Beartown State Park a classroom for West Virginia geology

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Beartown State Park a classroom for West Virginia geology
Visitors stroll the boardwalks at Beartown State Park in West Virginia. (Photo courtesy W.Va. Dept. of Commerce)

DROOP, W.Va. — Among the smallest state parks in West Virginia, 110-acre is nevertheless among its most fascinating. For decades, it's inspired visitors as a natural wonder—a densely shaded landscape of ferns and mossy rocks.

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Here on the summit of Droop Mountain—very near Droop Mountain Battlefield State Park—a thick layer of sandstone has weathered over millions of years into a "town" of house-sized boulders. Imaginative visitors can envision it hosting a town of bears, though bears aren't known to live among the visited areas of the park.

An elaborate series of stairs and boardwalks explores part of Beartown State Park. (Photo: W.Va. Dept. of Commerce)

How has the "bear town" come to be? Ken Ashton, a geologist with the West Virginia Geological and Economic Survey at Morgantown, says the rock formation is a classroom for the study of differential weathering—a kind of erosion determined by factors such as the composition of the rock.

The sandstone at Beartown, known by geologists as the Droop Sandstone, was deposited during the some 300 million years ago, with cracks or fractures forming in the bedrock.

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Typically, those fractures in the sandstone followed a pre-determined pattern, which gives its boulders their roughly cubic shapes, Ashton says.

Moss and fern thrive among the boulders at Beartown State Park. (Photo: W.Va. Dept. of Commerce)

“Those cracks have been forming for a long, long time,” he says. “There are certain fracture trends that they follow.” Those fractures served as conduits that allowed water to get into the rock, which affected their shape even more.

“It’s a little easier for water to find its way in through a fracture than solid rock,” Ashton says. “So, over time, as the Appalachians are eroded, more water is getting into those cracks, and as the water gets in, it erodes the rock.”

The freeze-thaw cycle also contributed to the formation of the rocks. When water freezes, it expands, and it contracts when it thaws.

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“When water gets trapped, it will expand and contract over time, and it makes that crack bigger, and that allows a little bit more water to get in there, which increases the process,” Ashton says.

Signage highlights points of interest along the boardwalks at Beartown State Park.

Over millions of years, cracks have expanded into wide passages and crevices. The boulders at Beartown are the remnants of what used to be a single layer of sandstone, as everything else has eroded along the weaknesses in the bedrock.

As the rock began fracturing, the Appalachian Mountains were uplifted, though Ashton says it is difficult to pinpoint precisely when the mountains were formed.

“Ever since the end of the Paleozoic period, the Appalachians have been eroding,” he says. “We’re ballparking it: it was a long process over time.”

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Another similar rock formation in West Virginia is Rock City at Cooper’s Rock State Forest, near Bruceton Mills, West Virginia. Its boulders also formed as a result of the differential weathering.

Beartown is a favorite getaway for lovers of geology and ecology. (Photo courtesy W.Va. Dept of Commerce)

“Bedrock weathers at different rates at different zones, so it leaves a bunch of weird rocks lying around, and you’re wondering: how the heck did that get here?”

Additionally, the balanced rock formation at Blackwater Falls State Park in Tucker County is one house-sized boulder sitting on top of another, which occurred because one rock weathered away faster than the other.

“So it looks like there’s this big balancing rock up there, but again, it’s just the differential rates of weathering of that particular sandstone bed,” Ashton says.

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The land was purchased in 1970 with funds from the Nature Conservancy and a donation from Mrs. Edwin G. Polan in memory of her son, Ronald Keith Neal, a local soldier killed in the Vietnam War.

Its development has been minimized to preserve the environment, though trails and boardwalks have been opened in part of the preserve. Markers explain the natural processes at work in the area.

The park is located off US-219, seven miles southwest of Hillsboro, West Virginia, near and Watoga State Park.

The park is open daily from April to October. Access during the off-season is available by appointment. No admission fee is charged. For more information on touring the area, visit the .

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