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Although during the American Civil War (1861–65) Richmond served as the capital of the Confederacy and Virginian Robert E.Lee and other generals led Confederate forces, the state developed in the 20th century into a bridge state between the North and the South.
The state’s highest point, Piedmont region of the eastern United States) consists of lower rolling hills, reaching from the Blue Ridge to the fall line, the place where rivers descend, often in rapids, from higher and geologically older regions onto the flatter coastal plains.
These temperatures allow growing seasons of up to eight months, three months longer than those in far western Virginia.
Elsewhere in the Tidewater and Piedmont regions, continental weather overcomes the eastern marine influence to produce colder winters.
In the mountains winter temperatures of 0 °F (−18 °C) may occur, and cool nights in summer follow daytime highs that usually stay below 90 °F (32 °C).
Throughout the state, precipitation averages from about 32 to 44 inches (810 to 1,120 mm).