tourists entered Natural Tunnel, a large cave in Scott County, until a railroad built a track through it
Source: Historical collections of Virginia, The Natural Tunnel (p.465)
Water created the 4,000+ caves in Virginia by dissolving limestone. Rainwater seeped down through the soil, becoming slightly acidic as it passed through decaying organic matter such as leaves. The acidic water slowly transformed the calcium carbonate - CaCO4, the predominant mineral in limestone and dolomite. (Dolomite includes more magnesium than ordinary limestone, and is formed when magnesium ions replace calcium ions in the original limestone formation.)
The chemical weathering created calcium bicarbonate - Ca(HCO3)2, which easily dissolved in water. Biological activity by sulfur-based microbial communities may also contribute, as at Cesspool Cave along Sweet Springs Creek in Allegheny County.1
As the calcium carbonate weathered away, the rock became pockmarked with voids and created a "karst" landscape with springs, sinkholes, caves. In Virginia, eroded remnants of cave systems are visible at Natural Bridge, Natural Tunnel, and Natural Chimneys. Acid rain may also be speeding up the creation of caves, by increasing the acidity of rainwater.
limestone layers are exposed by water-driven erosion at the Natural Chimneys, known as the "Cyclopean Towers" in the 1800's
Source: Henry Howe, Historical collections of Virginia (p.180)
The chemical weathering process is invisible when it occurs underground, but we can see the same process in cemeteries aboveground. On old marble gravestones, once-clear letters have eroded away. The calcium in the marble (which is metamorphosed limestone) has dissolved in just a few decades, until the carved letters on many gravestones are no longer legible.
The Chimneys (including the Great Tower) were a tourist attraction even prior to the Civil War
Source: Harper's New Monthly Magazine, Virginia Illustrated (February 1855)
Some minerals, such as silicon dioxide or quartz (SO2), are very hard to dissolve. Go to a Virginia beach and you'll see predominantly quartz sand grains, rather than calcium carbonate grains. Quartz is not very reactive; silicon dioxide is about the last mineral to dissolve, as rocks are washed down from the Appalachians. The quartz resists its inevitable fate of dissolving into the ocean. Granite headstones, with a high percentage of quartz and little or no limestone, retain their lettering longer than marble headstones.
The granite rocks of the Blue Ridge, and the sandstone ridges of Massanutten Mountain, are not riddled with caves like the limestone valleys in Virginia. In a few locations, rocks have fallen or eroded to create overhangs, crevices, and even a few spots tat could be labelled a cave.
hikers climbing up the Crabtree Falls trail in Nelson County will see a cave in the Blue Ridge created by fallen boulders
The metamorphic bedrock of the Piedmont and the sediments of the Coastal Plain also lack caves. There are only a few places in those regions where limestone or calcium-rich marl outcrops on the surface and caves might form naturally.
Where calcium carbonate (limestone) is the bedrock, caves will be more common. A map of cave locations in Virginia shows that nearly all the caves are west of the Blue Ridge, in the limestone of the Shenandoah Valley and in the equivalent valleys south of Augusta County. There may be cave-related museum exhibits in the Blue Ridge, Piedmont, or Coastal Plain physiographic provinces, but all the natural caves open to visitors are in the Valley and Ridge physiographic province.
the only site on the Virginia Cave and Karst Trail east of the Blue Ridge is the simulated cave exhibit at the Virginia Living Museum in Newport News
Source: Virginia Department of Conservation and Recreation (DCR), The Virginia Cave and Karst Trail
Several caves are located in Loudoun County, east of the Blue Ridge. The caverns formed in the Leesburg member of the Balls Bluff siltstone, and that member includes a limestone conglomerate known locally as "Calico marble." The Leesburg member was deposited in the Culpeper Basin during the Triassic Period. The lakes in which the conglomerate accumulated after big storms must have been visited by dinosaurs, but no dinosaur fossils have been found in that limestone.
Over 1,200 feet of passage have been explored in Rust Cave #1 in Loudoun County. Sinkholes are common at Temple Hall Farm, and a "window" into an underground chamber is exposed on the east side of Route 15 just north of the entrance into the Raspberry Falls subdivision.2
The Loudoun County caves are named for the Rust family, whose brothers explored the caves after the Civil War in hopes of finding a "show cave" comparable to what was developed at Luray. At the time, the caves were called Big Cave and Eddie's Cave, after Eddie Rust. The mansion house Carlheim in Loudoun County was also built on top of a cavern.3
in 2020, the Carlheim mansion site was occupied by the Aurora School
Source: ESRI, ArcGIS Online
There is one artificial cave in York County, which Cornwallis supposedly used before surrendering on October 9, 1781. Cornwallis' Cave is not a natural feature. That hole in the hillside was excavated as a shelter from French and American bombardment during the Revolutionary War battle.
The longest cave system in Virginia is the Omega System in Wise County, with nearly 30 miles of underground passages. There are over 80 cave systems in Virginia with more than one mile of passage, and at least eight caves in Virginia are at least 500' deep:4
gold miners created artificial caves in the gold-pyrite belt east of the Blue Ridge, stretching from Fairfax to Buckingham counties
Source: Gigmaster, Virginia Gold Mine!
the entrance to Dixie Caverns is a functional structure with minimal esthetic appeal, and many stalactites in the commercial cave have been broken off
1. Annette Summers Engel, Megan L. Porter, Brian K. Kinkle, Thomas C. Kane, "Ecological Assessment and Geological Significance of Microbial Communities from Cesspool Cave, Virginia," Geomicrobiology Journal, Vol. 18 Issue 3 (2001), http://www.tandfonline.com/doi/abs/10.1080/01490450152467787 (last checked June 16, 2012)
2. "Minutes of the Fall 2000 VAR Meeting," Virginia Area Region (VAR) of the NSS, September 24, 2000, http://www.varegion.org/var/theVar/varMeetMinutes/minutesFall2000.shtml (last checked June 11, 2013)
3. "Digging into history of Loudoun's limestone overlay district," Washington Post, June 6, 2010, http://www.washingtonpost.com/wp-dyn/content/article/2010/06/04/AR2010060404575.html; Eugene Scheel, "History of Loudoun's Limestone Overlay District," History of Loudoun's Limestone Overlay District, https://www.loudounhistory.org/history/limestone-overlay-district/ (last checked January 29, 2020)
4. "USA Longest Caves by State," compiled by Bob Gulden, June 17, 2014, http://www.caverbob.com/state.htm (last checked July 14, 2014)
entrance to Weyers Cave (1872)
Source: Picturesque America (p.212)