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  2. Norris Lake - Wikipedia

    en.wikipedia.org/wiki/Norris_Lake

    Norris Lake, also known as Norris Reservoir, is a reservoir that is located in Tennessee. The lake was created by the Norris Dam at the Cove Creek Site on the Clinch River in 1936 by the Tennessee Valley Authority (TVA) for flood control, water storage, and hydroelectric power. Norris Dam and its reservoir were the first major project taken on ...

  3. Where is Norris Lake where alligator was found? What to know ...

    www.aol.com/where-norris-lake-where-alligator...

    Norris Lake was created by the Norris Dam and, like the city of Norris, are named after George W. Norris, a former U.S. Senator from Nebraska who authored the legislation that created TVA ...

  4. Chart datum - Wikipedia

    en.wikipedia.org/wiki/Chart_datum

    A chart datum is the water level surface serving as origin of depths displayed on a nautical chart and for reporting and predicting tide heights. A chart datum is generally derived from some tidal phase, in which case it is also known as a tidal datum. [1] Common chart datums are lowest astronomical tide (LAT) [1] and mean lower low water (MLLW).

  5. Norris Dam State Park - Wikipedia

    en.wikipedia.org/wiki/Norris_Dam_State_Park

    Norris Lake spans a 73-mile (117 km) stretch of the Clinch from the dam to the base of River Ridge at the Claiborne-Grainger county line. The lake also spans the lower 56 miles (90 km) of the Powell River from the river's mouth to a few miles south of Harrogate , and the lower 12 miles (19 km) of Cove Creek.

  6. Lake level could hit lowest level by Saturday - AOL

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  7. Residents worry water level changes at Grand Lake will lead ...

    www.aol.com/residents-worry-water-level-changes...

    Upstream from Grand Lake is the Tar Creek Superfund site, an abandoned lead and zinc mining operation that left behind toxic heavy metals, pictured in 2008 near Picher.

  8. Lake stratification - Wikipedia

    en.wikipedia.org/wiki/Lake_stratification

    Lake stratification is the tendency of lakes to form separate and distinct thermal layers during warm weather. Typically stratified lakes show three distinct layers: the epilimnion, comprising the top warm layer; the thermocline (or metalimnion), the middle layer, whose depth may change throughout the day; and the colder hypolimnion, extending to the floor of the lake.

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