Beartown State Park
Beartown State Park: Walking Through a Sandstone Labyrinth in West Virginia’s Mountains
On the eastern summit of Droop Mountain in West Virginia’s Greenbrier County, an ancient forest drapes over a landscape that looks like something from another planet. Massive Droop Sandstone boulders — some the size of houses — stand fractured and tilted at impossible angles, creating a maze of narrow crevices, deep fissures, and cave-like passageways so dark that black bears once used them as winter dens. This is Beartown State Park, and a half-mile boardwalk takes you straight through the heart of it.
At only 110 acres, Beartown is one of West Virginia’s smallest state parks — and one of its most extraordinary. The boardwalk winds between, through, and above the boulder field, revealing surfaces pitted and sculpted by millions of years of weathering. Ferns, mosses, and hemlocks grow from every crack, and the air inside the rock passages stays cool even on the hottest summer days. It’s a 30-minute walk that feels like entering a geological cathedral.
Park Facts at a Glance
| Information | Details |
|---|---|
| 📍 Location | Droop Mountain, Greenbrier County, West Virginia |
| 📐 Park Size | 110 acres |
| 🪨 Feature | Droop Sandstone boulder field with boardwalk |
| 🛤️ Boardwalk | 0.5-0.6 mile loop (wheelchair-friendly sections) |
| 🐻 Name Origin | Black bears denned in the rock crevices |
| 💰 Admission | FREE |
| 🕐 Hours | April-October daily, winter walk-in access |
| 🅿️ Facilities | Parking lot, picnic area, restrooms |
| 📞 Phone | (304) 653-4254 |
The Sandstone Labyrinth
Beartown’s rock formations are Droop Sandstone — a hard, resistant rock layer deposited during the Pennsylvanian Period, roughly 300 million years ago. Over the eons, water seeped into fractures in the rock, and the freeze-thaw cycle gradually pried the boulders apart. The softer rock beneath eroded away, leaving massive blocks tilted at dramatic angles with deep crevices between them — some so narrow that only one person can pass at a time, and so deep that sunlight rarely reaches the bottom.
The surfaces of the boulders are deeply pitted and sculpted by chemical weathering, creating textures that resemble petrified coral or alien architecture. Thick carpets of moss and ferns cover every surface, and hemlock trees grow from seemingly impossible perches atop the boulders. The effect is simultaneously ancient and alive — a place where geology and biology have been negotiating for millennia.
The Boardwalk
A half-mile elevated boardwalk loops through the boulder field, providing access without disturbing the fragile ecosystem. The boardwalk passes through narrow passages between towering boulders, over deep fissures, and past overhangs that create natural shelters. Interpretive signs explain the geology and ecology along the way.
Visiting Tips
- Best time: Spring (wildflowers, waterfalls) and fall (foliage, cool temps)
- Duration: Plan 30-60 minutes for the boardwalk loop
- Combine with: Droop Mountain Battlefield SP (3 mi), Watoga SP (10 mi)
- Winter access: The gate closes in winter, but you can park at the entrance and walk in on foot to access the boardwalk
- Photography: The light filtering through the hemlocks into the rock crevices is exceptional in early morning
Frequently Asked Questions
How long does it take to walk the Beartown boardwalk?
The boardwalk loop is approximately 0.5-0.6 miles and takes 30-60 minutes depending on how much time you spend exploring and photographing the rock formations. It’s an easy, family-friendly walk on an elevated wooden boardwalk. There are no strenuous sections, though some passages between boulders are narrow.
Is there an entrance fee for Beartown State Park?
No — Beartown State Park is completely free to visit. There is no entrance fee or parking fee. The park is open daily from April through October. During winter months, the road gate closes, but visitors can park at the entrance and walk in to access the boardwalk on foot.
How were the rock formations at Beartown created?
The formations are made of Droop Sandstone, deposited about 300 million years ago during the Pennsylvanian Period. Over millions of years, water seeped into fractures in the rock. The freeze-thaw cycle gradually pried the boulders apart while softer underlying rock eroded away. The result is a field of massive, tilted sandstone blocks with deep crevices, cave-like openings, and elaborately pitted surfaces sculpted by chemical weathering.
