image of Etlan
www.etlan.com

Thanks for visiting our little community of Etlan, shopping, eating, drinking and enjoying time with friends and family. To be clear, Holiday cheer lives in Etlan, Virginia. Around here, it's like the rest of the country, we all shop on Amazon.com for the most part because access to mega malls is slim. It's not a complicated place we live in, it's easy. Make Etlan, Virginia your new home or just come to play. It's all here in Etlan!
It's June 22, 2018 start now and make plans to see Etlan today!

About Etlan

Etlan in Virginia can be found in the 22719 zip code or postal code and is the kind of place you come to and relax. Leave the day-to-day stresses of live behind. Discover your Etlan, discover your happy place.

Where is Etlan

On the map, Etlan is easy to spot, its that town right at the crossroads of The Best and Place in the World. Click more for more maps of Etlan and its surrounding countryside.

People of Etlan

One of our greatest assets are our people. Come and meet the citizens of Etlan

Etlan on Social

Etlan Real Estate

One of Virginia's up and coming communities, the Etlan real estate market is getting hotter by the month. If you've considered a move out of the day to day and were looking in Virginia, you should be taking a look at Etlan

Fun in Etlan

We have a lot of fun around in land of Etlan. Here are some things you might be interested in.

Old Rag Mountain is underlain by Old Rag Granite, named for its ubiquitous exposure on the mountain, formed during the Grenville Orogeny about a billion years ago. About 400 million years after the Grenville orogeny during the Catoctin Formation, deposition of basaltic magma occurred during the formation of the Iapetus Ocean, forming a layer of greenstone over the granite. This was followed by the Weverton Formation, Harpers Formation, and Antietam formation in which sand and rock sedimented on the ocean floor forming quartzite and sandstone deposits. Finally a period of sedimentation of shells and skeletons of foraminifera resulted in deposition of a layer of limestone. Approximately 700 million years after the Greenville Orogeny, the Iapetus Ocean began to close resulting in the Alleghenian Orogeny when the Old Rag Granite and layers of rock deposited upon it were transported westward and eventually thrust up over the limestone bed around it, forming Old Rag and the Blue Ridge Mountains.[4] Recreation View from the summit of Old Rag Mountain Hiking The summit of Old Rag is accessible via a system of trails in Shenandoah National Park. The shorter, most common way is from a parking area in Nethers near the end of Madison County's SR 601, off Virginia State Route 231, at the base of the mountain. A 9-mile (14.5 km) circuit hike[3] or a 5.4-mile (8.7 km) out-and-back hike to the summit can be made. The circuit hike makes use of the Ridge Trail which ascends the mountain 1.6 miles (2.6 km) to the first false summit. The trail then turns into a rock scramble, which can be strenuous for inexperienced hikers, for 1.1 miles (1.8 km) to the summit and intersection with the Saddle Trail which descends 1.9 miles (3.1 km) down the saddle of the ridge past Byrds Nest #1 shelter and Old Rag shelter to the junction with Weakley Hollow Fire Road. The Fire Road then descends 2.5 miles (4.0 km) to the Old Rag parking area. The upper Old Rag parking area was closed to public vehicles in 2010. Parking is now limited to the lower field parking area, adding a 0.9-mile (1.4 km) walk on asphalt. The summit can also be reached from Skyline Drive by following Old Rag Fire Road from the drive at milepost 43 to its eastern terminus with the Saddle Trail and then follow that trail to the summit.[5]