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Instruments at the gaging station record continuous river stage. <br />River stage is the height of the water surface above gage datum, a <br />reference elevation. Flood stage is the level where the stream <br />begins to overflow its banks. If the stage of the streambed is <br />known and subtracted from the water - surface stage, then the result <br />is the depth of water in the stream. Monitoring stage changes <br />provides information to river users about river stage due to <br />reservoir releases and significant rainfall. <br />Water - surface <br />Depth <br />of <br />stage <br />water <br />Streambed <br />Gage height graph <br />Knowledge of U.S. Geological Survey <br />(USGS) stage- monitoring information like 7 <br />this stage data recorded in May 1997 for the <br />Kansas River at Lecompton can make boating 6 <br />and other recreational activities on the river <br />c <br />much safer and more enjoyable. If river stages <br />CD <br />are at or near flood conditions, the river may n 5 <br />be unsafe. In contrast, when the river stages <br />are indicated to be near the streambed, the <br />stream may be too shallow or nearly dry in 4 <br />some places and may not be enjoyable for <br />recreational activities. _ <br />Typical USGS streamflow -gage house <br />equipment used to transmit data from <br />stream bank to satellite to the USGS <br />office and onto the INTERNET. <br />06891000 Kansas River at Lecompton (site 8) <br />Continuous river <br />stage via satellite <br />22 23 24 25 26 27 28 29 <br />May 1997 <br />INTERNET record of stage data recorded May 1997 <br />for Kansas River at Lecompton. <br />View of Kansas River near medium stage, looking upstream from the Lecompton bridge. <br />