Overview

Lost World Caverns, located just outside Lewisburg, West Virginia, is an underground natural series of caverns. In November 1973, the caverns were registered as a National Natural Landmark as they “feature terraced pedestal-like stalagmites, flowstone, curtains, rimstone, domepits, and waterfalls.” Originally named “Grapevine Cave”, the only entrance was a long vertical drop into which farmers used to dump dead livestock and other trash. Virginia Polytechnic Institute and State University “discovered” the cave in 1942. It was surveyed in the 1960s and found to contain over a mile of interconnected passages that reach a depth of 245 feet below the surface. In 1967, the remains of a prehistoric cave bear (Arctodus pristinus) were unearthed in the cave. In the early 1970s, a walking entrance was dug out, the trash was removed, walkways were installed and the cave was opened for tourism. In 1981, the gift shop and walking entrance were renovated. Since then subsequent owners have done extensive work on the lighting (making sure it does not allow the out-of-control growth of algae that old incandescent lamps cause) and many other cleaning and conservation projects as well as adding a dinosaur museum section to the gift shop.

The “walking” tour section of the cave consists of a large chamber (1000 feet long, 300 feet wide, and 120 feet high) with many formations like the Bridal Veil, Goliath, Snowy Chandelier, Ice Cream Wall, Castle and, perhaps the most storied, the War Club, where Bob Addis made it into the Guinness Book of World Records by sitting atop the 28-foot formation for nearly 16 days. In addition to the “walking” tour, one can opt for a rougher guided “wild” tour through the remote sections of the cave, visiting sights like the Angel’s Roost, Birth Canal, Keyhole, Glitter Pits, the Hall of the Mountain King and other passages and formations. Lost World Caverns is a publicly accessible cave for those who want to experience and understand the karst topography within the Greenbrier River watershed. Surrounded by farmland on all sides, the cave interacts with a constant influx of air, water, clastic and other additives and pollutants. The cave system is part of Greenbrier County’s karst plateau or “Great Savannah” where the average number of sinkholes are 18 per square kilometer.

There are wooden walkways and the option of wild caving in the deeper “wild” portions of the system. The cave drains into the Greenbrier River at Fort Spring through the Davis Spring, and there is much to be discovered about the underlying aquifers and science behind this drainage. The public tour section contains a stratum of hex (six-sided) stones. Cavers on the Wild Tour are asked to respect the encroaching threat of white nose syndrome in the Appalachian bat population, and perform sterilization protocols with their gear and clothing before they come in.