Difference between revisions of "Shenandoah National Park"
Revision as of 04:47, 12 October 2009
Shenandoah National Park  is a United States National Park located in the state of Virginia. The park is one of the most popular touristic destinations in the eastern part of USA visited by well over one million people a year. Although hundreds thousands drive along Skyline Drive in mid-late October to admire vibrant fall foliage, the park is no less spectacular (and a lot less crowded) in spring when the wildflowers and trees are in full bloom.
The oldest rocks in the Blue Ridge Mountains were created over a billion years ago as magma deep within the earth's crust moved upward. Over eons it cooled, fractured, and was joined by younger metamorphic rocks formed from sedimentary deposits. All were altered and eroded to shape today's granite peaks and sylvan hollows.
Around 8,000-9,000 years ago, but seconds in geologic time, the first traces of humans were recorded on the land that would become the park. Native Americans seasonally visited the area to hunt, to gather nuts and berries, and to find sources for and to make their stone tools.
Europeans first experienced the beauty of these mountains less than 300 years ago. First came hunters and trappers, and soon after 1750 the first settlers moved into the lower hollows near springs and streams. Over the next century and a half many hundreds of families built homesteads, mills and stores and planted orchards and crops. The mountains were logged and minerals were mined. Vacation resorts were established to allow guests to experience the mountain views, healthy water, and cool breezes. And American Society became urban, industrial, and yearned for special places for recreation and refuge.
In the early 20th century the first calls for National parks in the east were heard in the United States Congress. It would be two decades before Shenandoah National Park was authorized and another ten years before it was established. During that time President and Lou Henry Hoover established their Summer White House on the Rapidan River, the construction of Skyline Drive began, the Civilian Conservation Corps was established and moved into the park area, and over 450 families of mountain residents were relocated from the Blue Ridge.
With the establishment of the park in December 1935, the CCC began to build visitor facilities throughout the mountain, areas that were initially racially segregated. The core of the park's development was completed by the beginning of WWII and, to a great extent, the mountains were released to nature.
Shenandoah National Park includes 300 square miles of the Blue Ridge Mountains in the central Appalachians. The park rises above the Virginia Piedmont to its east and the Shenandoah Valley to its west. Two peaks exceed 4,000 feet. The range of elevation, slopes and aspects of mountain and hillsides, rock and soil types, precipitation conditions, and latitude interact to create a mix of habitats.
The park’s biota and natural features include: well-exposed strata of the Appalachians, one of the oldest mountain ranges in the world; diverse animal and plant populations and habitats; migratory bird stop-over points; and forested watersheds that perpetuate numerous streams flowing from uplands to lowlands.
Shenandoah is the largest fully protected area in the mid-Appalachian region.
Flora and fauna
Shenandoah serves as a refuge for many species of animals otherwise pressured by human activities, development and other land uses. There are over 200 resident and transient bird species, over 50 species of mammals, 51 reptile and amphibian species, and 30 fish species found in the park.
The Atlantic Ocean, and in particular the Gulf Stream, plays an important role in Virginia’s precipitation regime. Winter storms generally track from the west to the east and in the vicinity of the east coast move to the northeast paralleling the coast and the Gulf Stream. This shift to northeast results partly from the tendency of storms to follow the boundary between the cold land and the warm Gulf Stream. When sufficiently cold air comes into Virginia from the west and northwest, frontal storms can bring heavy snowfall. Thunderstorms occur in all months of the year, with a maximum in September and minimum in February. Storms and high runoff conditions can occur year-round in Shenandoah. Most locations receive 100-150 cm of precipitation per year. The average annual precipitation at Big Meadows is 132 cm, which includes about 94 cm of snow. South to southwest winds predominate, with secondary maximum frequency from the north. Lower elevation areas of the park experience modified continental climate, with mild winters and warm, humid summers. The mean annual temperature in the lowland area at Luray averages 12 degrees C, and average annual precipitation is 91 cm, with about 43 cm of snow.
Higher elevation areas of the park experience winters that are moderately cold and summers that are relatively cool. The mean annual temperature at Big Meadows averages about 9 degrees C. Mean maximum daily temperatures in July average about 6 degrees C cooler at Big Meadows then in the lowland areas of the park. Temperatures in January range from about –7 degrees C to 4 degrees C and in July from about 14-24 degrees C. Snow and ice are common in the winter, but they usually melt quickly, leaving the ground bare. Occasional major snow or ice storms can cause considerable damage to the trees within the park.
There are several ways to get into the park:
Shenandoah National Park is one of the NPS units that charge an entry fee. The following fee types are available:
The best way to enjoy the area is by taking any of the numerous hiking trails along the road. There is no public transportation in the area and the only way to get to the trails is by vehicle or by bicycle.
With over 500 miles of hiking trails, including over 100 miles of the Appalachian Trail, the park is also a premier destination for hikers.
There are maps, books for sale at the visitor centers. There you can also buy bundles of T-shirts and baseball caps with the Park logo and a range of souvenirs of the area.
The park has 6 picnic grounds and an uncountable number of spots where people can eat their own food, but build fires only in designated areas with grates. There are camp stores at or near all designated camp grounds, and only a few places where food is being served:
There are no bars in the area and only a few dining spots (see the Eat section).
There are three lodges in the park located at Skyland, Big Meadows and Lewis Mountain. These lodges are about the only accommodation in the park and they can be fully booked for months, especially during high season. Be careful about making reservations. There is a company called National Parks Reservation Service that charges a 10% booking fee and a cancellation fee of $15. Reservations should be made with Aramark  which runs the park hotels.
There are four campgrounds that offer sites on a first-come, first-serve basis and by reservation at phone number 877-444-6777:
There are also cabins:
A free permit is required for backcountry camping. You can get the permit at the visitor contact stations during business hours. Alternatively you can download a permit application from the park website .
The Luray Caverns are a short drive from the Thornton Gap Entrance Station. To reach the caverns, drive past Luray and turn right at the sign. The caves are the most extensive of the East Coast and feature large columns of white and pink stalactites, reflection pools, and the Great Stalacpipe Organ that operates by gently striking selected stalactites.