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  2. Lake Norman - Wikipedia

    en.wikipedia.org/wiki/Lake_Norman

    Lake Norman is a man-made fresh water lake in southwest North Carolina. The largest lake in the state, it was created between 1959 and 1964 [1] as part of the construction of the Cowans Ford Dam by Duke Energy. Located in Iredell County, 15 miles north of Charlotte, Lake Norman State Park boasts the region's popular mountain biking trail system.

  3. Lake Norman State Park - Wikipedia

    en.wikipedia.org/wiki/Lake_Norman_State_Park

    Lake Shore Trail is a 5-mile (8.0 km) trail on the shore of Lake Norman. Itusi Trail is a 30.5-mile (49.1 km) mountain biking trail system designed, built and maintained by the Tar Heel Trailblazers, a Charlotte based mountain biking club.

  4. New rule for Lake Norman boat rentals driven by recent ... - AOL

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  5. Developer wants to keep Lake Norman shoreline private ... - AOL

    www.aol.com/news/developer-must-open-lake-norman...

    Lake Norman waterfront developments must make at least 50% of their shoreline available to everyone, according to Mooresville zoning rules enacted in 2022. That can include docks, boat ramps ...

  6. Lake Thunderbird - Wikipedia

    en.wikipedia.org/wiki/Lake_Thunderbird

    Lake Thunderbird is a reservoir located in Norman, Oklahoma. The lake was constructed between 1962 and 1965 for the purpose of providing municipal water to the nearby communities of Del City, Midwest City and Norman. It is formed by an earthfill embankment 7,300 feet (2,200 m) long and up to 144 feet (44 m) high on the Little River. In addition ...

  7. The surprising reason lake-effect snow buries cities ... - AOL

    www.aol.com/surprising-reason-lake-effect-snow...

    Lake-effect snow, which can last for only a few minutes to several days, develops from narrow bands of clouds that form when cold, dry arctic air passes over a large, relatively mild lake.

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  9. Lake-effect rain - Wikipedia

    en.wikipedia.org/wiki/Lake-effect_rain

    Lake-effect rain clouds over the Iranian Caspian coast (June 2016) Lake-effect rain, or bay-effect rain, is the liquid equivalent of lake-effect snow, where the rising air results in a transfer of warm air and moisture from a lake into the predominant colder air, resulting in a fast buildup of clouds and rainfall downwind of the lake. [1]