Tucked in the northwestern corner of Virginia, only twenty minutes from Shenandoah National Park lies the majestic Luray Caverns. This expansive cavern system is a mythic wonderland of geology in motion. Experience features like (list)…
Luray Caverns has been on my bucket list for several years. While I’m not a daredevil spelunker, I love to visit showroom caves from Carlsbad Caverns (NM) to Mammoth Cave (KY). Luray Caverns is one of the most remarkable cavern systems I have visited. Each natural feature is graciously appointed as though heaven’s interior designer handcrafted each nook and pathway.
In this post we’ll learn a little about the geology and history of Luray Caverns. I’ll also share photos from my recent trip.
Luray Cave Geology:
*It takes an astonishing 120 years to grow just one inch of Luray Caverns. Over millions of years, this slow, steady process has sculpted a subterranean wonderland within the limestone.
The formation of Luray Caverns began centuries ago, when the Shenandoah Valley was submerged beneath an inland sea. As layers of limestone accumulated, they were gradually eroded by mildly acidic water infused with carbon dioxide. Rainwater, enriched with carbonic acid from decaying vegetation, seeped into the limestone, dissolving and wearing away the rock.
Over time, this acidic water widened the fissures and cracks in the limestone, eventually creating large chambers. As the water levels receded, a slower, more intricate process began. Nature, the ultimate interior designer, took over, shaping the caverns into the stunning formations we see today
Luray Caverns is adorned with an array of speleothems including towering columns, mudflows, stalactites, stalagmites, flowstone and mirrored pools
Key words:
- Speleothem: the word is derived from the Greek words ‘spelaion’ meaning cave and ‘thema’ meaning deposit. The speleothems that most people are familiar with are stalactites and stalagmites.
- Stalactites grow down from the cave ceiling, where Stalagmites grow up from the cave floor
- Flowstone: Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. At Luray, it takes 300 hundred years to form one cubic inch of flowstone.
Luray Caverns History:
Luray Caverns was discovered on August 13th, 1878, by five local men, including local tinsmith Andrew J. Campbell, William Campbell, John ‘Quint’ Campbell and local photographer Benton Stebbins.
Intrigued when they spotted a protruding limestone outcrop and a nearby sinkhole emitting cool bursts of air, the men began to dig. Four hours later, a hole was created for the smallest men (Andrew and Quint) to squeeze through. Descending into the darkness with only candlelight as their guide, they were met with a breathtaking sight. What they discovered would astound them beyond belief.
In addition to the remarkable columns and flowstone, they also found evidence of previous human occupation. In the area of Skeleton’s Gorge they found flint, charcoal and remains of a young Native American girl.
The discovery of Luray Caverns quickly spread with scientists from around the country investigating the site. A Smithsonian Institution report of July 13 and 14, 1880, concluded: “It is safe to say that there is probably no other cave in the world more completely and profusely decorated with stalactite and stalagmite ornamentation than that of Luray.”
In the early 1900s the land was sold to the Luray Caverns Corporation, who began to open the caves up to visitors. They also had a sanitarium (health spa) for some time in 1901 before it burned down. It is believed that the cool air from the caves could help with various ailments.
Today visitors can easily access the caves through a handicap accessible walking path that demonstrates many of the caves’ majestic wonders.
Touring Luray Caverns:
The self-guided tour allows visitors to learn about unique cave formations. The tour lasts about an hour, covering 1.25 miles. It is important to stay on the walkways and not touch any cavern features. Caves are a delicate ecosystem and you don’t want to disturb the cave geology or microbiology.
As I entered the amphitheater my jaw dropped, as my head moved around in circles taking in the unique beauty of the space.
Dream Lake was one of the cavern highlights to me. The small spring lake creates an illusion of a small sea of underwater stalagmites, but in truth it is just a reflection of the stalactites from the ceiling. The deepest part of the lake is 20 inches.
My imagination created a fantasy world as I navigated the pathways, especially in the deep chasm called Pluto’s Ghost.
The oldest part of the caverns on the tour is Titania’s Veil, Rooms in this section are larger and the formations are less active. The namesake attraction is a white flowstone on the far wall named after a character in Shakespeare’s A Midsummer Night’s Dream.
Saracen’s Tent displays cave drapery. As drapery grows larger, they become longer and thin. The formation resembles fine delicate drapery you’d expect to see in a Venetian Palazzo.
The area, Giant’s Hall lives up to its name…it is the deepest part of the caverns at 164 feet below the surface of the earth. It has the largest airspace of any room in the caverns.
The Cathedral Room is a music lovers’ dream. This expansive area at one point hosted ballroom dances, complete with a local band, hoop skirts, dress pants and a plank floor. Today it houses The Great Stalacpipe Organ. According to The Guinness Book of World Records, this unique ‘organ’ is the largest musical instrument in the world.
The organ was invented in 1954 by Leland W. Sprinkle, a mathematician and electronics engineer from Springfield, Virginia. It uses the stalactites as tone sources. Rubber-tipped mallets are electronically signaled to gently tap the stalactites producing musical tones. As each of the stalactites vibrate, a magnetic pick-up transports the electrical equivalent of its tone to the center of the chamber. The result is an ethereal musical experience.
For a tour guide on all the major features click here.
This video also provides a great overview of a cavern highlights
Tickets include access to other onsite museums including the Car and Carriage Caravan Museum, Toy Museum, Shenandoah Heritage Village and more. For more information and to purchase tickets click here.
Around Luray:
The town of Luray is a charming mountain community in the Shenandoah Valley. The area includes other nearby show caves like Skyline Caverns, as well as area Civil War battlefields. Luray is a great basecamp for exploring the northern part of Shenandoah National Park. It is also fairly close to Harrisonburg (home of James Madison University) For more information about Luray click here.
