station ID: 05517000

Stream Data: Gage height, discharge

Water-Quality Data: Water temperature, turbidity, suspended sediment

Atmospheric Data: Precipitation

View the Data

Station Description

Station Description

Latitude: 41°18'10"

Longitude: 86°37'14" 

Hydrologic Unit Code (HUC): 07120001

Datum: 679.93 feet above NAVD88

Drainage Area: 435 square miles (gage location)

County in which site is located: Starke County

Site managed by: Indianapolis Office

Station Funding

Station Funding

This station is operated and maintained in cooperation with the Kankakee River Basin Commission and the Indiana Department of Transportation.

Science Center Objects

"Super" gages provide real-time, continuous water-quality information for rivers and streams at selected Ohio, Kentucky, and Indiana U.S. Geological Survey (USGS) streamgages. By combining discrete and continuous data in statistical models, USGS scientists can continuously estimate constituents that are difficult to measure in real-time. For example, in-stream turbidity sensors are often used to continuously estimate suspended sediment concentrations. Continuously measured and estimated concentrations, as well as loads, are publicly accessible on USGS Web pages.

Hydrologic Conditions

Yellow Creek at Knox, IN - downstream view

Situated in northwestern Indiana, the Yellow River is a tributary of the Kankakee River with a length of approximately 60 miles and a total drainage area of 439 square miles. The headwaters of the Yellow River are in St. Joseph County. From there the river flows southerly into Marshall County then southwesterly into Starke County where it joins the Kankakee River.

The Yellow River lies in the Northern Moraine and Lake physiographic region of Indiana where the surficial geology consists of stratified sand and gravel. The primary land use is for agriculture.

Sample Collection and Use

Yellow River at Knox, IN is located between two additional super gages on the Yellow River. This super gage deploys a multi-parameter sonde to collect continuous measurements of water temperature and turbidity. Measurements are collected every 15 minutes and update to the web hourly. Additionally, hydrologic technicians collect water-quality samples to represent a variety of hydrologic and seasonal conditions. Samples are analyzed for suspended sediment concentration and percent composition of sand sized particles.

Yellow Creek at Knox, IN - calibrating QW equipment

Concentrations from laboratory analysis and corresponding values from in-stream instruments are mathematically combined to develop a statistical surrogate model. Then, the model is used to compute real-time concentrations based on continuous in-stream sensor readings of another, more easily measured value. At this site, turbidity is used as a surrogate for suspended-sediment concentration. Daily, monthly, and annual loads can be computed and compared to understand seasonal and annual variability.

Why Continuous Monitoring is Important

Over time, the Yellow River has been altered by excess sedimentation as a result of channelization and land use practices. A major concern to local residents and users of the Yellow River is that sedimentation is limiting the recreational, ecological, and overall usefulness of the river.


Yellow River at Knox, IN - bridge measurement


The Kankakee River Basin Commission (KRBC) is a local Indiana agency charged with overseeing water resources within the basin including the Kankakee River and its tributaries. In 2012, three member counties of the KRBC (LaPorte, Starke, and Marshall Counties) asked the USGS to install, operate, and maintain three super gages on the Yellow River. Continuous and discrete data were collected such that a suspended sediment concentration surrogate model could be developed. The model allows the estimation of suspended sediment concentration and load of the river, quantifying the amount of sediment being transported downstream. The effect that future bank stabilization projects and other management techniques may have on sediment reduction in the stream will be quantified.