Shenandoah National Park (often ) is an American national park that encompasses part of the Blue Ridge Mountains in the Commonwealth of Virginia. The park is long and narrow, with the Shenandoah River and its broad valley to the west, and the rolling hills of the Virginia Piedmont to the east. Skyline Drive is the main park road, generally traversing along the ridgeline of the mountains. Almost 40% of the park's land——has been designated as wilderness areas and is protected as part of the National Wilderness Preservation System. The highest peak is Hawksbill Mountain at .

Park purpose

As stated in the foundation document:

Shenandoah National Park

Geography

The park encompasses parts of eight counties. On the west side of Skyline Drive they are, from northeast to southwest, Warren, Page, Rockingham, and Augusta counties. On the east side of Skyline Drive they are Rappahannock, Madison, Greene, and Albemarle counties. The park stretches for along Skyline Drive from near the town of Front Royal in the northeast to near the city of Waynesboro in the southwest. The park headquarters are located in Luray.

Shenandoah National Park

Geology

Shenandoah National Park lies along the Blue Ridge Mountains in north-central Virginia. These mountains form a distinct highland rising to elevations above . Local topographic relief between the Blue Ridge Mountains and Shenandoah Valley exceeds at some locations. The crest of the range divides the Shenandoah River drainage basin, part of the Potomac River drainage, on the west side, from the James and Rappahannock River drainage basins on the east side.

Shenandoah National Park

Some of the rocks exposed in the park date to over one billion years in age, making them among the oldest in Virginia. Bedrock in the park includes Grenville-age granitic basement rocks (1.2–1.0 billion years old) and a cover sequence of metamorphosed Neoproterozoic (570–550 million years old) sedimentary and volcanic rocks of the Swift Run and Catoctin formations. Columns of Catoctin Formation metamorphosed basalt can be seen at Compton Peak. Clastic rocks of the Chilhowee Group are of early Cambrian age (542–520 million years old). Quaternary surficial deposits are common and cover much of the bedrock throughout the park.

The park is located along the western part of the Blue Ridge anticlinorium, a regional-scale Paleozoic structure at the eastern margin of the Appalachian fold and thrust belt. Rocks within the park were folded, faulted, distorted, and metamorphosed during the late Paleozoic Alleghanian orogeny (325 to 260 million years ago). The rugged topography of Blue Ridge Mountains is a result of differential erosion during the Cenozoic, although some post-Paleozoic tectonic activity occurred in the region.

History

Creation of the park

Legislation to create a national park in the Appalachian mountains was first introduced by freshman Virginia congressman Henry D. Flood in 1901, but despite the support of President Theodore Roosevelt, failed to pass. The first national park was Yellowstone, in Wyoming, Montana, and Idaho. It was signed into law in 1872. Yosemite National Park was created in 1890. When Congress created the National Park Service (NPS) in 1916, additional parks had maintained the western pattern (Crater Lake in 1902, Wind Cave in 1903, Mesa Verde in 1906, then Denali in 1917). Grand Canyon, Zion and Acadia were all created in 1919 during the administration of Virginia-born president Woodrow Wilson. Acadia finally broke the western mold, becoming the first eastern national park. It was also based on donations from wealthy private landowners. Stephen Mather, the first NPS director, saw a need for a national park in the southern states, and solicited proposals in his 1923 year-end report. In May 1925, Congress and President Calvin Coolidge authorized the NPS to acquire a minimum of and a maximum of to form Shenandoah National Park, and also authorized creation of Great Smoky Mountains National Park. However, the legislation also required that no federal funds would be used to acquire the land. Thus, Virginia needed to raise private funds, and could also authorize state funds and use its eminent domain (condemnation) power to acquire the land to create Shenandoah National Park.