A Mass Movement in the Blue Ridge

By Chuck Bailey

Mid-day on Sunday (May 2nd, 2021), I crossed the Blue Ridge Mountains along U.S. Route 250. As I traveled up the mountain, just to the west of the Albemarle-Nelson county line, I noticed a modest pile of rock debris and tilted trees on the uphill side of the highway. A small mass wasting event had recently occurred—this was no surprise as the southeastern slope of the Blue Ridge near Rockfish Gap is prone to mass movement because of its geology. In 2017, we wrote a guide to the geology of the Rockfish Gap area (pdf) noting that landslides and mass wasting posed a significant hazard. As I whizzed by on Sunday, I wondered whether this rock fall/slide would grow into something significant.

By Monday, enough rocks were moving downslope and out into Route 250 that the Virginia Department of Transportation closed Route 250. This major route across the Blue Ridge looks to be closed for the foreseeable future creating a significant traffic headache. In just one day, the size of the mass movement had significantly increased and the potential for a large catastrophic event exists.

In this post, I describe the geological particulars relating to mass wasting and landslides at this location in the Blue Ridge.

Rockfish Gap (pdf), erroneously called Afton Mountain, is the lowest point along the crest of the Blue Ridge Mountains in central Virginia. Because of its unique topographic position, Rockfish Gap has long been an important transportation route linking eastern and western Virginia. Both Interstate 64 and U.S. Route 250 transit the Blue Ridge at Rockfish Gap.

Along the southeastern side of the Blue Ridge these highways are cut into the underlying bedrock of the Catoctin Formation, a distinctive geological unit composed largely of meta-basalt or greenstone. 550 million years ago these were lavas that flowed across the Earth’s surface and were the forerunner of a massive continental break-up.

Two hundred million years later, eastern North America was battered by a sequence of tectonic collisions. During this orogenic mayhem the Catoctin Formation was buried to depths of 10 to 15 kilometers (6 to 10 mi.) and heated to temperatures of ~300˚ C (~600˚ F). Additionally, the collision of continental blocks crumpled and sheared these rocks. During this process, the basaltic lavas were transformed into schistose greenstone, a fine-grained foliated metamorphic rock. Foliation is the parallel arrangement of minerals within a rock that develops as rocks experience ductile deformation. Foliation is also a plane of weakness in these rocks—whack a greenstone with a hammer and it’ll typically break parallel to the foliation.

East of Rockfish Gap, the foliation in the Catoctin greenstone dips to the south-southeast at angles between 20 and 50 degrees. Here, the landscape slopes between 10 to 20 degrees towards the south. This presents a slope stability issue as the land surface and the rock structures are inclined in the same direction.

To make matters worse, the roadcuts along both Route 250 and Interstate 64 are inclined more steeply than the natural land slope. Thus, the foliation typically ‘daylights’ in the highway cuts—this is bad news because it produces an unstable geometry in which mass wasting is an inevitable consequence. When the existing planes of weakness in the rock dip downward, towards the road, trouble is likely not far off.

As rain percolates into the subsurface, it preferentially flows parallel to the foliation and through fractures in the greenstone. In the winter and early spring, as the water freezes and thaws, it may pry the rock apart causing slabs to move down slope towards the highway. Loose rock and the overlying soil may creep downward at velocities of a few centimeters (1-4 in.) per day, or rush downward at rates of >10 kilometers per hour (>6 mph).

The structural geometry of the underlying bedrock in this part of the Blue Ridge presented a huge challenge for both railroad and highway engineers. In the 1850s, Claudius Crozet struggled to build the first railroad across and under the Blue Ridge (pdf) here. More than a century later, highway engineers constructing Interstate 64 faced similar difficulties. Landslides were common during construction and clearly, they continue well into the 21st century.

The 2021 slide is (for the moment) relatively small and appears to be a reactivated landslide. That is, mass movement has occurred previously at this site as evidenced by the headwall scarps evident on the LiDAR-based map. It’s a ridiculously steep site that is tightly hemmed in with Route 250 below and Interstate 64 above.

Anne Witt, a landslide specialist at the Virginia Division of Geology and Mineral Resources, inspected the site on Tuesday and discovered a large tension crack at the surface to the east of the original headwall scarp. The photo below illustrates this impressive tension crack across which a mass of rock, soil, and vegetation moved 30 to 50 centimeters downslope. She also noted that the rock is well-foliated and dips towards the road. To quote Anne “it is a perfect place for rock slope instability”! The foliation is likely the sliding surface while the slide itself probably detached across a perpendicular joint set near the headwall.

Here’s the good news – Anne noted that there are no scarps or cracks uphill from the main headwall scarp, indicating that (as of Tuesday) the mass movement is not moving upslope and, in the process, ever closer to Interstate 64. VDOT will commence excavations to remediate this landslide yet that brings uncertainty, as undercutting the slope from below could trigger more movement.

This 2021 event raises questions relating to landslide hazards near Rockfish Gap:

1. How large can these landslides become? Could these mass movements become so large that they’d cause catastrophic damage? Landslides that don’t just drop rocks onto the highway, but rather take out an entire swath of Interstate 64 or Route 250. Numerous homes are cut into and built on the southeastern slope of the Blue Ridge near Route 250. Are these homes in harm’s way?
2. How fast do these mass movement events occur? Do they creep slowly down slope, causing damage to roads and structures but plod along slowly enough so as to not pose a risk to humans? Or can these events transition from the slow and creepy into major landslides that charge quickly down the mountainside leveling everything in its path?
3. What’s the trigger for mass wasting in the Blue Ridge? Heavy rains commonly lead to mass movement in mountainous terrain. Precipitation not only loads the slope with more mass, but also lowers the shear strength of soils/regolith. But there are other ways to trigger mass wasting – seismic shaking can jar a whole mountainside loose while pumping fluids in or out of the ground can change stress conditions. What triggered the 2021 movement?

With the LiDAR imagery it is a straightforward process to identity old landslides in the area. For the most part these are small slides of limited area, but nearly all of the slides appear to be related to slopes that have been steepened by human activities– primarily road or railroad cuts and at excavated building sites.

In summary, the local geology and topography of the Blue Ridge near Rockfish Gap are well-suited for mass wasting. Add to that the numerous over-steepened slopes associated highway cuts and construction sites and we’ve got a perfect place for rock slope instability. Mass movement events will continue to occur on the Blue Ridge, and the risk of a significant slide is ever present.